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INDIANS OF TECPAN, GUATEMALA.

dis iad,

eerie on NPs ENMABITAN TS.

NORTH AMERICA.

HLISHE RECLUS.

EDITED BY
A. H. KEANE, B.A,

MEMBER OF COUNCIL, ANTHROP. INSTITUTE; COR. MEMB. ITALIAN AND WASHINGTON ANTHROP, SOC. :
AUTHOR OF “ ASIA,” ETC.

VOL: (FE:

MEXICO, CENTRAL AMERICA, WEST INDIES.

ILLUSTRATED BY NUMEROUS ENGRAVINGS AND MAPS.

NPA UV ORK:
DRE LEON AND COMPANY,
1, 3, AD 5 BOND STREET.
1891.

ST CT TE Ce Le
À ) WAS Ke Frit LE TT

CONTENTS.

>
CHAP. PAGE
J. GENERAL SURVEY . . : = . : : 7 : : : : : : 1—13
Geological Changes, p. 2. Prehistoric Migrations, p. 3. Gradual Settlement, p. 4.
Political Changes, p. 6. Aborigines and Negroes, p. 8. Spaniards and Mestizoes,
p.9. The Isthmian Region, p. 12.
II. Mexico . : ° : : : : : : : : : - : : . 14—190
1. General Considerations, p. 14. Progress of Discovery, p. 15.
2. Mexico Proper, North of the Isthmus of Tehüantepec, D. 20. Mountains and Volcanoes,
p. 20. Rivers and Lakes, p. 36. Climate, p. 48. Flora, p. 53. Fauna, p. 56.
Inhabitants, p. 59. Lower California, p. 93. Sonora —Sinaloa, p. 95. Chihuahua
—Durango, p. 100. North-Eastern States : Coahuila—Nuevo Leon—Tamaulipas,
p. 102. Inland States: Zacatecas —Aguascalientes—San Luis Potosi, p. 106.
Guanajuato —Jalisco and Tepic—Colima—Michoacan, p. 109. Queretaro—Hidalgo
_—Mexico—Federal District, p. 115. Vera Cruz, p. 129. Morelos— Guerrero—
Oaxaca, p. 135.
3. Hast Mexico, p. 142. Chiapas—'Tabasco—Campeachy—Yucatan, p. 142. Physical
Features, p. 143. Rivers, p. 146. Climate—Flora—Eauna, p. 153. Inhabitants,
p.154. Topography, p. 161.
4. Economie and Social Condition of Mexico, p. 170.
5. Government and Administration, 187.

III. British Honpvras (BELIZE) . : : - - 5 : : : : : . 191—200
The Cockscomb Mountains, p.193. Kivers, p.194. The Seaboard, p. 195. Climate
—Flora—Fauna, p. 197. Topography, p. 197. Administration, p. 200.

IV. Cenrran America: Guatemana, Honpuras, Satvapor, Nicaracua, Cosra Rica . . 201—311

1. General Survey, p. 201.

2. Guatemala, p. 206. Physical Features, p. 207. Rivers and Lakes, p. 213. Climate
—Flora—Fauna, p. 217. Inhabitants, p. 218. Topography, p. 225. Material
Condition of Guatemala, p. 238.

3. San Salvador, p. 244. Physical Features, p. 244. Rivers, p. 249. Climate—Flora
—Fauna, p. 250. Inhabitants, p. 250. Topography, p. 251. Economic Condition
of Salvador, p. 254.

4. Honduras, p. 255. Physical Features, p. 256. Rivers—Islands—Inlets, p. 258.
Climate—Flora— Fauna, p. 260. Inhabitants, p. 261. Topography, p. 263.
Economic Condition of Honduras, p. 266.

iv CONTENTS.
CHAP.

5. Nicaragua, p. 270. Physical Features, p. 271. Rivers and Lakes,
—Flora—Fauna, p. 280. Inhabitants, p. 281. Topography, p.
Condition of Nicaragua, p. 289. The Nicaragua Canal, p. 290.
p. 292.

6. Costa Rica, p. 293. Physical Features, p. 296.
Fauna, p. 301. Inhabitants, p. 303. Topography, p. 306.
Costa Rica, p. 308.

p- 275. Climate
284. Economic
Administration,

Rivers, p. 300. Climate—Flora—
Economic Condition of

V. Panama’. : = - 4 5 : :
Physical don. p. 312. Rivers—Bays—Islands, p. 314.
—Fauna, p. 320. Inhabitants, p. 321. Topography, p. 323.
p.329. Administration, p. 337.

Climate, p. 319. Flora
The Panama Canal,

VI. Tue Amertcan MEDITERRANEAN : Gurr or Mexico AND CARIBBEAN SEA . :
Progress of Exploration—Soundings, p. 338. Catchment Basins, p. 341. Marine
Currents, p. 343. Atmospheric Currents, p. 345. 'Temperature—Marine Flora and
Fauna, p. 346. Land Flora and Fauna, p. 349. Inhabitants, p. 350.

VII. Cusa : - :
Physical Den en +. 355. Rivers, p. 359.
Flora—Fauna, p. 364. Inhabitants, p. 366.
dition of Cuba, p. 379.

Reefs and Cays, p. 360. Climate—
Topography, p. 370. Economic Con-

VIII. Jamarca
Physical Mesure p- "383.
p.385. Topography, p. 392.

Rivers—Climate—Flora—Fauna, p. 384. Inhabitants,

Administration, p. 394.
Hartt AND THE Dominican REPUBLIC à

Physical Features, p.397. Rivers—Lakes—Reefs, p. 400.
Inhabitants, p. 404.

IX. San Domingo:

1. General Survey, p. 396.
Climate—Flora—Fauna, p. 403.

2. Republic of Haiti, p. 410.
3. San Domingo, p. 418.
X. Purrro Rico

Physical Features, 7 423,
Condition, p. 428.

Inhabitants, p. 424. Topography, p. 425. Economic

XI. VIRGIN IszANDS AND Santa Cruz
St. Thomas, p. 430. St. John, p. 433.
Gorda—Anegada, p. 436.

Santa Cruz, p. 433. Tortola—Virgin

XII. Tue BAHAMAS . : 5 ‘ P =
XIII. Tue BERMUDAS . : : ‘

XIV. THe Lesser ANTILLES : € : : 2 : ;
Sombrero—The Dos es ete near oy 463. St. Bartholomew, p. 464.
Barbuda, p.465. Antigua, p.465. Saba and St. Eustatius, p. 467. St. Christopher
and Nevis, p. 468. Montserrat, p. 470. Guadeloupe, p. 471. Dominica, p. 475.
Martinique, p. 476. St. Lucia, p. 479. St. Vincent, p 480. Grenada and the
Grenadines, p. 483. Barbados, p. 485.

APPENDIX . ° °° ° ° ° ° ° e ° ° © ° ° °

FAGE
312—337
338—353
304—381
382—395
396—422

423—429
430—436
437—448
449—454
455—486

487

eS TOMBS A PIONS.

MAPS

PRINTED IN COLOURS.

AGE
Mexico and Central America . 16 | Havana . : : 4 : 6 : :
Mexico and its Valley 118 | The Guadaloupe Archipelago . . : -
West Indies 344
PLATES.

Indians of Tecpan, Guatemala : Frontispiece | Ilopango Volcano . : : To face page
Isthmus of Panama—View taken from the Honduras Scenery . : : c : .

Culebra To face page 12 | Tegucigalpa—View taken from La Concepcion
Popocatepetl—View taken from the Tlamecas Ceiba : : ; : : :

Rancho - : : : . 27 | Leon—View taken in the Main Thoroughfare .
Indian Village—View taken at the Huexoculco Port Limon and Uvas Island . F ;

Pueblo, Province of Mexico 75 | Panama Scenery—the Rio Chagres at Matachin
Panoramic View of Guanajuato 110 | Indian Settlements, Islands of San Blas Bay .
Street View in Morelia 115 | The Panama Canal—View taken at San Pablo
City of Tula—General View 117 | General View of Havana taken from Casablanca
General View of Mexico . 120 | General View of Matanzas
The Chapultepec Cypresses . : 123 | General View of Santiago, Caba . c .
Puebla—View taken from the South 126 | Turtle Island—View taken at the Mouth of the
Vera Cruz and Fort of St. John d’Ulua . 133 Three Rivers . : : é é °
Cenote of Valladolid, Yucatan 5 2 151 | General View of Port-au-Prince :
Ruins of Uxmal—The Governor’s Palace 167 | General View of San Juan Bautista, Puerto
The Metlac Viaduct between Cordoba and Rico : . c : , :

Orizaba, on the Mexico-Vera Cruz Railway 184 | General View of Hopetown, Abaco Island
Belize—View taken from the Harbour 198 | West Indian Scenery—View taken in the
View taken on Lake Atitlan 214 Saintes Islands :
Escuintla—General View : : . - 233 | View of Basse-Terre, Guadelupe
Indian Workwomen of the Hot Lands on the General View of Fort-de-France, Martinique .

Pacific Slope. : : : 238 | Kingston, St. Vincent Island .

FIG.
. Central American Isthmuses and Inland

D I D Nr

LIST OF ILLUSTRATIONS,

LIST OF ILLUSTRATIONS.

Seas

. CITLALTEPETEL— VIEW TAKEN FROM NEAR

ORIZABA

. Political States of Catal A estan
. Mexico before the

Annexation to the
United States

. Predominant Races in Central ees

. Canals and Routes across the Isthmuses
. First Mexican Itineraries,
. Chief Positions scientifically determined in

1517 to 1550

Mexico

. Regions studied by the ‘Officers of a

French Expedition

. Relief of Mexico

. Jorullo, according to D

. Orizaba Peak ;

. Volcanoes of Mexico

. Igneous Regions and Volcanoes ‘of Mdgico
. Convergence of the two Sierra Madres

. Various Altitudes of the Mexican Moun-

tains and Towns .

7. Tamaulipas Coast Lagoons

. Coatzacoalcos Bar

. Tue REGLzA Farts

. Lake Chapala .

. Colorado Estuary

2. Closed Basins of Mexico

3. Area of the Mexican Lakes ait Nan

Periods - 2 . “
. Vertical Disposition of the Mexican
Climates
. Isothermals of Mexico eee i Altitude
. Vegetable Zones in Mexico c 2 2
. Extent of the Aztec Conquests . = c

. ARTIFICIAL PYRAMID OF CHOLULA
. SACRED STONE OF Tizoc, IN THE Museum

or Mexico .

. First Conquests of Cortes .

. Portof Siguantaneo . ‘

. Scene of the War of Tadependenne

. Chief Native Populations in Mexico .
. WATER-CARRIER AND TORTILLAS WOMAN .
5. Chief Native Races in Mexico .

. Prevailing Diseases in Mexico .

5, IA

. Guaymas .

. Mazatlan .

. CATHEDRAL OF (ae

. Tampico

. Zacatecas . Z
. SAN Luis PR = Concent Bile :
. San Blas . à À : 5 ‘

. Manzanillo ; > 5 2

. Ancient Mexico À : s ë :

PAGE

. CATHEDRAL OF Mexico . 2 : 6
. Mexico and its Environments

. Tlalpam and Lake Xochimilco .

. INDIAN MARKET-GARDENER Ss CANOE.

. Puebla in 1862 .

. Orizaba

. Successive Dsdlavemen of Vers Grae

. From Vera Cruz to Anton Lizardo

. Harbour Works in Progress at Vera Cruz.
. Acapulco . :

. Chief Ruins of Cent Mae :

. Isthmus of Tehuantepec

. Salina Cruz, the new Port of Mean nes
. Minatitlan, Northern Port of Tehuantepec
. Bank of Yucatan é ‘ ‘

. Alacran Reef x À : 5
. Toe USUMACINTA— VIEW TAKEN AT THE

Paso YALCHILAN, ON THE GUATEMALAN
FRONTIER

. Mouths of the Grijalva aa re :
. Terminos Lagoon

. The Rio of Yucatan .

. Maya Yourus . £ 5 2

. Chief Ruins of Yucatan

. Ruins in the Lacandon and Tzendal Co

tries

. Merida and Norte West Yuvatan j

. Density of the Population in Mexico.

. PULQUERO .

. MAGUEY PÉANTATIONE. Ban FRANS

District, NEAR Mexico

. Chief Agricultural Produce in Mexico 5
. The World’s
. The World’s Yield of the Precious Metals
. Yield of Gold and Silver in Various Coun-

Yield of Silver .

tries since 1492

. Chief Mineral Regions of Me

. The Boca del Monte Ascent

. Mexican Railway Systems in 1890

. Political Divisions of Mexico

. British Honduras

. Parallelism of the Old and Recent Was

courses . .

. Belize and the Cookson ‘Mountains

. Domains of British Honduras .

. Old Straits in Central America . :

. Political Divisions of Central America

. Trend of the Guatemalan Ranges

. Chain of the Fuego Volcano

. Antigua: Ruins OF CHRISTCHURCH, Mae

VOLCANO IN THE BACKGROUND

. Pacaya Volcano ‘
. Golfo Dulce and the Lowen Moss
. LANDSCAPE IN SOUTH GUATEMALA— BAMBOO

JUNGLE

LIST OF ILLUSTRATIONS.

. Native Populations of Guatemala

. The Altos Region . :

. Solola and Lake Atitlan . :
. Successive Displacements of Guatemala ;
. Thickly-Inhabited Region of Guatemala .

. Lake Peten :
. Density ot the Bo pen: in CR ce

. Chief Products of Guatemala . i
2. GUATEMALAN ALCALDES, ALTOS REGION .
. Political Divisions of Guatemala

. AUSOL AT AHUACHAPAM .

. Volcanoes of West Salvador

. Lake Ilopango

. Volcanoes of East S
. San Salvador and its Environs

. La LiBerrTADn, Port or San SALVADOR

. Density of the Population of Salvador

. Interoceanic Waterparting, Honduras

. Bay Islands

3. Puerto Cortes and Tule Nivaraaa

. Fonseca Bay :

. Comparative Debts of Various Stared

. Debt per Head of Population in Various

eleadon

Countries

. Territory claimed at Veron Te by

Great Britain

3. MomMBACHO VOLCANO AND Son OF seen

NICARAGUA .

. Isthmus of Rivas :

. The Nicaragua Waterparting .

. Marrabios Range and Lake Managua

. Population of Honduras and Nicaragua .
. Density of the Population of Honduras

and Nicaragua

. San Juan del Norte before ihe Chases

tion of the Pier

. Projected Interoceanic Dante across Ne

Tagua .

. Lower San J'uan Canal

. Political Divisions of Nicaragua

. Gulf of Columbus 5
. ONE OF THE THREE CRATERS OF Bae 5
. Summit or Mount Irazu

. Plateau and Volcanoes of Costa Rica

. Gulf of Nicoya ; : © : ;
. Gulf of Dulce.

. Guaruso Inpran ,

. Youxc TaLaAMANcas Ter :

. Puerto Limon.

. Mitt ror HusxinG Gone EE

. Highways of Communication in Costa

Rica

. Administrative Tpeisions of Costa Bion é
. Course of the River Chagres

- Gulf of San Miguel.

. Gulf of San Blas

. Caledonia Bay

. Gulf of Panama

- Isthmus of Chiriqui

. Panama .

. Panama—ViIEw

TAKEN FROM Mouxr
ANCON

a Colon. 3 £ : 5 :

Ÿ ND ND N
1 HR
A Or

w bw
=I

bo
(oa)

. The ‘Mystery of the Strait”

at the
Beginning of the Sixteenth Century

0. Docks and Course of the Panama Canal .
1. Sill of the Lock Canal
. Projected Artificial Lakes on the Banana,

Divide.

. Projected Cuttings across the En a

Panama and Darien

. Projected Canal between Tira and ean

Miguel Bays

5. Cupica Bay

. The Raspadura Div ae

7. Gulf of Mexico

. Caribbean Sea :

. The Puerto Rico Abyss .

. Slopes draining to the NGS: ican Medi-

terranean

. Main Currents of the Ananas Mode

terranean

2. Deep-Sea Deere in ae ban

and West India Waters

. Deposits on the Bed of the Rian aad

West India Waters

. Anegad.i and the Horseshoe Reef
5. SNAKE - CATCHER AND CHARCUAL GIRLZ,

MARTINIQUE

. Preponderance of the White ene Black

Races in the West Indies

. La Coube (Cuba) and the Mer de nie
. Western Division of Cuba 4
. Eastern Division of Cuba 2

. Cape San Antonio and Corrientes Bay

. Jardinillos

2. Isle of Pines

3. PLANTATION OF Pan wippund

. Political Divisions of Cuba Batons the

Spanish Conquest

. CHorrexA Tower (‘‘BUCCANEERS’ Forr’ 2),

AT THE MOUTH OF THE ALMENDAKES

. Cuban Seaports West of Havana

. Matanzas :

. Trinidad and its Harbours 2 3 6
. Central Isthmus of Cuba

. Santiago de Cuba

. Port of Guantanamo 4 ; : 5
2. Railways of Cuba . : 5 =
. Hilly Region in West Jamaica c 4
. VIEW TAKEN AT THE NEWCASTLE SANA-

TORIUM, JAMAICA .

. District of Morant, Jamaica . : “
. Kingston and Port Royal

. Chief Towns of Jamaica .

. Chain of the Cayman Islands .

. Monte-Cristi Range and Vega Plain

. VIEW TAKEN FROM THE Môre Sr.

N1co-
LAS PENINSULA, Harrr. : 5

. Ozama and Brujuelas Basins .
2. Isthmus of the Lakes,
. Chief Slave-Trade Routes :
. Scene of the War of Independence .
. Disputed Territory between Haiti and

San Domingo .

San Domingo

. St. Nicolas Peninsula

LIST OF ILLUSTRATIONS.

7. Gulf of Port-au-Prince :

. South-West Peninsula of Haiti

. Les Cayes Bay 5

. Group or Harrrans

. Azua and Ocoa Bay

. Santo Domingo

3. Samana Bay

. Puerto Rico

. San Juan Bautista, Patio Rico

. South-west Corner of Puerto Rico .
7. St. Thomas Island .

. St. Thomas Harbour

. Virgin Island.

. Santa Cruz

. VIEW TAKEN IN HE Ganz eee

212. Bemini Island and Banks

. Tongue of the Ocean

bo bo
D D © wd bw w
ore © D Re

D ND we rw
oc

. Nassau

. Watling Hand
. The Bermudas :
. VIEW TAKEN FROM GiBB’s rl ie

MUDAS

. St. Kitts.

. A MARTINIQUE Giro Nat

. St. Martin

. St. John's Harbour, Anioan

. St. Eustatius .

. Sr. Kirrs — VIEW TAKEN FROM Navid
. Montserrat

. Martinique

. Lines of Navigation anid SHbmanre Cables

in the West Indies

ISLAND

. GENERAL VIEW OF CASTRIES, ST. ce CIA

PAGE
445
446
451

453

456
461
464
466
467
469
471
477

478

480

i =
à Q

THE EARTH AND ITS INHABITANTS,

MEXICO, CENTRAL AMERICA, WEST INDIES.

CHAP TERS.
GENERAL SURVEY.
ALE insular and peninsular regions which are watered by the Gulf
of Mexico and Caribbean Sea form with the Mexican triangle a

perfectly distinct section of the New World. Under the latitude
of the tropic of Cancer, which traverses the Mexican plateau and

touches the extremity of the peninsula of Lower California, the
continent has still a width of 550 miles, or about a tenth part of the distance
between the two oceans towards the middle of North America.

But south of that line the mainland tapers and expands successively, while
developing coastlines parallel with the escarpments of the plateau. Between
Mexico proper and Chiapas occurs a first contraction at the isthmus of Tehuan-
tepec; this is followed towards the south-east by other shrinkings and expansions,
terminating in the slender neck of land between the Gulfs of Panama and Darien,
which merges in the South American continent. |

The eastern chain of the American Archipelago, comprising the Bahamas and
Lesser Antilles, forms a cordon over 1,800 miles long, which sweeps round from
the north-west to the south-east in a serpentine curve roughly parallel with that
of Mexico and Central America. This vast outer rampart, of coralline formation
in the Bahamas, of volcanic origin in the Antilles, encloses the so-called “ Medi-
terranean”’ of the New World, which, like the Mediterranean of the eastern
hemisphere, is divided into secondary basins, but which in other respects presents
little resemblance to that great inland sea.

2 MEXICO, CENTRAL AMERICA, WEST INDIES.

The northernmost of these basins, that is, the Gulf of Mexico, which develops
an immense oval contour line between the peninsulas of Florida and Yucatan, is
limited southwards by the long island of Cuba, and communicates with the neigh-
bouring waters only through two passages with an average breadth of 120 miles.
The southern basin, that is, the Caribbean Sea, is of less regular form, presenting
between the Lesser Antilles and the Mosquito Coast a broad open expanse, which
is again subdivided towards the north-west by two almost completely submerged
ridges, indicated here and there by reefs and sandbanks. On one of these ridges
stands the Grand Cayman Chain, while the other connects the Tiburon peninsula
in Haiti through Jamaica with Cape Gracias 4 Dios. Thus the West Indies are
attached to Central America by three transverse hills which might be called those
of Cuba, of Cayman and Jamaica; all three begin at the chain of islands sweeping
round from Grenada and the Grenadines to Puerto Rico, almost presenting the
appearance of being three branches thrown off from a single stem.

All these lines of islands and peninsulas, which are interconnected in various
directions between the northern and southern continents, give evidence of cosmic
forces acting over vast expanses of the terrestrial crust. Nevertheless their
somewhat symmetrical arrangement in intersecting curves is no proof that the
upheaved lands were at any time continuous, or that the now partly submerged
ridges themselves are the remains of isthmuses formerly stretching from continent
to continent. On the contrary numerous indications drawn from the distribution
of the animal and vegetable species seem to justify naturalists in concluding that
certain contiguous islands have never formed continuous land during the geological
record. Cases in point are the Bahamas and the Antilles, which by their natural
history are more intimately connected with the distant Central America than with
Georgia and the Carolinas. In the same way Florida belongs rather to the West
indies than to the mainland of which it now forms part, while the Bermudas, lost
amid the Atlantic waters, are connected with the Antilles by the Gulf Stream.

The American Mediterranean lands, although lying almost entirely within the
tropics, are perfectly accessible to man for all purposes of permanent settlement.
In this respect they present an absolute contrast with the vast regions of Africa
situated under the same latitude. In the Old World the desert, which begins
with the Sahara, and which is continued across Egypt, Arabia, Persia, Turkestan,
and Mongolia, comprises millions of square miles, whereas in Central America
arid spaces are of limited extent, and in fact occupy that part of Mexico which
lies north of the tropic of Cancer. Thanks to the humidity of the atmosphere
and the moderating action of the marine waters, tropical America is almost every-
where clothed with a rich vegetation. In some places are developed almost
impenetrable forests forming a continuous mass of dense verdure, and wherever
clearings are effected, economic crops may be raised in superabundance.

The white race has even succeeded in perpetuating itself in the Antilles,
notably in Cuba and Puerto Rico, adapting itself to the climate sufficiently to
cultivate the land and engage in industrial pursuits.

In Mexico and in Central America the mean elevation of the plateaux, offering

GENERAL SURVEY. 3

a climate analogous to that of temperate Europe, has enabled Spanish and other
immigrants to occupy the land. Flourishing European colonies have been
founded on these uplands, where they have acquired sufficient influence to impart
their usages, language and culture to the great mass of the aboriginal populations.
Within 100 miles of the coast Citlaltepetel, the “Star Mountain,” which passing
seafarers beheld glittering at sunset and sunrise like a flaming beacon above the
arid and swampy plains of the seaboard, seemed to invite them to scale the inter-
vening heights and take possession of the breezy inland tablelands. They under-
stood the language of nature which attracted them to these uplands, where were
afterwards founded Orizaba, Cordoba, and other flourishing cities of ‘‘ New Spain.”

Fig. 1.— CENTRAL AMERICAN ISTHMUSES AND INLAND SEAs.
Scale 1 : 40,000,000.

New Orléan

à = C.Catoch

= QE: Éd

West of Greenwich

Depths.
0 to 500 500 to 2,000 2,000 Fathoms
Fathoms. Fathoms. and upwards,

620 Miles.

While physically distinct from the continental masses of north and south,
Central America itself is divided into secondary regions presenting such differ-
ences that the inhabitants, grouped in separate tribes and nations, remained
formerly almost completely isolated. Communications were rare and difficult, and
no ethnical cohesion had been developed amongst these isolated elements. Before
the conquest few migrations or interminglings took place, except in the Mexican
regions, which lay broadly open in the north towards the plains of Texas, the pla-
teaux and intermediate valleys of the Rocky Mountains and the Californian slope.

In the Mexican legends or annals are commemorated the peaceful or conquering
movements of the populations following in successive waves of migration from

4 MEXICO, CENTRAL AMERICA, WEST INDIES.

north to south, from the banks of the Colorado and Rio Bravo to the valleys of
the Sierra Madre, the Anahuac tablelands and southern isthmuses. But the same
records speak of the formidable obstacles encountered by those peoples, obstacles
by which they were-often arrested for decades and even centuries, and at times
compelled to retrace their steps to their original homes. To the difficulties created
by the resisting tribes were added those of the rough routes over the crests of
transverse ranges, and the changes of climate on their passage through the forests,
or on the descent towards the hot regions of the seaboard and isthmuses. Some
of those northern invaders were arrested in the various depressions of the Mexican
plateaux; others continued their march as far as Tehuantepec and Guatemala; while
others penetrated southwards to the plains of Salvador and the Nicaragua volcanoes.

There can be no doubt that at various epochs other hordes from the north
pushed even still farther south. But no documents dating from the American
mediæval period make any mention of such migrations on the mainland. In fact
in the narrow neck of land some 600 miles long, which bends round to the north-
west corner of the state of Columbia, the natural obstacles become almost insur-
mountable. Here nothing could be attempted except slow maritime expeditions
continued from age to age; but of such migrations all memory has perished.
The movements of the native populations must have been prevented or indefinitely
arrested by the rugged highlands stretching from sea to sea, by the impenetrable
tangle of tropical forests, the sudden freshets caused by tremendous downpours,
or the flooded tracts skirting the banks of the Atrato.

The numerous islands of all sizes stretching in chains between the basins of
the American Mediterranean, or along the borders of the Atlantic, were destined
by their very isolation to become the homes of communities either differing in
origin or else slowly differentiated by long seclusion. During the course of
centuries their common descent was necessarily forgotten even by kindred sea-
faring peoples, whose knowledge of navigation was rudimentary, although some
of their craft hoisted sails and were large enough to carry as many as fifty Indians.
The great diversity of languages formerly spoken in the Antilles and still current
in Mexico and the isthmuses is sufficient evidence of long isolation and dispersion
in the fragmentary world lying between the northern and southern continents.

For this region a certain unity, at least in a political sense, seemed to be
prepared by the discovery of the archipelagoes and adjacent mainland at the end
of the fifteenth and beginning of the sixteenth century. When they landed on
this new territory the Spaniards acquired definite possession: of the islands and
isthmuses, if not, as they supposed, for the dynasty of Charles V., at all events
as an inheritance of the Old World. The Antilles and Mexico never faded from
the memory of Europeans, as had. been the fate of the earlier Norse discoveries
in Greenland, Helluland and Vineland.

In virtue of Pope Alexander VI.’s Bull awarding to the Castilians and Portu-
guese all present and prospective discoveries, all those white settlers had to become
Spanish subjects. The vast continental amphitheatre sweeping round the double
basin of the inland sea, as well as its numerous chains of islands, was consequently

GENERAL SURVEY. 5

at first comprised within the Spanish domain. But the political unity of these lands
was purely official, and often little more than nominal; in many places the Conguis-
tadores never even set foot, and down to the present time certain territories supposed
to be within their jurisdiction have scarcely even been visited by the explorer.
Nor were the Spaniards strong enough to retain political possession of all the
regions discovered by their forefathers. The treasures which were brought to

Fig. 2.—CrTLALTEPETEL.— VIEW TAKEN FROM NEAR ORIZABA.

Europe by the first conquerors and which were multiplied a hundredfold in the
popular imagination, could not fail to excite the cupidity of adventurers from other
nations. Thus it happened that, either with the consent of their respective sove-
reigns, who furnished them with letters of marque, or else as roving pirates recognis-
ing no authority, daring mariners swarmed on all the seas of the Spanish Main,
capturing their vessels, wasting their plantations, or even seizing the islands them-
selves after massacring the first settlers. Some of the famous navigators of the

6 MEXICO, CENTRAL AMERICA, WEST INDIES.

sixteenth and seventeenth centuries were mere corsairs, scouring the high seas
and occupying islets, such as Tortuga at the north-west angle of Haiti. These
islands became the undisputed possessions of the buccaneers, as they were called,
from the Carib word houcan, smoked fish or flesh, doubtless in allusion to their
ordinary fare. With the exception of Portugal, which already possessed the vast
territory of Brazil besides the Kast Indies, all the European powers were anxious
to secure a portion of the Castilian world either by conquest, purchase or treaty.

Of her original American possessions, Spain now retains nothing but the two
islands of Cuba, the pearl of the Antilles, and Puerto Rico. All the rest has
been forcibly wrested from her, and even her hold on these has often been impe-
rilled by revolts or foreign wars.

England, an heretical nation in whose eyes the Papal Bull had no value,

Fig. 3.—Potrrican States oF CENTRAL AMERICA.
Scale 1 : 62,000,000.

ON
2

LU LULU

West of Greenwich

(7
WL
Independent E. Spanish. A. English. F. French.
Republics. H. Dutch. D. Danish.
1,240 Miles.

became the mistress of the large island of Jamaica, of all the Bahamas, the Ber-
mudas and most of the Lesser Antilles, beside a small district of the mainland on
the south-east coast of Yucatan. To the share of France, Holland, and Den-
mark have fallen some of the Lesser Antilles, and even Sweden till lately held
the islet of St. Bartholomew. All were anxious to have their sugar and coffee
plantations, and an independent insular depot for their colonial produce.

When the American Republic was controlled in its foreign policy by the southern
slave party, the Washington Government made repeated attempts to increase its
territory by the acquisition of Cuba, most valuable as well as largest of all the
Antilles. It also sought to establish a large naval station at the St. Domingan

GENERAL SURVEY. 7

port of Samana, one of the most important strategical harbours in tropical America.
But the opposition of the northern states, and to some extent that of the European
powers, prevented the realisation of their projects, which had for primary aim the
political supremacy of the slave-holding landowners. The only West Indian land
belonging de facto, if not to the States, at least to an American trading company
is Navaza (Navassa), a rock covered with a deposit of guano, off the west coast of
Haiti. As soon as the deposit is exhausted the useless islet will be abandoned as
several others have already been by the same company.

On the mainland the aspirations of the all-powerful republic have been more
abundantly satisfied than in the Antilles, and more than half of the territory
formerly belonging to New Spain, that is to say, Texas, California, New Mexico
and Arizona, henceforth forms an integral portion of the northern confederacy.
Negotiations have also been entered into for the purchase of the right of free
transit, in other words, of real sovereignty in the isthmus of Tehuantepec.

Moreover, some filibustering expeditions, not cfficially sanctioned, but encour-
aged in every way by irresponsible agents, were undertaken in the Central American
republics, at the time when the rush was made from New York and the New
England states to the Californian ‘ Eldorado.” In virtue of the same law by which
riverain populations gravitate towards the mouths of the streams on which they
dwell, the Americans claimed as belonging to them by “manifest destiny ”’ the
shortest route which at that period connected their settlements on both oceanic
slopes. But if their essays in this direction proved abortive, they at all events suc-
ceeded in thwarting the English, who, like themselves, were anxious to command the
shortest interoceanic highways, and for this purpose had occupied the Bay Islands,
near the Honduras coast, the so-called “ Kingdom” of Mosquitia, a natural de-
pendency of Nicaragua, and even the port of Greytown at the mouth of the Lake
Nicaragua emissary.

Then came the construction of the transcontinental railways in United States
territory itself, and this, combined with the energetic resistance of the Hispano-
American populations, postponed, at least for a time, the accomplishment of the
national aspirations for political ascendency in the Central American States.

Since the epoch that foliowed the discovery of the Californian goldfields the
independence of the Central American republics has not again been threatened by
the United States. But the Washington Government has steadily pursued a
policy calculated to prevent European influence from replacing their own, and at
the time of Maximilian’s accession to the throne of Mexico they co-operated by
their diplomatic action with the efforts of the natives to recover their autonomy.

At present all the mainland of Central America, British Honduras alone
excepted, is constituted in independent political states. Even in the archipelagoes
held by the European powers, one large island is divided between two sovereign
nations, the San Domingans, a mixed Hispano-Negro people of Spanish speech,
and the Haitians, of African descent and French speech.

Altogether the insular world presents a marked contrast with the neighbour-
ing mainland, not only in its political status, but also in the original elements of

8 MEXICO, CENTRAL AMERICA, WEST INDIES.

its inhabitants. Within a few years of the Spanish conquest, the West Indian
aborigines had almost completely disappeared. The natives of Haiti and Cuba,
by whom the first European mariners had been well received, have perished to a
man. The Carib populations of the smaller southern islands are also everywhere
represented, except in St. Vincent and Dominica, only by half-breeds.

According to Bartholomew de las Casas “the Christians caused by their
tyrannies and infernal deeds the death of over twelve million souls—perhaps
even over fifteen millions—men, women, and children.” However approximately

Fig. 4.— Mexico BEFORE THE ANNEXATIONS TO THE UNITED STATES.
Seale 1: 27,000,000.

TU
NN

K NX

¥.
SS A, :
ISAS

ec River
DIT

/
%

= —
sa
New Orléans

Westof Greenwich

WA,

Former Present

Territory. Territory.
620 Miles.

correct may be this frightful estimate made by the famous “defender of the
Indians,” it is absolutely certain that the massacres and grinding rule of the
Spaniards resulted in the extermination of the aborigines throughout the Antilles,
while those of Mexico and Central America have held their ground.

Hence the necessity of introducing another race into the islands of that “ Carib-
bean Sea,” where the Caribs themselves have been replaced by the negroes.
African slaves were imported by millions to fill the void made by the wholesale mas-
sacre of the natives. But no systematic records are now available to determine with
any accuracy the actual number of ‘‘human cattle ” thus transferred from the eastern

GENERAL SURVEY. 9

to the western shores of the Atlantic during the course of over three centuries.
Some writers speak of ten or fifteen millions; but in any case the slave trade has
cost Africa a far greater number of lives than it is now possible to calculate.

Nearly all the negroes imported during the early period of the traffic perished,
like the Caribs, without leaving any posterity. Despite their ready adaptation to
a climate which differed little from their own, most of them, being engaged chiefly
in the destructive work of the mines, died out within a few years.

Thus it happened that the negro race was very slowly established in the New
World, being gradually constituted of a thousand different ethnical elements
drawn from every part of the African seaboard, and diversely intermingled with
the blood of their European masters. Thanks to these endless crossings, the
native dialects of the slaves disappeared, and amongst the idioms current in the
Antilles only a few words can now be traced to an African source. The slaves
rapidly adopted the languages of their Spanish, French, or English owners. But
if in this respect, as well as in the usages and outward forms of civilisation, they
were brought under European influences, their physical constitution was better
suited for the environment of the West Indies, where they have now become the
numerically dominant race. Except in Cuba, where the Spaniards form the
majority of the population, and perhaps also in Puerto Rico, the blacks and
people of colour everywhere form by far the most numerous element.

_ This part of the New World, the first discovered by the Spaniards, has become
an ethnological dependency of the African Continent, and by a sort of retributive
justice, the negro race has even acquired political autonomy in the large island
of Haiti. Such an event is not without a certain historic importance. The des-
pised race, supposed to be doomed to everlasting servitude, has forcibly entered
into the number of sovereign peoples. It has not only victoriously resisted the
efforts made to again bring it under a foreign yoke, but despite a chronic state
of intestine strife and the rivalries of ambitious chiefs, it has for a century main-
tained its independent position amongst its powerful and hostile neighbours.

To the preponderance of the negro race in the Antilles corresponds that of
the Indians in Mexico and Central America. The Spaniards who at first played
the part of truculent masters and treated the aborigines abominably, are now
merged with them under the name of /adinos. So true is this that the mesti-
zos, or half-castes of the two races, constitute the chief element of the population
throughout the northern Hispano-American republics. According to the official
returns the white race is in a majority only in the State of Costa Rica. Thus
history has resumed its normal course. For over three centuries the Spaniards
had lived as parasites on the Mexican populations, and in accordance with a
constant law of nature, this parasitic existence had incapacitated them for vigorous
action. Throughout this long period, the peoples of the colonial empire misgoverned
by Spain remained without a history. Its annals were mainly reduced to a bald
record of the appointment, recall, or death of public functionaries.

But below a seemingly unruffled surface, important changes were maturing
in the social life of the nation. The heterogeneous racial elements were being

10 MEXICO, CENTRAL AMERICA, WEST INDIES.

gradually fused in a common nationality, with lke customs, ideas, and aspira-
tions, and with a growing capacity for acting in concert for the general welfare.
Thus it was that when the metropolis, overrun with foreign armies, found itself
unable to maintain its authority in the New World, Mexico, Guatemala, Honduras,
and the other Central American provinces, were suddenly seen to develop into
armed nations, in -which the descendants both of the Spanish conquerors and of
the conquered aborigines were animated by a common sentiment.

This sudden appearance of new nations, or rather the revival of the old Ameri-
can nations, clothed in a vesture of civilisation different from that which they had
formerly worn, was not confined to the central regions, but took place also in
Columbia, Venezuela, Equador, Peru—in a word, throughout the whole of Spanish
America. By a curious irony of fate, the Napoleonic epoch, which was supposed
to signalise the close of the revolutionary period, and the re-establishment of
autocratic government, led in the New World, on the contrary, to the outburst of
a general movement of independence for the Hispano-American race. From that
epoch dates the modern history of the southern continent.

But the new order of things had been prepared by the successful revolt of the
British North American colonies, which acquired their independence several
decades before the uprise of the Spanish provinces. Not only were the English
settlements emancipated at an earlier date, but they have also far outstripped the
mixed Spanish communities in social development and general culture.

Their work, however, was more easily accomplished, and in some respects is per-
haps of less significance in the history of mankind. The United States are, so to say,
little more than an expansion of the Old World; in their ethnical elements,
whether white or black, they reproduce the social conditions of Europe and Africa
in another environment, where the aboriginal element has been mainly eliminated.
The tribes that have not been extirpated, or that have not been effaced by complete
absorption in the surrounding populations, are not merged in the social system,
but live apart, either still in the wild state, or in reserves under Government
control.

But the conditions are very different in Spanish America, where the bulk of
the population consists of ‘‘ Hispanified Indians,” who, while receiving European
civilisation, and mixing in various degrees with their white conquerors, have none
_ the less remained the representatives of the old American race. The Anglo-
Saxons have destroyed or repelled the indigenous populations; the Iberians have
assimilated them, at least on the mainland. In Mexico, and in the other Spanish
republics, crossings-:and common usages have effected a reconciliation between
various races which were formerly hostile, and even totally alien, to each other.

Latin America, where heterogeneous elements still persist, cannot yet be
compared with Anglo-Saxon America for its relative importance as a factor in the
equilibrium of the world. But the various republics of which it is composed are
none the less increasing in power from decade to decade, and are already suffici-
ently consolidated to resist foreign encroachments. Collectively, they occupy con-
siderably more than half of the New World, for they comprise, besides the

GENERAL SURVEY. 11

Antilles, all the southern part of North America. But they are divided by the
region of the isthmuses into two distinct geographical areas.

In her almost isolated position, Mexico serves as an advanced bulwark for the
whole of Spanish America against the Anglo-Saxon world. Wars and diplomacy
have deprived her of all her northern territory, her outer ramparts, so to say ;
but she still retains nearly in its entirety the domain where the Spanish-speaking
populations are chiefly concentrated.

Characteristic of the Mexican nation as a whole is the incessant struggle it is
compelled to make against the growing influence of the United States. Doubtless,

Fig. 5.—Prepommvant Races IN CENTRAL AMERICA.
Scale 1 : 60,000,000.

aR (WER ra Sud

Casta Rita lin Pay]

West of breenneh

Full-blood Indians.

nul

Predominance—

ll HE a KE SRE
of Indians of Indians of whites of whites of blacks of blacks
over whites. over whites over blacks. over Indians. over whites. over whites
and blacks. and Indians.

FL) Nes.

the powerful northern confederacy has a large share in the changes which are
continually going on in Mexico. Nevertheless, the Mexicans seek their allies in
the rest of Spanish America, and especially in Europe, and even in France, which
not so long ago sent an expedition to destroy their political autonomy. They call
themselves and feel themselves “ Latins,” and the very term /adino has become syno-
nymous with “enlightened,” or “civilised” throughout Central America.

Should the emancipated nations of the earth ever group themselves according
to their natural affinities and regardless of distances, the Mexicans and the
other Latinised peoples of America will inevitably become associated with the
kindred Latin peoples of Europe. As in England and the British Colonies a

12 MEXICO, CENTRAL AMERICA, WEST INDIES.

strong feeling has sprung up for a more intimate alliance of all English-speaking
communities, in fact, for the constitution of a “Greater Britain” encircling the
globe—in the same spirit an “Ibero-American ” society has been founded for the
formation of a league between all Spanish-speaking states. At the first congress
held by this association in the city of Mexico in 1887, as many as nineteen states
were represented by their delegates. Belt’s prophecy, that in a few centuries
English would be the mother-tongue of all Americans, from the Frozen Isles of
the great north to the Land of Fire, does not seem likely to be fulfilled. Jules
Leclercq has even ventured to assert that in a short time all Mexico will be
English. But this is a delusion, as shown, for instance, by the extreme slowness

Fig. 6.—Canats AND ROUTES ACROSS THE ISTHMUSES.
Scale 1 : 20,000,000.

West of Greenwich

Railways. Projected Canal in Projected
Railways. progress. Canal.
245 Miles.

with which the process of assimilation is proceeding in New Mexico, a territory
where, at the time of the annexation to the United States, over forty years ago,
there were only fifty thousand people of Spanish speech.

Sooner or later, the region of the isthmuses must occupy a commercial position
of the first importance, for here will assuredly one day be traced the great line of
inter-communication between the Atlantic and Pacific Oceans. Accordingly, the
Americans might well suspect the European powers of the intention of seizing one
or other of these passages. It was, in fact, the fear of such a contingency that
inspired the “ Monroe doctrine” of “ America for the Americans,” thereby for-
maily reserving the possession of the isthmuses for the states of the New World.

Mit
WN

nt {x
l Whi)
À \

il
I (tr)

NRG

ISTHMUS OF PANAMA—VIEW TAKEN FROM THE CULEBRA.

GENERAL SURVEY. 13

The vital importance of these narrow tongues of land was perceived by
Columbus himself, as he coasted along the shores of Veragua, vainly seeking for
the marine channel through which the two oceans were supposed to communicate.
But this channel, or rather these channels, for there existed more than one, have
been closed by nature since the tertiary epoch, and the work of re-opening them
must now be undertaken by man. Pending the accomplishment of this enterprise,
roads, and even railways have been laid down from shore to shore. The southern
series of isthmuses is already traversed by two railways, those of Panama and
Costa Rica, and several others have been begun.

Unfortunately, the land itself is still indifferently adapted to serve as a high-
way of communication between West Europe and the East Asiatic and Austral-
asian regions. In many parts of Central America, journeys across the forests,
swamps, and unexplored tracts are attended by imminent risk. Not a single
explorer is known to have yet followed the direct overland route from Mexico to
Columbia. Even in the narrow spaces between the two seas it is dangerous to
deviate from the beaten tracks. So great were the difficulties of travel and trans-
port that till recently neither east Honduras, north Nicaragua, nor Costa Rica
possessed any outlets on the Caribbean Sea. In a commercial sense, these states
could scarcely be said to possess an Atlantic seaboard at all. All national life and
activity was centred exclusively on the side facing the Pacifie Ocean, and from
this coast the communications have been very slowly developed across the

isthmuses in the direct the Atlantic waters. Regarded as a whole, the
inter-oceanic region is st iimost an uninhabited wilderness, where the average
population scarcely exceeds ten persons to the square mile

e 5

CHAPTER II.

MEXICO.

I.—GENERAL CONSIDERATIONS.

XCLUDING the Yucatan peninsula, the territory of the ‘“ United
States of Mexico” is a triangular mass which forms the southern
extremity of the North American continent properly so called.
These Hispano-American United States are bounded on the east
- side by the long curve of the Gulf of Mexico, on the west by the
shores of the Pacific, which describe a still more extensive are of a circle. Both
curves gradually converge southwards in the direction of the Isthmus of Tehuan-
tepec, where Central America proper begins, if not in a political, at least in a geo-
graphical and historical sense. Both on the north and south sides, the frontiers

are purely conventional, corresponding in no way with the natural parting lines

of the fluvial basins.

Doubtless, the north-east frontier, for a distance of about 750 miles, is traced
by the Rio Bravo del Norte, which separates Mexico from Texas. But this
narrow stream is not a sufficiently salient geographical feature to constitute a
true dividing line; on both sides the plains and hills present the same general
aspect, and are subject to the same climate. No material change is perceptible
for a long way beyond tie Texan border, where the population grows more dense,
and arable lands begin to replace the unfertile savannas.

West of the Rio Bravo the frontiers, as laid down by the treaty between
Mexico and the United States, are a mere Succession of geometrical lines. At first
they coincide with 31° 47’ north latitude for a distance of 100 miles; then they
suddenly drop southwards to 31° 20’ N., along Which parallel they run westwards
to 111° W. of Greenwich. At this point, the line is drawn obliquely to the Rio
Colorado, 20 miles below the Rio Gila confluence, and then ascends this river to
the confluence at Yuma, whence it follow a straight line across the neck of
the Californian peninsula to the Pacific cout, 12 miles south of San Diego.

Despite the fantastic character of this geometrical frontier, it coincides at
certain points with prominent physical traits in the general relief of the land.
Thus it connects the upper Bravo valle’ with the head of the Gulf of California,
not far from the profound depression: between two distinet spurs of the Rocky
Mountains traversed by the Rio Gila.,

At the other extremity of the M-exican territory, the political frontier is less

EARLY MEXICAN EXPEDITIONS. 15

justified by the physical conditions. According to the treaty concluded with
Guatemala in 1822, the common frontier runs from the Pacific coast near the littie
river Suchiate, across the main range to the Tacanà volcano, and the Buenavista
and Ixbul heights, and thence eastwards along the parallel of 16° 40’ to. the left
bank of the Rio Usumacinta, the course of which river it should then follow to
within 15 miles to the south of the town of Tenosique. But in these roughly
explored regions, the river valleys have not everywhere been accurately determined
and certain points of detail still remain to be decided. Beyond the Usumacinta
the line runs westwards to the Rio Hondo, which marks the boundary of British
Honduras, and which falls into Chetumal Bay at the south-east corner of Yucatan.

Comprising all the outlying territories, and the remote Revilla-Gigedo
Archipelago, Mexico has a total area officially estimated at 790,000 square miles,
with a population (1889) of over 11,000,000.

Jn its main outlines, this vast region was already known about the middle of
the sixteenth century. Within twenty-four years of the conquest explorers had
visited all the coastlands, and had penetrated far inland from Yucatan to California
and the ‘seven cities” of Cibola. In 1502, Columbus had already met Yucatan
traders on the coast of Honduras; but it was only in 1517 that the Cuban planter,
Hernandez de Cordoba, during a slave-hunting expedition, discovered the first
point on the Mexican seaboard, the present Cape Catoche, at the north-west corner
of Yucatan. From that point he coasted Yucatan as far as Champoton, where a
disastrous engagement with the natives compelled the Spaniards to re-embark.

In 1518, the survey of the coast was continued by Juan de Grijalva, whose
primary object was to punish the natives for the reverse of the previous year, but
who pushed forward beyond Champoton some 600 miles to the spot where now
stands the town of Tampico.

A third expedition, under Cortes, followed in 1519; but instead of keeping
timidly to the seaboard, this daring adventurer aimed at the conquest of an empire.
How he effected his purpose, with what courage, sagacity, and prudence, but also
with what perfidy and ferocious contempt of the vanquished, is now a familiar
tale. In 1521, the. capital and surrounding districts were finally reduced, and
armed expeditions were sent in all directions to extend the bounds of “ New
Spain.” Olid and Sandoval penetrated through the provinces of Michoacan and
Colima westwards to the Pacific. Alvarado pushed southwards through the high-
lands as far as Guatemala. Cortes himself occupied the Panuco country on the
eastern slope of the mountains skirting the north side of the Mexican basin. Then,
being recalled southwards by the revolt of his lieutenant, Olid, who had crossed by
water to Honduras, he advanced south-eastwards to Tabasco, Chiapas, and the
territory of the Lacandons and Mopans.

Of all the expeditions undertaken by Cortes, none was more surprising than
this march across rivers, swamps, and uninhabited forests. In crossing the
Tabasco plains he had to construct as many as “ fifty bridges within a space of
twenty leagues.” Supplies“fell short, and his followers had to subsist on roots,
berries, and vermin. Even at present few travellers, with all the resources of

16 MEXICO, CENTRAL AMERICA, WEST INDIES.

civilisation at their disposal, have the courage to follow the route opened by Cortes.
After his time none of the Spanish conquerors took the trouble of occupying this
wilderness. They were satisfied with the reduction of Yucatan, the conquest of
which, nevertheless, occupied fully fifteen years, from 1527 to 1542.

Although the less wealthy and less densely peopled north-western regions had
fewer attractions for the invaders than the southern provinces, expeditions were
despatched in that direction also. Vessels, whose sails and equipment had been
conveyed from Vera Cruz across the Mexican plateau, coasted the seaboard towards
the Gulf of California, the entrance of which was reached by a squadron under

Fig. 7.—Frrsr Mexican ITINERARIES, 1517 To 1650.
Scale 1 : 30,000,000.

nee Carey 1523

À
ay O/.

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West of Greenwrek

620 Miles.

Cortes in the year 1533. To the great captain this burning region owes its very
name of calida fornax (hot furnace), afterwards corrupted to California.

In 1539, Francisco de Ulloa penetrated into the inner waters of the “ Vermil-
lion Sea,” so named either from the red sea-weed abounding in some of the inlets,
or, according to Pinart, more probably from the deep red colour of the sands
lining its shores. The following year Alarcon completed the exploration of the
gulf, and even penetrated 85 “leagues ’”’ up the River Buena-Guia, afterwards re-
named the Rio Colorado.

In 1542, Cabrillo, rounding the headland of Cape St. Lucas at the extremity
of the Californian peninsula, sailed northwards along the Pacific coast. to a pro-
montory supposed to be the present Cape Mendocino, beyond 40° N. lat.

On the mainland, Nuñez Cabeza de Vaca, escaping from the perils of a daring
march across the Floridas, reached Mexico from the north in 1536. Between

MEXICO

AND ¢

Scale, 1:12.000.000.

(23 SSeS es See
0 50 100 150 200 250

PRINCIPAL CAPITALS
TOWNS

Towns of 2% order
Other towns &villages *
Heights
Oto 3.000 feet
3.000to 6.000
6.000t0 12.000 ,
12.000t0 18.000 ,,
418.000 upwards

1891

41,6 310 Miles.

a Over 100.000mhahitants.
e ,, 50.000
° 10.000
«Under 10.000
Depths
Oto 500 fathoms.
500 to 1.000
1.000 to 2000
2.000. to 3.000
3.000. to 4.000
4.000. upwards.

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ENTRAL AMERICA.

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NEW YORK LE. & Co

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EXPLORATION OF MEXICO. 17

1530 and 1532 the atrocious Nuño de Guzman had reduced the provinces of
Jalisco and Sinaloa; then, in 1539, the Franciscan friar, Marcos de Niza, advanced
far into the region which is now known as New Mexico, and which lies within the
United States frontier. Here he claimed to have seen the marvellous Cibola,
which was soon afterwards shown by the expedition under Coronado to be nothing
more than one of those villages belonging to the Zuni nation, where the whole
population dwells in one huge fortified building erected around a central court.
Coronado’s expedition, which lasted over two years, from 1540 to'1542, and which
“was intended to co-operate with Alarcon's sea voyage, resulted in the occupation
and settlement of Sonora, the north-westernmost state of the present republic.

But although the Mexican territory, properly so called, had now been traversed
in all directions, the itineraries farther removed from the capital had not yet
been utilised for the construction of maps, nor could this be done with any ap-
proach to accuracy in the absence of astronomic determinations. In 1542, the
viceroy Mendoza was still engaged in fixing the position of the city of Mexico
at 25 degrees, 42 minutes farther west than its real meridian, the calculations
being deduced from the observation of two lunar eclipses. Even so late as 1579,
the map published by Ortelius gives only the central district round about the
capital with a fair degree of accuracy.

Despite all the explorations along the Californian seaboard, it was even still
maintained that California itself had been circumnavigated, and its insular character
thus fully established ; hence the Jesuit, Salvatierra, who began the settlement
of this region in 1697, gave it the name of Js/a Carolina, (Caroline Island). In
fact, the researches of the early explorers were not confirmed till the beginning of
the eighteenth century by the missionary, Kuhn, the Kino of Spanish writers.

It appears from the manuscript documents possessed by the Madrid Academia de
Historia, and from the collections preserved in Mexico, that as early as the seven-
teenth century the national archives, unfortunately closed to the student, contained
all the elements necessary for a complete and detailed description of New Spain.
Nearly all the memoirs forwarded to the Council of the Indies were accompanied
by plans. Nevertheless, even the best maps were disfigured by errors’ of half a
degree of latitude, and from one to two degrees of longitude.

Alexander von Humboldt’s journey in 1803 and 1804 has been described as a
“second discovery of Mexico.” All the known parts of New Spain were certainly
not visited by the great explorer; but his vast knowledge and intelligence enabled
him to co-ordinate the itineraries of his predecessors, comparing and controlling
one with another, and deducing from them, at least for the region of the plateau,
the true form of the Mexican relief.

He also studied the physical phenomena of the land, its igneous eruptions and
thermal springs, the vertical disposition of its climates and flora, the direction and
force of the winds prevailing on this part of the planet, the extent of its rainfall,
the variations of its magnetic currents. Besides all this, he compared the mineral,
agricultural, and industrial resources of Mexico with those of other regions, and
thus determined its relative value amongst the civilised regions of the globe.

18 MEXICO, CENTRAL AMERICA, WEST INDIES.

After the long sleep imposed upon Mexico by the system of absolute monopoly, the
labours of Humboldt were a sort of revelation; he showed what the Spanish colony
was capable of at the very time when its emancipation was already at hand.

The exploration of the country was necessarily interrupted during the revolu-
tionary period. But when Mexico at last established its independence, travellers
began again to visit this part of the American continent, henceforth declared free _
to all comers. After the wars Burkart followed in the footsteps of Humboldt,
and spent nearly ten years in traversing most of the mineral regions of the
republic.

Burkart’s work was continued by other explorers of every nationality, amongst

Fig. 8.—Cuter Positions SCIENTIFICALLY DETERMINED IN MEx1co.
Scale 1 : 30,000,000.

= ==
= = | Paso del Nort
= EAltar
= e
= SS I
Galeana
=—=s eriias| Urds resjdiodelNorte
ES Guayma
— — Lampazose
=,
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SR Durango
= Ne

azatlan resnillo Len
Zacatetas°

ney Luis of

San Bass sie! Seal À
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Morelia, *

SS Cam éch
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Petatiane

West of Greenwich

ie} e
Humboldt and his Other observators
predecessors. down to 1874.

620 Miles.

them the Americans, Stephens and Catherwood, who carefully studied the re-
markable monuments still standing in the southern part of the territory. But the
Mexicans themselves also began to take an interest in scientific investigations ; and
in 1839, a geographical and statistical bureau was founded in the capital. This
association, which is one of the oldest of the kind in the world, has issued valuable
memoirs on nearly every part of the confederacy. It has also prepared the mate-
rials for a general map of Mexico on a larger scale than that of Humboldt, which
was partly produced in sections, and afterwards as a groundwork for Garcia Cubas’
atlas, the first edition of which appeared in 1856.

Then came the trigonometric survey of the Anahuac Valley under the direction

EXPLORATION OF MEXICO. 19

of Covarrubias, which formed the starting-point for accurate geographical work.
Men of learning, such as Orozco v Berra and Pimentel, also made extensive
researches on the distribution of the aboriginal tribes of Mexico, on the history
of their migrations, the origin, affinities, and structure of their languages.

The American officers who penetrated into North Mexico during the war of
1846, and again in connection with the delimitation of the frontiers, also took
part in the topographical researches; the maps prepared by them for Sonora,
Chihuahua, Coahuila, Nuevo-Leon, and Tamaulipas still remain the best docu-
ments for the study of those provinces. The chief marine charts, especially
those of lower California, are also the work of United States surveyors.

But works are now in progress with a view to the preparation of a topo-

Fig. 9.— REGIONS STUDIED BY THE OFFICERS OF THE FRENCH EXPEDITION.

Scale 1 : 620 Miles.

*£bihuahua

ZY,
Monclov.
Ma ni

PSN

5
(ea

pa
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Bautista

those of the most advanced states, and which takes as starting-points on one
hand the Mexican Valley and environs of Puebla, on the other the northern
regions studied by the American and Mexican Boundary Commissions. The
cartographic service in the army of the republic comprises:as many as 120 persons
trained for the work.

The period of preliminary explorations is now all but closed, except perhaps
for some parts of the border-lands towards Guatemala, where so recently as 1882
a “dead city ” was discovered by Mr. Maudslay and explored by M. Charnay,

20 MEXICO, CENTRAL AMERICA, WEST INDIES.

II.—Mexico Proper, NORTH OF THE ISTHMUS oF TEHUANTEPEC.

Taken as a whole Mexico properly so called may be regarded as a lofty table-
land, on which stand mountain ranges and masses, which, despite Humboldt’s oft-
repeated generalisation, have no kind of connection in their relief or general
trend with the Andean system of South America. They should be grouped
rather with that of California, though still with numerous interruptions.

MounNTAINS AND VOLCANOES.

The mean altitude of the whole region is estimated at no less than 3,600 feet.
A plane passing at this elevation above the ocean would detach from the sustaining
pedestal an enormous triangular mass, whose apex would terminate in the south-
east above the Tehuantepec depression, and whose base would be prolonged by
two parallel horns projecting in the direction of the United States.

The great central Mexican plateau is thus seen to be limited on the sides
facing the Atlantic and Pacific Oceans by border ranges, or at least by a succession
of heights or ridges forming a more or less continuous escarpment. Both of these
border ranges have received the designation of Sierra Madre, “ Main Chain ;” a
term, however, which recurs in almost every part of Spanish America, where it is
freely applied to the dominating crests of the country.

Like all border ranges, the Mexican sierras present striking contrasts between
their opposite sides, those facing inland falling somewhat gradually down to the
plateau, while those turned towards the oceans are far more abrupt, intersected by
scarps and cliffs, furrowed by deep crevasses, continually modified by landslips,
and scored by tremendous barrancas (chasms or gorges).

The whole region, which contracts gradually southwards between the two
border ranges, forms, so to say, a large avenue terminating in a labyrinth. The
successive waves of migratory populations coming from the north were attracted
from stage to stage towards the southern angle, that is, towards the basin of
Mexico and the plains of Puebla, which are bounded on the south by the Junta,
that is, the “ Junction,” or converging-point of the two sierras.

To the triangular depression left between these sierras the expression Mexican
“plateau ”” is often applied ; it is also occasionally called the Anahuac plateau, or
simply Anahuac,.terms borrowed from Clavigero and Humboldt. Nevertheless

the mesa or “ table ” of Mexico presents no continuous level surface, as might be
supposed from the current expressions. The depression viewed as a whole
presents rather a succession of basins, for the most part of lacustrine origin, which
follow at constantly diminishing altitudes in the direction from north to south.
But the separating barriers present such slight obstacles to migrations and travel
that during the last century a highway was easily constructed from the capital to
Santa Fé in New Mexico; carriages could be driven from one city to the other
along this road, nearly 1,400 miles long.

In the southern districts round about Mexico the basins are of relatively small

MOUNTAINS OF MEXICO. 21

extent, but exceed 6,600 feet in altitude; even the Toluca basin, in the angle
formed by the two diverging main ranges, stands at a mean height of 8,500 feet
above the sea. Going northwards from Anahuac the continually diverging sierras
give more space for elevated plains, and in the northern regions the vast expanses
enclosed by the encircling ranges present almost perfectly level surfaces, broken
only by low ridges. As they stretch northwards these expanses fall in the direc-
tion of the east, and the east sierra itself is much narrower, its mean elevation
being 6,500 feet, or about 1,600 feet less than that of the western escarpment.

A third range, parallel with, but completely separated from, the two sierras

Fig. 10.—Rezrer or Mexico.
Scale 1 : 30,000,000.

i
|
Sit

als

7 7

7 =

Y Ys TOK ;
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DD,
—— Tene
77

bs
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= ;
0 to 3.300 3,390 to 6,600 6,600 to 9,900 9,900 to 16,500 16,500 Feet and
Feet. Feet. Feet. Feet. upwards.
Depths.
0 to 500 500 to 1,500 1.500 Fathoms
Fathoms. Fathoms. and upwards.
620 Miles.

enclosing the Mexican tablelands, traverses the Californian peninsula at different
elevations and with two interruptions. Isolated eminences, “lost mountains,” as
they are called, are dotted over the space comprised between the highlands of the
American California and the range traversing the peninsula which belongs to
Mexico, but which continues the axis of the Sierra Madre.

The mountains of this peninsula, varying as they do in height and form, must
therefore be regarded as forming an orographic system quite distinct from that of

22 MEXICO, CENTRAL AMERICA, WEST INDIES.

Mexico proper. Not far from the neck of the peninsula the system culminates in
Mount Calamahue, or Santa Catalina, terminating in a peak white as snow and
rising 10,000 feet above the sea.

The northern chain, which skirts the Pacific coast, ends north of the spacious
Sebastian Viscaino Bay, beyond which it merges through gently inclined plateaux
in a ridge rising above the eastern shores of Lower California. These mountains,
which are of tertiary formation, are interrupted by deep ravines, beyond which
rises the volcanic group of the Tres Virgenes (“Three Virgins’’), situated almost
exactly in the middle of the peninsula, which has a total length of about 1,300
miles. The peaks of this group appear scarcely to exceed 6,600 feet, though
raised by some authorities to 7,250 feet. But considerable discrepancies occur in
the elevations given by different writers for most of the Mexican mountains.

No eruption has taken place since 1857 in the Tres Virgenes group, where
nothing has been noticed except some vapours rising from the crevasses. All the
other volcanoes in Lower California are extinct, mineral and thermal springs, with
a few solfataras, being the only evidences of underground activity. West of the
igneous group a chain of hills traverses the peninsula at an altitude of 3,450
feet, and is continued seawards by some lofty islands at its north-west extremity.

South of the Tres Virgenes a ridge of tertiary sandstones, falling abruptly
eastwards and presenting a gentle incline towards the Pacific, extends as far as
La Paz Bay. But despite its name, the Cerro de la Giganta, the culminating
point falls below 4,600 feet, while the mean height of the ridge appears to be little
more than 3,000 feet. The extremity of the peninsula south of La Paz forms a
sort of granitic island terminating in two parallel crests, one of which has an extreme
height of 6,220 feet. Mineral deposits, including gold, silver, copper, and iron,
occur in nearly all these coast ranges; gold prevails in the schists of the west
coast, silver ores chiefly in the porphyries on the opposite side.

Lower or South California, however, notwithstanding its narrow width,
rendering it easily accessible to travellers, is a comparatively unknown region
owing to its excessive dryness and scanty population. The mountain heights have
for the most part only been measured or estimated at a distance by marine surveyors.
Mariners also have chiefly studied the character of the coasts, one, washed by the
Gulf of California, steep and rocky, the other falling in gentle inclines towards
the Pacific Ocean, which in many places is fringed by low beaches and sandy
islets. The ranges on the east side rise precipitously above the profound chasm,
through which the sea has penetrated far inland between Mexico and the peninsula.

The islands on the east side are disposed in a perfectly parallel axis with the
peninsular ranges, and rise to considerable heights. Angel de la Guardia, amongst
others, has an elevation of 4,320 feet, and collectively these islands of Lower
California have a greater extent than all the other Mexican islands taken together.

Intersected by the straight line forming the geometrical frontier of Arizona,
the various chains, which are limited northwards by tbe depression of the Rio Gila,
penetrate into the territory of Sonora and Chihuahua in parallel ridges with a
south-eastern trend. These various ranges are collectively grouped under the

VOLCANOES OF MEXICO. 23

general designation of Sierra Madre. In their central parts they consist chiefly
of granites and syenites, but sedimentary formations are also largely represented,
especially by a carboniferous limestone interspersed with thin deposits of anthracite.

As in the Lower Californian Mountains, igneous eruptions have occurred at a
great many points, and vast expanses on the plains and slopes of the hills are
covered with molten lavas. One of the cones is not even yet quite extinct, the
Pinacate volcano (5,450 feet), which lies beyond the Sierra Madre proper, some 60
miles east of the Colorado estuary. In the middle of a vast lava field stretching
south of the mountain, rise a few secondary cones, one of which is pierced by a
cave from which escape copious sulphurous exhalations. To the genius of the place
the neighbouring Indians bring propitiatory offerings of shells, darts, and the like.

The mean altitude of the Sonora Mountains scarcely exceeds 5,000 feet, but
some of the spurs projecting westwards rise much higher near the coast, where
they present an all the more imposing aspect that they are here visible from base
to summit, with their terminal cliffs and escarpments springing from the level of
the sea. Such are, near the Arizona frontier, the Sonoala highlands, one of whose
peaks has an elevation of 9,500 feet. Such, also, the Alamos, or “ Poplar” group
(9,900 feet), in the south of Sonora, followed by other coast ranges in Sinaloa. In
winter their lofty crests are streaked with snow, and all of them contain numerous
silver lodes irregularly crossing each other in all directions.

South-east of Sonora the Sierra Madre rises gradually, while still retaining the
same geological formation and general aspect. Here the Cumbre de Jesus Maria,
in the Tarahumara uplands, exceeds 8,240 feet, and the Frailecitos peak, near
Batopilas, is said to fall little short of 9,900 feet. As they increase in height the
crests draw continually nearer to the coast, and thus present more precipitous
flanks towards the sea. From the coast lagoons and dunes the horizon is bounded
by a long line of lofty crests penetrating into the zone of clouds and vapour.

The line of these crests and of the so-called bifas, or jagged heights, develops a
continuous chain at a mean distance of about 60 miles from the sea. Several of
its summits exceed 10,000 feet, while the Cumbre Pimal, in the Serra del Nayarit,
attains an altitude of 12,350 feet. But farther south the outer terrace of the
Mexican tableland, and the mountains dominating it, lose all apparent regularity
in their general outlines. The groups, connected together by passes at different
elevations, have no longer a uniform direction, and here the loftiest ridges, all
noted for their extremely rich argentiferous deposits, lie more to the east; south-
wards the whole system is interrupted by the deep valley of the Rio Lerma.

Immediately opposite this breach and about 60 miles seaward rises the insular
chain of the Tres Marias and the San Juanito, which are disposed in the direction
from north-west to south-east, parallel with the main continental range. In these
islands the highest cone, 2,420 feet, has been the scene of volcanic eruptions.

Nor were volcanoes formerly absent in the section of the Sierra Madre which
lies to the north of the Rio Lerma. In several places are still seen lava fields,
some destitute of vegetation, others forest-clad. Here also rise mounds of scoriæ
and ashes, and the Breña district especially, which stretches south of Durango. is a

24 MEXICO, CENTRAL AMERICA, WEST INDIES.

chaos of crevasses and lava streams, a #alpais, or ‘“ bad land,” very difficult to
traverse. But all the underground furnaces have long been extinguished north
of the Lerma valley. South of this parting-line begins the region of inland
lava seas, indicated by the chain of burning mountains which here runs obliquely
across Mexico from ocean to ocean. Some of the cones are quite isolated, or else
rise above detached groups, while others lie on the very axis of the main ranges.

Near its Pacific extremity, the Ceboruco or Ahuacatlan peak (7,140 feet) is
the first eminence in this igneous belt. It forms part of a chaotic group almost
entirely separated from the Sierra Madre by the valleys and passes commanded by
the city of Guadalajara. In 1870 it entered on a state of violent eruption, and
since then it has never ceased to emit gases and igneous vapours. Ceboruco is the
centre of numerous craters, of which the two largest, one extinct, the other still
smoking, are each 1,000 feet deep. They lie close together, being separated only
by a narrow ridge formed of cones in juxtaposition.

Farther south Colima, which also ejects vapours, presents in its collective
phenomena a general analogy to Ceboruco. Despite its great elevation (12,800
feet) this superb cone is merely the southern spur of a still more elevated
porphyry mass, which the natives call the Volcan de Nieve (“Snowy Volcano”),
although its crest does not terminate in a crater. The depression seen on the
summit, usually supposed to be an extinct crater, appears to be nothing more than
an amphitheatre formed of two ravines whose torrents descend to the Pacific.

On the slopes of the Volcan de Nieve the upper limit of the forest zone stands
no higher than 13,000 feet. Here begin the snows which are permanent through-
out the year on all the bare parts of the crest. From the terminal point (14,300
feet), the mountain slopes southwards towards the Volcan del Fuego, which is
separated by a rocky rampart from the neighbouring colossus.

At Colima eruptions, rare during the last century, have in recent years become
more frequent. In 1869, 1872, 1873, and 1885, masses of ashes have been
ejected, and borne by the atmospheric currents as far as San Luis-Potosi, 280
miles to the north-east. Lavas have also been discharged during these dis-
turbances, but nearly all have flowed from lateral cones, the ‘ Sons of Colima,”
and from eminences scattered over the surrounding valleys.

The Calabozo lagoon, whose deep and still unfathomed chasm discharges its
waters through the Rio San Antonio at the northern foot of the mountain, appears
to be an old crater filied by sulphurous springs. Situated on the very edge of
the Mexican uplands and ravined at its base by enormous barrancas leading down
to the plain, Colima occupies the centre of a vast horizon embracing lofty summits,
plains, and the distant ocean. Eastwards the view reaches as far as the glittering
peak of snowy Popocatepetl. Under the same latitude as the twin crests of Colima
stands the wooded Tancitaro volcano (12,100 feet) ; but it lies much nearer to the
main range, of which it is merely a southern offshoot. Tancitaro, which commands
a distant view of the Pacific, is connected with the Cerro Patamban (12,400 feet)
by the long jagged ridge of the Cerro Periban.

Farther east the almost isolated Jorullo (Joruyo) volcano rises to a height of

VOLCANOES OF MEXICO. 25

4,330 feet in the midst of a malpais, or pedregal, a stony tract of lavas enclosed on
the south by the Rio Mexcala. Since the description given by Humboldt, this is
one of the Mexican volcanoes of which most frequent mention is made. Jorullo
is commonly supposed to have made its appearance one night towards the end of the
year 1759 in the middle of cultivated plains, beneath which long rumbling sounds
had been heard for months before the upheaval. Tradition relates that the Cutza-
randiro cones, 50 miles to the east, had been in a disturbed state some years before
the appearance of Jorullo. Hence the theory that the underground forces opened
for themselves another vent by creating the new volcano, and since that time the
former craters would seem to have been completely closed.

This legend, although supported by the immense authority of Humboldt’s
name, is confirmed by no trustworthy documents, and is, moreover, at variance
with the facts since that time observed in every part of the world. One day nothing
was visible except a plain covered with sugar-cane and indigo plantations waving
in the breeze; next morning six large cones over 1,650—according to Burkart,
1,230—feet high, presented themselves to the astonished gaze of the peasantry, who
had taken refuge on the surrounding hills. The whole district was reported to
have become, so to say, ‘‘ embossed,” and raised by the molten matter, while the
semi-liquid rocks, pierced in the centre by a funnel, were upheaved above their
former level to form the cone which is now visible.

Such an hypothesis of a vertical thrust of the primitive soil is no less absurd
than another local statement regarding the vengeance of certain Capuchin friars,
who had not been entertained with sufficient honour by the proprietors of the
hacienda, and who on their departure consigned the whole district to the de-
vouring flames. The formation of Jorullo, like that of all other volcanoes, must
in fact be attributed to the ashes and lavas accumulating with each successive
eruption.

Since 1860 Jorullo has been quiescent, or, at least, subject only to slight dis-
turbances. From the crater, a yawning chasm over a mile in circuit and 650 feet
deep, nothing is now emitted except light vapours, which are mostly invisible,
condensing into fog or mist only before rainy weather. The slopes of the mountain
have been partly overgrown with forests, in which trees of the tropical are inter-
mingled with plants of the temperate zone. Even the hornitos, or “little
furnaces,” innumerable cones a few yards high, dotted round the base, have also
for the most part ceased to discharge jets of vapour. At the time of Humboldt,
the temperature of these vapours was 205° F.; since then it has gradually fallen
to from 120° to 140° F., within which limits it oscillates at present. The waters
have also cooled down in the Rio San Pedro and in another rivulet, which was
evaporated or covered by a bed of lava during the eruption, but which reappeared
in hot springs several miles from the volcano.

All these volcanoes, Colima, Tancitaro, Jorullo, and the extinct Tasco, far to
the east, but still north of the Rio Mexcala, are disposed in a line parallel with the
axis of the Sierra Madre, which runs at a mean distance of about 36 miles north-
wards. But this great range is itself composed almost exclusively of old or recent

26 MEXICO, CENTRAL AMERICA, WEST INDIES.

eruptive rocks, between whose foldings are enclosed lacustrine basins which are
still flooded, and in which quaternary alluvia have been deposited.

San Andres or Tajimaroa, a group of volcanoes lying east of Morelia, still
presents on one of its summits a funnel filled with boiling water, and emitting
copious sulphurous vapours. These vapours change to sulphates the argillaceous

Fig. 11.—JorutLo, ACCORDING TO HumBoLDT.
Scale 1 : 180,000.

YY lies YY» YW)

Section.

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101°5’ West of Greenwich

3 Miles.

clays of the surrounding district, and thus are periodically undermined the huts of
the workmen occupied in éollecting the mud richly charged with sulphur.

The Cerro de las Humaredas, another trachytic cone, owes its name to its
abundant fumaroles. Near it springs a geyser from the very summit of a siliceous
cone gradually deposited by the jets of boiling water. One of the craters, over
13,200 feet high, takes the name of Chillador, or “ Whistler,” from the hissing
sound of the vapours escaping from its mouth. In 1872 a series of violent earth-
quakes was followed by the appearance of a new Chillador by the side of the other.

AE CA M 4
(Reet es

A AY M y
oT ES
Hs) Sal
} sil

POPOCATEPETEL—VIEW TAKEN FROM THE TALMECAS RANCHO.

VOLCANOES OF MEXICO. 27

North of Morelia and of the great Lake Cuitzeo, another group, consisting of
seven volcanoes, is disposed in amphitheatrical form round the depression known as
the “ Vale” of Santiago. The craters of Alberca and of another of these cones are
filled with a slightly alkaline water like that of the surrounding distriet. The
‘local centre of underground heat is probably extinguished, but farther north the
geysers and jets of hot mud attest the continued action of the subterranean forces.

Xinantecatl, that is, the “Naked Lord,” usually known as the Nevado de
Tolica, rises almost due south of the city from which it takes its name. Itisone of
the highest peaks in Mexico, being over 15,000 feet, or, according to Heilprin and
Baker, who ascended it in 1890, at least 14,700 feet, that is about the height of
Monte Rosa, The Nevado, with its gentle and regular incline, is easily scaled ;
the traveller need not follow the example of Humboldt, who kept to the beaten
path made by the woodmen across the pine and fir forests, which become more open
towards the summit, where the trees are replaced by scrub and a short grass
growing in the fissures of the porphyry rocks near the rim of the crater.

Precisely at this point hes the parting line between vegetation and the per-
manent snows, which here persist on the northern slope even in September and
October, the two months of greatest evaporation. In the depression of the summit
two basins are flooded with fresh water, and after the rains meres are formed in
the neighbouring cavities. | The melting snows and rains are sufficiently copious
to prevent the two tarns from running dry at any season of the year. They have
an average extent of 80 acres, and fishes of a peculiar species are found in the
chief reservoir, which is over 30 feet deep. The water is very pure and cold,
43° F., and it has been proposed to supply the city of Toluca from this source.

From Nevado is seen on the eastern horizon the distant Cerro de Ajusco
(13,700 feet), which does not quite reach the snow-line. The lava streams from
this cone descend almost to the very gates of Mexico. Other less elevated and
now extinct cones, such as Culiacan and Ozumba, are disposed without apparent
order in the sections of the main range which stretches south of the capital.

Popocatepetl, the ‘Smoking Mountain,” most famous of the Mexican volca-
noes and one of those whose names most frequently occur in geographical works,
was long wrongly supposed to be the culminating point of North America,
although it is probably not even the highest peak in Mexico itself. The first
person known to have ascended Popocatepetl was the Spanish captain, Diego de
Ordaz. So early as the year 1519, while Cortes with his little band of conquerors
was still at Tlaxcala, this daring explorer penetrated into the Aztec country in
order to reach the summit of the “ mountain of Guaxocingo,” and to learn the secret
(saber el secreto) of the giant, whose crests were wreathed in dense vapour. But
it is uncertain whether he reached the top, Cortes stating that he was arrested by
the snows, while Bernal Diaz asserts that he really got as far as the crater.

During the period of the conquest, numerous Spanish soldiers, and even Fran-
ciscan friars, ascended to the crater, and special mention is made of Montano and
Larrios, who came hither in quest of sulphur for the maaufacture of gunpowder.
Since the beginning of the present century, the mountain has been frequently

28 MEXICO, CENTRAL AMERICA, WEST INDIES.

scaled. The ascent is in fact relatively easy, thanks to the regularity of the slope,
although the porphyritic mass of Popocatepetl exceeds Mont Blane by about 1,900
feet. The mean of eleven measurements yields 17,830 feet, or, according to Ponce
de Leon, 17,780 for the Mexican giant, which is consequently at least 820 feet
lower than its North-American rival, Mount St. Elias.

On the east slope the lower limit of the permanent snows is at 14,259 feet.
Here all the rugosities of the surface are filled with snow, which round the rim of
the crater is transformed to a crystalline mass 8 or 10 feet thick ; thus are deve-
loped a few small glaciers fissured by little crevasses, About the east foot of the
mountain are met a large number of scattered boulders, which should with great
probability be attributed to the action of much larger glaciers, which formerly
descended from the summits.

Above the crater rise two chief summits, the Pico Mayor and the Espinazo
del Diablo, which rest on a sharp ridge where the explorer has to maintain his
equilibrium between two profound chasms. On one side the view stretches east-
wards to the hot lands dominated by the plateaux ; on the other yawns the crater,
a cavity over half a mile in circumference, and 250 feet deep.

This cavity is filled with snow ; but jets of gas, which frequently shift their
place, melt the white mass round about the respiradero, that is, the orifice of the
crater. Thus are revealed from a distance those patches of a yellow gold colour,
which indicate the position of the sulphur deposits. The volcaneros, who almost
daily come in search of the sulphur, are let down to the bottom of the crater in a
large basket, which is lowered and raised by means of a windlass erected on the
brim of the chasm. The annual yield is estimated at about fifty tons, and the
mineral is supposed to accumulate at the rate of a tona day. A spring welling up
on the bed of the crater fills a lagoon, whose waters, according to report, reappear
in thermal fountains at the base of the mountain. Eruptions are rare, and have
been less violent during the present century than at the time of the conquest.

North of Popocatepetl rises the less elevated but still lofty Ixtaccihuatl, or
“ White Woman ” (16,300 feet), which, however, is not a voleano, although much
dreaded by the natives, and made the subject of numerous popular legends. The
mantle of perennial snows clothing its craterless porphyritic cone is nowhere
pierced by any fumeroles. According to the Aztecs the two mountains were
divinities, Ixtaccihuatl being the wife of Popocatepetl, which now serves as a
meteorological indicator for the populations dwelling at its base. When the vapours
are a dense black colour, and roll away from the crater in great wreaths in the direc-
tion of the north, rain may be expected. But when the smoke sets southwards it
is a sign of approaching frosts and cold weather. If again the column of vapour
assumes a vertical direction, it is regarded as a forecast of high winds, or else of
earthquakes. Two or three hours before a thunderstorm bursts over the plain,
the crater is seen to discharge at intervals quantities of ashes and pumice.

The two sister mountains which dominate the valley of Mexico stand at the
angle of the triangular bastion which is formed by the central plateaux of Ana-
huac. In the neighbourhood of Tehuacan the Western and Eastern Sierra Madres

VOLCANOES OF MEXICO. 29

cross their axes, and from this junta, or converging point, the two systems are
merged in one as far as the isthmus of Tehuantepec.

But if the Western Sierra Madre seems to be abruptly terminated at a short
distance to the east of Mexico by a rampart of mountains belonging to another
system of crests, the volcanic zone is continued far beyond Popocatepetl by the
eruptive character of the prevailing formations. Malintzin or Malinche, the
Matlalcueyatl of the ancient Aztecs, which is called also Dona Marina in honour
of Cortes’ young Indian interpretress, rises in isolated majesty to a height of
13,550 feet in the middle of the Tlaxcala plateau. According to the local legend
Malintzin was the daughter of Popocatepetl and Ixtaccihuatl, and had wandered
far and wide before finding a favourable resting place.

Other large eruptive cones stand on the verge of the uplands, on the border
range belonging to the Eastern Sierra Madre. In this range the two loftiest sum-
mits are the volcanoes of Cofre de Perote and Orizaba, both of which are visible
from the sea. The Cofre owes its name of “ coffer” to the quadrilateral form of
its summit (13,500 feet), which is often wrapped in aérial shrouds, looking like a
vast sarcophagus raised aloft. The Cofre, which was the Nauhcampa-tepetl or
“ Four-ridged Mountain” of the Aztecs, is surrounded by a malpais of lavas, on
the west side of which lies the famous Chinacamote cavern. This natural curiosity,
said by the natives to be six or seven leagues long, is of difficult access, owing to
the huge blocks that have fallen from the roof.

Parasitic craters, which are now extinct, open on the flanks of the Cofre, and
from its base long lava streams descend seawards. Even beyond the tertiary and
quaternary deposits which overlie the older formations of the seaboard, a chain of
reefs, derived from ancient eruptions, and known as the Boquilla de Piedras, is
disposed in a line with the shore. Macuiltepec, or the “ Five Mountains,” on the
slopes of which stands the town of Jalapa, is also an extinct crater now filled with
vegetation.

Orizaba, which overlooks the city of the same name some 30 miles south of
the Cofre, exceeds Popocatepetl in altitude. According to the lowest estimates
it is at least 17,500 feet high ; some observers raise it to 17,860, while Perez gives
it an elevation of 18,400 feet, or about 50 more than Humboldt’s calculation.

Orizaba’s Aztec name of Citlal-tepetl, or “Star Mountain,” may perhaps be
due to the fact that the summit of its cone is seen glittering amid the stars, unless
it refers to the burning lavas formerly discharged from its crater. No mountain
presents a more imposing appearance in the perfect symmetry of its outlines, and
the beauty of its snowy crest towering above the verdant belt of its forests and the
ever-shifting clouds of the lower atmospheric strata.

The lower slopes are easily ascended, but the topmost cone presents great
difficulties, so that but few travellers have succeeded in hewing a flight of steps
in the higher snows, and thus reaching the ashes and scoriæ of the great crater.
This culminating point was first reached in 1848 by Raynolds and Maynard, who
were serving in the American invading army. Three years afterwards Doignon
followed in their footsteps, and to him we owe the first description of the crest, with

30 MEXICO, CENTRAL AMERICA, WEST INDIES.

its three craters and intervening walls. The central oval-shaped cavity is over a
quarter of a mile in circuit-and from 120 feet to 130 feet deep.

The last great eruption of Orizaba appears to have taken place towards the
middle of the sixteenth century. About the middle of the present century vapours
and sulphurous jets were still ejected from the crumbling rocks, which were
peeling away like the plaster-work of some old ruin; but these almost transparent
vapours were seldom visible from the lower regions. Yet an inner wall could be
seen, disposed obliquely in such a way that its slope was confused with that of the
mountain itself. In 1878 the igneous forces were entirely extinguished, and the
crater is now usually filled with snow, which is regularly collected as on Popocatepetl.

Fig. 12.—Or1ZABA PEAK.
Scale 1 : 500,000.

= [1

a He
Nest of h

9Miles. a

Parasitic cones are dotted over the slopes of Orizaba, as well as on the surround-
ing plains. These cones, from 400 to 500 feet high, resemble huge barrows, and
in fact are said by the natives to be funeral mounds erected over the remains of
ancient kings. All must have long been extinct, for they are now clothed with
forest growths, and the craters themselves have become filled with a dense vegeta-
tion. Nevertheless a still active crater lies in the Derrumbaderos group (10,300
feet) on the crest of a volcanic cone north-west of Tepetitlan.

Orizaba is not the terminal cone in the Mexican igneous zone; beyond it an
isolated volcano, Tuxtla, 4,950 feet high, stands on the seashore near the extreme
curve formed by the Gulf of Mexico between the mainland proper and the Yucatan
peninsula. Tuxtla lies 135 miles in a straight line from Orizaba, and it is separated
from the Sierra Madre system by extensive tracts of alluvial soil watered by several
streams. In 1664 it discharged some molten lavas, and was then quiescent till the

THE LLANOS OF MEXICO, 81

tremendous outburst of 1793, when the ejected scoriæ were said to be wafted in one
direction as far as Vera-Cruz and Perote, in another all the way to Oaxaca. The
disturbances have been renewed in recent times.

According to the unanimous testimony of the natives the two volcanoes of Orizaba
and Tuxtla ‘ hold converse together”’ by means of muffled rumblings like the sound
of distant thunder. The headlands of lava projected seawards by Tuxtla form the
eastern extremity of the winding volcanic zone, whose central axis, about 730 miles
long, coincides very nearly with the 19th parallel of latitude, and is continued far
into the Pacific westwards to the Hawaii Archipelago. The uninhabited Revilla-
Gigedo islands, which lie on the track of this conjectural volcanie fault, are
probably of igneous origin; Poulett Scrope mentions the fact that vessels navigating
those waters frequently find the surface covered with floating pumice.

The region of the Mexican voleanoes also coincides with the principal zone
of earthquakes, whose undulations are usually propagated in the direction from
east to west in a line with that of the burning mountains. The province of Jalisco
especially is much exposed to these seismic movements. Buildings erected on
granite or porphyry rocks suffer more than others from such disturbances.

The Eastern Sierra Madre, whose culminating peaks are the Cofre and Citlal-
tepetl, forms, like the western system, a southern continuation of highlands lying
_ within the United States frontier. The parallel ridges of the Apache Mountains,
which are disposed in the direction from south-west to north-east, and which are
pierced by the gorges of the Rio Bravo, reappear on the right or Mexican side of
that river. Here they develop a long line of jurassic limestone ramparts running
south-eastwards and presenting precipitous slopes whose sharp crests are here and
there pierced by a few eruptive cones.

These crests do not exceed an average altitude of about 3,500 feet; but like
the western range they rise gradually southwards, and in the neighbourhood of
Saltillo some of the summits alzeady attain an elevation of 6,600 feet. In these
regions of north Mexico the two converging eastern and western sierras are not
yet connected by any transverse ridges, but are, on the contrary, separated by vast
plains and by basins of quaternary alluvial matter which were formerly deposited
by extensive inland seas, and which under the action of the winds have since
assumed the form of elevated dunes. Here they take the name of //anos, like the
grassy savannahs of Venezuela; but in Mexico these old lacustrine beds have a
different vegetation, and they are moreover divided into distinct depressions by
small ridges of volcanic or other hills rising above the plains. These ridges are
for the most part disposed in the direction from north-west to south-east, parallel
with the two great border ranges, and thus form narrow gulches, ravines or cañons,
which are traversed by rivulets and highways.

One of these steppes is the Llano de los Cristianos, which occupies some thousand
square miles south of the Rio del Norte and its affluent, the Rio Conchos, and which
is divided into a multitude of secondary plains by numerous sierras and chains of
hills. Farther south the Llano de los Gigantes, so called from the remains of

gigantic animals found in the clays and sands formerly supposed to be those of

32 MEXICO, CENTRAL AMERICA, WEST INDIES.

ancient giants, is far more level, its uniform surface being broken only by a few
knolls of low elevation. South-eastwards it develops into the Bolson or “ Purse ”’
of Mapimi, a vast sandy and saline basin, for the most part desert, about 40,000
square miles in extent. The Bolson de Mapimi is the Sahara of Mexico.

South of this depression the ground rises, and the two border ranges are here
connected by intermediate highlands and the crests of a mountainous plateau.
South-east of Saltillo a first group of summits attains a height of 8,450 feet;
farther south a peak inthe mining district of Catorce exceeds 9,000 feet; the crest
of the Veta Grande in Zacatecas maintains an altitude of 9,200 feet; the Cerro de
la Cruz, near Aguascalientes, is said to be exactly 10,000 feet high ; the Gigante,
or ‘‘ Giant,” near Guanajuato, exceeds it by 850 feet, while a neighbouring summit,

Fig. 13.—Votcanors oF Mexico.

Scale 1 : 11,000,000.

West of Graammieh

= 180 Miles.

despite its name of Llanitos or “ Little Plains,” approaches 11,500 feet. Lastly, all
the northern part of the states of Queretaro and Hidalgo is occupied by a chaos of
peaks and cones, some of which are distinguished by their fantastic outlines. Such
is the Mamanchota (about 10,000 feet), the “Organos ” of Actopan, so named
from its porphyry towers disposed like the gigantic pipes of an organ.

Owing to the sporadic disposition of the mountain masses scattered over the
plateau, they may almost everywhere be easily turned without having to be crossed.
It was thus that the migrating tribes and conquering hordes were able to advance
southwards by following the natural routes winding round Malinche and Popoca-
tepetl, and meandering amid the heights of Hidalgo, Queretaro, and Guanajuato.

On the other hand the escarpments of the plateau are in many places extremely
difficult to scale, and especially to turn horizontally, owing to the deep barrancas
excavated in parallel lines along the slopes of the hills. In the districts where
pumice and light scoriæ are the prevailing formations, the running waters have

THE MEXICAN PLATEAUX. 33

scooped out enormous gorges hundreds of yards deep, which converge in still larger
ravines before reaching the level of the plains. The best known of these barrancas
are those of the sierras of Tepic, of the Colima and Orizaba volcanoes and neigh-
bouring highlands. Sometimes a whole day is required to reach a village which
may be seen perched on a terrace only a few miles distant; but in the inter-
vening space the traveller has perhaps to cross four or five deep troughs, whose
crumbling slopes are scored by dangerous zigzag tracks. In some of the older
barrancas the slopes are entirely concealed by a dense vegetation.

But while nature is destroying in one place it is building up in another.
The plateaux, the isolated mountains, and even the volcanoes of comparatively

Fig. 14.—Ianrous REGIONS AND VOLCANOES OF Mexico.
Scale 1 : 12,000,000.

LE EX 4 4a
“ly” , F Vy
A

eZ, DE
Y hy Q
Vey of pide 5
Gp WG

einkS ;

16°

West of Greenwich

* CD WD °

Active Volcanoes. Eruptive Rocks. Sedimentary Rocks. Extinct Volcanoes.
The blank spaces have not yet been thoroughly survey ed.
180 Miles.

recent geological date, as well as the flanks of giants such as Popocatepetl, are
found to be covered with an argillaceous or marly layer to an average depth of from
15 to 30 feet. These layers are composed entirely of dust brought by the remolinos
de polvo, little whirlwinds rising at intervals on the plateaux, “like movable
minarets, disappearing and reappearing incessantly.” But this dust itself, which
now completely clothes the hill-sides, can come only from other formations of
recent origin, from the so-called tepetate, a clay detached by the rains from the
rocks, and elsewhere deposited in the form of fine alluvial matter.

South of the uplands, lying between the two border ranges, the surface of the
plateaux is occupied by a series of plains, the beds of old lakes, or inland seas.
One of these is the Bajio, a long sinuous depression which winds for about 125

34 MEXICO, CENTRAL AMERICA, WEST INDIES.

miles along the base of the Guanajuato Mountains, and which is covered with a
friable black clay, resulting from the disintegration of the basalt rocks.

In these regions, comprised in the triangular space which is enclosed by the
two converging sierras, the mean elevation of the pedestal exceeds 6,600 feet, and
here nearly all the towns stand at this altitude above the sea. Morelia, situated
in a low valley at the northern foot of the voleanic range, lies only about 200 feet
lower. Toluca is 8,500 feet, the neighbouring village of Tlaluepantla 9,180 above
the sea-level, and Mineral del Monte, in the province of Hidalgo, 65 feet lower.
Lastly, the farmstead of Tlamecas, which is inhabited throughout the year, lies

Fig. 15.—CoNvERGENCE or THE TWO Serra Maoprzs.
Seale 1 : 4,800,000.

estof

120 Miles.

on the flanks of Popocatepetl at an altitude of 12,560 feet, an altitude at which
the natives of the lower regions sometimes find it difficult to live. |

The uplands, which form a south-eastern extension of the Anahuac plateau,
present no kind of symmetry in their general design. They may be regarded as
the remains of an ancient plateau carved into irregular masses by the running
waters. These waters have eroded the rocks on .both slopes, leaving erect the
harder masses, which form irregular ridges disposed in various directions, some
parallel with, others transverse to the border ranges. By the old Aztecs, these
highlands were called Mixtlan, or “Cloud Land,” and the Spaniards still call
them Mixteca Alta, that is, Uplands of the Mixtecs, or “ Cloud-dwellers.”’

North of Oaxaca, the Cerro San Felipe del Agua, which may be regarded as

THE MEXICAN UPLANDS. 35

belonging to the central axis of the mountain region, attains a height of 10,300
feet ; but the culminating point is the Zampoal-tepetl, which lies on a secondary
branch, and which, according to Garcia Cubas, exceeds 11,200 feet. From its
summit a view is commanded both of the Pacific and the Gulf of Mexico.

South of these irregular uplands, which form the fractured stem of the central
chain, the Sierra del Sur, a more continuous and better-defined range, stretches
south-eastwards along the Pacific coast. This range, which is also sometimes called a
Sierra Madre, is said to reach an altitude of 9,200 feet in the Cimaltepec district,

Fig. 16.—Various ALTITUDES oF THE Mexican Movuntatns AND Towns.

Popocatepet/” oS Orizabs

«/xtacihuat/

Wevado de To/uca

Neyado de Colima
Mealinche .C. de Perote

*Jancitaro

CP imal,
40s Llanitos

5 “C?S7Fel;
C°oel Gigante VE

.Alamos de Catorce
“Toluca

Chihuahua, Zacatecas

: MEXICO
Fresnillo, $ +Apam

6 6001. Guanajuato, “Puebla

S.Cristobal ~

“Aguascalientes .Tehuacan

Guadalajara’ Oaxaca

Jalapa,

Santa-Cruz : ‘Oneala

SR EE roe a or ccc cr ee ee ee — —

Colima® Monterey ~9- Andres Tuxtla

Vera-Cruz, Merida,

West of G reenwich

south of Oaxaca. Near Juquila, on the sea-coast, stands an isolated headland, the
extinct Chacahua volcano, whose crater is now filled with sulphur. Another
cone, one of the ten still active volcanoes in Mexico, lies farther east near Pochutla.
Before 1870, when it suddenly ejected scoriæ and vapours, it was supposed to
be extinct, all memory of any previous explosions having died out.

In the isthmus of Tehuantepec the Mexican ranges are continued on the
Pacific side by a series of uplands which are crossed by six passes at a low eleva-
tion. The lowest, which takes the name of Portillo de Tarifa from a neighbouring

36 MEXICO, CENTRAL AMERICA, WEST INDIES.

village, is only 1,000 feet high. Most of the high grounds skirting the plains of
the isthmus affect the form of ‘tables ” ; seen from the surrounding mountains,
they merge almost entirely with the lowlands.

According to Spear, a geologist attached to one of the numerous expeditions
that have studied the isthmus of Tehuantepec, the terraced formations consist

partly of cretaceous rocks deposited at a time when the Atlantic and Pacific |

Oceans were here connected by a broad channel. After their upheaval the
flanks of these chalk cliffs became overlaid on both sides by more recent tertiary
and quaternary formations. The land still continues to encroach insensibly on
the ocean; the Pacific Coast, formed of late alluvial matter, is continually

advancing seawards, while the lagoons along the shore are gradually drying up. .

In the isthmus of Tehuantepec low-lying tracts occupy a larger space relatively to
the whole region than in any other part of Mexico.

The two oceans were also at one time connected farther north by another
marine passage, and the so-called “ Valley ” of Mexico in the very centre of the
Anahuac tableland is a remnant of this old branch of the sea. Towards the close
of Mesozoic times the marine waters winded over these lands which at present
stand over 6,500 feet above sea-level, and the volcanoes now surmounting them
had not yet discharged their lava streams. At this epoch the contour line of the
Gulf of Mexico also lay far more to the west than in our days. The rich silver
mines are nearly all situated in the two Sierra Madres north of the “ Valley,”
and are disposed along certain definite lines. Thus their main axis appears to run
due north-west and south-east between Batopilas and Guanajuato, and the famous
argentiferous lodes of Zacatecas, Fresnillo, Sombrerete, and Durango all lie on or
near this axis; the lodes themselves are disposed in the same direction.

Rivers AND LAKES.

The form of the Mexican plateau with its narrow escarpments, and its border
ranges disposed parallel with the seaboards, combined with the dry climate of the
northern and central regions, has prevented the development of any large fluvial
systems with extensive ramifying arteries. Of all Mexican rivers the most impor-
tant, if not for its volume at least for its length and for the part that it plays as
the political frontier-line between the Anglo-Saxon and Hispano-American repub-
les for over 720 miles of its course, is the Rio Bravo, or Rio Grande del Norte. The
Mexican part of its basin comprises about 94,000 square miles, or one-third of the
whole area of its drainage ; but it receives scarcely any copious or perennial streams.
Most of their beds are dry except during the rainy season, and their waters, ren-
dered saline by lodging in shallow basins, give a brackish taste to the Bravo itself.

The largest affluent on the Mexican side is the Rio Conchos, whose headstreams
are fed for a distance of over 200 miles north and south by the eastern slopes of
the great Sierra Madre between the States of Sonora and Chihuahua. From the
Eastern Sierra Madre flows the Rio Salado, or “Salt River,” whose very name
indicates a prolonged period of drought. In the same range rises the Rio San

THE MEXICAN RIVERS. 37

Juan, which is formed of the numerous sparkling streams that water the more
fertile districts of Coahuila and Nuevo-Leon. One of these streams towards the
southern extremity of the basin is the Puente de Dios, which plunges from a
height of 200 feet into a profound chasm 70 or 80 feet below one of those natural
causeways which are here called ‘ God’s

Bridges.” Fig. 17.—Tamavurpas Coast Lagoons.
Scale 1 : 2,500,000.

The alluvial matter brought down by
the Rio Bravo has caused the land to
encroach far beyond the normal coastline ;
but it has failed to fill up the coast
lagoons, so that here is developed a
double shoreline; the sandy strips, and
the seaboard proper. Elongated back-
waters, which continue those fringing the
coast of Texas round the north-western

shores of the Gulf of Mexico, are disposed

parallel with the sea in a continuous

chain, broken only by the alluvial banks
which have been deposited by coast

streams along both sides of their chan-

nels.

These inner waters, which have a

total length of about 200 miles, commu-

nicate with the open sea only by narrow

passages, which shift their position with

the storms and rains. The water also

varies in its saline contents according

to the freshets of the coast streams and

the irruptions of the sea. The lagoons

" EE
To Sarre
Soto /2 Nerina

are gradually silting up with the sediment

deposited by the two little coast streams,

the San Fernando or Tigre, and La Ma-
rina, the old Rio de las Palmas.

South of La Marina and of a few other
rivulets, the Tamesi and the Panuco, which

formerly flowed in separate channels, are = — == ==

now united i istri i 0 to 10 10 to 25 25t050 650 Fathoms
i. n a district studded with Fathoms. Fathoms. Fathoms. and upwards.
lagoons and swamps above the bar of lanl neice

Tampico; hence the name of Tampico

sometimes given to the two united rivers. The Pänuco, the more copivus of the
two, rises north of the Mexican Valley, and even receives some contributions
through the Huehuetoca cutting; under the names of Tula or Montezuma it
describes a vast semicircular bend towards the west across the Hidalgo uplands,
beyond which it collects the various streams flowing from Queretaro. One of

38 MEXICO, CENTRAL AMERICA, WEST INDIES.

these disappears near Jalpan in profound caverns about 2 miles long, which
like the arch at Nuevo-Leon also bears the name of Puente de Dios. In these
subterranean galleries human bodies have been found covered with stalactites.
Another of these tributaries forms the famous Falls of Regla, where the water
rushes over a breach opened in a cluster of basalt columns. On both sides the

Fig. 18.—Coatzacoatcos Bar.
Scale 1 : 60,000.

ÿ “2°

I Bo st 9 ER ,
OS Se Lighthouse
a so Pee.
ES

“à,

REO ee. lee AN SNS ==
5S. COATZACOALCOS fay

PO SOA). gs
STATE

om.
PALERS TOUS

West of Greenwich

0 to 16 16 to 32 32 Feet and
Feet. Feet. upwards.

2,200 Yards.

columns are festooned with wreaths of lianas, while the white waters are broken
into cascades, between which rise the hexagonal groups of bluish rock.

The united Panuco and Tamesi have together almost completely drained the
chains of lagoons formerly fringing this part of the coast; but south of the
Tampico river a small inland sea, the Laguna de Tamiahua, still exists, being
protected by a narrow cordon of sands from the surf. This rampart does not take
the slightly concave form presented by most of the other sandy strips gradually

THE MEXICAN RIVERS. 09

formed by the action of the waves at the entrance of the inlets along the coast,

Fig. 19.—Tue Recta Fatrs.

RL RAS
NY DR EM HIS & SC ey
ash DON dese Fe ae

On the contrary it projects some 25 miles in a convex curve at the Cabo Roxo, or

40 MEXICO, CENTRAL AMERICA, WEST INDIES.

“Red Cape,” a form evidently due to the presence of a group of rocks or reefs
which has served as a support for the two converging beaches.

In many places the shore is covered with dunes, which have been gradually
raised above the beach, and which drift inland under the influence of the pre-
vailing trade winds. Thus the “ Villa Rica de la Vera Cruz,” founded by Cortes,
near Zempoala, is now to a great extent covered by dunes of shifting sands.

The theory has been advanced that these dunes may perhaps have been
raised since the coast reefs, which formerly stood some 6 or 7 feet above the
surface, were removed by the builders engaged on the fortress of San Juan d'Ulüa
and the town walls. But this view is’ at variance with the fact that dunes even
higher than those of Vera Cruz have been formed on many other parts of the
coast, and especially near Alvarado; one of the sandhills in the vicinity of Anton
Lizardo is no less than 265 feet high.

Beyond this point the Alvarado estuary, near the southern inlet of the Gulf of
Mexico, receives a large number of converging streams, the largest of which are
the Papalodpam, or “ Butterfly River,’ and the San Juan. They are both very
copious, thanks to the heavy rainfall produced by the trade winds on the northern
slopes of the Oaxaca uplands.

The Coatzacoalcos, or ‘‘ Snake River,’
the Tuxtla voleano, and which had already been discovered by Grijalva before the
expedition of Cortes, is also an extremely copious stream, regard being had to its
length of about 220 miles. Its catchment basin is confined to the alluvial plain
and the amphitheatre of low mountains which form the northern slope of the isth-

’ which flows from the opposite side of

mus of Tehuantepec. Nevertheless, its lower course is no less than 800 or 900
yards wide ; large vessels after once crossing the bar are able to ascend as far as
Minatitlan, some 25 miles from its mouth, while boats reach the village of Suchil,
near the middle of the isthmus, and over 60 miles from the coast. But at the
point where the fluvial and marine waters meet there is formed a dangerous sill,
which, since the time of Cortes’ expedition, has always maintained a uniform depth
of from 12 to 14 feet of water. Many vessels have been wrecked at the entrance
of the river, and it is mainly owing to this danger that engineers have abandoned
the idea of constructing a ship canal across the isthmus of Tehuantepec.

On the opposite side the rivers flowing to the Pacific are obstructed by similar
formations. The large lagoon of Tilema, which lies just south of the narrowest
part of the isthmus, and towards which converge numerous watercourses, has only
from 7 to 10 feet of water on its bar, according to the seasons, and it is often inac-
cessible, even to vessels of light draft. One of the caravals built by Cortes for the
purpose of surveying the coast was wrecked at this point.

The mouth of the Rio Tehuantepec, which reaches the coast west of the great
lagoon, is completely closed by sands for a great part of the year. Shipping has
then to ride at anchor either in the open roadstead well named La Ventosa, or
“Windy,” or near the dangerous granite reefs of the Morro de Tehuantepec, or
else far from the alluvial lands of the isthmus in the Salina de Cruz inlet, terminus
of the railway, and now sheltered by a breakwater.

THE MEXICAN RIVERS. 41

Being skirted by loftier ranges running nearer to the sea, the Pacific side of
Mexico presents far less extensive low-lying coastlands and secondary beaches than
the Atlantic side. Nevertheless, even here there are a few coast lagoons, especi-
ally in the district west of Acapulco. Beyond it the sea receives the waters of
the Rio Mexcala or de las Balsas, one of the chief Mexican rivers, whose farthest
sources lie on the southern and some even on the eastern slopes of the volcanic
range. The Apoyac, its principal headstream, which flows by Puebla, rises on the
flanks of Ixtaccihuatl and is fed higher up by the snows melted by the thermal
springs, lower down by several saline rivulets.

The Rio de las Balsas, that is, “ of the rafts,” as indicated by its name, is, to a
limited extent, navigable along its lower reaches; above the bar it is accessible to
small craft, which, higher up, are arrested by rapids, whirlpools, and a high cas-
cade. For a space of 220 miles there occur no less than 226 obstacles of this sort,
eddies, rapids, or dangerous reefs. The volume discharged through the two
mouths of the Mexcala is estimated at 2,500 cubic feet per second. The Rio Tux-
pam, or de Colima, and the Amecas, two less copious streams which reach the
Pacific farther north, have a mean discharge of 1,100 and 750 cubic feet respectively.

The Rio Lerma, or Santiago, the Tololotlan of the Indians, is also a considerable
stream. By the riverain populations it is, in fact, known as the ‘ Rio Grande,”
while the inhabitants of Michoacan call it also Cuitzeo, from the large lake situated
in their province. It rises in the State of Mexico in the very centre of the Ana-
huac plateau, and its farthest sources, issuing from underground galleries, descend
from the Nevado de Toluca down to the twin lake of Lerma, the remains of an in-
land sea which formerly filled the upper Toluca valley north of the Nevado volcano.

At its issue from the lake, or rather marshy lagoon, the Lerma stands at the
great altitude of 8,600 feet, and during its winding north-westerly course across
the plateau, the incline is very slight. In this upland region it is swollen by
several affluents, some of which, like the main stream itself, flow from lakes dotted
over the tableland. After completing half of its course at La Barca, the Lerma is
still over 5,600 feet above sea-level. Here, some 280 miles from its source, it enters
the large lake Chapala, near its eastern extremity ; but about 12 miles below the
entrance it again emerges through a fissure on the north side of the lake, and still
continues to flow throughout its lower course in the same north-westerly direction.

Chapala, thus obliquely traversed by the current of the Lerma, is the largest
lacustrine basin in Mexican territory; but this flooded depression, about 600
square miles in extent, is very shallow, its mean depth being only 40 feet, and
the deepest cavities not more than 110 feet. Everywhere, but especially on the
north and east sides, its blue limpid waters are encircled by an amphitheatre of
hills, whose slopes are covered with a rich growth of forest trees and lianas. The
shores of this romantic basin present some of the loveliest scenery in Mexico ; but
till recently few travellers ventured to visit these almost uninhabited regions.

At present a railway runs along the north-east side of the lake, and it has even
been proposed to found a school of navigation on one of the inlets of the inland sea.
Other lakelets dotted over the slopes of the mountains about the western extremity

42 MEXICO, CENTRAL AMERICA, WEST INDIES.

of Chapala seem to imply that its basin was formerly far more extensive that af
present ; at that timeit appears to have discharged its overflow westwards through
the valley of the river now flowing towards the Bay of Banderas, and some
engineers have proposed to cut a canal through this old fluvial bed. At the point
where the outlet was situated lava streams descended from the neighbouring
heights in prehistoric times. The issue was thus obstructed, and the waters were
forced to expand into a lake or else considerably to raise their level, and after-
wards seek a new issue through the lowest breach in the encircling hills.

Fig. 20.—Laxe CHAPALA.

Scale 1 : 1,500,000.

West of Greenwich : 102°20*

30 Miles.

These hills are in fact traversed by the Lerma through a series of gorges exca-
vated by erosion in the eruptive rocks. To judge from the extreme irregularity
of its course, this fluvial valley would appear to be of comparatively recent
geological date. Its whole bed is disposed like a gigantic flight of irregular steps,
where the stream develops a continued succession of high cascades and rapids, all
the way to the vicinity of the coast. These gorges begin with one of the finest
cataracts in Mexico, named Juanacatlan from a neighbouring village. Rushing
over a precipice 65 feet high, the current acquires a tremendous impetus estimated
at 30,000 horse-power, and it is feared that the neighbourhood of Guadalajara may
tempt speculators to convert the falls into a series of reservoirs and mill races.

Despite its abundant discharge, estimated at 4,000 cubic feet per second, the
Lerma is not navigable, and its bed may in many places be easily forded. But its
numerous ravines are scarcely anywhere accessible to wheeled traffic or even pedes-
trians ; hence roads and tracks have had to be laid down across the escarpments of
the surrounding mountains.

At Santiago, where the Rio Grande at last emerges on the low-lying coastlands,
it is still 145 feet above sea-level; it enters the Pacific through a ramifying

THE MEXICAN RIVERS. 43

channel just north of San Blas Bay, opposite the Tres Marias islets, which continue
north-westwards the normal trend of the coast, as indicated by the direction of the
shore-line south of Cape Corrientes. The alluvial matter washed down by the
Lerma has filled up a part of the space separating the mainland from this insular
group; both northwards and southwards the land is encroaching seaward, and the

Fig. 21.—Cotorapo Estuary.
Scale 1 : 850,000.

Wy 4
WY

iN y

ip pa
UI
AU

S We

4
5 RU

Re =
à d

EAU
ZAR
A1)

di M al

Al:

AD
D

= ota! ©

15°10 West of Greenwich

oe
[SS aor Pech
= == asie
SSS == LDC

Oto 5 5 Fathoms Banks exposed
Fathoms. and upwards. at low tides,
18 Miles.

true coast at the foot of the hills is now washed by shallow lagoons which are pro-
tected by sandy strips from the open sea.

North of the Rio Lerma no other copious rivers reach the Pacific within the
Mexican frontier; even those which, like the Rio del Fuerte, the Rio Yaqui, and
the Sonora, have large catchment basins, roll down very little water. This is due

44 MEXICO, CENTRAL AMERICA, WEST INDIES.

to the slight rainfall and long droughts, during which the springs run dry and
large rivers become impoverished, though their sources lie far inland on the interior
of the plateau, and like the Rio Yaqui even on the eastern slope of the Sierra
Madre. Many noisy torrents rushing through foaming cascades over the heights
of the Sierra Madre fail to reach the sea, and run out in the sands of the lowland
plains. Others, especially in Lower California, are mere wadies which are seldom
flooded, and their stony beds are the only roads in the country. To obtain a little
water oozing up between the shingle deep holes have to be sunk, which are locally
known by the name of bataques. The old estuaries have become salt pans, and the
Rio Colorado, whose lower course alone is comprised within Mexican territory,
resembles the rivers of Sonora in the slight amount of its discharge compared with

Fig. 22.—Crosep Bastys or Mexico.
Seale 1 : 30,000,000.

Po /knaco
&

y S
> D

à ; =
= ext IR Z Tr Mie

13°40 West of Greenwich

=
Lakes of the closed basins,
620 Miles.

the vast extent of its drainage area; however, this great watercourse is navigable
for some hundred miles beyond the limits of the common frontier.

All that part of Mexico which is comprised between the two converging
border ranges is also too arid for all its watercourses to unite in perennial streams
and reach the ocean through the Rio Bravo or any other large river. Most of
them, being too feeble to surmount the heights enclosing or intersecting the plains,
lose their waters in some shallow lagoon which rises or falls with the seasons. All
the saline basins met in Chihuahua and Coahuila are depressions of this sort formed
by torrents descending from the mountains.

Such is the large Guzman lagoon near the Arizona frontier, where is discharged
the exhausted current of the Rio Casas Grandes at a lower altitude than the level

CLOSED LACUSTRINE BASINS. 45

of the neighbouring Rio Bravo del Norte. Other marshy tracts, like the lagoons
of Santa Maria and dos Patos, have a similar origin, and the bed of the Bolson de
Mapimi is also occupied by a closed reservoir, the Tlahualila lagoon.

Farther south the Rio de Nazas, which is a somewhat copious stream in the
upper valleys of the Sierra Candela, is arrested in the Laguna del Muerto, while
the Rio d’Aguanaval does not always reach the Laguna de Parras. In various
parts of these desert spaces occur numerous ojos or “eyes,” that is, springs, some
thermal, some cold, but nearly all richly charged with chemical substances.
Several have gradually raised circular margins of siliceous or calcareous deposits
round their orifice, and in some places these accumulations are high enough to
form veritable hillocks. Froebel saw astreamlet flowing from a knoll about thirty
feet high, which had been built up in this way by the water itself.

In the State of San Luis, where the plateau is already divided by the mountain
ranges into numerous small basins, there are no extensive lagoons like those of the
northern provinces; but this district contains over one hundred small lakes or
rather ponds, nearly all of which have become saline. The plains are largely
covered with various kinds of efflorescences, some composed of saltpetre, others
consisting for the most part of carbonate of soda. They still retain their old Aztec
name of fequesguite in Mexico, where the smelters use them in treating the various
silver and argentiferous lead ores.

Closed lacustrine basins are also found in the valleys of the border range south
of the plateau. Such is the Patzcuaro or “Greater Lake,” in the State of Mexico,
an island-studded depression encircled on all sides by mountains, and containing a
slightly brackish, but still potable water. Such is also the Cuitzeo, a deep reser-
voir which is filled by the river Morelia, whose extremely salt water sterilises all
the surrounding lands during the inundations.

But of all these flooded depressions the most remarkable are those from which
the Mexican plateau takes its name of Anahuac, that is, Anal-huatl, ‘“‘ Amid the
Waters,” a term afterwards extended to all the upland plains of this region.
These lakes, or rather shallow ponds, are disposed in a chain running north and
south for a distance of about 46 miles; but their superficial area varies from year
to year and from season to season, so that they present different contour lines on
maps constructed at different periods.

The southern lakes Xochimilco and Chalco really form only a single sheet of
water divided into two basins by a narrow dyke. Thanks to the copious streams
descending from the neighbouring hills this depression has maintained its old
outlines with little change. A canal, running northwards to the city of Mexico,
discharges the overflow into Lake Texcoco, which occupies the bed of a periodically
flooded basin from five to seven feet below the level of the capital. The northern
Lakes San Cristobal, Xaltocan, and Zumpango stand like Xochimilco and Chalco
above that level. Hence during the inundations, when the rivulets converge
from the plain of Pachuca, descending from basin to basin towards the south, the
city would be threatened with total destruction were the embankments to burst
which have been constructed below each reservoir.

46 MEXICO, CENTRAL AMERICA, WEST INDIES.

From the descriptions handed down by the Spanish conquerors, and the
comparative observations made at different epochs, it is evident that the extent
and volume of these Mexican lakes have continued to diminish during the last
three hundred and fifty years. The capital was formerly represented as a
“lacustrine city’? surrounded by flooded plains, whereas at present it stands on
dry land, the lakes no longer occupying even a third of the “valley”? They
have also become shallower, and the bed of the Texcoco basin is steadily silting
up with the sands of the plains moving forward under the action of the winds.
Its level would even be raised and its contents discharged on the city but for the
excessive evaporation, by which the volume of water is gradually diminishing.
In 1804, at the time of Humboldt’s visit, its depth varied from 10 to 16 feet, but
in 1885 it had fallen to 5 feet 6 inches in the deepest parts, with an average
of scarcely more than 2 feet. In 1881 it was even much shallower, little over
12 inches in many places, and in exceptionally dry years Texcoco, San Cristobal,
Xaltocan, and Zumpango have been exhausted. In fact this brackish depression
would have long ago been emptied but for the flow from Chalco and Xochimileo.

It is generally supposed that the local climate has really become drier since
the time of the conquest. The disappearance of the forests from the slopes and
plains would appear to have increased the evaporation by giving greater play to
the winds, without a corresponding increase, perhaps even a decrease, in the
rainfall. At present the contents of the lacustrine basins in the valley of Mexico
are insignificant compared with their volume in a former geological epoch. The
bed of the old lake, that is, the so-called ‘“ valley,” consists of quaternary débris,
sands, clays, pumice, scoriæ, organic remains, superimposed in successive layers
so thick that they have not yet been pierced by the shafts of an artesian well sunk
to a depth of 1,270 feet. In some places the calcareous strata of lacustrine origin
have yielded spring water at a comparatively slight distance from the surface; but
elsewhere nothing has been met except the quaternary deposits.*

The chemical composition of the Texcoco waters is itself an indication of their
gradual concentration in a continually narrowing basin. Xochimilco and Chalco
are both fresh-water reservoirs, their contents being constantly renewed; on the
opposite side of the valley the other small depressions are also flooded with fresh-
water. But the central lake is always brackish even after the heavy rains, when
it covers a considerable surface.

At a remote geological epoch, when the whole valley of Mexico was filled with
fresh water, the overflow was discharged through a breach in the mountains
northwards to the Tula or Montezuma, a headstream of the Panuco river. But

* Superficial area and relative altitude of the lakes in the Valley of Mexico (1865) :—

Extent. Height.

Sq. miles. inches.
Texcoco . : M > : . 77 below the capital.
Chalco . : De Ab UE 3 . 48 above ,, 40
Xochimilco : C'ADDOÉE : AEE “sgt ae 5
San Cristobal . = Sn: : MAR EN SE x
Xaltocan . : 4er 0 NE 4 JET Sg uch .

Zumpango ; ARLON : OD: RO: 2

CLOSED LACUSTRINE BASINS. 47

during the historic period, when a city stood on an island in the central lagoon
at a lower level than several of the separate basins which had formed part of the
original lake, it became necessary to protect the habitations and temples from
the inundations by which the lower part of the depression might have been

Fig. 23.— AREA or THE Mexican Lakes at Various PERIODS.
Scale 1 : 550,000.

ah,
PTE ce

Z 2
alco. =”

:-Guadalupe Ne

—— TD

X COL:

himalhuacan

xta pala pa— = == ax

Mi del Etoile

uae lxta paf

West of Greenwic

aS | 2 —

1520. 1600. 1700. 1865. Highest Floods.

Northern Lakes in 1880.
12 Miles.

flooded. The Aztecs had accordingly constructed strong defensive works, traces
cf which may still be seen near the cities of Ixtapalapa and Guadalupe.

But these embankments at last yielded to the pressure, and under the Spanish
rule the capital was for a time exposed to all lacustrine floodings. Towards the
beginning of the seventeenth century the situation became so dangerous that it

48 MEXICO, CENTRAL AMERICA, WEST INDIES.

was resolved to run an underground tunnel through the sill which confined the
flood waters on the north side. The viceroy summoned a vast army of Indian
labourers in order to complete the work within a single winter or dry season
from the end of November, 1607, to the middle of May, 1608. The Huehuetoca
or Nechistongo gallery, as it was called, had a total length of 9,000 yards, and a
mean height of 12 feet ; but it was not arched and the soil gave way. The outlet
was completely closed in 1629, when a terrific storm burst over the city, flooding
the streets to a depth of 10 feet. All traffic was carried on by boats, and five years
passed before Mexico again stood on dry land. The works had to be resumed,
but were carried on without any general plan and even on mutually destructive
lines, in one place by underground galleries, in another by open cuttings. The
latter system at last prevailed, and in 1789 the great undertaking was com-
pleted.

At several points the channel, excavated between high rocky walls, presents
the appearance of some of the boldest cuttings executed by railway engineers in
modern times. For a length of about 860 yards the height of the escarpments
exceeds 165 feet, and the opening of the passage is more than double as wide.
The river Cuautitlan, which discharged into Lake Zumpango a volume of about
400 cubic feet per second, was diverted to this desagüe, or emissury, and the
northern lakes also sent their overflow through the same channel.

But the friable parts of the cutting were frequently eroded, filling its bed
with mud and refuse. Hence the works had to be incessantly renewed, and during
the revolutionary wars they were abandoned altogether. Then came the great
floods of 1866, which threatened to swamp the capital with the swollen con-
tents of the northern lakes rushing through breaches in the embankments, and
during which the channel rolled down a volume of from 1,050 to 1,100 cubic feet
per second. To prevent such a disaster a new emissary was projected, which was
intended to carry off the overflow, not only of the northern lakes, but also that of
Texcoco. But little more than a beginning was made with the gallery six miles
long, by which the waters were to be drained off through the Tequisquiac Mountain,
For twelve years all operations were suspended and not resumed till 1881; at
present there is some prospect of the works being completed in 1893.

But scientific men in Mexico are far from being of accord on the subject of
drainage. According to L. de Belina the important question is not how to drain
the “valley,” but on the contrary, how to increase its humidity. Arid, dusty,
and treeless, the surrounding plains must be transformed to a desert unless the
running waters issuing from the uplands are husbanded for irrigation purposes,
and unless the slopes of the hills be replanted to improve the climate and regulate
the annual discharge.

CLIMATE—FLoRA—FAUNA.

Taken as a whole the Mexican climate is one of those that present the greatest
contrasts in a narrow space. Here the normal climate, as represented by the
parallels of latitude, is profoundly modified by the elevation of the land, the aspect

CLIMATE OF MEXICO. 49

of the mountain slopes, the force and direction of the winds, the distribution and
quantity of the rainfall.

Nevertheless, in certain regions a uniform climate prevails over vast spaces.
Thus the northern states contain extensive plains remote from both oceans, where
the extremes of temperature characteristic of the American Far West are continued
far to the south on all those plateaux where the prevailing vegetation are the
cactus and thorny plants, which constitute a special zone combining the characters
of both zones.

On the other hand the narrow region of the Tehuantepec isthmus belongs
entirely to the humid tropical zone, even on the mountains which form the divide
between the two oceans. The climatic contrasts caused by the different altitudes
are produced in a large way only in the central part of Mexico, on the Anahuac
plateau and the two border ranges. The route from Vera Cruz on the Atlantic,
across the plateau between the Puebla and Oaxaca uplands, and down to the
Pacific at Acapulco, is the highway where these sharply contrasted climates may
be studied to the best advantage.

The low-lying maritime zone comprises both the swampy and unfertile sandy
coastlands, and the well-watered plains and first slopes which are thickly clad
with leafy trees intertwined with festoons of hanas and surmounted by the tufted
crests of tall palms. This is the tierra caliente, the “hot land,” where the normal
temperature exceeds 74° F. Some places on the Mexican seaboard are in fact
amongst the hottest on the globe. Such is, for instance, the port of La Paz, which
earned for California the name of the ‘“ Hot Furnace ” given to it by Cortes.

Above the coast zones, one facing the Atlantic, the other the Pacific, follow
the tierras templadus, or ‘temperate lands,” comprised mainly between the
altitudes of 3,000 and 6,000 feet, but rising to a higher elevation in the southern
than in the northern states of the republic. These are the regions which corres-
pond to south-west Europe, at least in their mean temperature, vegetable products
and suitability for settlement by the white race.

The #erras templadas are succecded by the tierras frias, or “cold lands,”
which comprise the plateau proper with the encircling highlands. The less
elevated part of this region, growing maguey and cereals, is the most densely
peopled region in Mexico, whereas on the higher grounds, some of which rise
above the snow line, the climate is too rude to support a forest vegetation, or a
dense human population. Sometimes these higher grounds are grouped together
as a fourth zone distinguished by the name of tierras heludas, or ‘“ frozen lands.”

In many parts special conditions have placed the different vegetable zones
in close proximity without any graduated transitions. From the summit of
certain headlands, occupied exclusively by plants of a European type, the traveller
sees at his feet palm groves and banana thickets. From the crests of the great
voleanoes all three zones may even be seen superimposed one above the other.
Thanks to the increased facilities for rapid travelling, it is now possible in a
single day to traverse the three distinct zones, which elsewhere are separated
one from the other by intervals of many hundreds and even thousands of miles.

50 MEXICO, CENTRAL AMERICA, WEST INDIES.

But although in some exceptional districts the zones are brought into sharp
juxtaposition, they merge almost everywhere by successive transitions one into
another. It is only in a very general way that any given region can be said to
belong to such or such a zone, and the parting line oscillates greatly, especially
about the base of the mountains. A zone of mutual overlapping has been
developed under the thousand modifying conditions of soil, temperature, winds, .
the struggle for existence between the various species of plants. Certain glens
and slopes even occur, which, in their vegetation, form tropical enclaves in the
very midst of the temperate zone.

Regarded as a whole, Mexico, which is intersected by the tropic of Cancer

Fig. 24.—Verticat DisposrrioN or THE Mexican CLIMATES.

Seale 1 : 12,000,000.

102°40 West of G TE

CZ U)
Warm.

Temperate. Cold.
310 Miles.

almost exactly in the centre, is a hot country. Assuming its mean elevation to be
3,600 feet, the average temperature of these latitudes would be about 60° F., or
nearly the same as that of Nice or Perpignan in the south of France, but far below
that of African regions, such as the Sahara and Nubia, lying under the same parallels.
The Anahuac plateau may be described as a temperate region upheaved
above the tropical zone. It corresponds to the temperate and cold regions of ©
Abyssinia, which also dominate “hot lands,” such as Massawah and the Danakil
territory. But however favoured the Abyssinian plateau may be in its climate,
it is vastly inferior to Mexico in the advantages of position and means of access.
In its latitude, Mexico lies well within the zone of the trade winds, which
blow regularly from north-east to south-west, or from east to west, on the shores

CLIMATE OF MEXICO. 51

of the Gulf and the slopes of the mountains. But their normal direction is
frequently modified by the great inequalities of the relief and the trend of the
mountain ranges. The so-called norées, or northern gales, which prevail especially
from October to March in the Gulf waters, and which are justly dreaded by
skippers bound for Tampico or Vera Cruz, are nothing more than the trade winds
deflected from their course, and attracted southwards by the heated and rarefied
atmosphere of the low-lying plains of Yucatan. United with the cold current
which sweeps down the Mississippi, the trades blow with tremendous fury along
the seaboard, the storms often lasting for several days, and even a whole week,
to the great danger of the shipping on these exposed and harbourless coasts. The

Fig. 25.—IsoTHERMALS oF MEXICO MODIFIED BY ALTITUDE.
Scale 1: 30,000,000.

L _ _ Wi
Vy g

West df Greenwich
0 to 50° F, 50° to 59° 59° to 68° 68° to 77° 77° and upwards.
620 Miles.

full force of the norte is scarcely felt on the plateaux, and its strength is completely
exhausted before it reaches the Pacific slope.

The shores of this ocean have also their special atmospheric currents, which
are determined by the disposition of the coastline, and the form and elevation of
the neighbouring mountains. At irregular intervals during the summer the arid
and superheated plateaux attract the aérial masses from the equatorial waters, and
the Mexican uplands are at least once a year visited by sudden squalls sweeping
along the Columbian and Central American seaboard. At times they assume the
character of a veritable cyclone, blowing in a few hours from every point of the
compass. In 1839, one of these gales wrecked twelve vessels in the port of
Mazatlan ; and Manzanillo, the Port of Colima, was destroyed by another in 1881.

52 MEXICO, CENTRAL AMERICA, WEST INDIES.

The southerly or south-easterly storms, which have received from the missionaries
the curious name of Cordonazo de San Francisco, or “Scourge of St. Francis,”
rarely penetrate far into the interior, although a town of Michoacan, near the
verge of the central Mexican uplands, has with good reason been named 470,
that is, the “Stormy ” in the Tarascan language.

On the west side, the prevailing currents are the so-called papagayos, or north-
easterly trades, and the south-western monsoons, that is, the trades of the southern
hemisphere attracted to the north of the equator, and deflected from their original
course. |

Owing to the contrasts in the relief of the land, the differences of temperature,
and the irregularity of the winds, the rainfall is distributed very unequally through-
out Mexico, though it is chiefly regulated according to the seasons. Towards the
middle of May, when the sun stands near the zenith of the northern hemisphere,
the rains begin to fall. The clouds, following the track of the sun along the
ecliptic, discharge frequent torrential downpours, at least on the slopes facing
seawards. Usually, the approaching storm is indicated by a great black cloud

rising from the sea “like a huge torso with half-mutilated limbs.” It is locally
called the giganton, or “Giant,” who will soon swallow up all the heavens. In
the afternoon the clouds are rent asunder, and lit up by flashes of lightning
accompanied with thunder, in which the ancient Aztecs recognised the voice of
the god Tepeyolotl, or “ Heart of the Mountain,” rumbling in long echoes over
the hills. The sudden downpours are followed by rain lasting usually till
nightfall. Then it clears up, and by dawn the winds have already dried the
ground.

On the Mexican plateau the tropical rains, brought by the north-easterly
winds, fall regularly only during the four months from June to September, and
the showers generally last less than an hour. The rains are also interrupted,
especially in Juiy and August, by numerous fine days, and even by weeks of dry
‘weather, “St. Anne’s Spring,” asit is then called. They cease altogether in Octo-
ber, when winter begins, which however presents some of the features of a Euro-
pean summer ; hence its name of estéo, “summer,” or tiempo de secas, “ dry season.”

It is the lack of moisture in the ground, rather than the low temperature,
that strips the trees of their foliage, and thus imparts a wintry aspect to the land-
scape. But the lofty ranges also assume their snowy mantle at an altitude of
13,000, and even 12,500 feet. In exceptional years, the Ahualco Pass (11,520
feet) has been covered with snow all the way from Popocatepetl to Ixtaccihuatl,
and a few flakes have even at times fallen so low as Morelia (6,400 feet).

Numerous irregularities, however, are everywhere caused by the differences
in the relief and aspect of the land. Thus two contiguous districts will some-
times have a totally different distribution of moisture. In certain regions, notably
the temperate zone of Jalapa and Orizaba, from 1,500 to 8,000 feet high, the
vapours brought by the northern winds are condensed in fogs which lie on the
surface and precipitate.a fine but persistent mist. This is the so-called chipichipt,
which is awaited with impatience by the natives, for whom it is the essential

CLIMATE.—FLORA. 53

condition of prosperity, the salud del pueblo. During its prevalence the sun
remains clouded generally for a period of about eight days.

At all times the rainfall is more copious in the southern provinces, where the
land is contracted between the Atlantic and Pacific inlets, and where the sun twice
crosses the zenith of the earth. Here the annual fall ranges from 80 to 120 inches,
gradually diminishing thence northwards to the regions beyond the tropic of
Cancer. Thus in Sonora the rains scarcely begin before the month of July, and
are frequently interrupted during the normal season. Those northern regions
especially which lie between the two main ranges have a very dry climate, the
moisture-bearing clouds being here intercepted by the slopes of the Sierra Madres.
On these excessively arid plateaux a display of extremely vivid sparks is often
produced by the friction of two hard bodies. A continuous crepitation or crackling
sound is sometimes even heard escaping from all the rugosities of the rocky soil.

As a whole the Mexican climate, if not one of the healthiest, is certainly one
of the most delightful in the world. The zone of “ temperate lands” on both
oceanic slopes enjoys an “everlasting spring,’’ being exposed neither to severe
winters nor to intolerable summer heats; in every glen flows a rippling stream;
every human abode is embowered in a leafy vegetation, and here the native plants
are intermingled with those of Europe and Africa. Lach traveller in his turn
describes the valley in which he has tarried longest as ‘the loveliest in the world,”
that nowhere else the snowy crests or smoking volcanic cones rise in more im-
posing grandeur above the surrounding sea of verdure all carpeted with the
brightest flowers. In these enchanting regions there is still room for millions
and millions of human beings.*

The Mexican flora is, so to say, a living illustration of its climate, for the
plants thrive or droop according to the varied conditions of temperature, aspect,
and moisture. From the character of the vegetation the botanist knows at once
whether the heat or cold is excessive, the oscillations of the thermometer mode-
rate or extreme, the rainfall abundant or slight. In these respects Mexico presents
the greatest contrasts, deserts and steppes alternating with scrub, and mighty
forests bound together in an inextricable tangle of creepers and undergrowths.

In the. northern regions the rocky Chihuahua and neighbouring provinces,
where rain seldom falls, have an extremely sparse vegetation, consisting of greyish -
thorny plants with large hard leaves, a vegetation which adds little to the

* Meteorological conditions of some Mexican stations taken in the direction from north to south :—

Stations. Latitude. He oe i Te eee eae je ad
Monterey (1888) . . . . 25° 40’ 1,636 70° F. 137
Mazatlan (six years) . . 23°11’ 150 76° o9
Zacatecas (1888) . . . . 22°47’ 8,100 58° 19
San Luis Potosi (2 years) . 22° 05’ 6,230 62° 16
HeouMiSS8)) 3.) tu. le 219,7 5,920 65° 35
Guanajuato (1888) . . . 21° 1’ 6,645 63° 33
Guadalajara (6 years) . . 20° 41’ 5,180 72° 34
Mexico'(12 years), . : . 19°26’ 7,400 60° 30
Colima (15 years) . . . 19° 12! 1,655 78° 42
Puebla (2 years). . . . 19° 7,110 60° 39

Ghaoa: (1879) na + . L 17°. 3 5,108 67° 38

54 MEXICO, CENTRAL AMERICA, WEST INDIES.

general aspect of the landscape. Nevertheless in spring their arid plains are
suddenly decked with many-coloured flowers, the mezquite shrub is covered
with a pale yellow blossom, clusters of white bells shoot up from amid the glossy
foliage of the yucca, the shingly tracts are enlivened by the bright red petals cf
the mamillaria. Thanks to its soft velvety turf, Europe may have more cheerful,
but assuredly not more brilliant, grassy meads.

But this “ flowery season ” is soon over, and nature presently resumes its dull
and sullen aspect, relieved here and there only by a few thickets of delicate green
thorny shrubs. The prevailing species are the mezquites (a/garrobia glandulosa),
for the most part very different from those found in the United States, but, like
them, still exuding a substance resembling gum-arabic. In New Mexico they are
mere bushes whose stems branch off directly from the root ; in south Texas they
develop into shrubs; but within Mexican territory, and especially in Sonora, they
assume the proportions of veritable trees, here and there grouped in large groves.

Elsewhere, notably on the slopes of the Western Sierra Madre, in the states
of Chihuahua, Sonora and Sinaloa, the oak is the prevailing species ; hence the term
encinal, or “oak lands,” applied in these regions to any extensive wooded tracts.
The term chaparral, which, strictly speaking, should be applied only to the deci-
duous oak, is in the same way given by the northern Mexicans to all spaces under
scrub or brushwood ; in ordinary language every grove or thicket is a chaparral,
even where the mezquites and large cactus are the dominant types.

Except along the river banks fringed by poplars and willows, the only woody
plants in certain northern regions of Mexico are the cactus. Of these the most
remarkable are the pitahayas, which assume the form of thorny fluted columns. The
branches stand out at right angles from the stem, and then grow parallel with it, thus
forming prodigious candelabra, some of which are 35 or 40 and even 60 feet high.

Other species are reckoned by the hundred which have adapted themselves to
the arid climate by developing an abundance of sap in their thick leaves, and
protecting themselves against animals by thorny armour. Amongst these fantastic
plants there are some which at a distance might be taken for blocks of greenish stone.

In certain places the ground is completely carpeted as by a kind of green
sward with dwarf agaves, which are still known by their old Aztec name, ixtle or
ixtli. The larger species of this useful plant, whose fibre is used for weaving
coarse textile fabrics, and whose sap serves for the preparation of brandy and other
national drinks, flourish especially in the inland states of San Luis Potosi,
Zacatecas, Durango, Aguascalientes, and even on the colder plateaux. In many
districts the general character of the scenery is determined by these agave planta-
tions, with their enormous thorny leaves, associated with hedges of other species,
such as the organos, so named from their resemblance to the pipes of an organ.

The three superimposed zones, ranging from the foot of the mountains to the
upland valleys of the plateaux, are characterised by special types, which impart
to the several floras their distinctive features. Thus on the coastlands of the hot
zone are seen extensive savannahs of dense herbage, magnificent palm groves and
all the trees of the Antilles noted for their fruits or flowers, their wood, bark or

FLORA OF MEXICO.

Or
Qt

essences. Higher up follow those glorious woodlands where the European and
tropical floras are everywhere intermingled; here flourish the coffee shrub, the
banana, the orange, and especially maize and beans, which supply the staple diet of
the inhabitants. Then comes the cold region, yielding wheat; a cereal, however,
which is here of far less economic value than maize.

On the plateaux the prevailing trees are the oak and pine, the former between
the altitudes of 5,000 and 8,500 feet, the latter rising from 8,000 to above 13,000 feet.
On most of the higher crests the conifers reach or even exceed the altitude of
13,500 feet. They are the last arborescent trees that grow on the flanks of the
mountains, the space between them and the lower limit of perpetual snow being

Fig. 26.—VxEGETABLE Zones In Mexico.

Scale 1 : 30,000,000. _

Op Ph
4 Us
/ LU
ET

Alpine Flora. Pinus ponderosa Prairie Flora. Sequoia. Cereus
and edulis. giganteus.
7 ee Uy ee
Algarrobia Pinus Quercus crassifolia Hæmatoxylon Deserts.
glandulosa. Aus:ralis. and reticulata. campechianum.
620 Miles.

exclusively occupied by short herbage and grasses. But owing to the overlapping
of the vegetable zones of different temperatures, the pines of the uplands have
almost everywhere encroached upon the temperate regions, and have even descended
below the line of 3,500 feet.

The dominant types of trees are represented by a great number of species, about
seventy-five varieties of the oak having been found on the slopes of Orizaba alone.
The ahuehuetes or “ cypresses ”’ of Chapultepec, Atlisco, Oaxaca, which belong to
the same species as those of Louisiana ({axodium distichum), grow to a colossal size ;
they are classed by Humboldt with the giants of the vegetable kingdom.

56 MEXICO, CENTRAL AMERICA, WEST INDIES.

Many of the numerous species of the Mexican flora have found a home in the
eastern hemisphere. From Mexico comes the chocolate plant, which has pre-
served its Aztec name; a species of arachis, the cacahuate, which also retains its
native designation in a modified form (#/acacahuatl) ; the pine-apple, the tomato
(tomatl of the Indians) ; the agave, and the various species of cactus, jalap, sarsa-
parilla and other medicinal plants, balsams, gums, and resins. Both the potato
and tobacco are also indigenous to Mexico.

The European gardens, orchards, and conservatories are being continually en-
riched by exotics from Mexico; the naturalist Poyet alone has introduced into
France as many as sixty species of fruit trees and ornamental plants from the
single province of Jalapa. On the other hand all foreign species may be acclima-
tised in the vast ‘“‘ botanical garden ” formed by the successive terraces which rise
from the seaboard at Vera Cruz or Mazatlan to the uplands of Guadalajara and
Zacatecas. The banana, whose name is of Sanskrit origin, and which has no
original designation in any American language, was probably introduced into the
New World through the Canaries and Haiti. Wheat was brought by a negro
slave belonging to Cortes, and Bernard Diaz tells us how he himself planted seven
or eight orange pips which grew to be fine plants, the “ first”? in Mexico. The
conquerors also planted the first vine in this fertile soil, where every industry
depending on the products of the vegetable kingdom might be practised.

At a comparatively recent epoch, that is, during tertiary and quaternary times,
the Mexican fauna comprised several species of large quadrupeds comparable in
size to those of the Old World. Bernard Diaz had already noticed certain “ giants’
bones,” which he attributed to the predecessors of the Aztecs, and to similar finds
are due such names as cerro, loma or Uano del gigante, now occurring in various parts
of the republic. These remains, which have from time immemorial been used in the
native pharmacopæia, and which appear to be really efficacious in several maladies,
are for the most part those of mastodons, rhinoceroses, elephants, deer, and horses.
Under the Tequisquiac hill, north of Mexico, a new species of gigantic armadillo
has been discovered, which has been named the g/yptodon clavipes.

The present Mexican fauna belongs, like its flora, to the North American zone, so
far as regards the plateau regions, and to the Antilles in respect of the coastland
round the Gulf, while that of the Pacific seaboard is intermediate between the
Californian and South American. In the general aspect of its terrestrial animals,
Mexico is connected more with the United States, whereas in its marine forms
the reverse movement has taken place. Thus the prevailing species in the Gulf of
Mexico as far as Tamaulipas and Texas, and the Pacific coast northwards to
Sonora and Lower California, have migrated from South America. The species in
the two oceanic basins differ almost completely, and despite the proximity of the
Pacific and Atlantic shores, their shells are quite distinct.

In the hot lowlands, where the atmosphere is most charged with vapours, are
concentrated the largest number of genera and species ; but this may be due to the
fact that here the populations are less dense, and the work of extermination conse-
quently less advanced than in the temperate regions. Three species of monkeys

FAUNA OF MEXICO. 57

dwellin the tropical forests, where the vampire hangs from the boughs of the
trees, and the humming-bird, the “solar beam ” of the old Mexicans, flits from
flower to flower. Every town has its organised bands of ‘scavenger ” vultures,
(cathartes atratws, zopilote or black vulture), while the king zopilote or white vul-
ture (sarcoramphus papa) holds sway in the rural districts; when the royal bird
swoops down on the carrion, the other species stand respectfully round, awaiting
their turn to share in the banquet.

In the thickets have their lair the powerful carnivora, puma, jaguar or tiger-
cat, as well as the tapir, largest of the Mexican ungulata. All the emydide-
terrapins or mud tortoises, are found in the shallow marine waters along the coasts,
while the lagoons, and especially the fluvial estuaries, are infested by the alligator ;
the seashore and forests of the coastlands are also the haunts of the gecko, basi-
lisk and iguana. <A large number of the snake family, poisonous or harmless, is
confined to the hot zone, which also swarms with batrachians ; here are found most
of the numerous characteristic species of toads and salamanders.

The waters of the estuaries and coast streams teem with fishes, all the numerous
varieties of which differ on the two oceanic slopes, but still present a certain analogy
in their general distribution. The marshy plains and dark forests of the hot lands
are also infested by clouds of mosquitoes. To escape from his tormentors the ox
plunges into the nearest quagmire, leaving muzzle alone exposed ; on this presently
alights the pretty little “commander” bird, which lives on mosquitoes, and thus the
unwieldy beast and dainty winged creature combine against the common enemy.

The temperate lands have also their special fauna, and certain species of snakes
and tortoises are found only in this zone; such is the boa-imperator which ranges
to an altitude of over 4,000 feet, and whose deified image formerly adorned the
temples of the Aztecs. Specially characteristic of the northern provinces which
form a prolongation of the American Far West, are the lizards met nowhere else
in Mexico. Within a recent period bisons were still seen on the uplands of Chi-
huahua, but this animal has disappeared altogether from the North Mexican
provinces.

On one occasion Froebel witnessed the passage of a herd of antelopes, num-
bering at least a thousand head, in the neighbourhood of Lake Encinillas in the
north-west of Chihuahua. The grey bear of Oregon, and the wild sheep, preyed
upon by three species of the coyote, by the puma and the jaguar, also penetrate
into North Mexico and Lower California, as do also the Virginian opossum and
the prairie marmot. The peccary dwells in the forests, and lays waste the neigh-
bouring plantations. This animal is much dreaded for the furious way a whole
herd will sometimes precipitate itself on the wayfarer.

But of all the Mexican fauna, two only have been domesticated: the huaholotl
(meleagris mexicana), which is a species of duck, and the turkey, introduced into
Europe by the Spaniards from the “ West Indies,” hence by the French called
“coq d'Inde.” The ¢echichi, an edible dumb dog, was soon exterminated when
taxed by the Spanish authorities. The other farmyard animals have all been intro-
duced into Mexico by the conquerors.

58 MEXICO, CENTRAL AMERICA, WEST INDIES.

Scorpions are one of the plagues on the plateaux, where the fields are also
ravaged by various species of acrita. The nights in the tropical zone are lit up at
night by the firefly (cocwyos), flitting and flashing in the air like coruscations.
The ant is represented by numerous species, one of the commonest of which are the
arrieros, or “ muleteers ” (æcodoma mexicana), who excavate their crater-like habi-
tations in the hardest rock.

One of the most interesting of the lower organisms observed by naturalists on
the Anahuac plateau is the curious axolotl, which has been the subject of pro-
found studies in connection with the theory of evolution. It abounds especially
in the saline and sodic waters of Lake Texcoco, and has rarely been met in other
parts of the New World. It is a species of amphibious lizard, furnished with
bronchial tufts or gills, but liable to such Protean changes that its classification
presented great difficulties to the first observers of this eccentric creature. They
gave it all sorts of scientific names, even that of Zusus aquarum, “ sport of the
waters,” and it was then constituted a separate genus under the title of siredon.

Nevertheless, many zoologists already pronounced it to be the larval form of a
large species of amblystome, and this view was at last proved to be correct by
Duméril, who gradually transformed the axolotl to an amblystome. Most of the
axolotls remain for several generations in the larval or tadpole state, and a few
only develop into the perfect animal. The Indians consider its flesh a great
luxury, and they also greedily devour the eggs deposited by two species of the
arayacatl fly (especially the corixa femorata) amongst the sedge of the Mexican
lakes. These eggs are pounded and mixed with other ingredients to form cakes, and
nests of other larvæ, clustered together like sponges, are also eaten. According to
Virlet d’Aoust the eggs of the axayacatl deposited on the bed of lakes, hardens to
a kind of oolitic limestone exactly similar to that of the oolites of the Jura, which
were probably formed in the same way.

The marine waters on both sides of Mexico abound in animal life. Amongst
the cetaceans that visit its shores are some manatees. Hundreds of new species of
molluscs have been discovered on the Pacific side, amongst others the aptisia
depilans, which would appear to be the same as that from which the Tyrians
extracted their purple dye. The Indians of Tehuantepec use it for dyeing their
fibres, without requiring a mordant to fix the colour.

In the Gulf of California, and especially near Paz and the neighbouring archi-.
pelagoes, extensive beds of pearl oysters are fished. Some other islands in the same
gulf are frequented by myriads of various species of aquatic birds, and have already
yielded many hundred cargoes of guano.

It is noteworthy that the Pacific islands lying at some distance from the coast
have all a fauna different from that of the mainland. Thus the little Tres-Marias
group, about 60 miles off the coast of Jalisco, has a special species of humming-
bird. The Revilla-Gigedo archipelago also forms a separate zoological zone, and
the island of Guadalupe, 155 miles distant from Lower California, has eleven
species of land birds, every one of which differs from the corresponding species on
the adjacent continent.

INHABITANTS OF MEXICO. 59

INHABITANTS OF Mexico.

The hypotheses that have been advanced regarding the origin of the various
populations found by the Spaniards in Mexico at the time of the conquest are
almost as numerous as the works written on the ethnology of this region.
Naturally, the early writers, being obliged to harmonise their fancies with the
Biblical texts, had to trace the Mexicans back to one of Noah’s sons, arriving either
by sea with the waters of the Deluge or by land after the subsidence of the flood.

Even during the present century certain authors have endeavoured to show
that these natives are descended from the Jews “dispersed over the earth ” after
the Babylonian captivity. According to them, the kinship is attested by the
physical appearance, the national character, the religious manners, customs, myths,
traditions, even the véry language of the Mexican nation. Other writers sought
in classical antiquity, amongst the Egyptians, Phoenicians, or Carthaginians, for
some indications of a former immigration into the New World, and Plato’s
Atlantis could not be overlooked in the conjectural history of the old Mexican
races. “The Atonatiuh, that is to say, the Atlantides,” says Alfredo Chavero,
“are the mother people of the civilised nations of Europe and America; the
Spaniards and the Toltecs alike descend from them.” Brasseur de Bourbourg even
fancied he had made out from the Nahuatl manuscript known as the Codex Chimal-
popoca that an ‘eruption of volcanoes stretching over the whole extent of the
American continent, which was at that time double its present size, blew up the
globe, and between two risings of the morning star engulfed the richest regions of
the earth.” Fortunately, the Atlantides of the present Mexico escaped the
disaster, and survived to record it on those monuments of American literature
and architecture which no savant had hitherto been able to interpret.

But putting aside these vagaries, the most accepted hypothesis, expounded under
various forms by Guignes, Humboldt, Prescott, Quatrefages, and Hamy, regards
the Mexicans as immigrants from Asia, arriving either by Bering Strait or the
Aleutian Islands, or else directly across the ocean, or from group to group of the
Polynesian Islands. The relative proximity of the two continents of Asia and
North America, and the undoubted fact that Japanese junks had actually been
cast ashore on the Californian seaboard during the historic period, could not fail
to suggest such views, and commend them to the serious consideration of many
superficial enquirers. There is, however, no authentic proof that the mysterious
region where grows the fusang, and which was supposed to have been discovered
by a Chinese expedition at the beginning of the seventh century, is really Mexico
or Central America; nor does the description of the country given by the old
Chinese writer agree very well with that of the Anahuac plateau, still less with
the habits and customs of the natives as described by the Spanish conquerors.

The religion of the Aztecs differs also too profoundly from Buddhism or any
other east Asiatic system to recognise in it the teachings of any Chinese mission-
aries. On the other hand the fancied coincidences of symbolical signs and figures
are far too vague to establish anything more than the faintest presumption in

60 MEXICO, CENTRAL AMERICA, WEST INDIES.

favour of former relations between peoples separated from each other by the broad
waters of the Pacific. The communications that may have taken place at various
epochs, and even the resemblances noticed between the Mexicans and Chinese,
can in no way justify the assumption of the common origin of the two races, or
even of their cultures. As far as history and tradition go back, the Mexican
lands have always been inhabited ; whether aborigines or not, these populations
would have been spoken of by the Greeks as “ autochthones,” or indigenous.

Asin other places, such as the neighbourhood of Puy, in the south of France,
geologists have also discovered the fossil remains of a quaternary man on the
Anahuac plateau, near the city of Mexico. These interesting remains, dating
from an epoch long anterior to Aztec civilisation, were brought to light in 1884
at the foot of the Penon de los Baños in the saline plains formerly flooded by the
waters of Lake Texcoco to the east of the capital. The bones were found
in the vegetable humus under a layer of lava in association with some kitchen
refuse.

The osteological characters of this fossil Mexican man are the same as those of
the pure indigenous race of Anahuac, in which the canine teeth scarcely differ
from the incisors. The man of Peñon was contemporaneous with the elephant,
deer and horse which inhabited the same region at a time when the level of the
waters in the Texcoco lagoon was 10 feet higher than at present, and when vol-
canic eruptions anterior to history had not yet taken place.

Elsewhere, flints or cherts, evidently worked by the hand of man, have been
found amongst deposits also containing the teeth and other remains of the Ameri-
can elephant (e/ephas Colombi). These primitive races must consequently have
flourished many thousand years before the present time.

At atime when Rome was hastening to its fall, and the barbaric peoples of
North Europe were overrunning the empire, the Anahuac tableland in Central
America was.already the seat of an advanced civilisation. Doubtless, it is far
from easy to classify peoples as barbarous or civilised according to their various
degrees of culture; but the latter term, which has so often a purely conventional
meaning, may justly be applied to the Aztecs, or Mexicans, as well as to the
Mayas of Yucatan, the Chibchas (Muiscas), Quichuas, and Aymaras of South
America. It might even be extended to the Pueblo Indians, and perhaps to other
native communities in North America.

Amongst the less advanced nations, whom they, nevertheless, resembled in
their political and social evolution, the Mexicans were distinguished by their
national cohesion, by their highly developed economic system, their arts and
sciences, as well as the knowledge of numerous technical processes enabling them
to facilitate labour. Like the early civilisations of the Old World, such as
those of Egypt, Chaldæa, India, and China, that of Mexico took its rise at some
distance from the ocean on the uplands encircled by lofty border ranges or steep
escarpments. It had neither a Nile nor a Euphrates, by which the riverain
populations could be merged in a compact nation; but it had its lakes, far more
extensive than at present, whose shifting levels, periodical floods and subsidences

INHABITANTS OF MEXICO. 61

imposed on the inhabitants the necessity of co operation, of mutual aid and soli-
darity, in which lie the germs of all progress.

Nevertheless, compared with the early historic civilisations of the eastern
hemisphere, that of Mexico had the disadvantage of remaining, if not completely
isolated, at least almost entirely encircled by barbaric communities. It lacked the
proximity of other centres of progressive life, with which to exchange those recip-
rocal influences whence might spring another and a higher culture. Despite the
vertical disposition of the climates, rendering the hot lands highly dangerous for
the inhabitants of the plateaux, the Aztecs had doubtless established distant rela-
tions with the Mayas and the various groups of Nahuas dispersed over Central
America ; but elsewhere they were cut off from contact with all cultured peoples,
until their seclusion was suddenly and violently invaded by the Spanish conquerors.
Henceforth, civilisations and races became forcibly intermingled.

So rapid was the work of destruction which followed the first arrival of the
Spaniards that antiquarians might well have feared the complete disappearance
of all documents relating to the ancient history of Mexico. Such records were
often deliberately destroyed, as by Archbishop Zumarraga at Tlatelulco, Nuñez
de la Vega at Chiapa, and others who, aping the zeal of Paul at Ephesus,
burnt, as suspected of necromancy, all the Mexican works they could discover.
Later they were satisfied with concealing the precious manuscripts, which they
kept locked up in their libraries, neither able nor willing to make any use of
them.

Fortunately the ancient lore had been kept alive in a few noble families allied
by marriage with the Spanish conquerors. The aid of these men could thus be
secured in the later attempts made to restore the annals of Anahuac. Many
natives contributed in this way to rescue from oblivion the early records of
the Aztecs and the allied peoples. In the year 1548 Tadeo de Nica, an Indian of
Tlaxcala, at the request of the viceroy, composed a history of the conquest, which
was attested by the signatures of thirty Tlaxcaltec nobles.

Gabriel d’Ayala, of Texcoco, wrote in the Aztec language a history of Mexico
from the year 1243 to 1562. Contributions to the history of her native land,
now unfortunately lost, were even made by a Mexican lady, Maria Bartola,
Princess of Ixtapalapa. Several pure or half-blood natives, such as Tezozomoc,
Chimalpahin and Camargo, have also left important historic manuscripts; lastly
the family of the Ixtlilxochitls, descended from the old kings of Mexico and
Teotihuacan, had several representatives amongst the national historians, and one
of them, Fernando de Alva Cortes, had even the courage to exalt his ancestry and
denounce the “ frightful cruelties ” of the conquerors of Mexico.

But even amongst the Spanish missionaries men were found who recognised
something more in Mexican history than the artifices of the devil, and who went
to the trouble to procure explanations of the pictorial records, and collect the
ancient traditions of the people. Such were Bartolomé de las Casas, Sahagun and
Torquemada. The historians of the present century have also been able to throw
further ight on the pre-Columbian history of the Mexicans, thanks to the

62 MEXICO, CENTRAL AMERICA, WEST INDIES.

discovery of new manuscripts, the partial interpretation of the hieroglyphics, and
a more careful study of the early writers.

Aided by these resources the student may now roughly trace the sequence of
events for at least a thousand years before the conquest, and dimly contemplate
the first glimmerings of national life amongst the Mexican populations. At this
epoch the land was already occupied by most of the half-civilised Indian nations,
such as the Otomi, Chichimecs, Huaxtecs, Totonacs, Mixtecs and Zapotecs, by
whom it is still inhabited, and according to the national tradition, it was in their
midst that the Nahuas, that is, the “ Clear-spoken People,” made their appearance
in the twofold capacity of conquerors and civilisers.

These intruders, coming from the “Seven Caves” of the north, divided into
seven tribes, each with seven sub-divisions, and advancing southwards in seven
successive expeditions, had to vanquish a race of giants before securing possession
of the “Terrestrial Paradise.” Then the demi-god, Quetzalcoatl, a mythical
legislator, coming up from the sea, appeared amongst them, and after instructing
them in the arts, sciences and social institutions, suddenly disappeared with a
promise some day to return. This was the long-awaited Messiah, and when
Cortes emerged, as it were from the bosom of the deep, and presented himself
at the head of his followers, the prophecy was supposed to be at last fulfilled, and
the people looked forward to the dawn of a new millennium.

The sixth century of the new era is usually regarded as about the time when a
group of Nahuas arrived in Anahuac, after a long series of wanderings from
Huehue-Tlapallan, a city or region which the commentators have hitherto failed
to identify. Some place it in the north, others to the south, of Mexico. Never-
theless, most of the indications point to the northern regions as the cradle of the
Nahua race; the very form of the Mexican tableland, broadening out northwards,
and contracting southwards to a labyrinth of separate districts, shows the direction
in which the migrations must have taken place. The whole group of these con-
quering Nahua tribes is represented in the legends as issuing from the “ White
Dove of Cloudland,” a personification of the northern regions.

Towards the close of the seventh century, the Nahuas, commonly designated
under the name of Toltecs, are already found grouped round a city constituting
the centre of their power. Modern archeologists have rediscovered this city in
the ruins of Tollan, now known by the name of Tula, which lies fifty miles, by
railway, north-west of Mexico.

These early Nahua invaders were themselves replaced by others of the same
race, vanquishers of the Quinames, or “Giants.” The Olmecs and Xicalanes, as
they were called, are represented as coming from the east, where they had doubt-
less already constructed several of those monuments which were later attributed
to succeeding tribes of different speech. In any case there can be no doubt that
the so-called Toltec epoch was’ one of the richest in works which still attest the
culture of these early Nahua peoples. The very word foltecat/, whatever its
original meaning, had become synonymous with a craftsman of skill and taste, an
“artist,” as we should say. The same term was also applied to those traders

) INHABITANTS OF MEXICO. 63

who made long journeys to distant lands, and who were the “ torchbearers ” of
Nahua civilisation in Central America.

Altogether it would seem probable that “Toltec” was not the name of any
particular people, and that the “artists”? were simply Nahuas like their Aztec
successors. The term Colhua, or “ancestors,” which is also applied to them, is
also an indication of their common ethnical unity.

The Tula domination lasted till the second half of the eleventh century, when
the strength of the powerful Nahua tribes was for the first time broken by
intestine strife, foreign wars, and the invasion of the Chichimecs, or Barbarians,

Fig. 27.—ExTENT oF THE AZTEC CONQUESTS.
Scale 1 : 13,000,000.

QU
[LI Oe S
NS

no
(=)

West of Greenwich

YW
Aztec Conquests.
186 Miles.

accompanied by famine and pestilence. The chronicles speak of millions perishing
amid all these disorders, and, for whatever reason, after this date no further
mention is made of the “Toltecs,” or else they are represented as fugitives
dispersed amongst the surrounding populations, or else going southwards to found
new states in Yucatan, Chiapas, or Guatemala.

Numerous migrations are also related of the Chichimecs, who displaced the
centre of Nahua power southwards to the Anahuac plateau properly so called,
first to the shores of Lake Xaltocan, then to the plains around Lake Texcoco not
far from the present confederate capital. Lastly, the royal residence was estab-

64 MEXICO, CENTRAL AMERICA, WEST INDIES.

lished at Texcoco or Acolhuacan, the “ Ancestral City ” ; but in 1325 the rival
city of Mexico-Tenochtitlan rose on an island amid the waters of the lake.

The Aztec founders of this place were themselves of the same Nahua race as
their Toltec and Chichimec predecessors. They had reached the Anahuac plateau
towards the close of the twelfth century, having a hundred and twenty-five years
previously quitted their insular home of Aztlan, which has not yet been identified
with certainty by geographers. During those years of wanderings they had dwelt
in the mythical land of Chicomoztoc, that is, the “Seven Caves,” and traversed
many strange regions in search of the ‘‘ Land of Promise.” The legend also speaks
of them as the “inventors of fire,” that is, as an ingenious people, rivalling the
Toltecs in their knowledge of the arts and sciences.

Thanks to its insular position, easily defended against all sudden attack, the
lacustrine city grew rapidly, and round it were formed the famous chinampas, or
floating gardens, which supplied the people with provisions during times of siege.
Even after it was divided into two hostile towns, the old and democratic Tenochtit-
lan and the modern trading town of T'latelulco, it continued to develop rapidly,thanks
to the inflow of immigrants from all parts, seeking refuge in these strongholds.

When the Chichimec ascendency was finally destroyed, in 1431, by intestine
wars and the revolt of the oppressed populations, Mexico succeeded to the power
hitherto exercised by Texcoco. It stood at the head of the confederacy formed by
the three cities of Mexico, Texcoco, and Tlacopan.

Under the hegemony of the Aztec capital their conquests soon spread ee

the limits of Anahuac proper. The annals of this period, which agree on all the
essential points, despite the partial accounts of writers of different nationalities,
describe the Mexicans as reducing the surrounding populations for the twofold
purpose of increasing their store of gold, precious stones, and ornamental feather-
work, and procuring victims for the altars of their gods. Westwards they failed
to subdue the tribes of Michoacan, and towards the north-west they scarcely
advanced beyond the limits of the Anahuac valley. But in the direction of the
south and south-east they had conquered the whole region as far as the coast, from
the mouth of the Panuco to the Alvarado bar. But on the plateau they left the
independent nation of the Tlaxcalans, who, with hundreds of revolted tribes, greatly
facilitated the overthrow of the Mexican empire by the Spanish invaders.

Prodigies and scourges of all kinds, say the chronicles, foreboded the approaching
ruin of the Aztec power, which had already been seriously threatened by the insur-
rection of its own subjects, when Cortes and his Tlaxcalan allies presented them-
selves before the doomed capital. Nevertheless the name of this opulent city has
been extended not only to all the surrounding territory, but also to an aggregate
of provinces or states far more extensive than the empire of Montezuma. The
term “Mexican,” formerly restricted to a fraction of the Aztecs, themselves
merely one of the numerous branches of the Nahua race, is now claimed by a great
nation of about twelve million souls.

The Spanish conquerors could not fail to recognise in Mexico an empire like
that of their native land, where the will of a potent ruler was implicitly obeyed’

MEXICAN CULTURE. 65

throughout his wide dominions, where he nominated the provincial governors,
imposed tribute and levied troops. They fancied that here also all authority
emanated from the imperial power which was regularly maintained in the same
dynasty by a sort of right divine. They were unable to understand that the
Aztecs, after having lived in family communities without any private ownership
of the soil, had established a military democracy formed of kindred groups who
selected their own “speakers,” that is, chiefs.

Surprised, on the other hand, to find in the New World a great city, larger and
wealthier than their own capitals, the conquerors naturally exaggerated the
resources of Mexico and the culture of its inhabitants. Nevertheless certain docu-
ments relating to the native language, the sciences and the art of transmitting
thought, the care also bestowed on agriculture and irrigation, lastly, the objects
preserved in our museums, and the monuments still standing in the neighbourhood
of the cities or buried under dense forest growths, make it evident that Mexican
civilisation had raised itself far above the level of barbaric populations.

The Aztec language, which was probably identified with that of the Toltecs
and Chichimecs, and certain dialects of which were and still are spoken far to the
south in Guatemala, Salvador, and Nicaragua, was by far the most prevalent idiom
in Mexican territory. It was current throughout the greater part of the Anahuac
plateau, on the’ Gulf of Mexico as far as the Coatzacoalcos delta, and on the
Pacific coastlands from the Gulf of California to that of Tehuantepec. It is still
in use, side by side with Spanish, in all these regions, although the modern dia-
lects scarcely retain a third of the stock of words in the literary standard. As
the exclusive medium of civilised intercourse Aztec had become the language of
diplomacy and trade; as each province was conquered, the speech of the ruling
people assumed an official character, and the inhabitants were compelled to learn it.

Aztec belongs to the polysynthetic order of speech, and of this class it is a
typical specimen ; the words of the sentence are fused together by modification to
an extraordinary extent, and in accordance with many subtle laws of euphony.
The language is wonderfully plastic, and those writers who have studied it
thoroughly vie with each other in vaunting its varied qualities of grace, subtlety
and wealth of descriptive terms; in his work on natural history Hernandez
enumerates two hundred species of native birds and twelve hundred of plants, all
of which have distinct names in Aztec. It also abounds in abstract terms to such
an extent that translators have had no difficulty in finding Mexican expressions
for such metaphysical or religious words as occur in the New Testament, the
Imitation of Christ, and other works of a like character. Its finest literary monu-
ments are of an ethical order, moral exhortations breathing a lofty sentiment
unsurpassed even in Hindu classical literature.

A remarkable indication of the high degree of civilisation attained by the
Mexicans is afforded by their knowledge of astronomic phenomena. They were
able to describe the movements of the sun, moon, and some planets, and the exact
duration of the solar year; the return of each “ new plant,” as they expressed it,

was more accurately known to them than it is even now in official Russia, where
38

66 MEXICO, CENTRAL AMERICA, WEST INDIES.

the present calendar is twelve days behind time. Like that of their Zapotec and
Michoacan neighbours, their year was divided into eighteen months of twenty
days, to which were added five supplementary days, often regarded as of bad
omen. But in order more completely to harmonize the conventional with the
astronomic year, after every cycle of fifty-two years a period either of twelve or
thirteen days was intercalated according to the necessities of the calculations.

The numeral system was vigesimal, that is, four times five, the days being also
grouped in fives, the fifth answering to our seventh, and possessing a certain
importance as set apart for feasts and markets. But the years were differently
divided, each tlalpilli, “knot” or “ bundle,” consisting of thirteen, and four of
these, that is, a series of fifty-two years, constituting the æiwkmolpilli, or cycle.
In the eyes of the Mexicans this formed the chief period of time, and with it
were accordingly associated certain mystic ideas on the government of their daily
life and of society. To them the normal duration of human existence seemed to
coincide with the xiuhmolpilli, and from the few men to whom the gods granted
the privilege of living through two of these periods, the double cycle took the
name of huehuetilitstli, or “old age.” According to a law—which, however, was
not always enforced—the Toltec chiefs should rule for exactly a cycle, and when a
chief died before completing the period, a council of elders assumed the government
in hisname. On the other hand those who exceeded the term had to abdicate,
and their successors began their reign from the hour indicated in the calendar.

As amongst the peoples of the Old World, the solar had been preceded by a
lunar year ; hence it was that the revolutions of the moon continued to regulate
the religious calendar of feasts and observances, which are always more faithful
to established usage. In the same way, in the various European religions the
great feast of Easter, which had originally been the feast of the spring-tide,
that is, of renewed nature, is still determined by the revolutions of the moon.

Although the Mexicans had not invented a writing system in the strict sense
of the term, they were still able to perpetuate their records, to draw maps by
“painting in a natural way all the rivers and harbours,” to establish their
genealogies, to publish their laws and edicts, to describe the industrial arts, the
occupations of the household, lastly, to transmit even abstract thought, by means
of hieroglyphical figures. Usually these figures, of square form with rounded
angles, were painted in vivid colours on a kind of paper made from the fibres of
the maguey and anacahuite, the “ paper tree” (cordia boissieri), or else on skins or
strips of cotton covered with varnish and bound together like a fan, forming an
amatl, or book with wood boards for covers. The public buildings, and here and
there the face of the rocks, especially in the Western Sierra Madre, were also embel-
lished with hieroglyphics inscribed on the stone.

A careful study of these documents shows that in the employment of such
characters the Mexicans had advanced beyond the purely figurative and symbolic
sense, in many combinations already using them as phonetic signs, so as to form a
kind of rebus; in this way were written, for instance, the names of cities. From
the earliest historic times the Toltecs possessed extensive libraries of these painted

MEXICAN CULTURE. 67

manuscripts, which, however, the Aztecs are said to have destroyed through
jealousy of their predecessors’ fame, In their turn the Aztecs were themselves
the victims of the iconoclastic zeal of their conquerors, who burnt nearly all the
older documents. Most of the extant manuscripts date only from the end of the
sixteenth century, a period when the Church, already reconciled with what
remained of Nahua civilisation, permitted the faithful again to practise the
traditional hieroglyphic system. But the manuscripts of this epoch consist mostly
of religious confessions, catechisms, land surveys, and judicial endorsements.

The industrial arts were highly developed, although the Nahuas had not
reached the age of iron, the only metals known to them being gold, silver, copper,
tin, and lead. Very thin plates of copper were used as currency, as were also
cacao berries and a multitude of other objects, differing in every province.
Cutting implements were made of an alloy of copper and tin nearly as hard as
steel. Nevertheless, nearly all their weapons were still made of hard stone, and
especially from chippings of if, or obsidian. Knives of this substance were also
employed by the priests for immolating human victims.

The agricultural implement which most resembled the European plough
consisted of a wooden apparatus to which were attached hard-wood sticks tipped
with copper. The Spaniards were amazed at the skill of the native lapidaries and
jewellers, who excelled especially in carving small animals and insects. According
to contemporary chronicles, the European goldsmiths could not pretend to rival
the artificers of the New World in perfection of workmanship. One process has
certainly been lost, that of making little hollow figures of thin gold without any
soldering. These objects, of which even the museums contain but few examples,
seem quite inexplicable to the European craftsmen.

Mexico had also its potters, millers, and paper-makers. The various plants of
the cactus family, the palms and cotton trees, yielded their fibres for weaving
textile fabrics, some of which were extremely delicate. In the art of dyeing the
natives were also past masters, employing cochineal, besides a large number of
herbs, barks, and fruits, the knowledge of which has been lost since the Spanish
conquest; in this respect Mexican art has deteriorated during the last three
centuries. One of its triumphs was the application of feathers to the adornment
of textiles, garments, tapestries, and coverlets. This feather work, which has
been preserved in a degraded state by numerous families of artists, was regarded
as one of the liberal arts. The “ council of music,” a sort of academy founded
to encourage art, comprised the workers in feathers amongst its members.

Architecture also flourished amongst the Nahuas, whose low, solid houses, for
the most part only one-storeyed, rested either on a platform or on piles. The towns
were regularly planned with narrow streets running at right angles and large
spaces round the temples ; they were abundantly supplied with water by means of
aqueducts and reservoirs, and had also their quays and embankments, while the
rivers were crossed by suspension bridges made of lianas, and the rivulets by stone
causeways. Some of the cities were fortified, and the great wall, six miles long,
which closed the highway, leading through a defile, to the republic of Tlaxcala,

68 MEXICO, CENTRAL AMERICA, WEST INDIES.

was pierced by an ingeniously constructed gateway terminating in a parapet,
behind which its defenders could keep under cover.

But the chief architectural works of the Nahuas were the temples and
pyramids, such as those of Teotihuacan and Cholula ; these with the strongholds are
the only structures which in certain places have survived to our times, though
careful exploration has revealed a few traces of the private dwellings formerly
occupied by the Mexicans. The religious monuments were constructed on a plan
analogous to that of the Babylonian temples, being like them step pyramids
formed by a series of rectangular parallelopipeds, superimposed and receding
upwards; but as a rule the American were proportionately much broader at the
base than the Asiatic structures. Some were of prodigious size, a proof that
human labour was little valued on the Anahuac plateaux.

At the time of the Spanish conquest the native civilisation was already on the
wane, a fact recognised by the people themselves when speaking of the Toltec age
as the flourishing epoch of the arts, sciences, and industries. Hemmed in on all
sides, without any regular communications seawards, and relieved from the
necessity of foreign trade by the great variety of products: yielded by its three
superimposed climatic zones, the Aztec world had been reduced to live on its own
resources ; there was no inflow of commodities, no interchange of thought to
renew the vital forces; the social system gradually became foul and stagnant, like
the floodwaters that lodge in the depressions of a level plain.

Trade was doubtless held in high honour, so much so that caravans could
traverse the lend without danger even in time of war; but the traffic was always
confined to the beaten tracks affording communication between the plateau and
the lower zones on both slopes. Thus shut out from free intercourse with distant
countries, Mexican civilisation was unable to find the elements of renewed life
within itself, with the result that the people gradually lost all spirit of enterprise,
enslaved by traditional and increasingly oppressive formularies. A rigid etiquette
regulated all relations between the classes, and society became, so to say, petrified,
while public worship grew more and more atrocious.

Yet at its origin the Mexican religion had been exempt from all sanguinary
rites. The first of the gods, bearing the name of Teotl, in a pre-eminent sense
was Atonatiuh, the “ Sun of the Waters,” whose rays, heating the seas, caused all
things to rise out of chaos. Tlaloc, issue of the sun, yearly reviver of the spring-
tide, is the trade-wind bearer of the fertilising rains, the bird that comes from the
sea, the snake that glitters in the lightning flash, and glides into the fissures of
the earth, emblem of the running waters.

At the time when the Aztecs founded Tenochtitlan, the memory was still
preserved of a mild religion, at which suppliants offered to ‘“ Father Sun,” to
“ Mother Moon,” to “ Brother Earth, ’ and to the wind-god nothing but seeds and
fruits, to obtain a blessing on the future crops. Hopes were even cherished that,
in a coming age of gold, these placid rites might yet be restored; at least they
were associated with the advent of another Tlaloc, Quetzacoatl, the “ Plumed
Serpent,” who comes from the east with the east wind and thither returns.

MEXICAN CULTURE. 69

Many of the vanquished nations, such as that of the Totonacs, groaned under
the burden of having to supply human victims to the Mexican gods, while their
own divinity, ‘ Mother of Men,” demanded only seeds and flowers. Even in the
Aztec temple of Texcoco, raised by Nezahualcoyotl to the “unknown god,” public
worship was confined to the burning of incense at the altar of the deity. But
elsewhere wars, and the practice of adding captives to the other offerings, had

Fig. 28.—ArtiriciaL PYRAMID or CHOLULA.

gradually imposed a religion of blood on the whole Nahua nation. Not the
symbol of life, represented by the first-fruits of the earth, but life itself has now to
be incessantly offered on the altars of the gods. Even when corn was presented
it had first to be reduced to a paste, kneaded with the blood of children and
maidens ; a dough was also prepared from the ashes of the fathers mingled with
the flesh of their offspring.

To appease the wrath of the wicked gods, to avert the evil machinations of the

70 MEXICO, CENTRAL AMERICA, WEST INDIES.

unseen world, the Mexicans had recourse to sacrifices, in this differing in no way
from Aryans, Semites, Negroes, and all other races. But their sanguinary rites
probably surpassed in horror those even of Dahomey itself. Even the most timid
practised self-torture like the fakirs of the East and the Aïssawas of Algeria ;
they scarified their flesh with the cruel maguey thorn; they prolonged their
fastings for days together ; they abstained from sleep till the mind wandered.

The Benedictine friar, Camillo de Monserrate, explained the dento-liquid sounds
tl, etl, which seem so strange to most European ears, by the Mexican habit of
piercing the tongue with large cactus thorns during their fits of religious frenzy ;
thus he supposed might have been produced a sort of stammering which became
hereditary in the course of ages.

But it was mainly by proxy that they sought to conjure the caprice of the
gods; the stain of sin was vicariously cleansed by immolating alien victims. In
the Old World, which abounds in animals of all kinds, their blood was usually
regarded as sufficiently efficacious. But on the Mexican plateaux there was little
except men to torture and mangle in honour of the jealous deities. Human hearts
were torn from the still-warm breast by the gory hands of priests, and held up
towards the invisible spirits. To Tlaloc were immolated sucklings or children
killed with fright, and their flesh was then consumed by the nobles at a religious
banquet. The necropolis of Tenenepanco, discovered by Charnay, at an altitude of
over 13,000 feet, on the northern slopes of Popocatepetl, contained nothing but the
remains of hundreds of children, probably the victims offered to Tlaloc, god of the
lofty heights, whence descend the winds and the clouds.

At the great ceremonies, blood was shed in torrents to flood the trenches dug
round the feocalli, that is, the temples, literally “ God’s house.” Towards the
close of the fifteenth century, at the consecration of the great temple of Mexico to
Huitziloputzli, the war-god, which had been begun by his predecessor Tizoc, King
Ahuizotl immolated nearly eighty thousand captives. - But despite the ‘statement
of the chronicles, this tremendous butchery must have been made, not on one
occasion, but at numerous successive ceremonies, as has been shown by Charnay.

Each sovereign, on ascending the throne, had to begin his reign by a vast
man-hunting expedition, in order to provide food for all the sacred shambles ;
each of the a ee months of the year had to be blessed by a massacre. Accord-
ingly “holy wars” had been formerly established by treaty between. the various
states in order to secure sufficient victims for the altars.

Every temple washed its foundations in the blood of captives mingled with
offerings of the precious metals, of pearls and the seeds of all useful plants. These
temples, stained with black gore, full of human flesh, fresh, charred or decomposed,
presented a ghastly spectacle; some were entered through a door in the form of a
throat, in which thousands of skulls lined the jaws of the monster. Close by rose
pyramids, ‘each containing over a hundred thousand skulls.”

One of the yearly feasts was that of the “ flaying,” when the priests traversed the
various quarters of the city clad in the dripping skins of the victims. But the
very multitude of the offerings rendered the gods insatiable, and their wretched

MEXICAN CULTURE. 71

devotees sought for still nobler subjects to propitiate them. In the Christian
religion, a Son of God, God Himself, expiated the sins of the elect on the cross;
but those who crucified Him were at least unconscious of His divinity. The
Mexicans, on the contrary, created gods to immolate them to still more powerful
deities. During the great national ceremonies, a scion of the royal house would
not have satisfied them ; they required a son of God, and the young men whom
they offered up were raised by them to the divine rank. Before slaying these
gods incarnate, the priests followed in the triumphal procession, falling down in
worship before them. Then, after the sacrifice, those who tasted of the sacred
flesh, and who “ate god,” as indicated by the very name of the feast, assimilated
the divine substance, and thought they thus became participators in the nature of
the gods. Such was the hideous form that “ god-eating” had assumed in Mexico.

Such religious practices were naturally completed by a ferocious legislation,

Fig 29.—Sacrep STONE or Tizoc, IN THE Museum or Mexico.

yet the people seem to have been of an extremely kind disposition, mild and
affectionate. ‘My dear son, my jewel, my fair feather!” thus spoke the
mother to her child. According to Ixtlixochitl, a theft exceeding in value seven
maize cobs was punished with death. For whole communities, a violent seemed
far more probable than a natural ending; this alone would sufficiently explain the
sense of sadness that had fallen on this unhappy nation, from which the divine
favour seemed to be withdrawn in inverse ratio to the number of their victims.
The emperor Nezahualcoyotl, sovereign of Texcoco, the crowned poet, who
staked his throne on a throw of dice, to show how little he cared for power, this
emperor expressed the universal sentiment when he depicted ‘the approaching
day when the gloomy fate, the great destroyer will be revealed.” Even the
Spanish conquest, with the massacres and other scourges which accompanied it,
and the servitude by which it was followed, was a relief for the nations of Anahuac ;

72 MEXICO, CENTRAL AMERICA. WEST INDIES.

it rescued them from a hopeless fatalism; it introduced them, though doubtless
through a thorny path, into the new world of common human interests.

This era of transformation began in a terrible way for the populations of
Anahuac. The Spanish conquerors acted in Mexico as they had acted in the
Antilles ; they massacred the natives that resisted, and reduced the survivors to a
state of merciless slavery. ‘A long experience,” said Peter Martyr Anghiera,
“has shown the necessity of depriving these men of freedom and giving them
guides and protectors.” Thanks to these “ protectors,’ whole provinces were
nearly depopulated in a single generation. The siege of Mexico, “where men
were numerous as the stars of heaven and the sands of the seashore,” is said to
have cost the lives of 150,000 persons; and according to Pimentel, the native
population of Nueva Galicia, which has become the present state of Jalisco, was
rapidly reduced from 450,000 to 12,600.

In the swift work of conquest and enslavement, the Spaniards were aided by
the very apathy of the wretched inhabitants themselves. The conquered multi-
tudes, whom their former masters had crushed beneath an intolerable burden of
oppressive laws and statute labour, seemed indifferent to a change of tyrants.
They even found it easier to bend the neck to the yoke of the cou gods armed
with thunder, than to rulers of their own race.

The change, or at least apparent change of religion which went on, so to say,
simultaneously with the conquest, was also effected without difficulty. When
the Franciscan Friars, soon followed by the Dominicans and Augustinians, offered
to the Mexican populations the baptism that cleanseth from sin, a rite which
in any case scarcely differed from the analogous purifications of the Aztec religion,
the surprising success of their propaganda is not to be exclusively attributed to
their prestige as conquerors, or to the support which they received from the secular
arm. Allowance should doubtless also be made for the happiness of being at last
released from the terrorism that the native religions had imposed on the people.

Toribio de Benavente relates that nine million Indians were baptised during
the fifteen first years that followed the conquest. The priests found themselves
surrounded by hundreds of kneeling suppliants, and such was the eagerness of the
candidates “ suffering from the thirst of baptism,” that the officiating clergy lacked
the time to perform the prescribed ceremonies, and satisfied themselves with
moistening the brow of the neophytes with a little saliva. The names of saints
supplied by the calendar no longer sufficing, the Indians were grouped in batches
each of which received collectively the same name.

Apart from the sanguinary rites the two religions differed so little in their
outward forms that the natives felt little difficulty in conforming to both. When
called upon to overthrow their idols, and replace them, in the same temples and on
the same sites, with the statue of the Madonna and her Child, the caciques had
merely to set up the image of Tecleciguata, the “ Great Lady,” and the change
was effected. But no crucifix was erected, says the Dominican monk, Remesal,
‘because the Spaniards, claiming immortality for themselves, were reluctant to
teach the neophytes that their God could die.”

RESULTS OF THE CONQUEST. 73

Multitudes accepted baptism without any intention of abandoning their old
rites, and continued long to celebrate the pagan mysteries in the depths of the
forests. Thus a chapel was built and a cross set up immediately above the spot
where had been hidden the proscribed image of an idol. When bowing before
the cross it was to the god that they addressed their invocations.

But by force of habit the two cults became gradually merged in one ; at present
when any of the old idols happen to be disinterred, it is in perfect good faith that
the natives call them santos antiguos, ‘old saints.” The same pious souls that
crowd the Christian churches and devoutly kiss the relics of the martyrs, secretly
assemble in the woods to crown the images of the former deities with garlands.

But the conversions, in virtue of which they could claim to be the spiritual
brethren of the “ Christians,” that is, of the Spaniards, did not raise the natives to
a position of equality with their conquerors. In the converts the latter at first
saw only inferior beings, useful especially when dead, as their fat then served to
staunch the wounds of men and horses. They addressed the natives whip in hand,
and even in the lifetime of Bernal Diaz a new saying had become current amongst
the whites: “ Donde nace el Indio nace el bejuco!”’ or, as we might say, “ Where the
Indian is born there grows the cane.” Even in recent times the poet Galven
could exclaim: “TI am an Indian, that is, a worm cowering in the grass, avoided
by all hands, crushed by all feet.” Accordingly the children of the Aztecs may
well have more than once sighed for the old order of things. ‘ Why were we
happier in the days of barbarism and debasement than since our conversion to your
faith ? ”” the elders of a native community asked Bishop Zumarraga.

The period immediately following the conquest was the most terrible for the
natives. At first some districts were transformed almost to solitudes by those
maladies which nearly always break out when distinct races are brought suddenly
into contact. The first epidemic of smallpox, said to have been introduced
by a negro in the expedition of Narvaez, and which struck down Cuitlahuatzin,
Montezuma’s successor, was more destructive than the Spanish arms.

But far more terrible was the matlazahuatl, probably scarlet fever, which raged
in 1576, and which, according to Torquemada, carried off nearly two millions in the
dioceses of Mexico, Michoacan, Puebla and Oaxaca. In a period of two hundred
and seventy-five years as many as seventeen great epidemics visited Mexico, from
all of which the Spaniards remained exempt. According to the missionaries the
race itself seemed to have become physically decayed, as if doomed to extinction.

Those who escaped the plague were more than decimated by the oppressive
burdens imposed on them. Although protected from slavery properly so called by
the ‘laws of the Indies,” they still remained serfs attached to the soil, and thus
fell in tens of thousands with the large estates into the hands of the religious
orders by which they had been converted, or else into those of the great capitalists
the responsibility of the proprietors being in all cases merely a legal fiction. Nor
were the laws themselves enforced, for the province of Panuco was nearly depopu-
lated by its own governor, Nuno de Guzman, who openly sold men and women to
the traders from the Antilles, after first branding them with the hot iron.

74 MEXICO, CENTRAL AMERICA, WEST INDIES.

Under the Aztec regime the lack of pack animals had introduced the custom of
making captives and outcasts ¢/amemes, or carriers, for the transport of goods and
supplies. This service they continued to perform under the Spanish administration,
though the law fixing the load at “two arrobas,” or about sixty pounds, was too
often violated. The landed proprietors, more ignorant than the natives of the
climatic conditions, often employed bands of porters in zones where the tempera-
ture was fatal; those descending from the plateaux perished in thousands on the
hot coastlands, while others, transferred to the bleak uplands, yielded to the cold.

But while the race of aborigines was rapidly diminishing and even disappear-
ing in certain districts, another race, that of the Mestizoes, was being developed
and acquiring ever-increasing importance. The conquerors, having brought no
women with them, soon formed alliances with the natives, Cortes setting the

Fig. 80.—Frirst Conauests oF CORTES.
Seale 1 : 4,000,000.

luejotli

LM: “oe & g
5°", Yxigamastitlan A
À eo) 2 Se » y

Qi ARE Tay HN A

Ne of. iG 2

60 Miles.

example by his connection with Malitzin or Doña Marina, who proved so useful
in times of extreme peril. All his captains and soldiers were presented with
native wives; all Indian chiefs, whether pleading for favour or concluding an
alliance, sealed the treaty by cementing unions between the new arrivals and the
women of his household or kindred; every tribe suing for peace brought women
as presents for the conquerors.

Even after the conquest the adventurers and traders attracted to the New
World by the fame of the treasures of Mexico were seldom accompanied by
Spanish helpmates; hence most of the unions continued to be made with native
women, despite the decrees which declared null and void all grants of land made
to whites who left their wives behind them. Thus the Mestizoes continued rapidly
to increase, and soon outnumbered the Spaniards.

In ordinary language this term “Mestizo” indicates rather the class than the
origin, and is applied exclusively to the proletariates who do not keep aloof from

INDIAN VILLAGE—VIEW TAKEN AT THE HUEXOCULCO PUEBLO, PROVINCE OF MEXICO.

—ss

RESULTS OF THE CONQUEST. 75

the Indian communities. But taking it in its true sense, the Mestizo element
may be said at present to constitute over four-fifths of the population. Even
the “wild” Indians are slightly mixed, while the so-called “ pure”
occasionally boast of their descent from the ancient rulers of the land. No less
than three families jealously preserve in Mexico and Spain the records tracing

whites will

their lineage back to Montezuma.

On the other hand the African element never acquired any importance in
Mexico, although negroes were introduced from the first years of the conquest.
But after an insurrection, suppressed by drastic measures, the Spanish landowners
were forbidden to purchase Africans in order to replace the natives. In any case
the black race could scarcely have become acclimatised in the cold regions of the
plateau. At present the negroes are almost exclusively confined to the towns of
the seaboard, and these have come for the most part from Cuba and Jamaica.
In the whole of Mexico they do not appear to exceed 20,000 persons.

During the three centuries of colonial administration between the fall of
Tenochtitlan and the proclamation of Mexican independence, the one great
event in the national history may be said to have been this slow formation of
the Mestizo race from Nahua and Iberian elements. Doubtless the full-blood
Spaniards, constituting the first social caste, continued to keep haughtily aloof,
claiming the exclusive right to the title of gente de razon, or “rational beings.”
But they were divided amongst themselves; to the Spaniards born in the
Peninsula were reserved the lucrative offices, as well as all honours and authority.
But the Creoles, however pure their blood, however great their merits, were
kept in the background ; they were even refused admittance to a large number
of the monastic establishments. By the very fact of their birth in the New
World they seemed to have almost ceased to be Spaniards and were insulted
at every turn. But this treatment was bitterly resented, and until recently the
term usually applied to the Spaniards by birth was Gachupines, derived from two
Nahuatl words meaning “ Men of the Spurs.” ‘‘ Mueran los Gachupines” ( Death
to the Gachupines!”’) was the war-cry of the insurgents.

The Indians properly so called, whether wild or mansos, that is, “civilised,”
were also regarded as inferiors, beings intermediate between man and animals.
On some rare occasions acts of courage or devotion might perhaps earn for a
native recognition as a brother, and then he was raised to the rank of hombre
blanco or “a white,” as if great qualities were incompatible with the nature of
the red man. But the true feeling was embodied in the current Mexican saying
that an Indian would never rule the land so long as there remained a muleteer
from La Mancha or a Castilian cobbler.

However, the lack of “reason ” attributed to the natives at least exempted
them after about the middle of the eighteenth century from the privilege of
being burnt by the Inquisition. They were regarded as possessing too little
human responsibility for their heresies to rouse the unger of the Inquisitors. But
the terrible tribunal had long been at work, and three years after its introduction

in 1571 had begun operations by an auto-da-fé of five persons.

76 MEXICO, CENTRAL AMERICA, WEST INDIES.

It should be noticed that the transitions between Spaniards and Mestizoes,
between Mestizoes and Mansos, are far less abrupt about the capital than in the
northern regions, where the populations are scattered over a much wider area,

Fig. 31.—Porr or SIGUANTANEO.
Scale 1 : 42,000.

RS
SIGUANTANEO

101°3 4" West of Greenwich _ [O1 32’
: Depths.
0to5 5 to 10 10 to 25 25 Fathoms
Fathoms. Fathoms. Fathoms. and upwards.
2,200 Yards.

and where the divisions between the races are more sharply drawn. In those
regions miscegenation has taken place to a smaller extent; till recently the

struggle between the hostile elements was still continued, and was occasionally
attended by massacres on both sides.

THE SPANISH ADMINISTRATION. AT

The exclusive mercantile system to which the country was subjected during
the Spanish rule had the effect, so to say, of sequestrating New Spain, and of
concealing from the eyes of the world the changes that had been accomplished
since the days of the conquest. It was in fact a system of absolute monopoly.
From the standpoint of the Spanish Government, the Aztec populations existed
only for the purpose of enriching the treasury and the commercial ‘“ farmers-
general.” But these vast monopolies, and the incessant manipulation of the
customs, combined with the oppression and empoverishment of the natives,
naturally resulted in exhausting the sources of all trade.

All violation of the fiscal laws was severely punished, and often involved the
death of the offender. All trading relations with strangers were interdicted
under pain of death; even shipwrecked mariners were thrown into prison, and
occasionally even executed, to prevent them from entering into commercial
relations with the natives; the very highways leading seawards were systematic-
ally abandoned, and the Mexican seaboard became a wilderness. Thus the
English navigator, George Anson, warned by the Indians of the neighbourhood,
was able to put into the port of Siguantaneo (Zehuatanejo), between the two
hostile garrisons of Zacatula and Acapulco, and wait quietly for the sailing of
the valuable galleon freighted with ingots for Manilla.

The system was at last pushed so far that the fleet destined for Spain was only
allowed to sail every third year, and to make for any other port but Seville or
Cadiz was declared to be a crime against the State. The search for quicksilver
mines was prohibited in order to maintain the monopoly of the Almaden mines in
the south of Spain. Till the year 1803, the Mexicans were forbidden to cultivate
the vine ; it has even been asserted that Hidalgo first raised the standard of revolt
in the Dolores district, because this revolutionary parish priest had been compelled
to destroy his vineyards. The olive was also interdicted, as well as many other
plants whose products might replace those introduced from Spain; even these
were imported only in small quantities to keep up the tariff of high prices.

At one time the people were forbidden to brew any more pulque, the national
drink extracted from the maguey plant, the sale of which interfered with that of the
Catalanian brandies. In the same way certain trades were officially abolished as
being prejudicial to the national industries of the Peninsula, or rather to the
interest of a few private speculators. Even so late as 1819 a royal decree pro-
hibited foreign vessels from entering the port of Vera Cruz “ under any pretext.”

Such an administration could end only in the total ruin of the colony, or in a
revolution. The moment the mother country became engaged in a war of inde-
pendence against the French, and was thus obliged to leave her ultramarine posses-
sions almost entirely to themselves, a change of the political equilibrium became
inevitable. The imprisonment of the Spanish Viceroy, Itturigaray, in 1806, by
the other members of the State Council, may be said to have been the first act in
the Mexican Revolution.

Doubtless the Creoles were far from being unanimous in their opposition to the
old order of things, and many even allowed themselves to be seduced by titles,

78 MEXICO, CENTRAL AMERICA, WEST INDIES.

privileges, or money. But they entertained the most divergent views on the
general situation. The more daring ventured to foster the idea of independence,
which to others seemed a dream, while the majority aspired to nothing higher
than a share in the administration of their native land, and the abolition of the
absolute commercial monopoly enjoyed by the Cadiz traders.

On the other hand the great bulk of the native population felt little interest
in the form of government. What they wanted was the possession of the land, a
little light to relieve their gloomy lives, a modest share of liberty. Under the
Spanish régime they had never attempted to revolt, although for two hundred years
after the conquest the armed forces consisted only of the Viceroy’s bodyguard ; even
under the Bourbon dynasty the ‘“‘ greens ’’—as the regular troops were called, from
the green facings of their uniforms—never exceeded 6,000 infantry and cavalry.

Nevertheless the Indians themselves had also a vague instinct of political inde-
pendence, as is evident from the persistent legend about King Montezuma. The
name itself they obviously learnt from the Spaniards; but they eagerly rallied
round it as a watchword, and adopted his colours, blue and white, for their
standard of battle. To him were attributed all the ruined monuments of the
country, and it was said that, like a second Quetzalcoatl, he slept in some cavern
awaiting the great day of national awakening. We know with what fury the
natives fought during the early days of the revolution. Impelled by the frenzy
of certain triumph, armed with nothing but clubs or knives, they fell upon solid
regiments of well-equipped troops; they even threw themselves on the guns in
order to stop the touch-holes with their rags or straw hats.

Such was the confusion of ideas and of factions caused by the prevailing
ignorance, and the long debasement of the populations, that the revolution began
by a rising of some fanatical Indians of Dolores, ‘“ in the name of the holy reli-
gion and of the good King Ferdinand VII.” On the other hand the insurgents
suffered their first defeat by troops composed of Creoles and led by a Creole.

In 1813, two years after the first conflict, independence was for the first time
proclaimed by a congress of refugees wandering from mountain to mountain.
But this voice of freedom sounded like blasphemy to those accustomed to servitude,
and the moderate party hastened to return to obedience. No Indians in the more
remote provinces had risen, and the seat of war had hitherto been confined to the
central districts, which were more densely peopled than elsewhere. The insur-
gents no longer formed regular armies, and had been reduced to mere guerilla
bands ; nearly all their prominent leaders had been shot, or were lurking in the
woods and marshes ; all seemed lost when, in 1817, Mina, a Spaniard twenty-eight
years of age, who had already fought bravely for freedom in Spain, crossed the seas
and devoted himself to the same cause in Mexico against his own fellow-countrymen.

But after gaining a few victories he also perished, and the struggle for inde-
pendence, so fiercely begun in 1811 by the priest Hidalgo and his extemporised
armies, was reduced to a handful of outlaws and brigands. Nevertheless the old
régime suddenly fell with a crash, so to say, under its own weight at the very
time when the Viceroy Apodaca was proclaiming the final restoration of order in

THE MEXICAN REVOLUTION. 79

1820, and when the victorious Spanish forces were sweeping the last “herds ” of
rebels before them. To effect the transformation all that was needed was the
treason of the ambitious Colonel Iturbide, in whom destiny “selected the least
worthy to be the successful champion of independence.”

Fig. 32.—Scenz or THE WAR or INDEPENDENCE,

Scale 1 : 11,000,000,

DEVESK
TE

106° West of Greenwich

86 Miles.

Now the whole nation enthusiastically adopted the “ plan of Iguala,” that is
to say, the project of a new constitution proposed in the town of Iguala, de-
manding full and complete autonomy for the Mexican people under a monarchical
form of government. The new order of things was accepted throughout the
whole extent of the land, and the capital itself was surrendered by O’Donoju,

80 MEXICO, CENTRAL AMERICA, WEST INDIES.

last of the viceroys. This was in 1821, and two years later the republic was at
last proclaimed.

The very term Guadalupes given to the insurgents in opposition to that of
Gachupines, by which the Spaniards were known, is a proof of the influence exer-
cised by the clergy over the bulk of the Mexican population. The multitudes of
native rebels were regarded merely as devout pilgrims enrolled under the banner
of the Madonna of Guadalupe, whose worship had been confounded with that of
Toci or Tonantzin, the “ Notre-Dame ”” of the Aztees.

But the priests, like the other whites, were themselves divided into factions
according to their origin, alliances, wealth or poverty. Hidalgo, who first raised
the standard of revolt, was a Creole priest with a mixture of Indian blood. Morelos,
another priest, was the chief hero of the war on the side of the national party.
Even anun, Maria Quitana, was seen to leave the convent and take part in the
struggle. But bishops and the officers of the Inquisition had in the name of the
Pope hurled excommunications against the rebels, and it was in honour of the
Church that on Good Friday in 1814, Iturbide, at that time in the service of Spain,
caused several of these excommunicated patriots to be shot.

Hence the clergy were unable to contribute towards fostering such a common
national sentiment as might have ensured internal peace. On the other hand the
political revolution was of no service in improving the condition of the native
peasantry, for it made no change in the system of land tenure. The soil still con-
tinued, as heretofore, to be monopolised by the great proprietors, whose power
was exercised over hundreds or thousan:ls of the agricultural population. Doubt-
less an agrarian revolution seemed imminent at the very outset of the insurrection,
when the domains of the Spaniards were sequestrated in the name of the nation,
and were freely occupied by the Indians. But the whites forming part of the
rebel forces hastened to put a stop to these confiscations, which might have had
fatal consequences, and the elements of the social struggle were thus maintained on
the same lines as before. ;

These profound inequalities, which largely coincide with racial distinctions,
sufficiently explain the state of chronic revolution which was the normal condition
of Mexico for the half-century following the proclamation of independence. The
nation sought without finding some new principle of economic equilibrium. By a
curious parallelism each civil war corresponded to a fresh outbreak both in Spain
itself and in her other revolted colonies, as if the dismembered branches of the old
empire were still connected by a common social life.

In Mexico the accomplishment of national unity is all the more difficult that a
considerable section of the Indians are associated with the civilised populations
only in terms of official documents. None of the natives still grouped in tribes
living apart in remote provinces, speaking the old languages, and practising the old
customs, can be regarded as yet forming part of the Mexican nation. But they
become assimilated in increasing numbers fiom year to year, thanks to the develop-
ment of education, industrial centres and highways traversing their territory.
Even the Indians of the Californian peninsula who are most removed from the

THE MEXICAN INDIANS. 81

centre of Mexican civilisation have acquired a knowledge of Spanish, and those
settled in the vicinity of the missions and the mining stations differ in no respects
from the Jndios mansos in other parts of the territory. But they are a mere handful,
scarcely mustering 3,000 altogether, and the Pericu tribe, recently mentioned as
still living at the southern extremity of the peninsula, has completely disappeared.
The other two who still survive, Cochimi in the north, and Guaicuri (Guayacura)
in the middle, of the peninsula, are related to the Arizonian Yumas, and, like them,
formerly occupied the northern plains which are now inhabited by the Cocopas,
and from which they were gradually driven we:t of the Colorado.

Both Cochimi and the Guaicuri lead an extremely nomad existence, shifting their
camping grounds at least a hundred times during the year. At night they shelter
themselves against the wind under some brushwood or line of rocks, but their only
roof is the canopy of heaven, though a few dens or lairs are constructed for their
sick. Formerly the Cochimi regarded with shame any kind of raiment ; but they
wore necklaces and bracelets, and encircled the head with an arrangement of skins,
reeds, or feathers.

The Cochimi and all other tribes of Lower California are grouped by Pimentel
with the Nahua family, that is, with the Aztecs, on the ground of their physical
appearance and speech. But other authorities hold that the Lower Californian
languages show no resemblance to Aztec or any other known language.

Nearly all the Indians occupying the north-western region of Mexico, from the
Arizonian frontier to the mountains skirting the right bank of the Rio Lerma,
belong to a widespread family commonly named from the Pimas and the Opatas,
two of their most powerful groups. The term Pimeria, or “ Pima-land,” is even
still, though incorrectly, applied to the north part of Sonora. The conventional
frontier laid down between the American and Mexican republics is not an ethnical
parting-line, and north of it the Pimas and the kindred Papagos are, in fact, repre-
sented in the largest numbers.

The Opatas also, who are said still to number 35,000 souls, dwell especially in
the Sierra Madre in the upland valleys of the Sonora and Yaqui rivers. They are
an agricultural people, who have been half assimilated to the Spaniards, and who
have always sided with the whites in the racial wars. Hence the Mexican writers
have always praised their valour, sobriety and steadfastness, and have given them
the title of ‘“ American Spartans.”

The Yaqui and Mayo tribes, who occupy the east side of the Gulf of California,
that is, the almost desert regions watered by the two rivers named from them, are
fully as brave as the Opatas, but they are no friends of the whites, and have even
frequently risen in revolt. In 1825, after the proclamation of Mexican indepen-
dence, they also proclaimed their own autonomy, and declared themselves exempt
from all taxes. Since that time their territory has remained somewhat inacces-
sible to strangers.

Yet the Yaquis and Mayos, who are sometimes collectively called Cahitas from
their common language, are by no means a numerous nation, probably not

exceeding 20,000 altogether. Despite the wars they have had to wage against
39

82 MEXICO, CENTRAL AMERICA, WEST INDIES.

the whites, they are naturally of a peaceful disposition, energetic, and industrious.
Like the Kabyles of Algeria, their young men emigrate every year in large
numbers, seeking employment in the farmsteads of Sonora or Sinaloa, or as
porters and menials in the towns. But they still remain attached to their homes,
and those who are not too far removed make an annual visit to their native valleys.
They are said to be excellent musicians, and, like the Hungarian gipsies, learn to
play the fiddle, guitar, or harp, merely by listening to the village minstrels.

The Seri people of Tiburon Island and the neighbourmg mainland appear to
form a distinct subdivision, with a few other scattered family groups known by
various names. Orozco y Berra has compared them with the Caribs, adding that

Fig. 33.—Curer Native PoPuLATIONS IN Mexico.
Seale 1 : 30,000,000.

oyetes Srcarillas js
Es Mèscaleros ore
Eros

I
on

Cosnanches

Al !
À 5
IL
‘

FRS

ë
à

LACS
aa

_—_
LS

4.
D

Nes CES S822 wat]
: LE.

AVA
=
a
py
F3
=
=

West of Greenwich

620 Mules.

he would not be surprised to find that they belong to the same race. These
natives, who are now reduced to a mere fragment, defended their homes and
valleys with great vigour; their poisoned arrows especially were much dreaded,
and Spanish expeditions had often carefully to avoid their territory. |

Amongst the numerous north-western populations the Tarahumaras, or
Tarumaros, are one of the most remarkable for the tenacity with which they have
preserved their ancient customs. The inhabitants of Chihuahua give the name of
Tarumaros to all the mansos, or “ civilised” Indians, of the state; but the true
Tarahumaras, who still number about 40,000, live in seclusion in the upland
valleys of the Sierra Madre on both the Atlantic and Pacific slopes. Their
villages, most of which end in the syllable chic—* place,” “ town’’—are scattered
over the highland region of the three states of Chihuahua, Sonora, and Sinaloa,
and according to Pimentel penetrate even into Durango.

THE MEXICAN INDIANS. 83

Some of ‘their groups are still cave-dwellers, and numerous caverns are shown
which were formerly inhabited. According to many writers the old troglodytic
customs explain the legend of the Aztecs regarding their residence in the ‘“ Seven

> The Tarahumaras who have settled in the towns of the whites now

Caves.’
speak the language of their rulers; but the full-blood communities of the Sierra
Madre have preserved their old tongue.

Discovered in their remote retreats by the Jesuit missionaries at the beginning
of the seventeenth century, the Tarahumaras have never offered any serious
opposition to the Mexican Government ; nevertheless they have always refused to
accept Spanish institutions. According to the traditional custom marriages are
contracted after a novitiate of the bride in her future husband’s house and under
the surveillance of his parents. The land has been preserved from confiscation,
and is still held in common. Each group of villagers is collective proprietor, and,
as in the Russian mir, the arable land is parcelled out amongst the families
according to their numbers. One portion is reserved for the sick and aged, and
this is cultivated by all the members of the community in their turn. The maize,
wheat, haricot beans, potatoes, and other produce are then stored in a public
granary under the eyes of the more honoured men and women of the village, and
the residents draw what they require from this common store.

They call themselves ‘‘ Christians” and erect a cross at the foot of their fields
at sowing time; but the parish priest is not allowed to assist at the feast, which
concludes with the sacrifice of a sheep or a calf. Those of the southern districts
near the common frontier of Chihuahua, Sonora, and Sinaloa, are said still to
practise the old religion. They keep entirely aloof from the Mexicans, and when
their villages are forcibly invaded, they refuse to answer the questions put to them
by the intruders. They decline all payment for the provisions they may be called
upon to supply, and even allow their cabins to be plundered without protest ; in
fact the only force they understand is that of passive resistance.

They are said to be a gloomy, sullen people; nevertheless when they fear no
disturbance to the national feasts they amuse themselves cheerfully, and ‘“ dance
with their gods.” They are specially fond of tilting and racing, whence their
tribal name, which is said to mean “ Runners,” though the etymology is somewhat
doubtful. At times whole tribes spend days in contending for the prize, women
with pitchers of water being stationed at regular intervals along the course to
revive those overcome by fatigue.

Some of the southern valleys of the Sierra Madre are inhabited by the remains
of another Indian nation, the Tepehuans, or “ Lords of the Mountains,” a name,
however, to which they are no longer entitled. After some conflicts with the
missionaries, they were almost exterminated by the Spaniards of Durango. These
natives, who are now Christians, and gradually merging with the populations of
the Sierra, have in some districts preserved their language, which by certain
authors is said to contain a large proportion of terms analogous to those of the
North Asiatic tongues.

The full-blood Tepehuans have a dull yellow complexion, prominent cheek-

84 MEXICO, CENTRAL AMERICA, WEST INDIES.

bones, and oblique eyelids, features which are all characteristic of the Kerghiz and
Kalmuck types. Like some Siberian peoples, they also plait the hair in a single
tress, which falls over the nape of the neck.

But whatever be said of the hypotheses affiliating these tribes to the Asiat'es,
both the Tepehuans and their southern neighbours, the Coras, have been classed
by Buschmann and Orozco on linguistic grounds in the same family as the Pimas,
Opatas, and Tarahumaras. On the other hand the Sabaibos, Acaxees, and Xiximes
of Durango, as well as the Conchos of Chihuahua, who dwell on the plain watered
by the river Concho, would appear to be rather Nahuas.

The space comprised between the Rio Grande and the east slope of the Sierra
Madre belongs to the various Apache tribes, who form a separate family related
in speech to the Athabascans of the Mackenzie basin. Their name, which is
probably of Opata origin, is said to mean “ Bad Dogs”; but they call themselves
Shis Inday, or “Men of the Woods.” Till within a recent epoch, all the northern
provinces of the republic were exposed to the raids of these ferocious Indians, and
even in Durango, over 360 miles from the American frontier, crosses set up on
the outskirts of the towns recalled the murders committed by the Apache savages.
Districts which, during the first years of the conquest, the Spanish troops were
able to traverse without fighting, and where peaceful colonies had been founded,
were afterwards invaded by the marauders, and all security disappeared beyond the
fortified towns and stations. Journeys could be made only by large companies or
caravans, and the armed men, whose track was followed by the savages lurking in
the surrounding brushwood, took care not to lag behind the main body.

How were these irrepressible foes to be got rid of? Mounted on their swift
and hardy horses, they could cover 60 or even 120 miles in a single day.
Everywhere they found shelter in the cactus scrub or thickets, and the shepherd,
aware of their presence, dare not betray them. The system cf large landed estates,
which had brought about the invasion of Italy by the Barbarians, also facilitated
the incursions of the Apaches by suppressing the little centres of culture and
resistance formerly scattered over the land, by replacing tillage with stock-breed-
ing, and lastly by leaving the defence of the country to mercenaries who had often
strong inducements to come to an understanding with the plunderers.

To get rid of the Apache robbers, a war of extermination was proclaimed
against them. A price was put upon their heads, the tariff being regulated accord-
ing to the age and sex of the slain. The Apaches on their part put to death all
adult men that fell into their hands, sparing the women and children to recruit their
bands, which, by this process of miscegenation, at last became a mongrel group
of all tribes and races. In this atrocious war, it often happened that the heralds
themselves were not spared. The military authorities, jealous of their privileges,
contributed on their part to prolong the “reign of terror’’ by arrogating to them-
selves the exclusive right of carrying on defensive operations, and absolutely
prohibiting the municipalities from combining against the common enemy. But
the regular troops proved insufficient for the task they had undertaken, and an
appeal had to be made to foreign mercenaries. Thus in 1850 a band of Texans

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peaceful travellers, and bring their scalps to the Government for the stipulated

At last Indians were hurled against Indians, and the extermination

rewards.

Fig. 34.—WATER-CARRIER AND TORTILLAS Woman.

of the Apaches was entrusted to their hereditary foes, the southern Comanches,

The few survivors have

The north-east region of Mexico comprised between the Rio Bravo and Tampico,

lways that now traverse their former hunting-grounds.

become shepherds, “cowboys,” horse-dealers, even guards of the stations on the
rai

who roamed over the Bolson de Mapimi plains.

85 MEXICO, CENTRAL AMERICA, WEST INDIES.

and between the central plateaux and the Gulf of Mexico, has been an exclusive
domain of Spanish speech since the last century. Scarcely any traces still survive
of Nahua or other native languages, and the “one hundred and forty-eight
nations ” of Coahuila, the ‘‘seventy-two” of Tamaulipas, the “thirty-one” of
Nuevo Leon, the Manosprietas, the Irritilas, Tamaulipecs, Cuachichils, and
Zacotecs, have all been merged in the general mass of the Mestizo populations,
abandoning their old usages and distinct idioms. Wherever the people were in
the nomad state the native tongues almost invariably disappeared, but held their
ground much longer among the settled or agricultural classes.

In the very neighbourhood of the capital the more secluded hills and upland
valleys are still inhabited by scattered groups of the Otomi, an Indian nation
which seems to have undergone little change since the epoch of Toltec rule,
The designation of “ Red-haired”’ often applied to them has probably reference
to their practice of dyeing the hair red when on the war-path. Round about
Queretaro, which may be taken as the centre of their domain, they occupy nearly
all the mountainous parts of the Anahuac plateau between San Luis Potosi and
the Sierra Nevada; hence the term Serranos, or “ Highlanders,’ commonly applied
to them.

The Otomi are estimated at over 600,000, including those who have exchanged
their language for Spanish or Aztec, and at probably 1,000,000 if the Pamé and
Mazahua branches be included, Despite their name, which in Aztec means
“Wanderers,” the Otomi are a very sedentary people, little given to travelling
except between their mountain villages and the market towns.

Physically they have large heads with coarse black hair, swarthy complexion,
heavy carriage, yet are excellent runners. By some writers these rude loutish
populations have been regarded as the remains of an old Chinese colony, an
hypothesis scarcely in accordance with the view that assigns a Chinese origin to
the Aztec culture. The theory was first suggested by the fact that the Hiashiu,
that is, the “Old,” as the Otomi language is called, is, like Chinese, almost entirely
monosyllabic. The two languages also present numerous coincidences in their
vocabularies ; but such coincidences are almost inevitable, the series of mono-
syllabic words being naturally somewhat restricted or at least presenting far less
diversity of ferm than that of polysyllabic terms.

In Michoacan, west and south-west of the capital, the bulk of the population
are the Tarascans (Tarascos), who occupy nearly the whole of Michoacan itself,
besides a small part of the neighbouring state of Guanajuato. But in various
districts they are intermingled with the Otomi, the Mazahuas, the Matlaltzincas,
as well as some more or less mixed descendants of the Aztecs. So recently as
the beginning of the present century, the Tarascan language was still dominant
in their territory, Spanish being almost unknown except in the towns; it is
even still the chief medium of intercourse in many rural districts; but Spanish,
being taught in the schools, is gradually prevailing. The Tarascans, formerly
rivals of the allied Aztec race in general culture, were, like them, acquainted
with pictorial writing, and even excelled them in some branches of industry.

THE MEXICAN INDIANS. 87

Their religion was also of a milder character, and sanguinary rites had been
introduced only a short time before the Spanish conquest. They long held
ont valiantly against their Aztec “ Fathers-in-law;”’ their own name (Tarhascue)
had, according to Lagunas, the meaning of “ Sons-in-law,” and was said to have
reference to their exogamous practice of taking their wives from their Aztec
neighbours.
On the east slope of the plateau, facing the Gulf of Mexico, are found some
groups of distinct populations isolated amid the surrounding Aztec people, who

Fig. 35.—Curer Native Races IN MEx co.
Scale 1 : 30,000,000.

SPA I
N

NI
A

NNN
SES

West of Greenwich

Aziees. Mayas, Quichés, Tarascans. Zapotecs,
Huaxtees, Totonacs. Mems. Mixtees.
: rm mo
Opata-Cora. Otomi, &e. Zoqué, Mixé Choroteg’. Lencas,
Chontals, &e.
620 Miles.

have become more or less assimilated to their Spanish rulers. Such are the
Huaxtecs (Huastecos), that is, “Our Neighbours,” so named in courtesy by the
Aztecs, although, according to Pimentel, the term means “ People of the Huaxi
land,” so called from a kind of fruit common in their territory. They occupy the
northern part of the State of Vera Cruz, and stretch thence northwards to the
plains watered by the lower course of the Tampico river. The Huaxtecs are allied
in race and speech to the Mayas of Yucatan, although no tradition survives of
the events by which they became severed from their southern kinsfolk. Judging
from the archaic form of their language, Stoll concludes that they were the first
who became isolated from the primitive Maya group, and various names of places

88 MEXICO, CENTRAL AMERICA, WEST INDIES.

and peoples show that the Maya nation, at present confined to the Vucatan
peninsula, formerly occupied the Tlaxcala plateau.

On their southern frontier, that is, in the hills whence flows the Rio Cazones,
the Huaxtecs are conterminous with the Totonacs, that is, the “ Three Hearts,” .
said to be so named because they formerly made a solemn triennial sacrifice of
three youths, whose hearts were offered to the gods. According to the national
traditions the Totonacs also accomplished many peregrinations at an epoch even
antecedent to the wanderings of the Chichimecs and Aztecs, and, like them, at last
founded new homes on the Anahuac plateau, but more to the east. Most ethno-
logists adopt the views of Sahagun, who groups the Totonacs in the same family
with the Huaxtecs and Mayas, while other authorities regard them as quite
distinct. Alphonse Pinart also makes a separate division of the few thousand
Akal’mans, who appear to speak a peculiar language, and who live between the
Huaxtecs and Totonacs in the northern part of the State of Hidalgo andin Vera
Cruz, but chiefly round about the city of Huejutla.

The last group of native races in Mexico proper beyond Chiapas and Yucatan
is formed by the various Indian populations who dwell, to the number of about
600,000, in the southern uplands and on the Pacific slope between the Acapulco
district and the isthmus of Tehuantepec. Here the chief languages, which, how-
ever, present but slight differences, are those of the Mixtecs and Zapotecs, that is,
“ People of Cloudland,” and of the “ Zapotas” (casimiroa edulis). Like the
Tarascans these nations were fully as civilised as the Aztecs, and it was their
strong national sentiments that enabled them to offer a vigorous resistance to the
Spaniards, and even to maintain a state of semi-independence down to quite recent
times. Now, however, they form part of the common Mexican nationality, and
by their energetic habits contribute as much as any other native element towards
the general prosperity of the commonwealth. Spanish will soon take the place
of the local languages as the medium of general intercourse, as it has already
become that of popular instruction. The Mixés also, as well as the Zoqués, the
Chinantecs, and other peoples of East Oaxaca, who are usually grouped under the
general name of Chontals, that is, “Savages,” are being gradually absorbed in the
mass of the civilised population. Their Mixé neighbours are said to have such a
poor language that it has to be supplemented by numerous loan words taken from
the Spanish. Formerly they had to eke out the sense by means of gestures, so
that after nightfall, or when the lights were put out, all conversation ceased.

Doubtless many of the Atzec aborigines were in some respects inferior in
culture to the ancient subjects of Montezuma. But, on the other hand, numerous
tribes which formerly possessed no culture at all, have now entered the general
movement of national development. In any case the multiplicity of idioms still
current in Mexican territory, some spoken by a few hundred thousand, some only
by a few thousand or even a few hundred persons, prevent all comparison between
such many-tongued states, for instance, as Austria-Hungary or the Turkish
Empire. In these two states the current languages belong not to small groups,
but to powerful nationalities all contending for supremacy in the very heart of the

THE MEXICAN INDIANS. 89

monarchy itself; but in the Mexican republic Spanish, recognised by all as the
national language, is steadily and surely encroaching on all the others. But,
excluding the Aztec, Otomi, Tarascan, Mixtec, and Zapotec, the “one hundred
and twenty ” languages still current in Mexico are spoken only by obscure and
scattered communities of but sight numerical importance ; many of these are also
actually disappearing, just as at least sixty have already disappeared since the
arrival of the Spaniards in the country.*

The indigenous populations differ so greatly in their origin and other respects
that it is impossible to draw a general picture of the Mexican Indian equally
applicable to all. The accounts given by various authors refer chiefly to those that
are met along the highway between Vera Cruz and the capital and in the other
more important towns on the plateau. In fact, these writers have almost exclu-
sively taken as the typical representatives of the aborigines the more or less
civilised Aztecs and the still barbarous or almost savage Otomi. On tke elevated
tablelands most of the natives have a skin soft as velvet to the touch, but so thick
that it conceals as with a vesture all prominences and play of veins and muscles.
The blood is not seen as through a transparency on the cheeks, except amongst the
young girls, whose features are said at times to “beam like copper lit up by the
sun.” An extremely mild expression is imparted to the whole physiognomy by
the cheekbones, which, though prominent, are still enclosed in a thick layer of
flesh, by the nose with its wide nostrils, the tumid lips and rounded chin. The
glance also acquires a highly characteristic expression from the peculiar disposition
of - the eyelids, the upper being scarcely curved above the median line of the eye,
while the lower describes a more decided arch towards the cheek than is found in
any other race. The skull is brachycephalic, this rounded form, however, being
due in many districts to the custom of moulding the head of the infants on the
inner curve of a calabash. The hair is black, coarse, and lank, like that of all full-
blood American aborigines.

A distinguishing feature of the upland populations is their broad and highly
convex chest ; they are also noted for the great muscular strength of their iegs ;
when resting by the wayside or in their homes they squat down on their toes, and
show no signs of fatigue even after hours of such an apparently uncomfortable
posture. On journeys they always walk in single file, with a light springy step in
unison, and bent somewhat forward, as if to present their broad back to the
burden. The attitude, in fact, is that of pack animals, and such was the condition in
which they had been till recently kept by their Spanish taskmasters. The women

* Chief languages spoken in Mexico proper, excluding Chiapas and Yucatan :—

Nahuatl or Mexican (Aztec), with Acaxee, Sabaibo, Xixime, Cochimi, Concho, and other members
of the same family.

Seri, Upanguaima and Guaima.

Papago, Opata, Yaqui, Mayo, Tarahumara, Tepehuan, Cora, &c.

Apache or Yavipaï, Navajo, Mescalero, Llanero, Lipan, &c.

Otomi or Hia-hiu, Pamé, Mazahua, &c.

Huaxtec, Totonac.

Tarascan, Matlaltzincan.*

Mixtec, Zapotec, Mixé, Zoqué, Chinantec.

90 MEXICO, CENTRAL AMERICA, WEST INDIES,

when kneeling, with motionless head and bust, fixed gaze, and upheaved chest,
have the aspect of ancient Egyptian statues ; so striking is the resemblance that, in
the language of Lucien Biart, ‘we dream despite ourselves of a possible kinship
between the two peoples.” The Mexican Indian is extremely frugal and regular
in his almost exclusively vegetable diet, consisting mainly of beans, maize,
pimento, and bananas. In the family circle he is fond of occasionally drinking to
excess ; but whatever quantity of pu/que or other intoxicating liquors he may take,
he is never affected by delirium tremens. The natives suffer from few ailments, and
those who escape from the convulsions and other disorders of infancy generally
arrive at mature age, though seldom taking the trouble to count the years of their
unchequered lives.

Nevertheless the Indians who have kept aloof from the European and settled
Mestizo communities, rejecting the culture and customs of civilised society, betray
that appearance of gloom and incurable sadness which seems to hang over races
destined to perish. They are always serious, silent if not sullen, and justly
suspicious. They seek the solitude, and reluctantly quit their native homes,
which are carefully enclosed by tall cactus hedges. Beyond their lowly hamlet
with its belfry fondly raised by the villagers, nothing seems to awaken their
curiosity. Nevertheless they follow with a furtive glance the man from whom
they have suffered wrong ; they can dissemble while awaiting the opportunity for
vengeance.

The half-castes, who tend more and more to constitute the bulk of the popula-
tion, are on the whole of more graceful form and more delicate frame than the
full-blood Indians. Like them, they have black and mostly lank hair, straight
and at times slightly flattened nose, and depressed brow. But what the features
lack in regular outline is always compensated by a kindly expression and winning
smile. The articulations of hands and feet are extremely delicate, notwithstanding
the tendency of the women to corpulence. It was stated at a recent meeting of
the French Anthropological Society* that of all clients of the French glove-
makers the Mexican and Peruvian creoles have the smallest hands. The Mexican
civilian is noted for his quiet, easy carriage ; he is always courteous even towards
his most intimate friends; unaffectedly polite even towards those against whom
he may bear a grudge. But despite a clear intellect he seldom betrays any marked
aptitude for any profession, and in youth he is easily led into dissipated, frivolous
ways. He is open-handed, shares freely with his friends, and with a light
heart will stake his all at a single hazard. “His purse burns,” says a local
proverb, to give some idea of the recklessness of the Mestizo, which contrasts so
strangely with the greed of the pure Indian. Thus the Mixtecs and Zapotecs of
Oaxaca, for instance, are said still to hide away all their savings, concealing them
even from their own families, so that at the day of resurrection they may have
all the enjoyment to themselves. A prodigious amount of treasure is supposed to
lie buried in the ground in consequence of this practice, which, however, dates
from pre-Christian times. Property accompanied its owner. to the grave, and

* February 6th, 1890.

THE EUROPEANS OF MEXICO. 91

rich finds may yet be expected to be brought to light from the old burial-places
in this region.

The Spanish element amongst the Mestizo populations of the Mexican plateaux
was drawn chiefly from Galicia, Asturia, and the Basque country, whereas the
settlers in the low-lying district of Vera Cruz were mostly Andalusians. Later
came the Cataloniaus ; but at no period did this tide of immigration assume any
considerable magnitude, and it was arrested altogether during the war of independ-
ence. A large proportion of the 80,000 Spaniards at that time living in the
country were driven into exile, and then took place the opposite movement of a
return to the old country. Since the revolution a small stream of emigration has
again set towards Mexico, and especially towards the uplands; amongst these
more recent arrivals are many natives of France and Italy, as well as of North
Europe, and several thousand English and German settlers now reside on the
elevated plateaux of the cold zone.

It was long supposed, on the faith of Humboldt’s statement, that in Anahuac
altitude compensated almost exactly for the more northern latitudes of Europe,
and that consequently the European could here be rapidly and permanently
acclimatised. “With the exception of a few seaports and some deep valleys,”
wrote the great German naturalist, ‘New Spain must be regarded as a highly
salubrious country.” Such it certainly is for the natives, who have become adapted
to their environment from time immemorial. But the comparative researches of
Jourdanet and other physiologists plainly show that northern and even southern
Europeans cannot settle with impunity on the higher tablelands, where the
barometric column stands normally at about 23 or 24 inches, consequently
where atmospheric pressure is one-fifth less than at sea-level ; hence the lungs
inhale in an hour about one ounce less of oxygen on these plateaux than on the
coastlands. The stranger residing on the uplands, where he supposes himself
to be acclimatised, runs more risk than the Indian, despite his greater attention to
hygienic precautions. He has especially to dread the dry season, that is to say, the
three months of March, April, and May, when the aqueous vapour is insufficient to
stimulate the respiratory functions. Children born of Europeans are usually frail
waifs, difficult to rear and nearly always overtaken by premature old age. Even
for the natives themselves the yearly increase of the population is far greater in
the temperate than in the cold zone. The immigrants are more threatened on
the plateaux than on the lower slopes; those even who settle on the burning
plains of the seaboard are relatively better armed after overcoming the yellow
or marsh fevers, and thus become more acclimatised than their fellow-countrymen
on the elevated lands, where affections of the lungs, as well as dysentery and
typhoid fevers, are more prevalent.

On the seaboard phthisis is common enough, and often assumes a highly acute
form, except in the swampy districts where, so to say, it is driven out by the
marsh fevers. Thus these two formidable disorders divide the coastlands between
them. Another terrible scourge on the shores of the Gulf and especially at Vera
Cruz is yellow fever, which, though less frequent in winter, occasionally prevails

92 MEXICO, CENTRAL AMERICA, WEST INDIES.

at all seasons. It would almost seem as if this malady was unknown before the
arrival of the Europeans in the country; at least, medical men have failed to
identify it with any of the other contagious epidemics mentioned in the history
of Mexico. The first certain indication of its presence occurs so recently as the
middle of the seventeenth century in connection with some extensive earthworks
causing a disturbance of the soil. Its range is limited to about 3,300 feet on the
eastern slope of the plateau, and cases are very rare above 2,500 feet. But the
germs of the disease contracted on the coast may be developed on the uplands a few
days after the arrival of the patient, and then it assumes a very dangerous form,
frequently ending fatally. On the Pacific side the ports of Acapulco, San Blas, and
Tehuantepec enjoy immunity from yellow fever, which, however, is replaced by a

Fig. 36.—Prevattine Diseases IN Mexico.
Scale 1 : 24,000,000.

P
el
ae

per
ds

AUD.

|
Kid

=
SS
-————>
===
=
=
SS
SSS
SS
SS
=
<i
SSS

106° West of Greenwich

292 ae OT ANNE CERTES

Cold Zone. Altitude of 2,300 feet, limit of Yellow Fever.
620 Miles.

bilious fever, whose attacks are rarely dreaded by the indigenous populations. The
vitiated taste which often develops a craving for earth, especially amongst the
women, is common in South Mexico. Even on the plateaux little pastilles of a
perfumed earth are exposed for sale at the markets, and never lack purchasers.
Mexico is also noted for certain ailments which have been observed in no other
part of the world. On the Atlantic slope, and especially at Orizaba, a serious
affection occurs caused by the moyoguil, a species of insect whose larva, deposited
under the skin, burrows into the flesh, where it raises a tumour as large as a hen’s
egg. It is cured by the application of a turpentine plaister, by which the sore is
suppurated and the germ drawn out. Much more frequent is the so-called pinto
malady, which affects whole populations, especially in the states of Guerrero and
Oaxaca. This is a cutaneous affection which destroys the uniform colour of the

LOWER CALIFORNIA. 93

skin, in one place raising a patch of white on a black ground, in another a dirty
red on white; then these patches gradually expand, often with a certain regularity,
until the body becomes mottled over like a piebald horse or certain snakes and
salamanders. Hence the term pinto, or “ painted,” applied to this malady, which
in many upland valleys prevails jointly with goitre over the whole community.

Lower CALIFORNIA.

Lower California, at once the most remote, and geographically the most
distinct region of the republic, is at the same time the least important from the
political standpoint. It may, in fact, be said to be useless, except as presenting
arampart of some 750 miles on the Pacific side of Mexican territory. With a
scant population of little over 30,000, and with scarcely any resources beyond its
mines, fisheries and salt-pits, it has not even been considered worthy of constitut-
ing a separate state, and still remains a simple territory belonging in common to
the whole commonwealth. It is so indifferently administered that the North
Americans have frequently crossed the frontier of the peninsula to work the
deposits of ores and salt at their pleasure without even the formality of a previous
concession. Extensive salt-beds were long known to stretch along the west coast
round the shores of Sebastian Vizcaino Bay; but basins of saline efflorescences are
so numerous in other parts of Mexican territory that the Spaniards had no induce-
ment to work these vast Californian deposits. In 1884 some Mexican explorers
visiting the inlet known as Ojo de Liebre from a neighbouring spring, discovered
to their astonishment the remains of large mining works that had been constructed
by some American speculators. Here were landing-stages, platforms, dépots,
railways, trucks, and other rolling stock, occupying altogether a space of over 34
miles. Evidently a large number of hands had been employed on the works; yet
the Mexican Government had never been informed of these extensive operations,
either because of the remoteness of the peninsula and lack of local population or
more probably owing to the remissness or venality of the officials.

About half of the Lower Californian population is concentrated towards the
southern extremity of the peninsula, and chiefly in the vicinity of La Paz Bay.
The provincial capital, founded by the Jesuit missionaries, stands in the bed of a
waterless torrent on the north side of the bay, which is sheltered on the east
side by the rocky headland of Pichilingue.

A well-kept road, lined by norias or draw-wells, winds between orchards, vine-
yards, coffee and other plantations from La Paz southwards to the flourishing
village of Todos Santos, on the Pacific coast. This district is watered by a
perennial stream, a rare phenomenon in Lower California. La Paz thus possesses
considerable agricultural resources; but its chief wealth still consists in its gold
and silver mines, which were formerly far more productive than at present,
yielding large supplies of the precious metals under the Jesuit administration.
The richest lodes were said to have been blocked in 1767, when the missionaries
were expelled, and if so their position has been faithfully kept a profound secret
by the Indians ever since that epoch.

94 MEXICO, CENTRAL AMERICA, WEST INDIES.

But however this be, certain mines, such as those of San Antonio, south of
La Paz, are still very rich in auriferous ores, their annual yield exceeding
£480,000. At Marques, north-west of La Paz, a quicksilver mine is also worked.

La Paz is also the centre of important pearl fisheries in the Gulf of California,
The submerged rocks off Cape Pichilingue are covered with pearl oysters, which
are fished up by the Yaqui Indians. Whole forests of coral flourished in the
straits separating the island from the mainland, and here are collected as many as
nineteen different species of sponges, all, however, of a somewhat coarse texture.
Although the value of these fisheries, like that of the mines, has gradually fullen

Fig. 37.—La Paz.
Scale 1: 11,000,000.

0 to 5 5 to 25 25 Fathoms
Fathoms. Fathoms. and upwards.
12 Miles.

off, the average annual yield is still estimated at about £10,000 on the spot. The
pearls are bought up by Jewish dealers of New York, who realise considerable
profits on the transaction.

Loreto, which, like the capital, lies on the Gulf some 160 miles farther north,
was formerly the religious centre of Lower California. Here the Jesuit mis-
sionary, Salvatierra, established in 1697 the first fortified station, whence expedi-
tions were made into the interior to bring back captives, who were then manu-
factured into devout believers.

At the western foot of the neighbouring Giant Mountain lies the village of
Comondu, where a small detachment of Mexican soldiers held out for four months

gainst greatly superior American forces. The architecture of this village, like

— rs

SONORA. 95

that of all the older settlements in the peninsula, differs little from that of the
Zuni Pueblos in New Mexico. It consists of one huge square block enclosed by a
trench, and without any windows or other apertures on the outer sides. This
common stone dwelling is disposed in two storeys, the first of which recedes a few
yards from the basement, and is reached by a ladder placed against the wall. A
second ladder leads to the top of the building, whence the inmates get access by
trap-doors and more ladders to the rooms and inner court.

In recent years some commercial activity has been developed in districts which
were formerly desert or almost uninhabited. Thus the village of HMulege, lying on
the shores of Santa Inez Bay, over 60 miles north-west of Loreto, has become a
busy mining centre since the discovery of auriferous deposits in the valleys of the
interior. Near the United States frontier the village of Todos Santos gives its name
to the neighbouring bay, which offers excellent shelter to vessels engaged in the
coasting trade. The port of San Bartolomé, which stands on the opposite side of
Cape San Eugenio, also attractsesome shipping. But the best haven on the whole
coast is that of Santa Magdalena, the narrow entrance to which has over 100 feet
of water in the channel. The spacious inner basin is large enough to accommodate
whole fleets.

SONORA—SINALOA.

The State of Sonora, which faces the northern part of the Californian peninsula,
is also one of the least inhabited regions in the republic; with an area of nearly
80,000 square miles, its population scarcely exceeds 150,000, or rather less than
two to the square mile. In 1859, the adventurer, Raousset Boulbon, who had
placed himself at the head of a band of French miners returning from California, ,
was for some time master of Sonora. The arable tracts, where the civilised Indians
and Mestizoes have formed settlements, are confined to the bottom lands of the
mountain valleys. Every town and village is encircled by a zone of irrigated land,
the settlements thus forming so many oases, some of which are connected together
by narrow strips of verdure. The very name of the country, from the Opata word

Sonoratzi, a “ Place of Springs,”

originally applied to a cattle ranche, indicates the
important part played by wells in this arid region. |

Amongst the Sonoran towns Santa Magdalena lies nearest to the United
States frontier, being situated on a headstream of the Rio de la Asuncion, which
flows west to the north end of the Gulf of California. At the time of the
annual fairs the whole of the surrounding populations, white and red, American
and Mexican, form temporary camping-grounds in the valley of the river. Far-
ther south several settlements have been founded in the basin of the Rio Sonora :
such are Avispe, in the territory of the Opata Indians, formerly capital of the
state; Ures, which succeeded it as centre of the administration, and which lies
near the narrow gorges where the river escapes from the Sierra Madre on its
westerly course to the Gulf ; lastly Hermosillo, formerly Pitic, or the ‘‘ Confluence,”
the largest town in Sonora and centre of a considerable agricultural industry. The
district which is irrigated by the last waters of the Sonora, and its Cucurpe

96 MEXICO, CENTRAL AMERICA, WEST INDIES.

affluent, grows sugar and wheat, and its inhabitants claim that the yield of wheat
is proportionately higher than in any other part of the world. Nevertheless,
Hermosillo owes its importance not to its agricultural resources, but to the
mineral deposits discovered in the vicinity. Between 1867 and 1888, the local
mint coined a total sum of £2,640,000, chiefly in silver pieces. South-west of the
town rises the famous Cerro de la Campana, or “ Bell Mountain,” whose porphyry

Fig. 38.—Guaynas.
Seale 1 : 170,000.

ZA SW
AIN

NN"

CZ
Se eee ee
ae ee —

WE
Q 4 IC
EN NZ

West of Greenwich

Depths.
=
9 to 24 23 to 5 5 to 10 10 to 25 25 Pathoms
Fathoms. Fathons. Fathoms. Ta homs. and upwards.

3 Miles.

blocks appear to vibrate with a silvery sound. The Yaqui river basin, although
less thickly peopled than that of the Rio Sonora, contains in its upper valleys
a few industrious places, such as Oposura and Sahuaripa, where the Indians are
engaged especially in the manufacture of cotton fabrics. Oposura, the old capital
of the Opata nation, has recently taken the name of J/octezwma, in memory of the
former rulers of the land.

4 D a sr)

SINALOA. D7

The State of Sonora possesses on the Colorado river the little port of Lerdo,
situated near a cluster of low islands where the Cocopa Indians gather the wniola
palmeri, an alimentary cereal till recently unknown to botanists. Much farther
south lies the seaport of Gwaymas, so named from an extinct Indian tribe,
which was a member of the Pima family. The harbour of Guaymas is one of the
best in Mexico, and in a better-peopled and more flourishing district it could
not fail to acquire considerable economic importance. But the whole of the
seaboard is an arid waste; not a tree is to be seen, not a drop of water
wells up for miles around the port, which is encircled like a flooded crater by bare
rocks. The very shrubs growing in the town are rooted in soil brought from
the United States, and are irrigated by a brackish water drawn from deep wells.
Nevertheless its excellent anchorage attracts to Guaymas an increasing number
of vessels, and the place has been recently brought into railway communication
with the mining and agricultural district of Hermosillo, as well as through Arizona
with the network of United States lines. The Guaymas traders export marine
salt and a little guano collected on Patos, or “ Duck” Island, an arid rock lying
north of the large island of Tiburon, or the “Shark.” To these products may some
day be added an anthracite coul of excellent quality, large deposits of which are
found in the valley of the upper Mayo river.

Towards the southern extremity of Sonora lies the mining town of A/amios, or
the “ Poplars,” which, like Hermosillo, has its own mint, where are annually issued
from £350,000 to £400,000 worth of coins. Alamos lies just within the basin of
the Fuerte river, so named from the old Sinaloan fort of E/ Fuerte or Montes
Claros, which guarded the seaboard from the Mayo and Yaqui Indians, and which
has now become a flourishing little town.

The natural port both of Alamos and El Fuerte is Agiabampo, where are shipped
dyewoods and silver ingots and ores, but only by small craft, there being only ten
or twelve feet of water on the bar at ebb tide. The old Indian town of Sinaloa,
which has given its name to the State of Sinaloa, has for its outport the deep and
perfectly-sheltered haven of San Carlos, which communicates with the sea through
the strait of Topolobampo, which is accessible to vessels drawing sixteen or
eighteen feet.

Culiacan, present capital of the State of Sinaloa, is one of the old cities of
Mexico. In 1531, ten years after the conquest, it had already been founded near
Hue-Colhuacan, that is, “Snake Town,” one of the stations on the line of the Nahua
migrations. At this place the Spaniards organised all their expeditions of disco-
very and conquest made in the direction of the north. Culiacan, which lies on the
river of like name in a fertile district encircled by hills, is connected by a railway
nearly 40 miles long with its port of A/fata, on a deep lagoon which is sheltered
from the surf by a long strip of sand. All the gold and silver ores of Sinaloa are
forwarded through this place, and between 1846 and 1888, the Culiacan mint
issued gold and silver specie to the value of £8,200,000.

In South Sinaloa lies the important city of Mazatlan, the mo.t active seaport
on the west coast of Mexico. Its Indian name means “ Deer-land,” and one of

98 MEXICO, CENTRAL AMERICA, WEST INDIES.

the islets on the neighbouring coast bears the Spanish designation of Venado,
which has much the same meaning. The researches made in the surrounding
alluvial districts have brought to light numerous remains of stags’ antlers
associated with arrowheads, axes. and other stone weapons and implements. As
a seaport Mazatlan cannot compare in natural advantages either with Guay-
mas or Acapulco; the roadstead is exposed to all winds, and in order to avoid
the nor’westers, especially dangerous in these waters, vessels have to ride at

Fig. 39.—Mazatuan.
Scale 1 : 30,000.

FRE JE

= f ?
Mit
Melt
Wh

West of Greenwich 106'97' -
Depths.
Sands exposed at 0 to 16 16 to 32 82 10 64 64 Feet and
low water. Feet. Feet. Feet. upwards. .

1,100 Yards.

anchor in a part of the bay where the ground-swell rolls in from the south and
south-west. But for the export trade with California Mazatlan has the advantage
of lying exactly under the latitude of Cape St. Lucas; in other words, itis the first
Mexican seaport reached by vessels arriving from San Francisco. Heace it has
become one of the chief ports of call for the regular steampackets, and thus have
been developed numerous local industries, such as saw-mills, rope-walks, foundries
and spinning factories, employing a large number of foreign hands,

Some 36 miles due south-east of Mazatlan is the little town of Chametla, that

SINALOA. 99

is “Cabins,” in Aztec, a place which the early Spanish navigators had endeavoured
to utilise as a seaport long before their attention was drawn to Mazatlan. From

Fig. 40.— CarHEnrAL or CHIHUAHUA.

\
SVS

Chametla Cortes sailed in 1535 on his expedition of exploration in the ‘ Vermillion
Sea.”

100 MEXICO, CENTRAL AMERICA, WEST INDIES.

CHiHUAHUA, DuRANGo.

On the east slope of the Sierra Madre, the chief city in North Mexico is
Chihuahua, which is variously explained to mean the “City of Water” or the
City of Pleasure.” It stands at a mean altitude of 4,600 feet at the foot of the
lofty Cerro Grande, between two streams whose united waters form the Conchos
affluent of the Rio Bravo del Norte. An aqueduct derived from one of these
streams winds round the flanks of the mountain, separating the region of scrub
from the irrigated fields and gardens of the slopes. Chihuahua is a decayed place,
which in the last century, during the flourishing period of the surrounding mines,
is said to have had a population of 75,000, that is, about six times more than at
present. The cathedral, erected and long maintained at the cost of the miners,
is an imposing structure towering above all the surrounding buildings. Here
is also a mint, which has become the third most important in Mexico since the
work of exploring the metalliferous lodes has been resumed by American miners.
The ores which supply the Chihuahua mint come chiefly from the deposits of
Santa Eulalia, a village lying about 20 miles to the south-east in a narrow glen
flanked by inhabited caves. The argentiferous lodes of Santa LKulalia have
already furnished to the trade of the world a quantity of silver estimated at
£28,000,000. The ore is poor, but occurs in great abundance, so that when the
deposits are not worked by companies the so-called gambusinos, or private miners,
find enough metal to earn a livelihood. The very slag, which has been used to
build hundreds of houses in Chihuahua, or to enclose fields and gardens, is said
still to contain a percentage of silver valued at not less than £80,000,000, so that
it has been proposed to submit it to a further process of reduction.

Another decayed place is Cosihuiriachi, which lies some 60 miles to the south-
west in a valley of the Sierra Madre, and which during the last century had a
population of over 80,000. Batopilas, which stands in the upper basin of the Rio
de] Fuerte within the Chihuahua frontier, has yielded altogether £12,000,000
during the 250 years that have followed the discovery of its deposits. Scarcely
less productive than the Batopilas mines are those of Guadalupe y Calvo, in the
Sinaloa river basin at the south corner of the state. |

The eastern section of Chihuahua is an almost completely desert region,
whereas the western zone, comprising the slope of the Sierra Madre, is a land
of mines and forests, of grassy heights and arable tracts. Here is ample room
for a large population, and in the upland valleys stock-breeding and horticulture
might be successfully carried on. Nearly all the towns in the state, San
Pablo Meoqui, Santa Cruz de Rosales, Santa Rosalia,- Hidalgo del Parral, follow
in the direction from north to south parallel with the Sierra Madre, and lie
at the issue of the various fluvial valleys, whose streams form the Rio Conchos.
The railway from Denver City to Mexico traverses the state in the same direc-
tion, and penetrates into Mexican territory through the historic town of Paso
del Norte, which stands on the right bank of the Rio Bravo at the point where
this river becomes the common frontier between the two republics. Paso is

DURANGO. 101

the oldest station in north Mexico, having been founded in 1585 by a Franciscan
missionary. This “ford,” as the word means, was formerly much frequented by
the American convoys which conducted the transport service across the western
prairies between the Missouri and Mexico, but it gradually lost its importance,
owing to the competition of the ocean highways. Paso, however, has acquired
great commercial value since it has become the junction of the four railways
running to San Francisco, to New York through Denver, to New Orleans and to
Mexico. In 1889 its exchanges amounted to over £4,000,000. At the confluence
of the Rio Bravo and Conchos river stands the frontier military station of
Presidio del Norte, which lies beyond the trade routes, and, despite its strategic
value, has never risen to the rank of a town.

In the hilly region stretching west of El Paso parallel with the Rio Bravo
prehistoric ruins are very numerous; here are found the Casas Grandes, “ great
houses,” of Chihuahua, the largest of the Nahua settlements whose remains still
survive in the northern part of Mexican territory. All that now remains of the
ramparts are some grassy mounds dominated here and there by the fragments of
crumbling walls. On the highest mound stood the ancient temple, and here has
been discovered a block of meteoric iron still carefully wrapped in cloth; it
was probably an object of worship, like the black stone at Mecca.

In its general outlines the State of Durango, lying to the south of Chihuahua,
presents the same aspect and forms part of the same geographical region that was
formerly comprised under the designation of Nueva Vizcaya, or “New Biscay.”
The settlers are to a large extent of Basque origin, fully as energetic and indus-
trious as their Iberian ancestors. In this part of the republic the purely European
element is more strongly represented than elsewhere in Mexico. Like Chihuahua,
Durango comprises on the west the parallel ranges of the Sierra Madre, and on
the east side vast arid and partly desert plains, Consequently here also the chief
towns are all situated in the western section along the foot of the mountains.
Durango, however, occupying a more elevated and less arid part of the plateau, is
also more fertile and relatively more densely peopled than Chihuahua; the latter
state has only two, the former from four to six, inhabitants to the square mile.

Durango, the capital, is named from the Basque town of Durango, having been
founded in the year 1551 as a strategic post in the territory of the Chichimec
Indians. Standing on a plateau 6,350 feet high, it commands a superb prospect
of the most diversified character, the view in one direction sweeping over the
gloomy ravines and fantastic gulches of the Brena, in another embracing the
highlands crossed by the highway to Mazatlan, the nearest port on the Pacific.
Durango is famous in geological records for its meteoric stones, which resemble
those found in many other parts of the Sierra Madre; one block, mentioned by
Humboldt, is said to weigh from sixteen to twenty tons. But the great geological
curiosity of Durango is its huge rock of native iron, the Cerro de Mercado, so
named from a captain whom the hope of finding gold had attracted to these regions
in 1562, and who on his return from the vain quest perished in a conflict with
the Indians. This mass of iron, which lies over a mile to the north of Durango,

102 MEXICO, CENTRAL AMERICA, WEST INDIES.

is 650 feet high, and contains above ground 460,000,000 tons of metal, enough to
supply the whole of North America for a hundred years. Like Chihuahua,
Durango prides itself on its sumptuous cathedral, and the city is dominated by an old
palace of the Inquisition. The local mint issues gold and silver coins: to a yearly
average value of about £200,000. Durango has often been called the “ City of
Scorpions,” and in 1865 a small price having been put upon these arachnidæ, as
many as 95,000 were brought to the municipality in two months.

All the other towns in the state, such as Dezquital, Guarisamay, San Dimas,
Papasquiaro, Tamazula, and Inde in the highland region, and Nombre de Dios, San
Juan del Rio, Cuencame, Nazas, and Mapimi on the lower parts of the plateau, owe
their origin and prosperity to their silver mines ; but the deposits also contain gold,
lead, and tin.

Extensive burial-grounds have been discovered in the caves amid the hills and
mountains encircling the Bolsonde Mapimi wilderness. In these graves the bodies
are buried in a crouching attitude, and are wrapped in shrouds of agave fibre over
which are wound coloured scarfs. A single cave contained over a thousand of
these mummies, nearly all of which were carried off by American explorers, and
distributed amongst various collections in the United States.

Norru-Eastern SrATES—CoaHuiILA, Nuevo Leon, TAMAULIPAS.

Coahuila, which is conterminous on the east side with Chihuahua, and which, like
it, is separated by the Rio Bravo from the United States, also resembles it in its
general relief. Coahuila has also its Sierra Madre, but on the opposite or east side,
while westwards it expands into vast desert wastes, where the running waters are
lost in saline meres or lagoons. The slopes of the mountains, which are drained
by streams descending from gorge to gorge down to the Rio Bravo, are disposed
in delightful and fertile valleys suitable for cultivating all the plants of the tem-
perate and sub-tropical zones, Yet this region has still a population of less than
two to the square mile, and till recently it was exposed to the annual incursions of
the murderous Apache and Comanche marauders. In 1879, after the complete
submission of these ferocious Indians, a large number of immigrants were attracted
to the Sierra Mojada, where auriferous silver ores, apparently very productive, had
lately been found. But the hopes of the speculators were not realised, and most of
the immigrants were compelled by the lack of water and provisions to retire from
these arid uplands. The coalfields, also, which skirt the course of the Rio Bravo,
and from which one of the Mexican riverain stations took the name of Piedras
Negras, or “ Black Stones,” are no longer systematically worked. The future wealth
of Coahuila will be derived not from its mineral stores, but from the produce of
the soil. Monclova, formerly Coahuila, which stands en a headstream of the
Salado affluent of the Rio Bravo, is surrounded by fertile plains, and long staple
cotton is grown at Santa Buenaventura in the environs.

Saltillo (£7 Saltillo or Leona Vicario), capital of Coahuila, lies at the foot of a
slaty eminence towards the south-east corner of the state, in an upland valley on
the slope of the mountains separating Coahuila from Nuevo Leon. The running

NUEVO LEON. 103

waters descending from the sierra flow northwards through a gorge in the range
to the San Juan affluent of the Rio Bravo. Saltillo was founded in 1586 by the
Spaniards, who placed here a garrison of Tlaxcaltecs to defend it against the sur-
rounding wild tribes, and from that time it continued to be the chief town of the
province, to which they had given the name of New Estremadura.

Some six miles farther south, the highway enters an angostura, or ‘“ narrow
pass,” between elevated hills, where stands the famous farmstead of Buena Vista.
From this place are named a large number of localities in the United States
in memory of the two days’ battle fought in 1846 by the Americans against the
Mexican defenders of the pass.

Monterey, capital of the State of Nuevo Leon, is one of the old cities of
Mexico, its foundation dating from the last years of the sixteenth century. The
cirque of which it occupies the centre, and which is watered by the little Rio Santa
Catalina, an affluent of the San Juan, is surrounded by mountains of a forbidding
aspect, with bare rocky flanks and craggy peaks. Southwards is continued the
chief range of the Sierra Madre; westwards is developed the Silla or ‘ Saddle”
ridge, while to the north the system terminates in a bluff which, from its peculiar
shape, takes the name of the “ Mitre.” The grey, yellow, and red flanks of the
surrounding hills rise to a height of from 1,600 to 2,600 feet above the whole town,
which is encircled by a zone of orchards and orange groves. Monterey les still
within the hot zone 1,600 feet above the sea, with long sultry summers and mild
winters free from.snow. Its annual fair, held in the month of September, is much
frequented both by Mexicans and Americans.

The well-cultivated plains of the irrigated zone in Nuevo Leon yield heavy
crops of maize, besides wheat, beans, sugar, oranges, and all kinds of fruits. From
Monterey and the other agricultural centres of the state, such as Cadereyta Jimenez,
Montemorelos, Linares, and Doctor Arroyo, Tamaulipas and the other surrounding
regions draw their supplies of alimentary produce, giving in exchange horses and
cattle. Thanks to the industry of the peasantry, Nuevo Leon, though not always
favoured with a sufficient rainfall, has flourished, and the local population has
increased rapidly. Its present density is about eight persons to the square mile,
that is to say, four times more than that of the other states of North Mexico.

Monterey forms the bulwark of the republic towards its north-west frontier :
hence in the war of 1846 the Americans began operations by seizing this strate-
gical position. Two railways converging at Monterey connect it on the one hand
through Nuevo Laredo on the Rio Bravo with the United States system, on the
other with the riverain towns of Mier, Camargo, Reinosa, and Matamoros. Thanks
to this line Monterey has become the Mexican emporium for the lower valley of the
Rio Bravo. Each of the stations on the right bank confronts another on the left
through which the American traders introduce their wares, either by legitimate
traffic or by smuggling. The two lines converging at Monterey are continued
through the republic by the grand trunk line of Mexico.

Of all the towns in the State of Tamaulipas, Matamoros lies nearest to the
mouth of the Rio Bravo. Allowing for the winding of the river, it is 48 miles

104 MEXICO, CENTRAL AMERICA, WEST INDIES.

from the sea, the coast route having had to be constructed at some distance from
the Gulf in consequence of the fringing backwaters. Matamoros is of recent origin,
its site down to the beginning of the present century being still occupied by the
hamlet of Congregacion del Refugio, that is, the “ Refuge ”” of all the French and
Mexican corsairs scouring the surrounding waters. In 1825, at the time of its
official foundation, it received its present name from one of the heroes of the |
Mexican war of independence. Soon after the annexation of Texas to the United
States, Matamoros acquired great strategic and commercial importance as a frontier
station near the coast. Its outlet near the mouth of the Rio Bravo has received
the ambitious name of Bagdad, which, however, is scarcely justified by this humble
coast village. The bar is too high and too dangerous to admit large vessels.

Beyond Matamoros, North Tamaulipas is almost uninhabited. Nothing is
anywhere to be seen except a few scattered hamlets and vast haciendas, where
thousands of horses and cattle are reared. But in the centre of the state a con-
siderable population is grouped in towns and villages, which owe their existence
to the streams descending from the Sierra Madre. This part alone of Tamaulipas,
that is, ‘‘Olive-land,”’ justifies its name. Here is Aguayo, capital of the state,
now called Ciudad Victoria. It lies on a main branch of the Santander, or Marina,
famous in Mexican history as the old Rio de las Palmas, where the fleets of Garay
and Camargo landed at the time of the conquest. Here also the ex-emperor
Iturbide attempted to re-enter the country for the purpose of again seizing the
reins of government; but having been arrested he was brought to the village of
Padilla, at that time the capital, and shot by order of the Tamaulipas congress.

The city of Tula, which lies near the frontier of the State of San Luis Potosi
and on the plateau at an altitude of 4,100 feet, is an agricultural centre, whence
large supplies of maize, beans and pimento are forwarded to the lowlands.
Although founded in the middle of the seventeenth century, Tula of Tamaulipas,
like the Tula of Hidalgo, has replaced an ancient city where have been discovered
the vestiges of temples and numerous vases, weapons, implements, and other
objects of the pre-Columbian age. .

The route leading from Tula to Tampico, after crossing a pass 4,800 feet high,
descends to Santa Barbara, beyond which it rounds the base of the Cerro Bernal,
a nearly isolated mountain of a perfectly conic shape. Tampico occupies in the
south of Tamaulipas a geographical position somewhat analogous to that of
Matamoros; it stands on a river not far from its mouth, and is surrounded by
extensive low-lying and unproductive plains. The present city dates from
the year i823, when the Spaniards still held the fortress of San Juan d’Ulua,
which commands Vera Cruz, and which consequently obliged Mexico to seek
new outlets for its foreign trade. The old town lies within the State of Vera
Cruz on a thick bank of upheaved shells, and on a shallow creek accessible only
to craft of light draft. Another Tampico occupies the site of an old Huaxtee
village amid the dunes east of the Tamiahua lagoon. The new town, though
better situated on the chief river a short distance below its confluence with the
Tamesi and six miles from the sea, is not accessible to large vessels; those drawing

TAMPICO. 105

more than eight or nine feet have to remain outside the bar, where they are
exposed to the winds and surf. But, higher up, the river is navigable for small
steamers some 30 miles above its mouth. The trade of Tampico has, at different
times, undergone great vicissitudes ; it was enriched at the expense of Vera Cruz
whenever this place was blockaded or occupied by foreign powers; at other times
it was itself deprived of its export trade in consequence of local revolts or
political strife. Recently a large share of the American traffic has been diverted
from this port by the opening of the continuous railway from the States through
Paso del Norte to Mexico; but it has again recovered its commercial importance

Fig. 41.—Tampico.
Seale 1 : 130,000

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ata Redonda ,\,
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Fathoms. . Fathoms. and upwards.

3,300 Yards.

since the construction of the railway connecting this port through San Luis Potosi
with the Mexican system. Several lines of steampackets also connect Tampico
with the other large seaports on the Gulf and in the Caribbean Sea, as well as
with New York, Liverpool, Havre and Hamburg.

Some 30 miles above Tampico, and on the right bank of the Panuco, or
“Ford,” stands the village of Panuco, formerly San Esteban del Puerto, which
recalls the memory of the Huaxtec kingdom conquered by Cortes, and so cruelly
laid waste by Nuño de Guzman. The whole district is still but thinly inhabited
compared to its flourishing condition before the arrival of the Spaniards. Higher
up on an affluent of the Panuco stands Tamquian, a town of Huaxtec origin, where

106 MEXICO, CENTRAL AMERICA, WEST INDIES.

archeologists have made numerous finds, especially of monos, or ‘‘ monkeys,” that

is, rude human figures.

INLAND STATES—ZACATECAS, AGUASCALIENTES, San Luis Porost.

The central or “inland” states, which rise in terraces towards the southern
extremity of the Anahuac tableland, are relatively to their size far more densely
peopled than the northern provinces; the greater diversity of their relief, more
abundant supply of water and more exuberant vegetation, enable them to support a
far larger number of inhabitants. Yet the same arid aspect of the northern
regions is still maintained without much modification as far as the central parts of
Zacatecas and San Luis Potosi. Numerous local names, such as Rio Salado, Salitre,
Laguna Seca, Pozo Hondo, sufficiently attest the arid nature of the soil and the
brackish quality of its waters, while many villages owe their designation of Mez-
quite or Mezquital to the thickets of thorny scrub by which they are surrounded,
The traveller arriving from the United States by the Central Mexican Railway
detects no marked change in the scenery until he reaches the town of Fresnillo.
This place stands, in fact, at an altitude of 7,300 feet, exactly on the divide between
the waters flowing north to the closed basins of the Bolson de Mapimi, and those
draining to the Pacific through the Rio Lerma.

Zacatecas, capital of the state and of the old Zacatec territory, is one of the
earliest Spanish settlements in Mexico, having been founded by Nuno de Guzman
in 1540. The city occupies a group of deep and winding gorges, which are com-
manded on the north-east by the porphyritic escarpments of La Bufa surmounted
by a citadel and a church. Zacatecas is hemmed in between other rocky ramparts
furrowed by crevasses, whence the rain-water descends in cascades to swell a rising
tributary of the Lerma. Zacatecas owes its prosperity to the silver mines of the
surrounding porphyritic and schistose mountains interspersed with quartz and
calcareous beds. Some of the lodes are extremely rich, and those of San Bernab,
worked for three hundred and fifty years, are not yet exhausted. The most pro-
ductive are usually found, not in the ravines or on the gentle slopes of the hills,
but in the steepest places and even on the jagged topmost crests. Thus the veta
grande, or “ great lode,” running north-west and south-east, three miles north of
Zacatecas, is embedded in a lofty summit 8,650 feet high, on which are perched
the dwellings and workshops of a mining village. Since 1810 the Zacatecas mint
has coined a sum of over £68,000,000 in gold and silver, and during the decade
from 1878 to 1888 the average yearly issue has been £1,150,000, almost exclu-
sively in silver dollar pieces. The little mining town of Sombrerete, lying about
125 miles north-west of Zacatecas, on the Durango road, had also its mint, which,
however, has been closed since the war of independence. At the time of Hum-
boldt’s visit the “ black lode ” of Sombrerete had yielded more metal than any other
vein in the whole of America. A village not far from Sombrerete bears the name
of Chalchihuites, or “ Emeralds,’ from the greenish stones here found, which
resemble jade, and which were highly valued by the ancient Aztecs. The Zaca-
tecas district abounds in natural curiosities. Several small lakes contain carbonate

AGUASCALIENTES. 107

of soda, aud some of these tarns are like deep natural wells with vertical walls, in
which the water rises and falls according to the seasons, but never runs dry. Hot
springs bubble up in several places, especially near the town of Ojo Caliente, south-
east of Zacatecas.

The capital of Aguascalientes (“Thermal Waters”), a small state almost entirely
enclosed in that of Zacatecas, has also its thermal mineral waters, which are sul-

phurous at a temperature of from 77° to 95° F.

Fig. 42.—Zacatecas.
Seale 1 : 110,000.

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3,300 Yards,

Near Villanueva, some 30 miles south-west of Zacatecas, stands a hill of tufa
naturally carved into circular cliffs, which give it the appearance of a fortified
plateau. This eminence is crowned with a group of structures, which must have
formerly presented an imposing effect, and amongst which archeologists have
identified palaces and other dwellings, a citadel, a temple, and a pyramid bearing
the statue of a god. But the finest remains on this “ Cerro de los Edificios”’ are
a series of steps, on which the spectators assembled in thousands to contemplate

108 MEXICO, CENTRAL AMERICA, WEST INDIES.

the public feasts and sacrifices, but where the solitary traveller now surveys
nothing but ruins overgrown with scrub. Traces of these buildings are met strewn
over a space of 70 square miles. According to Clavigero, the Cerro de los Edificios
is the famous Chicomoztoc of the Nahua legends, that is, the “Seven Caves,”
whence the Aztecs set out on their wanderings to the Anahuac plateau. Another
ancient city, formerly capital of the confederation of the Nayarit people, lies 60 miles
south-west of the Quemada, as the ruins are called, in a lateral valley of the Lerma.
Here, also, are seen the remains of a fortress and a temple overlooking the plain ;
Teul, the name of the old city, is the same as Teol, the Aztec title of the sun-god.

The State of San Luis Potosi resembles that of Zacatecas in its physical
appearance and the disposition of its two watersheds, one inclining towards the
northern depressions, the other facing the Gulf of Mexico, and comprised within
the Panuco basin. Like Zacatecas, it is also one of the most productive mining
regions in the republic. But its agricultural and industrial importance is increasing
from year to year, and these sources already yield a larger income than its argenti-
ferous ores. Even the city of Catorce, although lying in the arid northern part
of the state at an altitude of 8,850 feet, has discovered a considerable source of
wealth in the preparation of the ixtli fibre. Nearly all the silver coined in the
San Luis mint, from two to three million dollars a year, comes from the Catorce
mines. The city, which is said to take its name from the massacre of Catorce
(‘fourteen ”) soldiers, lies in a narrow gorge on a mass of rocky débris formed by
an old landslip; its foundation dates from the discovery in 1773 of the rich lodes
in the neighbouring mountain, the pyramidal double-crested Cerro del Fraile.

San Luis, distinguished from so many other places of the same name by the
epithet of Potosi, indicating its great mineral wealth, no longer deserves its title
since the famous San Pedro mine and most of the surrounding deposits have
been abandoned. The city stands on the site of the ancient Tangamanga of the
Chichimecs, in a depression on the edge of the plateau 6,230 feet above sea-level,
whence the running waters flow through the Rio Verde to the Panuco. San Luis
is so completely embowered in a zone of gardens and plantations that nothing is
visible from a distance except the domes of the numerous churches rising above
the surrounding verdure. Like Monterey, Chihuahua, and some other places, the
capital of the State of San Luis Potosi was for a time the seat of the Mexican
Government during the French invasion. It had already lost half of its popula-
tion, owing to the exhaustion of the mines to which it owed its prosperity in the
eighteenth century. The opening of the railway between Vera Cruz and Mexico
also diverted much of its trade southwards, causing a further decrease of popula-
tion. But the new line to Tampico has at last given it a direct outlet seawards,
and this cannot fail to be followed by a revival of its languishing trade and
industries. The district yields an abundance of cereals, fruits, vegetables, textile
fibres, and fermented drinks extracted from the maguey or other plants of the
same family. The citizens, noted for their enterprise and energetic habits, look
forward to the time when San Luis will take the second rank, if it does not rival

Mexico itself in commercial importance.

GUANAJUATO, 109

All the other more populous and flourishing towns of the state, such as Rio
Verde, Santa Maria del Rio, Ciudad del Maiz, are situated on the south-eastern
slopes of the plateau facing towards Tampico. The mining town of Guadualcazar,
which lies in a limestone district to the north-east of San Luis, is a decayed place,
while Salinas, to the north-west, as indicated by its name, abounds in salt-mines
and saline lagoons, the most actively worked in the republic.

GUANAJUATO, JALIsco AND Tepic, Cotima, M:cHoacan.

The political divisions of the different states are far from coinciding with their
natural limits. This is largely due to the fact that the present frontiers were
fixed by the Spanish administration according to the distribution of the tribes

Fig. 43.—San Luis Potost—Government PALACE.

and languages, religious or executive considerations, and especially the interests
of the great European or Creole landed proprietors.

Nevertheless a certain accidental coincidence may occur between the political
boundaries and physical conditions of the various provinces. Thus the four States
of Guanajuato, of Jalisco with the Tepic territory, of Colima and Michoacan,
constitute a sufficiently distinct natural region, comprising the basins of the Rio
Lerma and other streams, which flow from the western slope of the Anahuac
plateau down to the Pacific. These regions, where the hot, temperate and cold
climates are disposed in vertical order one above the other, possess a great
abundance of different products. But they do not yet enjoy the same facilities
of communication as the eastern slope of the Mexican tableland, the seaports on
the Pacific side not being yet connected with the general railway system. The

110 MEXICO, CENTRAL AMERICA, WEST INDIES.

population, however which has considerably increased during the last few decades,
is relatively dense, averaging nearly forty to the square mile.

Of these states Guanajuato, which lies nearest to the capital, is best provided
with communications and has been longest settled by the whites ; hence it is also
the richest and the most thickly peopled in proportion to its extent. Guanajuato,
its capital, stands at an altitude of 6,700 feet in a deep and narrow gorge flanked
by bare jagged cliffs, and accessible only by a single winding path. Here the
houses with their flat roofs rise one above another like a heap of dice piled up
in disorder. The mining villages are grouped here and there along the escarp-
ments, and the workshops are scattered over the terraces and in the depressions.
One of these industrial centres is the famous Valenciana, where the veta madre,
or main lode of Guanajuato, nowhere less than 30 and in some places over 160
feet thick, constitutes an enormous mass of argentiferous ores, which, between the
years 1768 and 1810, gave an annual yield of over £1,520,000. This is the
deepest mine in Mexico, having been worked down to 2,000 feet below the surface.
But since the war of independence it has been flooded, and more than one English
company has in vain attempted to resume operations, yet the lode is still supposed
to contain from £280,000,000 to £320,000,000 of silver.

Le Luz, a town lying a short distance to the north-west in the group of the
Gigante or ‘‘Giant”’ Mountains, is also surrounded by mineral deposits. At
present the Guanajuato mint yearly issues specie to the value of £950,000, of
which £160,000 in gold, the rest silver, nearly all derived from the surrounding
mines. These Guanajuato mines have become famous in physiography for the
subterranean rumblings often heard in them. In 1784 they were so violent that
the terrified inhabitants took to flight, although the underground thunders were
accompanied by no earthquakes. One of the neighbouring hills takes the name
of the Bramador, or “ Roarer.” Guanajuato is one of the historic cities of the
war of independence. Here the insurgents, aided by about 20,000 Indians and
armed only with knives and sticks, gained their first victory; the plunder was
enormous, about £1,000,000 having been taken in the citadel alone. The little
town of Dolores, whose parish priest was Hidalgo, leader of the insurrection, lies
some 25 miles north-east of Guanajuato; since the revolution it has taken the
name of Dolores Hidalgo.

Guanajuato is rivalled in population by Leon de los Aldamas, which, like the
capital, lies on an upper affluent of the Rio Lerma, but in a far more accessible
position and under a more agreeable climate, The city, which is dominated on
the north by the group of the Giant Mountains, spreads over a fertile and well-
cultivated plain at the north-west extremity of the alluvial zone, which, under the
name of Bajio, sweeps in crescent form right across the whole State of Guanajuato.
Leon, which despite its large size has never ranked as a capital, possesses nume-
rous factories,and here are specially produced the rich saddles and trappings so
much affected by the Mexican cavaliers. The railway which traverses the Bajio
zone, and one branch of which runs to Guanajuato, passes close to nearly all the
important towns of the state. Such are Si/ao, dominated by the Sierra de Cubilete,

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JALISCO. 111

and rich in silver-mines and thermal springs ; Zrapuato ; Salamanca with its cotton
mills; Celaya, a watering-place and a manufacturing centre, producing cloth,
carpets, soaps and leather. San Miguel Allende, or simply Add, another indus-
trial town, dating from the first years of the conquest, lies on a plain to the
east of Guanajuato, while Salvatierra and Valle Santiago occupy depressions
in the lake-studded plateau which stretches southwards in the direction of
Michoacan.

The Rio Lerma, which at Sa/amanca enters the formerly lacustrine basin of the
Bajio, sweeps southwards round the San Gregorio heights, and then traverses a
second very broad valley before losing itself in Lake Chapala. La Piedad and
La Barca, both surrounded by numerous hamlets, have sprung up on the banks of
the river, and in the interior towards the south stands the town of Zrllan, with its
hundreds of mud volcanoes dotted over the plain. Westwards along the banks
of the great lake there are no large towns. Chapala itself, which lies on the
north side, is an obscure place, remote from all the highways of communication.

East of this town is seen the island of HMexcal, which is identified with the
mythical Ast/an, whence the Nahuas trace their origin. In 1812 the Indians
of the surrounding shores took refuge in this island under one of their priests,
and here defended themselves for five years against all the attacks of the
Spaniards.

Guadalajara, capital of Jalisco, lies some twelve miles from the left bank of
the Lerma, at an altitude of 5,120 feet, on a plateau watered only by a few inlets.
Founded in 1542, it has always been one of the chief cities of Mexico, thanks to
its geographical position at the converging-point of the highways ascending from
the Pacific seaports towards the plateau. Its population has increased from 20,000
at the beginning of the century to over 100,000; it has thus greatly outstripped
the Spanish city from which it has been named. As a mining centre Guadalajara
cannot be compared with Zacatecas or Guanajuato ; nevertheless its mineral wealth
is considerable, for the local mint annually coins silver picces to the value of from
£240,000 to £280,000. But Guadalajara takes the second place amongst Mexican
cities as an agricultural and manufacturing centre, being noted especially for its
rebozos and other textiles, its paper, starch, cigars, metal and glass wares, and
sweetmeats of all sorts. The springs which supplied the city having proved
insufficient for the rapidly increasing population, it has been proposed to supply
it with water by a canal derived from the Rio Lerma above the Juanacatlan Falls ;
this aqueduct might also be so constructed as to furnish motive power for the
workshops of the city.

The pleasure resorts of the wealthy classes of Guadalajara are for the most
part scattered over the San Pedro hills, some miles from the city. Towards the
east the Rio Lerma, here 540 feet wide, is crossed by the bridge of Totolotlan, a
work dating from the Spanish period. Farther on the route is carried over a
northern affluent of the Lerma by the famous bridge of Calderon, where the insur-
gents met their first reverse in a battle which was long supposed to be decisive. In
the neighbourhood, between the towns of Zipotlanejo and Tepatitian, is still seen the

112 MEXICO, CENTRAL AMERICA, WEST INDIES.

ruined pyramid of a temple known as the “Cerrito de Montezuma.” On an
affluent of the Lerma, north-east of Guadalajara, stands the town of Lagos, in an
angle of the state midway between Aguascalientes and Guanajuato. Thanks to
its geographical position Lagos promises to become the common emporium of
several of the upland states; its markets are already much frequented, though to
a far less extent than the annual fairs of the neighbouring San Juan de los Lagos,
which lies at a much lower elevation in a depression of the valley. Bo/anos, a
smaller place than Lagos but formerly more important as a mining centre, also
lies on a northern affluent of the Lerma, the Rio Jerez, but in a region of difficult
access at the outlet of a formidable gorge dominated by jagged rocky walls. South

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of Bolaños and beyond the Lerma, the town of Tequila stands at the foot of a high
precipitous cliff ; this place is famous for its maguey brandy, commonly known as
tequila.

The town of Tepie, capital of a separate territory, lies like Guadalajara some
distance to the south of the Rio Lerma, thé lower course of which it may be said
to command, Its prosperity is due to the salubrity of its position, 3,000 feet
above sea-level, in the midst of gardens and orchards, and on the edge of a
voleanic plateau within sight of the Pacific Ocean. It thus serves as a health
resort for the ports of this malarious seaboard, on which are deposited the alluvia
of the Rio Lerma. When the conqueror, Nuño de Guzman, took possession of this

JALISCO. 113

region, he selected another site some twelve miles farther south, but also on the
edge of the plateau, and at the same distance from the coast. Here was founded
the town of Compostela, which was long the strategic centre of the whole of west
Mexico, but which isnow a decayed village. The old Indian city of Jalisco, which
has given its name to the state whose capital is Guadalajara, lies four or five miles
to the south of Tepic on the slopes of the igneous Cerro San Juan.

At the issue of the mountain gorges, where the Rio Lerma, called also Rio
Grande de Santiago, debouches on the low-lying coastlands, stands Santiago, now
a mere village of no maritime importance; large vessels can no longer force the
dangerous bar to ascend the course of the river to any inland port. Hence San Blas,
the present port of the Lerma basin, lies to the south of the alluvial plain, not
far from the escarpments of the Sierra de Tepic. Formerly one of the lateral branches
of the Lerma discharged into the San Blas harbour, but it was obstructed during
the war of independence, and since then it has remained closed. The port is well
sheltered from the winds; but the approach is narrow, and has a depth of less than
thirteen feet at low water. But such as it is, San Blas is the most frequented
seaport on the west coast of Mexico between Mazatlan and Acapulco. The old
town stood above the harbour on a bluff of black basalt, accessible only from the land
side. Since its destruction during the civil wars, it has remained a mere ruin
almost entirely overgrown with vegetation. The present San Blas, which lies on
the coast, consists of a group of houses and cottages shaded by cocoanut groves
and inhabited chiefly by people of colour,

Tke Rio Ameca, which discharges into Banderas Bay south of San Blas, has
given its name to the chief town in its basin. -Ameca and the neighbouring Cocu/a,
lying in an extremely fertile district studded with lakes and dried-up lacustrine
depressions, will one day present a shorter route from the coast to Lake Chapala
than the roundabout road running north by Tepic and Guadalajara. But Ban-
deras Bay is everywhere exposed to the surf, and the town of Mascota, occupy-
ing a sheltered position in a glen at the foot of the Bufa de San Sebastian cliffs,
has no haven on this inhospitable seaboard. The nearest anchorage is that of the
little port of Chamela, over 60 miles farther south.

South of Lake Chapala, the two industrial and picturesque towns of Sayula
(4,420 feet) and Zapotlan (4,320 feet), the latter called also Ciudad de Guzman,
form convenient stations on the route leading from Guadalajara to Colima. This
provincial capital, formerly Santiago de los Caballeros, was founded by Cortes in
the first years of the conquest, at an altitude of 1,485 feet, on the advanced spurs
of the hills which form the pedestal supporting the two volcanoes of “ Fire ” and
“Snow.” <A river, whose numerous feeders descend from the deep gorges scoring
the flanks of the mountains, passes to the west of Colima, irrigating its gardens,
coffee, sugar, and cotton plantations. So favourable are the conditions of soil and
climate that the plains of Colima might become one of the most productive regions
in the world under a less primitive system of husbandry.

The future railway, by which these fertile plains are to be connected with the
general Mexican system, has already made a beginning with a coastline which

114 MEXICO, CENTRAL AMERICA, WEST INDIES.

runs from Manzanillo, the port of Colima, along a strip of sand on the south side
of the Cuyutlan lagoon. This shallow basin is entirely dry during the hot season,
and it is now proposed to place it in constant communication with the sea by
cutting a canal through the narrow intervening neck of land. The port of
Manzanillo, which is developed in the rocky coast immediately to the west of this
sandy isthmus, is spacious, deep, and well sheltered from all winds except those
blowing from the west and south-west. These prevail especially during the rainy
season, from May to October, that is to say, the healthy period of the year; but
during the dry season the climate of Manzanillo is much dreaded. Some sixty
miles south-east of this plain lies the little port of Marnata, which, while quite as

Fig. 45.—MANZANILLO.
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unhealthy, is even more exposed than Manzanillo. The coast salines between
these two ports occupy during the season from 5,000 to 6,000 native hands.

The State of Michoacan is one of those regions that have long resisted assimila-
tion with the rest of Mexico. The Tarascan nation had never been subdued by the
Azteés, and their chief bore the title of “Booted” in a pre-eminent sense, because, of
all native princes, he alone had the right of wearing his boots in the presence of
Montezuma. Proud of their ancient liberties, the Tarascans had at first welcomed
the Spaniards as mere allies, and three hundred years later, during the war of
independence, no other Indian warriors displayed greater valour and steadfastness
against the disciplined troops of Europe. It was in the town of Apacingan, in one
of the low-lying fluvial valleys converging on the Rio Mexcala, that was held the

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STREET VIEW IN MORELIA.

MICHOACAN. 115

first deliberative assembly of the revolted populations. The national council was
later transferred to Zitacuaro, on the uplands between Morelia and Toluca.

The capital of the state also bears a name which recalls the great deeds of the
struggle against Spain. Under the old régime it took the designation of Vadladolia
from the famous Castilian city; but it is now better known as Morevia, from
Morelos, one of the heroes and martyrs of the insurrection. Situated at an altitude
of 6,200 feet, on the plateau in the basin of Lake Cuitzeo, Morelia lies between
two streams in a fertile valley commanded on the west by the superb Mount
Quinceo, 8,950 feet high. The city, which stood aloof from the great highways
of communication, is, nevertheless, one of the best built and cleanest in Mexico;
it is adorned with beautiful public grounds, and a fine cathedral with two towers
in simple and correct taste. |

The branch line connecting Morelia with the Mexican railway system is one
of the most picturesque on the plateau; it skirts the shores of Lake Cuitzeo, which
is everywhere encircled by. hills, grassy slopes, and woodlands. West of this
magnificent lacustrine basin, the region between the mountains and the Rio Lerma
is dotted over with other lakes, one of which mirrors in its clear waters the houses
of Puruandiro. South-west of Morelia the railway is continued in the direction of
Patzcuaro, which was the capital of the country from the time of the conquest to
the year 1541, when the Spaniards founded Valladolid. Patzcuaro had itself
succeeded in 1520 to Tzintzontsan or Huitzizila, the ‘‘ Humming-bird Town,” resi-
dence of the native ruler, which was said to have a population of 40,000. Bishop
Vasco de Quiroga removed the Christians from the old to the new town, which
stood on a neighbouring terrace, whence a view was commanded of Lake Patzcuaro
about three miles off. Tzintzontzan is now a mere village, whereas Patzcuaro has
become a populous city. The mounds scattered about the district are said to
conceal the ruins of temples and palaces. Lake Patzcuaro still stands at an alti-
tude of 7,260 feet ; bat from this point the traveller soon reaches the edge of the
plateau, whence the route descends rapidly to the coast through the towns of
Tucamburo, Ario, Uruapan, and some other places situated in the lateral valleys
of the Rio Mexcala. Near Ario, at an elevation of over 6,700 feet, and within
sight of the summit of the Tancitaro voleano, stands the village of Caninzio, tili
recently inhabited by a group of French settlers, who acclimatised in the district
numerous species of fruit trees, flowering, and other ornamental plants. The wine
made in the colony of Francia, or “ Little France,” was famous throughout
Mexico. But the invasion of the country by the French troops in 1864 excited the
natives against the foreign settlers, who were obliged to disperse. The so-called
ayacates, or sepulchral mounds, erected by the ancient Tarascans are scattered in
hundreds round about Ario.

QuERETARO, Hipatco, Mexico, FEDERAL District.

The various states occupying the Anahuac plateau properly so called, and
draining through fissures in the mountains to both oceans, but mainly to the Gulf
of Mexico, constitute collectively the most productive, the richest and most

116 MEXICO, CENTRAL AMERICA, WEST INDIES.

densely-peopled region in the republic. Here the population is in the proportion
of about 64 to the square mile, so that the centre of gravity of the Mexican
nation has not been shifted since the epoch of Toltec. civilisation, that is to say,
for a period of at least a thousand years. This centre, however, could scarcely be
removed to any other region, such as Durango and Zacatecas, possessing greater
mineral resources, or Michoacan and Oaxaca, enjoying the advantage of a more .
exuberant vegetation ; for the Anahuac tableland has the still greater advantage
of being the natural converging-point of all the routes coming from the north
between the Mississippi and the Rocky Mountains, while at the same time com-
manding like a citadel both slopes of the country.

The State of Queretaro, where rise the first headstreams of the Panuco, is of
relatively small extent. Its northern section, also, where are situated the towns
of Jalpan, Toliman, and Cadereyta, is but sparsely peopled, most of the inhabitants
being concentrated in the southern division, where begin on the one hand the
great plain watered by the Bajio tributary of the Rio Lerma, and on the other the
headwaters of the Rio San Juan, a main branch of the Panuco. In this valley lies
the town of San Juan del Rio, a delightful “ city of gardens.” Queretaro, which
gives its name to the state, is situated at an altitude of 7,000 feet, close to the
waterparting between the two slopes. Its foundation is attributed by historians
to the Otomi people; but although it is said to date from the middle of the
fifteenth century, all its buildings are of Spanish origin. Of these the most
remarkable is an aqueduct of seventy-four arches, rising about 80 feet above the
ravine. A reservoir, recently constructed above the city, contains a volume of _
over 35,000,000 cubic feet of water. Queretaro is one of the industrial towns
of Mexico, being noted especially for its soaps, cigars, and cotton yarns; the
spinning-mills occupy thousands of native artisans. About half a mile west
of the city is situated the Cerro de las Campanas, on the slope of which is the
little monument of three stones, indicating the spot where the ill-fated emperor
Maximilian and his two generals, Miramon and Mejia, were shot in 1867.

The state bearing the name of Hidalgo, in memory of the priest who first
summoned the Mexicans to rise against Spain, is of recent formation. Here the
towns, such as Zimapan, Jacala, Mextitlan, and Huejutla, the ancient city of the
Huaxtec nation, all stand at considerable distances one from the other. Thus
the population is centred chiefly in the extensive fertile plains of the south, which
are enclosed by a highly productive hilly mineral region. Here lies, not far from
Actopan and the fantastic “Organ” Mountains, the capital, Pachuca, an ancient
city, now connected by a branch line with the Mexican railway system; in the
neighbourhood are the gold and silver mines, which were already worked by the
natives in pre-Columbian times. The mining district of Regla, between Pachuca
and Atotonilco, has become famous under the name of Real del Monte, recently
changed to Mineral del Monte. Vast quantities of silver were extracted from these
deposits before the mines were ruined by inundations and the burning of the
surrounding forests. Since the war of independence, the works have been
reopened by Cornish master miners, who now employ thousands of native hands.

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‘MOIA 'IVAANHO—-V'INL AO ALTO

HIDALGO. 117

These enterprising English speculators have introduced some very powerful
machinery, which enables them to supply the Mexican mint with the largest part
of the metal it now coins. Pachuca lies about midway between the two ancient and
powerful cities of the Toltec people, Tulancigo and Tula. The former, that is,
« Little Tula,’’ which is said to be the oldest, stands at the foot of a volcano east
of the present capital, near the eastern verge of the plateau. Before the conquest
the natives worked into all kinds of cutting instruments the obsidian collected on
the neighbouring Cerro de las Navajas, or “Mountain of Knives.” These
quarries and workshops seem to have sufficed for the wants of the whole of the
Anahuac plateau from prehistoric times down to the arrival of the Spaniards.
Tula, the ancient Tollan, is now a mere village, situated in the charming district
traversed by the railway running from Mexico to Queretaro. Here, also, are found
the remains of animals, arrowheads, and other implements in great abundance ; but
a more interesting discovery is that of the ancient buildings brought to light by
M. Charnay, on the summits of mounds or hillocks commanding an extensive
view of the surrounding plains. The ruins are supposed to represent all that now
remains of several ancient temples, and of a palace. It is noteworthy that the
architects of Tula employed the most diverse materials, wood, stones, pebbles,
cement, mortar, and even the true baked brick, but not the adobes, or sun dried
bricks, which were so extensively used by the Aztecs.

The State of Mexico has been shorn of its former proportions, and in a sense
dismembered, by the detachment of Hidalgo in the north, and Morelos in the
south. Moreover, the ‘“ Federal District ” which encircles the capital forms a
distinct enclave within the state, being administered, like the district of Columbia,
in the United States, directly by Congress. But although thus reduced to less
than half its original size, it still constitutes an extensive territory, which might
even admit of further subdivision by separating the districts lying south of the
snowy range on the slope which drains through the Rio Mexcala to the Pacific.
Nearly all the mountainous parts are uninhabited, except in the mining regions,
such as the environs of Jrt/ahuaca. Nevertheless, the population is relatively
very dense, especially towards the eastern extremity of the state, which, so to say,
forms the suburbs of the federal capital. TZv/uca, the state capital, is not an
important place, its development having been retarded by its great elevation of
8,600 feet, rigorous climate, and lack of communications. Lerma, some eight
miles farther east, on a lake traversed by the headstream of the Rio Lerma,
occupies a position analogous to that of Toluca. Round the corn-growing
“valley” rises an amphitheatre of hills, dominated southwards by the Nevado
de Toluca volcano, whose long slupes are flecked or draped in snow towards the
summit. The pass running east of this mountain is guarded by the town of
Tenango, near which is a romantic waterfall. On the opposite slope the chief
places are Tenanciigo, or “ Little Tenango,” Tejupilco, and Temascaltepec.

Mexico, capital of the republic, still bears its Aztec name, which has been
variously interpreted by etymologists, but which is usually derived from one of
the appellations of the war-god Mexitli. Nevertheless, the city was more com-

118 MEXICO, CENTRAL AMERICA, WEST INDIES.

monly known, even during the first years of the Spanish conquest, by the name
of Tenochtitlan, or “ Nopal Stone ;” in fact, its arms, now adopted by the republic,
represent a stone rising above a lake, and bearing a nopal tree, on which an
eagle has alighted. The European city has sprung up precisely on the site of
Montezuma’s capital. During the siege of Mexico, Cortes systematically destroyed
every block of buildings, in order to deprive the advancing enemy of all cover.
But when he rebuilt the city in 1522, he followed exactly the original plan, street
for street, quarter for quarter, every Spanish barrio thus succeeding every Mexican
calpulli. The centre of the ancient city in this way became the great plaza, or
square, and the cathedral rose on the site of the chief temple dedicated to the god

Fig. 46.—Ancrent Mexico.
Seale 1 : 400,000.

H-ENOCHTITLAN

BY MEXICO

West of Greenwich

6 Miles.

of war. The city of Tiatelolco, which had originally formed a sort of trading —

quarter distinct from the military city of Tenochtitlan, was also absorbed in the
New Mexico. It stood on the ground at present occupied by the northern quarter.
But although standing on the site of the ancient Aztec capital, the aspect of the
modern Mexico has been so completely changed that its former inhabitants could
no longer recognise it. Tenochtitlan was essentially a lacustrine city, entirely
surrounded by water, and connected with the mainland by causeways and embank-
ments. But the waters have now subsided sufficiently to leave the new capital
high and dry, and even surrounded by a grassy zone. The causeways formerly
traversing the lake have become highways, and the canals in the interior have
been filled up and transformed to avenues. Seen from a distance, the federal
capital presents an imposing appearance. This white city, overtopped by domes

Se UE A

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MEXICO ANDITS VALLEY.

Stink Baoan
"4

APULCO 4]

4 “7 nif ?, mi Y

An ed té à
West of Greenwich

Seale, 1450000
i) 12 Miles.

NEMWMORE 4D: APPEETON &/€°

Fig. 47.— Carmenraz or Mexico.

CITY OF MEXICO, 119
and pinnacles, spreading widely over the vast plain, and bounded in the hazy

TENTE

———— a ———_—_—_—_—E

distance by an amphitheatre of majestic mountains, harmonises completely with

120 MEXICO, CENTRAL AMERICA, WEST INDIES.

the natural environment. The traveller, viewing it from some commanding site,
might well be tempted to exaggerate the part played in history by a city occupying
such an imposing position. ‘“ We stood rapt in amazement,” exclaimed Bernal
Diaz. ‘ We declared that the city resembled those enchanted abodes described in
the book of Amadis, and some of our men asked whether the vision was not a
dream.”

Mexico is laid out with great regularity, the streets, mostly too narrow, being
disposed at right angles, like those of Chicago and Philadelphia; but this monoto-
nous arrangement is somewhat broken by the squares and gardens occurring at
intervals. The houses, with their terraced roofs and inner courts like those of
eastern cities, are solidly built with a yellowish sandstone, or a red lava called
tezontle, and are usually of only one storey, the better to resist the slight but some-
what frequent earthquakes. In the centre of the city is situated the great square
(plaza), where are celebrated all public solemnities, and where converge the currents
of business and pleasure, alternating with the hours of the day. On one side of the
square stands the cathedral, which replaces the church erected by Cortes on the
spot where stood the feocalli, or temple of the war-god, ever reeking with the blood
of human victims. The very pillars of the new edifice rested on the great idols, in
order that they might be for ever crushed by the indestructible column of the holy
Christian religion. The present church, which took nearly a century to build, is
a sumptuous monument of imposing appearance, and to it is attached the Sagrario,
another church with a fagade as luxuriously carved and sculptured as a Hindoo
palace. A second side of the plaza is occupied by the National Palace, which is
said to have been erected on the site of Montezuma’s palace. It is a vast building,
with a frontage considerably over 220 yards long, and containing the senate, the
Government offices, the ministries, besides the post office, museum, and library.
The other two sides of the square are skirtcd chiefly by houses with portales, or
arcades, where there is a constant movement of loungers, pedestrians, and itine-
rant dealers. In the middle of the square is the fine promenade of the Zocalo, or
“ Socle,” shaded with the eucalyptus, and adorned with flower beds, fountains,
and statues.

In the Mexican museum are preserved valuable natural history collections,
amongst which are those fossils which the conquerors supposed to be the “ bones
of giants,” but which are now known to be the remains of large animals belonging
to the quaternary fauna. Still more interesting is the archæological collection,
comprising such antiquities as escaped the iconoclastic fury of the first conquerors
and the research of foreign collectors. Here is the precious “‘ Mexican Calendar,”
on which is sculptured the division of time according to the ingenious Aztec
system. It isa huge block weighing 21 tons, which must have been brought
from a great distance, for no rocks of the same geological formation occur in the
neighbouring mountains. The “Stone of Tizoe ” (p. 71), which represents the pro-
cession of people vanquished by that hero, and which was long supposed to be the
“stone of sacrifice ?” belonging to the great temple, is another treasure preserved
in this museum, where may also be seen the hideous statue of Huitzilopochth,

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GENERAL VIEW OF MEXICO.

CITY OF MEXICO. 121

“ood of war,” hieroglyphic paintings, Montezuma’s shield, and the effigies of
several deities. Every year adds to the contents of the National Museum, and
systematic explorations made in the ground, and especially in the lacustrine
depressions, cannot fail to reveal numerous other treasures. Mexico already
possesses some large scholastic establishments, notably a school of medicine now
installed in the old palace of the Inquisition, and a preparatory school occupying the
old convent of the Jesuits. Aztec literature is studied in a college founded for
the Indians; several learned and literary societies publish useful memoirs; the
chief library has over 150,000 volumes; the picture-gallery is one of the richest
in the New World.

The population of Mexico has increased fivefold since the beginning of the
century; nevertheless it has already been outstripped by many cities of more
recent origin. A hundred years ago it was the largest place in the New World ;
now it is exceeded not only by New York and several other cities in the United
States, but also by some of its rivals in Latin America. Nevertheless, Mexico,
situated on the “bridge of the world” between the two oceans, is assuredly one
of the vital points of the planet one of those points whose historic importance
cannot fail to advance with the general progress of the world. It has doubtless
lost the trade between the Philippines and Spain which it had formerly enjoyed
through colonial monopolies ; but on the other hand the internal traffic has greatly
developed. Bernal Diaz already remarked that “no European city possessed a
market comparable to that of the Anahuac capital; at least none possess such a
fruit market, where are seen in abundance the products of every zone—cherries and
pears side by side with pineapples and bananas.’’ One of the most curious sights
in Mexico is that presented every morning on the Viga Canal by the flotillas of
boats ladened with flowers, fruits and vegetables. The wholesale import trade is
almost entirely in the hands of English, American, German, French and other
foreign traders, These industrious strangers have nearly all acquired a position of
comfort, while the native population of mendicants, /eperos, pelados or pordioseros,
still swarms in the suburbs.

Despite the pure air descending from its snowy mountains, Mexico is not a
healthy place. The mortality, which in certain years has exceeded the births
four times, averages from 32 to 33 per thousand, which is much higher than
that of London, Paris, and most other cities of West Europe. This high death-
rate is due mainly to the impurity of the soil and waters. Mexico stands only a
few inches above the level of Lake Texcoco, with a subsoil of impermeable argil-
laceous deposits: hence the least excavation on the surface of the ground beconies
at once flooded with a brackish water saturated with organic substances. The
gradual upheaval of the bed of Lake Texcoco threatens destruction to the city, which
has already been more than once laid under water. After every downpour, the
streets are filled with slush, and when the rains iast long enough the whole place
becomes transformed to a swamp or even to a veritable quagmire. The roadways
are also badly kept, while the drains, flooded with an almost stagnant water, con-
tribute much to the putrefaction of the suil. “The city is threatened with asphyxia,”

122 MEXICO, CENTRAL AMERICA, WEST INDIES.

is an expression occurring in a report on the sanitary state of the place But if
foul water abounds in Mexico, the pure water brought from a distance by
aqueducts is far from sufficient for the wants of the people; in 1882 it was scarcely
880,000 cubic feet per day, or less than twenty gallons per head of the population.
The drainage of the subsoil itself presents grave difficulties; by carrying off the
overflow, which gives consistency to the marshy ground, the buildings are apt to
lose their centre of gravity and to topple over at the least vibration of the surface.
The gradual drying up and shrinking of the land has already caused rents and
fissures in most of the large structures, while others have sunk several feet in the

Fig. 48.—Mexico AND 11s ENVIRONMENTS.

Scale 1 : 120,000

ae CaN a
+2 Pantaco : X =":
SAS ae

"Magdalena “

+. Calpatitian *

3, 300 Yards.

ground. It is now regretted that, in order to secure his triumph, Cortes decided
to rebuild the city exactly on the site of the old capital, and ay the foundations of
his churches on the temples of the gods, instead of selecting a new position on the
more elevated land which stretches westwards to the neighbouring mountains.
The wealthy quarters, however, are already stretching out in this direction. Certain
villages, such as Casablanca and Tucubaya, where the national observatory has been
established, are gradually expanding and becoming connected with the capital by
avenues lined with buildings. Mexico is thus steadily moving westwerds towards
the less tainted rising grounds. The city is adorned with some fine promenades,
such as the Paseo and the Alameda, where a fountain indicates the site of the
of the Inquisition. Victims of

”

ancient Quemadero, that is, the “ burning-place,

‘SHSSHHAXIO OWdALTAdVHO AHL

ENVIRONS OF MEXICO. 123

this horrible institution were especially the “heretical” sailors captured by the
Spanish cruisers.

Mexico is rapidly growing along both sides of the road leading to Tacuba,
which replaces the old highway by which the Spaniards made their disastrous
retreat during the Noche Triste or “Sorrowful Night.” Near the village of
Popotla is still seen the old cypress under which Cortes sat vainly awaiting the
arrival of over 400 of his men, whose bodies lay heaped up in the gory mud at
the breaches of the causeway. Round about this historic tree stretch vast
marshy gardens, and farther on are seen the houses of Tacuba. Under the name
of Tlacopam this place was formerly one of the three cities of the Nahua confede-
ration. Farther north, on the road leading to the desagüe of Huehuetoca, stands
Cuautitlan, the “ Kagle-town,” which gave rise to the Mexican saying, “Beyond
Mexico naught but Cuautitlan,” meaning that except Mexico there was nothing
in the world worth seeing.

A superb avenue shaded with eucalyptus-trees leads from the capital to the
porphyritic eminence of Chapu/tepec, or “ Mountain of the Cicada.” This avenue
is lined with statues, one of which commemorates the last Aztee king, Guatimozin,
‘heroic in the defence of his country and sublime in his martyrdom,” burnt alive
by the infamous conquistadores. On the rock of Chapultepec formerly stood
Montezuma’s suburban residence, which has now been replaced by a palace of vast
size. This huge pile was erected in the last century by the Viceroy Galvez, with
the intention, said his Mexican subjects, of making it a stronghold from which
to proclaim his independence as Emperor of Mexico. The palace, a part of which
has become the military school, commands from its terraces the finest panoramic
view of the capital with its lakes and encircling mountains. The surrounding
promenades are also the’ most umbrageous on the Anahuac plateau. Here are
found the gigantic “‘cypresses”’ (cupressus disticha), or ahuehuetes, that is, “Old
Men of the Waters,” which already existed before the arrival of Cortes. Some
of these giants of the vegetable kingdom, with their wide-spreading branches and
foliage shaped like a “Spanish beard,” have a girth of 50 and a height of 160
feet. At Churubusco, a little to the south of this place, the Americans gained the
decisive victory which made them masters of the capital in 1847. The following
year was signed the treaty of peace of Guadalupe Hidalgo, by which half of the
national territory was ceded to the United States.

The aqueduct, which is fed by the various springs from the mountains south-
west of Mexico, supplies both the Chapultepec gardens and the aristocratic suburb
of Tacubaya, whose villas are dotted over the district south of Chapultepec.
From this place excursions are made round about to San Angel, to the picturesque
group of hamlets nestling in the valleys of Mount Ajusco, and to the pedregal,
or lava streams, which have flowed from this voleano, but which are now over-
grown with cactus and brushwood. TZva/pam, famous as a place of pilgrimage,
hes in a deep ravine between two masses of scoriæ; it was through this ravine
that the Americans penctrated into the valley of Mexico.

North-east of the capital the Tepeyacac heights, source of a spring of ferru-

124 MEXICO, CENTRAL AMERICA, WEST INDIES.

ginous waters, are crowned by the church of Guadalupe, formerly one of the
richest in the world, but now spoiled of its treasures by the National Government.
The Virgin of Guadalupe is the special patron of the Indians, while Our Lady
de los Remedios was formerly regarded as the tutelar saint of the Spaniards.
Under the old régime an incessant struggle was carried on between the devotees
of the two sanctuaries; but the war of independence secured the definite triumph
of Guadalupe, so that religion and patriotism are now merged in a single cult.

On the west side of Lake Texcoco, east of the capital, a voleanic eminence
rises above the saline waste, which is made a receptacle for the refuse of the

Fig. 49.—TLALPAM AND Lake XOCHIMILCO.
Scale 1 : 190.000.

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neighbouring towns. The Peñon de los Baños, as this eminence is called, is the
source of a copious ferruginous spring, and here geologists have found some
fossil human remains.

The Viga Canal, whose waters reach the capital at its south-east extremity,
is derived from Lake Xochimileo, or the “ Flower-garden,” one of the southern
basins of the Mexican valley. This canal traverses a low-lying district cultivated
by Indian market-gardeners, and their plots are commonly designated by the
same term, chinampas, which was also applied to the floating islands of the Aztecs,
formerly moored in hundreds on the surface of Lake Texcoco. But Lake Chalco,
or the “ Emerald,” forming an eastern continuation of Xochimilco and encircling
a cone with a perfectly regular crater, bears in this respect a much more close

ENVIRONS OF MEXICO. 125

resemblance to the Texcoco of Montezuma; in the middle of the marshy depres-
sion may still be seen numerous other chinampas, resting on matted beds of
aquatic plants and covered with soil brought from a distance. But these plots,
which are intersected by acalotes, or trenches, are not supported by movable
rafts; on the contrary, they gradually form compact masses attached to the shore
and steadily encroaching on the lacustrine basin. Jixtapalapa, or “ White Town,”
formerly a great Mexican city with “fifteen thousand houses,” according to Cortes,
stands near the head of the Viga Canal at Lake Xochimilco, under the Estrella

or “Star” peak, famous in the religious history of Mexico. Here the priests

Fig. 50.—Inp1an MARKET-GARDENER’S CANOE.

assembled at the end of every cycle of 52 years in order to keep up the succession
of time by solemnly opening a new cycle. Fac'ng the capital at a distance of
sixteen miles in a straight line on the opposite side of the lake is seen the now
obscure town of Texcoco, which preceded Mexico and which was long its rival.
Texcoco was the ancient residence of the Toltec chiefs and the ‘“ Athens”’ of
Anahuac, for here the Nahuatl language was spoken in its greatest purity and
elegance. Texcoco has the advantage over Mexico of being built on healthy
ground above the level of the highest inundations. The Puerto de las Brigantinas,
that is, the spot where Cortes built a flotilla to reduce Mexico, lies now consider-
ably over a mile from the margin of the lake. North of Texcoco stands the
still more ancient city of O/wmba, formerly Otompan, which would appear to have

126 MEXICO, CENTRAL AMERICA, WEST INDIES.

been the capital of the Otomi nation before the arrival of the Toltecs on the
Anahuac plateau; it was on the plains of Otumba that Cortes by a decisive
victory repaired the disaster of the “Sorrowful Night.” Otumba and its eastern.
neighbours, Jo/o and Apam, surrounded by the most productive maguey planta-
tions in the republic, are important strategical points guarding the entrance to
the plains north of the snowy Ixtaccihuatl range. The migrations of conquering
or vanquished peoples must for the most part have passed through ‘this gateway,
the possession of which was in former times frequently contested. But it was
avoided by Cortes, who boldly ventured to cross the great range directiy by the
Ahualco pass between Ixtaccihuatl and Popocatepetl. Practicable tracks may
also be found by rounding the southern flanks of this mountain through the
village of Amecameca, which encircles the old eruptive cone of Sacro Monte, now
overgrown with oak-trees. Near the gorge of Apam, or between Texcoco and
Otumba, there still stand two temples which are supposed to have been erected
by the Totonacs; these are the two pyramids of Teotihuacan (Teutlihuacan), or
‘ Abode of the Geds,” which are known as the ‘‘ House of the Sun” and “ House
of the Moon.” Reduced to the condition of mere mounds overgrown with agave
and thorny scrub, they are now difficult to recognise as human structures. Never-
theless the explorations made on the spot leave no doubt as to their artificial
character. The first or southern pyramid is the broadest and highest, forming
a square of 700 feet and 180 feet high; the second, that of the Moon, is both
much smaller and 36 feet lower, and both face the cardinal points, though not
with mathematical accuracy.

Farther south other mounds are scattered over the plain, in some places
numerous enough to form avenues, such as the ‘“ Way of the Dead,” so named
either because these knolls are really old burial-places, or because it indicates the
‘route formerly followed by the processions of human victims on their way to the
sacred slaughter-houses. East of Apam the plateau rolls away to the southern
foot of a border range inhabited by a population of Totonac miners, who are
chiefly grouped round the towns of Zacatlan and Tvtela del Oro, On this plateau
stands the town of Taxco, and farther south in a narrow glen is seen Tlaxcala,
formerly capital of the brave republic which espoused the cause of Cortes against
Montezuma. At present it is the chief town of a small state, which about coin-
cides with the limits of the old republic, and which is dominated eastwards by
the .Malinche voleano. But Tlaxcala is no longer the great city which could at
one time marshal 100,000 warriors against the invader. Another decayed
Mexican city is Huevrotzingo, which was founded by the Olmecs, and which is
constantly mentioned in the reports of the conquerors.

In this district the most important place at present is Pucbla de los Angeles,
“ Angel Town,” which was built by the Spaniards on an uninhabited plain in the
year 1530 asa residence for those whites who had been left unprovided for in the
distribution of offices after the conquest. This flourishing city, capital of a thickly
_ peopled state on the plateau and the first slopes facing the Pacific and Atlantic,
is sometimes called the “ second capital of the republic.” Under the ephemeral

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PUEBLA, CHOLULA. 127

reign of Maximilian there was even a question of removing the administration to
Puebla, which enjoys a far more healthy climate and lies in a more fertile region
than Mexico. It stands at an altitude of 7,160 feet, that is, something less than
the federal capital, on an inclined plain, whose rapid streams flow westwards to
the Mexcala, which winds away to the Pacific. All these rivulets are fed by the
melting snows, and serve to irrigate the surrounding plains, which yield abundant
crops of all sorts. Dominated by the two square towers of its sumptuous cathedral
and by the belfries of over fifty churches, Puebla was formerly inhabited by a
fanatical population extremely hostile to strangers ; more than once travellers had
to. seek the protection of the troops to avoid being stoned as “ Englishmen,”
“ Jews ” or “ heretics.”” The place is noted especially for its vebozos, or scarfs, its
cotton yarns, and for the preparation of little figures in wax or alabaster, sculptured
vases, Onyx stands, and similar objects connected principally with church decora-
tion. Lying about midway between Mexico and the edge of the plateau, Puebla
formerly stood on the main route of nearly all the transit traffic between the inte-
rior and Vera Cruz. But it has lost this commanding position since the opening
of the main railway from Vera Cruz to the capital, though still connected with
the general system by branches running eastward, west of the Malinche volcano.
Puebla owes its prosperity to its great agricultural resources. It also promises to
become a much-frequented health resort, especially for strangers suffering from affec-
tions of the chest; in the neighbourhood are copious sulphurous thermal springs,
which probably owe their special properties to the volcanic deposits of Popocatepetl.
The two steep hills of Guadalupe and Loreto, rising north-east and north of Puebla,
recall the two most important military events in the modern records of the nation.
During the war undertaken against Mexico for the restoration of the monarchy,
General de Lorencez, after forcing the passes and reaching the edge of the plateau at
the head of 6,000 men, had sent off a despatch announcing that he was already “master
of Mexico.” But right in front of Puebla he found the route blocked by a force
of 12,000 troops, under Zaragoza, which held possession of the city and of the two
fortified convents on the hills. The attack made on May 5th, 1862, ended in failure,
and the French invading army had to retreat to the lower slopes of the plateau.
Next year an army 20,000 strong again advanced on Puebla, and began a
regular siege of the place. The investment lasted 62 days, during which the
Mexican garrison defended every post and station, yielding only after exhausting
ammunition and supplies, and then partly dispersing to join the troops that held
the plains.

Although a large place, Puebla is still inferior in size fo the famous city of
Cholula, which formerly stood in the neighbourhood. ‘This holy city of the Olmecs
and later of the Aztecs, at one time centre of the textile and pottery industries
of Anahuac, and founder of the colonies as far south as Nicaragua, is now an obscure
village and railway-station eight miles from Puebla on the opposite side of the
deep gorge traversed by the Rio Atoyac. Churultecal, as Cortes calls it, is described
by him as containing 20,000 houses in the central part, and an equal number
in the outskirts. “From the summit of one of the temples,” he adds, “I

128 MEXICO, CENTRAL AMERICA, WEST INDIES.

have counted over 400 towers, all belonging to other sanctuaries.” But a
few days after contemplating this panoramic view, the conqueror began the
work of destruction by fire and sword. Of the 400 temples nothing now
remains except a few shapeless mounds covered with vegetation. But one of
these lying to the south-east of the city is a veritable hill of bricks and layers of
earth, as shown by the explorations and the cuttings made for the road and the
railway passing at its foot. According to the local tradition this hill was con-
structed by order of a giant in honour of the god Tlaloc, who had saved him from
a deluge, and all the bricks used in the building were passed from hand to hand
by a string of workmen reaching all the way from the slopes of Popocatepetl
to Cholula. Its present height, though greatly diminished as shown by the
irregular sky-line, is 175 feet above the plain, while its enormous base covers an

extent of 42 acres, nearly four
Fig. 51.—Puesra 1N 1862.

SO UN times more than that of the

pyramid of Cheops. No other
isolated human monument
S-Felipe approaches these, vast propor-
tions. The platform on the

NVallarino

Roh? de St? Maria®
summit, where the chapel of

Our Lady de los Remedios
now replaces Quetzalcoatl’s

Rancho de Posadas

temple, has an area of about
5,000 square yards, forming a
etes stupendous esplanade whence
Grn pe, Le > Des. Ù the eye giances from the vil-
F esas ; “i lage and gardens of Cho-
HE delaNoria EE LA lula to the glittering domes of

. SIN es eee Puebla, from the forest-clad

slopes of Malinche to the snows

of Popocatepetl.
Before the construction of

2,300 Yards.

the Vera Cruz railway Puebla
had as its outpost towards the Atlantic the town of Amozoc, at the converging point
of the roads to Jalapa and Orizaba. Tepeaca, a little farther on near the outer ram-
parts of the plateau, also possessed great strategical importance, and Cortes himself
had chosen this place as a stronghold and Spanish colony under the name of Segura
de la Frontera, ‘Safeguard of the Frontier.” Next to Vera Cruz, Tepeaca was the
earliest Spanish foundation in Mexico. This angular corner of the plateau has
suffered a loss of trade since the main line of the Mexican railways passes farther
north by Huamantia and San Andres de Chalchicomula, the station dominated by
the cone of Orizaba. Near Chalchicomula, on the very edge of the plateau, the
station of Esperanza lies about midway on the main line between Mexico and
Vera Cruz. Although occupying a part of the plateau draining to the Paciñc,
neither Pucbla nor Cholula is connected by railway with that ocean. But the

VERA CRUZ. 129

locomotive has already descended to the temperate zone on this slope, reaching
Matamoros de Izucar through Atlixco, where is seen a cypress 74 feet in circum-
ference. Towards the south-east angle of the state another line runs from the
plateau down to Tehuacan, or Teotihuacan, “City of the Gods,” whose sumptuous
temples were compared by the Spaniards to the palaces of Grenada.

VERA CRuZz.

This state occupies all the hot zone skirting the Gulf of Mexico, besides a part
of the temperate lands, from the Rio Panuco to the Rio Tonala beyond Coatzacoalcos.
It thus extends north-west and south-east a total distance of about 410 miles. Despite
the marvellous fertility of its upland districts, which lie half-way up the slope, and
are well exposed to the fogs and rains of the Atlantic, Vera Cruz is not one of the
populous states of the confederacy ; within its limits are comprised some forest
lands, as well as sandy, desert, or marshy tracts. The capital has often been
di-placed, and the city which gives its name to the state was itself for some years
the seat of the government. Orizaba also, fur a time, held the same position,
which at present is enjoyed by Ja/apa. This place stands on the slope of the
extinct Macuiltepec volcano, which is furrowed by deep gorges. Formerly it
occupied the rim of a plateau, also scored by eroded gullies. But according to
the local tradition, the inhabitants of this first Jalapa were so decimated by the
epidemic of 1547 that they left the place in a body, and settled a little distance
off on a sunny slope on the opposite side of a neighbouring gorge. The new city,
with its regular streets winding amid the gardens, is one of the healthiest places
in Mexico. From its superb avenues is unfolded a magnificent prospect, embracing
on the one hand the forest-clad heights of the Cordillera from the Orizaba peak
to the Cofre de Perote, on the other stretching over the orchards and meadows of
the meandering Rio San Juan valley, and again in the far east to the strip of dunes
fringing the blue Atlantic waters. Although a small place, Jalapa is one of the
most important historic cities in Mexico. It occupies a station which is indispens-
able to all invading armies, to all travellers and traders journeying between the
coast and the plateau. Formerly, when the commercial monopoly belonged to
Cadiz, and when the trade with Europe was limited to a fleet forwarded every four
years, Jalapa was the great market-place for the distribution of the imports and
the purchase of Mexican produce ; hence its title of Jalapa de la Feria, or, as we
should say, “ Market-Jalapa.” It has now lost this commercial rôle, but it is still
a health resort, at once a hospital and a convalescent home for the people of the
lowlands. The yellow fever has never reached Jalapa, which as a sanatorium is
not only extremely salubrious, but also possesses in the neighbourhood numerous
efficacious mineral waters, hot and cold, saline and sulphurous. The numerous
products of the district surrounding Jalapa, Ciudad de las Flores, “ City of Flowers,”
fruits, cereals, and vegetables, serve mainly fer the local consumption ; it exports
little beyond its medicinal plants, especially the root of ipomea purga, which bears
the name of this place. The plant is collected by the Indians of the surrounding

130 MEXICO, CENTRAL AMERICA, WEST INDIES.

communes, especially Chiron-Quiaco, a village which lies 20 miles farther north,
and the products of which are the most highly esteemed.

Jalapa is connected with the Mexican railway system by a branch which skirts:
the north side of the Cofre de Perote, and then traverses the little town of that
name. Here is a magnificent and apparently impregnable citadel, which was
built at a great expense by the Spanish viceroys for the purpose of guarding the —
highway between Vera Cruz and Mexico. Merely to keep it in repair cost over a
million dollars yearly. Butit may now be easily turned, and the citadel of Perote,
deprived of its strategic importance, has been transformed to a state prison.

Coatepec, which lies in the midst of erehards and plantations some nine miles
south of Jalapa, is also a favourite resort of the coast people. But the little
centres of population following lower down in the direction of Vera Cruz already
lie within the dangerous zone which is yearly visited by yellow fever. Several of
these places have an historic name, having been the battleground of armies con-
testing the possession of the routes leading up to the plateau. Amongst them is
the Cerro Gordo, the passage of which was forced by the American troops in 1847.
Lower down is the Puente Nacional, formerly Puente del Rey, a monumental bridge
which crosses the deep barranca of the Rio Antigua. South of Jalapa and Coatepec
several other towns occupy positions on the escarpments of the plateau analogous
to that of Jalapa itself. The roads which here creep up the slopes at heights
varying from 2,800 to 4,000 feet, are scarcely rivalled in the whole world for
their magnificent views and endless variety of scenery. On emerging from the
leafy avenues formed by the overhanging branches of conifers and other forest
growths, the traveller suddenly beholds snowy Orizaba and surrounding ranges,
with their spurs, terraces, wooded lava-fields, and the lower plains extending in
the hazy distance down to the curved margin of the blue Atlantic. The flanks of
the mountains are furrowed from base to summit by gloomy gorges several
hundred yards deep; but the walls and taluses of these gorges, where the tracks
descend as into bottomless wells, are concealed by dense taickets, in which are
intermingled plants of the torrid and temperate zones. Along the banks of the
creek flowing on the bed of the barranca, the explorer treads his way as in a vast
conservatory beneath the pendent foliage of palms and tree ferns.

Orizaba, which les in the very heart of the mountains at the foot of Borrego,
has also a more continuous rainfall than Jalapa, and the exhalations rising from
the ground are more dangerous. It stands on the site of the ancient Ahuwilitzapan,
or “Glad Waters,” over 4,000 feet above sea-level, on a terrace whose thriving
plantations are irrigated by copious streams of pure water.

Nearly all the maritime trade of the state, and about half of all the exchanges of
the republic, are concentrated in the port of Vera Cruz. ‘The village of Pueblo
Viejo (Old Town), over against Tampico, in Tamaulipas, is little more than a
detached suburb of that place. Farther south, Tuxpan, accessible only to small
craft, has a yearly trade of scarcely £200,000. For some time the works have
been in progress which are intended to connect it with Tampico by a navigable
canal traversing the Tamahua and ‘other coast lagoons. On the whole seaboard,

VERA CRUZ. 131

stretching 135 miles south of Vera Cruz, no sheltered haven anywhere occurs, the
shore being here everywhere fringed with sands and surf. The old port of Naut/a,
which formerly gave its name to the whole coast, is now choked with mud.

The modern city of Vera Cruz is not the same place as that to which its
founder, Fernan Cortes, gave the name of Villa Rica de Vera Cruz. Nevertheless,
the first camping-ground must have stood on the beach not far from where the

Fig. 52.—Onr1zABA.

Scale 1 : 60,000.

if a)
Mi NY
i WA
cA

SKK

N A Zn LI
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2,200 Yards.

present quays have been built. It was then removed farther north to the village
of Quiahwitzlan, which, however, was badly chosen, being unhealthy and destitute
of any shelter. Hence, four years later a third city was founded farther south near
the populous Zempoala, capital of the .Totonac territory. The river watering the
plantations of the surrounding district took the name of Antigua in 1599, when
this settlement was also abandoned, owing to the bar which prevented all access to
the estuary. The fourth city is that which now exists, and which was founded on

the coast over against the fortified island of San Juan d'Ulua. It was certainly

132 MEXICO, CENTRAL AMERICA, WEST INDIES.

difficult to find a favourable site on such an inhospitable coast, studded with shoals,
and surrounded by arid or sandy flats and marshy wastes. Æ/edanos, or dunes, raise
their yellowish slopes immediately beyond the outskirts of the city, changing their
form and positions with every storm; under the influence of the north winds, some
of these sandhills rise to a height of 160 or 170 feet.

Seen from a distance Vera Cruz, surrounded by all these medanos, presents a

Fig. 53.—Suocessive DIsPLACEMENTS OF VERA Cruz.
Scale 1 : 600,000.

2 SS
GNU EVA=VE RA=CRUZ

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a4 QUE Te le ne) .. . À
ANT Oren are RO V7 CAEN
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Depths.
0to5 5 Fathoms
Fathoms. and upwards.

12 Miles.

far from attractive appearance; hence most travellers not detained by business, and
aware of its evil reputation as a hotbed of fever, pass rapidly on to the more agree-
able cities of the interior, especially in the hot season when “ yellow jack ” prevails
on this seaboard. The epidemic is said to have carried off 2,000 persons in 1862 in
the Ciudad de los Muertos, “ City of the Dead,” as it is called in Mexico. Neverthe-

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VERA CRUZ AND FORT OF ST. JOHN D'ULUA.

VERA CRUZ. 133

less, after the scourge has passed the place is not so unhealthy as might be supposed,
and the whites who have escaped a first attack may consider themselves acclima-
tised. They run even less risks than those settled on the plateau. By sinking wells
in the sandy soil, water is reached at a depth of three or four feet, but mostly con-
taminated by filtration from the neighbouring marshes ; hence good water has had
to be brought by aqueducts from the River Jamapa. Till recently there was not
sufficient to water the streets or flush the sewers, and all the scavengering was
left to the sopilotes, or carrion vultures, which were protected by police regulations.

Fig. 54.—From Vera Cruz to Anton Lizarpo.

Serle 1 : 240,000.

pan ee

RTE

iy “VERA CRU = = =
Pos Pre | ee ae Z ces

Us © = se
Mii Nees
Mity “HNoeN.

West of CORRE

6 Miles.

On the Gulf of Mexico, Vera Cruz is the historical city in a pre-eminent sense.
Here the Spaniards first landed at the time of the discovery and conquest; here
also they still held out for four years after losing their possessions. In 1838 the
Prince de Joinville seized the fortress of San Juan d’Ulua (Ulloa), which stands
on a low island over half a mile from the city, and which was again occupied by
the Americans in 1847 and by the French in 1862. In those times the possession
of this stronghold cut the Mexicans off from all political and commercial relations
with the rest of the world. At present a mere prison crumbling to ruins, it is

134 MEXICO, CENTRAL AMFRICA, WEST INDIES.

said to have originally cost Spain and Mexico £8,000,000. Such a sum might
have been applied to a better purpose by constructing the piers and breakwaters
required to convert into a sheltered harbour the dangerous roadstead where ship-
ping has hitherto had to ride at anchor. Such works, however, have at last been
taken in hand.

Still farther south lies the roadstead of Anton Lizardo, formerly San Antonio
Nizardo, which is sheltered by a large cluster of islets and reefs. But with all
its disadvantages, the port of Vera Cruz still remains the chief trading-place on

Fig. 55.—Harsocur Works IN Progress at Vera Cruz.
Scale 1 : 40,000.

i se il |

ER SS 2

0 te 24 2} to 5S 5 to 10 10 Fathoms
Fathoms. ’ Fathoms. Fathoms. and upwards.
2,200 Yards.

the Mexican seaboard, monopolising nearly two-thirds of the exchanges of the
republic. But any further delay in constructing a safe and deep harbour could
not fail to divert the traffic of Vera Cruz to more favoured places. A large
number of travellers proceeding to Mexico already prefer the more expensive
railway route to the sea voyage across the Guif of Mexico. The largest
share of its trade is with England, after which follow the United States, Germany,
and France in the order indicated. Coffee and hides are the chief articles of
export, England and France also taking the fibre of a species of zacaton (epicampes)
used in making fancy brushes |

MORELOS. 155

The village of Medellin, nine or ten miles south of Vera Cruz, recalls the visit
‘of Cortes, who in 1522 named this place after his native town in Estremadura.
The railway is continued beyond this place south-westwards across the dunes and
forests to the port of A/varado, on the north side of a large estuary where converge
the Papaloapan and other streams. The port, which is encircled by high sand-
hills, is accessible to vessels drawing eight or ten feet. Here is chiefly shipped
dried fish cured in large quantities by the fishermen who comprise nearly the
whole population. These fishermen are said to be descended from Spaniards who
took part in the battle of Lepanto, the anniversary of which vietory is still so'emnly
kept. The local skippers also visit the port of T/acollapam, the “City of Mos-
quitoes,” which is situated at the confluence of the two navigable Rivers Papa-
loapan and San Juan.

MoreE.os, GUERRERO, AND OAXACA.

The section of the republic lying south of the great volcanic chain, comprises
only the three States of Morelos, Guerrero and Oaxaca, together with parts of
Mexico and Puebla. Although all the inhabitants of this region, whites, Mestizoes
and even Indians, took an active part in the war of independence, their country
has remained far more secluded from the general industrial and commercial move-
ment than the other provinces. South of Morelos and Yautepec no railway has
yet been constructed down to the Pacific, and all the feeders of the general system
stop within a short distance of the plateau. But whenever they become connected
with the rest of Mexico these southern provinces, abounding as they do in natural
resources, will scarcely continue to lag behind the other states; for their inhabi-
tants are amongst the most energetic and industrious, and at the same time the
most upright in the whole commonwealth. They have also the advantage of
possessing on their seaboard the best harbour in Mexico.

Cuernavaca, capital of Morelos, is not a Spanish foundation, as might be
supposed from the name, which is a corruption of the Aztec Cuauhnahnac.
Communicating directly with Mexico, through a pass running east of the Cerro
de Ajusco, this ancient city lies on the Pacific slope about 2,000 feet below
the federal capital and consequently in the temperate zone. Its lovely oasis of
verdure is enclosed on three sides by profound ravines, and its climate is one of the
mildest and most equable in the republic; all the plants of West Europe here
flourish side by side with those of the torrid zone. Fernan Cortes made a good
choice when he asked for the fief of this valley, where his castle is now replaced by
the municipal palace. South-west of this place stands the best-preserved Aztec
fortress in the republic, the so-called Xochicalco, or “Castle of Flowers.” It
occupies an isolated hill 386 feet high, which is encireled by trenches cut in sucha
way as to form five successive terraces with steps of dressed stone. The whole struc-
ture presents the appearance of a truncated pyramid, with its four sides exactly
facing the cardinal points. Its basaltic porphyry blocks, all brought from a distance,
ure embellished with hieroglyphies and figures in relief, amongst others those of
fantastic animals with human or saurian heads, seated cross-legged, Asiatic fashion.

136 MEXICO, CENTRAL AMERICA, WEST INDIES.

The city of Morelos, which, although not the capital, takes the same name as
the state, is the ancient Cuautla Amilpas, the “Saragossa”? of New Spain, which
for several months held out against the united forces of the Spaniards. Jt enjoys
the same delightful climate as Cuernavaca and the neighbouring Yautepec ; here
the sugar-cane thrives, and the fruits raised in the district are now forwarded to
Mexico by a railway which crosses a sadlleback, strewn with little volcanoes, at
an elevation of 9,730 feet. Morelos, like the other towns of the state, is watered
by copious streams flowing to the Rio Mexcala. On a northern aifluent of the

Fig. 56.—Acarunco
Seale 1 : 120,000.

———_—

Depths.
0 to 5 5 to 10 1) to 25 25 to 50 50 Fathoms
Fathoms. Fa homs. Fathoms. Fathoms. and upwards.
3,300 Yards.

same river, but in the State of Guerrero, stands the town of Turco, whence the
Aztecs obtained lead and tin, and where the Spaniards made their first essays at
mining work in New Spain. On another tributary lies the famous Zguala, where
in 1821 was issued the “plan” which the belligerents accepted, and which put
an end to the Spanish rule in Mexico. Between Taxco and Cuernavaca lies the
famous Cacahuamilpa cave, whose marvellous galleries, sources of springs and
rivers, have already been explored for a distance of six miles.

The semicircular roadstead opening east of the Mexcala delta is too much
exposed for shipping ; a more favourable anchorage is afforded by the neighbour-

GUERRERO, OAXACA. 137

ing bay of Siguantaneo, some 60 miles north-east of Zacatula. According to the
plans of Gorsuch and Jimenez, this should form the Pacific terminus of the Mexcala
valley railway, a southern section of the interoceanic line, 450 to 500 miles long,
which it is proposed to construct from Tuxpan right across the republic.

Chilpancingo, capital of the State of Guerrero, is a small place standing at an
altitude of 4,560 feet on the elevated parting-line between the Mexcala valley
and the Pacific Ocean. ‘Acapulco, its admirable seaport on the Pacific, has but
little traffic. Sailing vessels have ceased to visit it, but it remains a regular port
of call for steamers. The harbour, which presents the form of a vast crater
breached towards the Pacific, is accessible to the largest vessels, which here find
complete shelter. But the fringe of palms and bananas does little to mitigate
the intense heat in this pent-up cirque, where the solar rays are reflected from
side to side of the surrounding granite cliffs. An opening has been made at
great expense through the west side, to give access to the cool sea breezes.

Antequera, an old Spanish foundation dating from the year 1522, has resumed
the name of the Zapotec fortress of Huaxiacac (Oaxaca), which lies three or four
miles farther west. This place, laid out with perfect regularity, is almost un-
rivalled in Mexico for the beauty of its gardens and the fertility of the surround-
ing plains. À river bearing the Aztec name of Atoyac, or “Running Water,”
traverses the district, where, at a mean elevation of about 5,000 feet, the plants
of both zones are intermingled in endless variety. One of the chief industries of
Oaxaca is the spinning and weaving of the fibre extracted from the species of
bromelwort known by the name of pita. The whole “valley” of Oaxaca, with a
present population of about 150,000 souls, was formerly the private domain of
Cortes, whence his title cf “ Marques del Valle.”

A few remains of Zapotec structures are seen in the neighbourhood of Oaxaca,
especially towards the west, where the city of Huaxiacic formerly stood on Mount
Alban. The ruins of Mitda, the best preserved and according to some travellers
the finest in Mexico, lie some 30 miles to the east. Standing midway up the
slope of moderately elevated hills, which, like those of Greece, stand out sharply
against the horizon, the group of Mitla palaces, with the great pyramid whose
temple is now replaced by a Catholic shrine, presents somewhat the aspect of a
dilapidated Acropolis. These edifices may also be compared with the Hellenic
monuments of the better epoch in the beauty of their proportions and workman-
ship. The walls are disposed in great parallelograms arranged in long horizontal
bands, all embellished with regular designs, cross lines, lozenges, fretwork in
straight or inclined lines, but with scarcely any curves.

The waters flowing from Oaxaca, Mitla, and the intervening hills all converge
six miles south-east of the capital near the village of Santa Maria del Tule, or of
the “ Reeds.”” Trees of colossal size are not rare in this region, and the houses
of the village are grouped round the largest of these giants, which was formerly
regarded as sacred. It is a sabino, or ‘‘eypress”’ (éaxodium mucronatum), which
is said to be the largest tree in the whole world; at least it exceeds in thickness
all those of which measurements have been taken. The so-called ‘“ Hundred-

138 MEXICO, CENTRAL AMERICA, WEST INDIES.

Horse Chestnut” is now divided into three distinct stems, through which a road
has been driven; the dragon-tree of Orotava, which had a girth of 46 feet, has
disappeared; the gigantic sequoias of California were felled in 1855; the Mon-
travail oak near Saintes is 86 feet round, and the largest baobabs and other
African giants are described by Cadamosto, Adanson, and others as from 96 to
112 feet in circumference. But in 1882 the Tule cypress had a girth of no less
than 118 feet three or four feet from the ground, and 150 feet including all the
promineices and cavities of the trunk.

The route from Oaxaca to the sea, leaving on the right the valley of the

Fig. 57.—Cuier Ruins or Cenrrat Mexico.
Seale 1 : 9,000,000.

ofihuac#p, .Otumba
cocinbae

Tlacotepe

Cholutas entla®
Xochicalèo

Taxco°

West of Greenwich

124 Miles.

Atoyac, which winds away westwards to the frontiers of Guerrero, runs at an
altitude cf 7,460 feet over the crest of the Cimaltepec coast range. Near the summit
stands the industrial viliage of Miahwatlan, whose inhabitants are skilful straw-
plaiters, which they work into a thousand fancy articles exported far and wide.
The cochineal industry was formerly the chief resource of the district, but the
southern slopes are now covered with coffee plantations which yield excellent
results. Hence the cultivation of the shrub has been rapidly developed even to
a distance of 40 or 50 miles inland. The high prices obtained by the growers
have enabled them to introduce costly machinery for drying and sorting the
berry. Thanks to this growing industry Puerto Angel, the badly sheltered outlet

OAXACA. 159

of Oaxaca, has acquired some commercial importance since its foundation in 1868.
On this coast the best harbour is that of Huatulco (Guatulco, Coatolco), where a
channel 650 yards wide gives access to a well-sheltered basin from 25 to 50 feet
deep. The little fishing station of Crespon, which collects pearl oysters and the
purple-yielding murex, stands on the beach within the harbour. At a neighbour-

Fig. 58.—Istumus oF TEHUANTEPEC.
Scale 1 : 2,500,000.

Go acs

RC (Rese

eam Sz JCoatzacodlcos .

LE Minatitlanie ff 0 it. ee
Me sre! + &Moloacan
ee falaltipam op et) igs lo:

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asp
PAMÊE

Fave :

japa

apa:
© SEP TES
\D > Cis SSS

West of Greenwich

60 Miles.

ing headland the sea plunges into a cavernous recess, reappearing farther off in
a bufadero, or jet, about 150 feet above the surface.

About one-third of the state is drained by the Rivers Papaloapan and Coatza-
coalcos, which belong to the Atlantic basin. On this northern slope the chief
place is Izvtlan, which lies in a fertile district of the upper Papaloapan valley
over against the superb Mount San Felipe. Ixtlan now also bears the name of

140 MEXICO, CENTRAL AMERICA, WEST INDIES.

Villa Juarez, from the most distinguished of its citizens, the Juarez who main-
tained Mexican independence against Maximilian. In the eastern part of Oaxaca
the chief town is Tehuantepec, or “Tiger Mountain,” an old city of the Huabi
people, which was founded at an epoch previous to the Zapotec occupation of the
land. It is the only place in the district deserving the name of “town,” and it
is so completely divided into separate quarters by mounds and ridges that it has
rather the aspect of a group of villages. In the vicinity are some magnificent
palm and orange groves, and gardens yielding choice fruits.

While proud of its past, Tehuantepec is still more confident of its future, as
controlling one of the future commercial highways of the world. The railway

Fig. 59.—Satmna Cruz, THE NEW PORT or TEHUANTEPEC.
Seale 1 : 60,000.

West of Greenwich

0tod 5 Fathoms
Fathoms. and upwards.
2,200 Yards.

across the isthmus is making rapid progress, and has already surmounted the
highest passes of the hills between the two oceans, so that the coffee grown on the
Pacific slope is now often forwarded by the overland route, saving several thousand
miles between Central America and Europe.

About nine miles to the south-west lies the old port of Tehuantepec, on a
badly sheltered bay, which would have to be protected by expensive hydraulic
works to make it suitable for its future traffic ; meanwhile choice had to be made
of Salina Cruz Bay, where the shipping finds some shelter behind a pier at the
terminus of the interoceanic route.

East of Tehuantepec, on the strips of sand between the lagoons and the sea, are
scattered some 3,000 Huabi fishers, the last of a race whose ancestors contended

TEHUANTEPEC. 141

with the Mijes and Zapotecs for the supremacy in this region. In the north-east,
towards the centre of the isthmus, the two towns of Chimalapa, distinguished by
the names of their tutelar saints, are inhabited by the interesting Zoque Indians,

who speak a language of unknown origin.

Fig. 60.—Minatitnan, NoRTHERN Port or TEHUANTEPEC.

Scale 1 : 200,000.

fe G

hegre LATE
.: {Drabloff [gs -
ay :
Eu 2° =:

ardoise
DAC

60 =

0 to 5 5 Fathoms
Fathoms. and upwards.
3 Miles.

Minatitlan, on the Coatzacoalcos, at the head of the navigation for ships drawing
ten or twelve feet, is the northern or Atlantic port of the isthmus. At present an
obscure trading place, it seems destined soon to become a flourishing seaport. It
is already connected with the mouth of the Coatzacoalcos by a railway, which is
continued southwards in the direction of Tehuantepec. Minatitlan, standing at

142 MEXICO, CENTRAL AMERICA, WEST INDIES.

the northern approach to the isthmus, has also been chosen as the junction of the
line which is intended to run from Vera Cruz towards Yucatan and Guatemala.

The neighbouring town of Ju/tipan is dominated by a mound which, according
to the local tradition, was raised by Cortes to the memory of Malintzin, or Doña
Marina, the Indian woman to whose sagacity and foresight he was probably indebted
for the conquest of Mexico. A French and Swiss colony founded in 1828 at Los
Almagres survived a few years despite the climate and homesickness. The few
remaining settlers were at last dispersed amongst the Mexican towns. A Chinese
merchant of San Francisco, owner of extensive estates in the isthmus, has recently
introduced a large number of his fellow-countrymen into the same district, where.
they are employed on the rice and tea plantations.

III.—Easr Mexico.
CHrapas, Tapasco, CAMPEACHY, YUCATAN.

The Chiapas highlands, distinctly separated by the depression of the Tehuan-
tepec isthmus from the Mexican tablelands, belong evidently to the sume natural
region as the highlands and plateaux of Guatemala. Both are disposed in a con-
tinuous chain, with their steep escarpments turned towards the Pacific, while
the opposite slopes fall gently northwards towards the alluvial lands of Tabasco
and the plains of Yucatan. This peninsula, whose roots are, so to say, sunk in the
morasses and branching deltas of Tabasco, projects its huge quadrilateral mass
beyond the continental coastline in the direction of Cuba, and is continued by a
submerged plateau, which forms geographically a part of that island. Thus the
whole of Hast Mexico from Chiapas to Yucatan constitutes a natural region quite
distinct from the rest of the republic, from which it also differs in the origin and
history of its inhabitants, both in pre- and post-Columbian times. But in pro-
portion to its size it is greatly inferior in importance to West Mexico. It is but
sparsely peopled, and its great natural resources have scarcely begun to be utilised.
The four eastern states have an estimated population of not more than six or eight
to the square mile.

The natural parting-line of the two regions indicated by the Tehuantepec
peninsula was also furmerly a political frontier. Under the Spanish rule Chiapas
was temporarily attached to the administrative division of Oaxaca in 1776, but for
nearly the whole of the three hundred years that elapsed from Alvarado’s con-
quering expedition of 1523 to the proclamation of independence in 1823, Chiapas
and the Pacific province of Soconusco were simple dependencies of the viceroyalty
of Guatemala. When Guatemala entered the Mexican union, the two dependent
provinces also became an integral part of Iturbide’s empire. But when Guatemala
again asserted its political autonomy, it was unable to recover more than a small
part of Soconusco, and the disputed frontier was not determined even in diplo-
matic documents till the year 1882.

Yucatan, also, which had constituted a special division in the viceroyalty of
New Spain, became a Mexican province after the proclamation of independence.

CHIAPAS, 148

But in 1840 an insurrection was caused by the numerous abuses of the central
government. The Mexican garrisons were expelled and the officials deposed ; so
unanimous was the public sentiment of the Yucatan people that the change was
effected without bloodshed. Two years afterwards a Mexican force of 11,000
men besieged the town of Campeachy, but the besiegers themselves, reduced by
battle and fever to a fourth of their original strength, had to capitulate, and the
Mexican Government recognised the complete autonomy of Yucatan, which on its
part gave a nominal adhesion to the federal union. But after the national victory,
discord broke out between the two rival cities of Campeachy and Merida, both
of which aspired to the title of capital.

Then the Indians themselves, trained to warfare during these incessant struggles
in which they had been compelled to take part, seized the opportunity to proclaim
their own independence against their white masters. Thus it happened that in
order to maintain their existeuce and privileges, the white populations had first to
settle their own differences, and then come to terms with the Mexican republic.
The social war lasted many years, and ended in the triumph of the Indians, who
succeeded in maintaining their independence in the southern part of the peninsula.
From this district the Mexicans are now excluded, and even European travellers
are not allowed to penetrate into the country except under the protection of a
native chief. In this direction Yucatan is thus separated from Guatemala by a
broad zone of unreduced populations, just as it is separated from Mexico proper by
still uninhabited wastes.

Puysicar, FEATURES.

The mountain range which begins east of the Tehuantepec isthmus and is
continued through Guatemala and Central America is more entitled, by its
regularity and relative altitude, to the name of Sierra Madre, which is of such
frequent occurrence in Hispano-American lands. The first summits rise abruptly
above the forests of the isthmus, where the Atravesado ridge is already 5,000 feet
high, and is followed eastwards by several other summits exceeding 6,500 feet.
The formation is mainly porphyritic, with volcanic cones appearing at intervals,
amongst others the famous Soconusco (7,900 feet), the ancient Xoconochco, which
gives its name to the surrounding plains and to the whole southern slope of the
State of Chiapas. According to the natives, Soconusco still emits vapours, but
no mention is made of eruptions which would appear to have occurred in within
comparatively recent times. On the other hand the Indians greatly fear the
Tacana volcano, which has been chosen as the common frontier between Mexico
and Guatemala. Tacana is a regular cone which, according to Dollfus and De
Mont-Serrat, must certainly exceed 11,500 feet. It is nearly always wrapped in
smoke, and frequently in a state of eruption.

Towards the Pacific the Sierra Madre falls very abruptly, the crest of the
range here running at a mean distance of 25 to 30 miles from the shore. On the
other hand the Atlantic slope is comparatively gentle, though the declivity is
not regular like that of an inclined plane. It is broken by deep valleys and

144 MEXICO, CENTRAL AMERICA, WEST INDIES.

rugged chains, which the running waters have carved into isolated masses or
irregular ridges, but which are mainly disposed parallel with the Sierra Madre.
The central part of Chiapas may be regarded as a hilly plateau, above which
rise sharp peaks such as Hueitepec, east of San Cristobal, which is said to be 7,450
feet high. Northwards the plateau has been cut by the streams into rounded
hills, which gradually merge in the alluvial plains. Towards the west the
plateau terminates above the plains of the isthmus in the superb Mount Gineta.

Fig. 61.—Banxk or Yucatan
Scale 1 : 6,500,000,

—=— tA ——

os A ———
——— —

— — —_ _ — is Cayo de Alacrar™ ed

—— i ferezs Yy Pxjaros. = SS

= L'AFERRS =f =

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£ = —

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= == ty LAGS EOS SOL € =
= —Profreso-—_ = A! A = ==
= Sisa => <a alley ———
_E— a D Motul .Tizimin D
== re nE le —> PE: Tixkokob ==

= es fy MERID lzamal _———
————-— Pf’! Desconociaa, eee: , » =
= eu) À Le
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— °Tekax — À
20° A — 49
: VE ’Bolonchen :
Y Campeche À

Santa-Cruz

= x Iturbide”

‘ West of Greenwich
Depths.

0 to 100 100 Fathoms
Fathoms. and upwards.

124 Miles.

This gently undulating country, covered with woods and diversified with running
waters, is one of the finest regions in Mexico.

In Yucatan proper there are no mountain ranges; only in the southern
parts of the peninsula towards the Guatemalan and British Honduras frontiers
the surface is broken by a few low spurs and offshoots from the orographic
systems of those regions. The quadrangular mass limited southwards by a con-
ventional line drawn across the solitudes from the Terminos to the Chetumal
lagoon, is nothing but a huge limestone plateau rising above the surrounding
waters, and broken here and there by a few narrow ridges. The mean altitude
scarcely exceeds 100 feet, while the highest rising grounds would appear to

PHYSICAL FEATURES OF ZUCATAN 145

attain an elevation of not more than 500 feet above the average height of Yucatan.
These rising grounds constitute a sort of backbone disposed in the direction
from south-east to north-west towards the blunt angle of the peninsula, and
connected with a ridge that skirts the west coast of Campeachy. Wooded Hills

Fig. 62.—Atacran REEr.
Seule 1 : 230,000.

West of Greenwich

Tep‘hs.
0 to 10 10 Fathoms Upheaved
Fathoms. and upwards. Reefs.

31 Miles,

also run from south-west to north-east in the direction of Cape Catoche. This cal-

careous mass, forming an almost geometrical square, is continued by a submarine

bank far beyond the coastline, except on the east side, which is washed by deep

waters where the plummet plunges into depths of several hundred yards within

a few cable-lengths of the shore. The large island of Cozumel, with the banks
43

146 MEXICO, CENTRAL AMERICA, WEST INDIES.

forming its northern continuation, is separated from the mainland by a profound
channel where the waters of a coast current set steadily from south to north at a
velocity of two or three miles an hour. South of Cozumel the dangerous Chin-
chorro bank, as well as Arrowsmith on the north side, is also a corailine limestone
mass rising from the bed of a deep basin; but the creeks, bays and other inlets
on the coast, especially those of Espiritu Santo and Asuncion, are almost completely
choked with sands and reefs.

The submarine pedestal of Yucatan begins at the north-east angle of the
peninsula, and extends over 125 miles northwards, thus embracing the island of
Mujeres and the cluster of islets in the vicinity of Cape Catoche. The escarp-
ment of the submarine bank, as indicated by the sounding line plunging suddenly
into depths of 100, 250, 1,000 and even 1,500 fathoms, thus describes a great
curve round Yucatan, roughly parallel with’the coast. The still-submerged
portion is far more extensive than the upheaved peninsula itself, and may be
estimated at about 60,000 square miles. Should it*ever rise above the surface of
the sea, it will present the aspect of an almost horizontal limestone mass, in its
general appearance exactly resembling the present peninsula. The numerous
cayos (cays or reefs) scattered over this submarine piateau, Alacran, Arenas, Los
Triangulos, Arcas, are all coralline rocks similar to those fringing the coast of the
mainland, and all have their most active colonies of polypi on the outer face turned
towards the surf rolling in from the high seas. It was at the Alacran, or
“Scorpion,” Reef that the Valdivia was wrecked in 1511, the crew escaping ina
longboat to the Yucatan coast near Cape Catoche. Geronimode Aguilar, one of the
two survivors, afterwards became Cortes’ interpreter during the conquest of
Mexico.

The Arenas cays, near the south-west corner of the bank, consist of a few
islets frequented by myriads of aquatic birds and covered with guano. In 1854
the Mexicans first began to work these deposits; they were followed by the
Americans, who claimed to be the first occupants, and on that ground pretended
that the cay belonged to the United States. This claim to a bank obviously lying
in Yucatan waters gave rise to long diplomatic discussions.

Rivers.

The fluvial systems of East Mexico present in Chiapas and Yucatan a contrast
analogous to that of the relief of these regions. In Chiapas the running waters
flow in superabundance on the surface of the ground; in Yucatan, water has to
be sought at great depths in the chasms of the rocks. East of the Rio Tonala,
which forms the boundary between the States of Vera Cruz and Tabasco, the
whole of the Atlantic slope as far as Yucatan belongs to the two united basins of
the Grijalva and Usumacinta, which rise in the same district on the Guatemalan
uplands and enter the Gulf of Mexico through the same channel. The Grijalva,
which flows under several different names at different parts of its circular course,
has its chief sources in the province of Huehuetenango, and the town of this name
is itself watered by one of its headstreams. After entering Mexican territory

THE USUMACINTA. 147

itis Jo ned in quick succession by most of its upper affluents, and here it takes the
name of Rio Grande or Rio de Chiapa, from the town standing on its banks. In
this part of its course it falls in a steep incline through a series of rapids and
cascades, and near Chiapa suddenly plunges into a rocky chasm whence it escapes
at a much lower level farther down. Where it becomes navigable it describes
a great bend towards the west under the name of the Rio Mezcalapa, and on

reaching the low-lying plains only a few yards above sea-level, it assumes its

Fig. 63.—Tue UsuMACINTA.— VIEW TAKEN AT THE Paso YALCHILAN, ON THE GUATEMALAN FRONTIER.

official title of Grijalva from the navigator by whom it was discovered in the year
1519. But the natives have preserved the old name of Tabasco, which Bernal
Diaz learnt from the Indians during the same expedition. On reaching the
alluvial plains the main stream begins to ramify in various directions, throwing
off some branches seawards, others to the Usumacinta, which is much the larger
of the two rivers.

The Usumacinta, less known than the Grijalva because traversing a very

148 MEXICO, CENTRAL AMERICA, WEST INDIES.

sparsely peopled region, also receives its first contributions fiom the “altos,”
or uplands, of Guatemala. According to Bras eur de Bourbourg, the Rio Blanco,
the main headstream, soon after the Rio Negro confluence trends at first eastwards
in the direction of Honduras Bay. But after changing its name ten times accord-
ing to the tribes settled on its banks, the Rio Chixoy or Lacandon, as it is here
usually called, turns north and north-west to its confluence beyond the uplands
with the Rio de la Pasion, a yellowish stream from the border ranges south of
British Honduras. It mostly flows sluggishly between its wooded banks, but
during the rainy season it floods its banks and at times rises 50 feet above low-
water level. Below the confluence the united stream takes the name of
Usumacinta, under which itis indicated in the diplomatic conventions, according
to which it has been chosen for a space of nearly 70 miles as the common frontier
of Mexico and Guatemala. Navigable by canoes throughout a great part of its
upper course, the Usumacinta pierces the last range of hills by a series of gorges
and rapids which obstruct all navigation by large craft. This section, where the
stream is contracted between vertical walls, takes the name of Boca del Cerro, or
“Mouth of the Mountain.” The people employed in felling mahogany and cedar
in this district mark the blocks and throw them into the current, by which they
are carried from rapid to rapid down to Tenosique. Here the stream resumes its
placid course, and is soon joined by the Rio San Pedro from Lake Peten in
Guatemala. The waters of this affluent are so thoroughly saturated with carbonate
of lime that the snags arrested by the reefs are rapidly petrified and thus form
bars athwart the stream. .

Beyond the confluence the Usumacinta follows a winding course through the
flat plains, till the first branches of the delta begin to ramify from the main stream
some 60 miles above the Gulf. Some of these branches trend north-eastwards
towards the Terminos lagoon, some flow straight to the sea, while others intermingle
their waters with branches from the Grijalva and from the secondary affluents of
the twin river. Including the channels discharging into the Terminos lagoon,
the face of the delta has a development of about 125 miles, while all the ramifica-
tions occupy a space that may be estimated at 6,000 square miles. Scarcely any
other fluvial basin of like size has created such an extensive accumulation of sedi-
mentary matter in the waters of a marine inlet.

The Barra de Tabasco, or principal channel, lies about the middle of the delta
region, and has a depth of from seven to ten feet according to the seasons. This
channel is deepest during the prevalence of the north winds, especially in the dry
season. During the floods, when the sea is covered with a yellowish water fora
distance of 35 miles from the coast, the bar is considerably raised by the sediment
brought down with the flood waters, so that at such times vessels drawing no more
than six or seven feet will not always venture to force the obstruction. The San
Pedro, another branch of the delta lying farther east, although shallower, is more
constant. The deepest, but also one of the most shifting, passages is that of Chil-
tepec in the east, where the sounding-line occasionally reveals a depth of thirteen
feet. Here is discharged the Rio Seco, or “ Dry River,” which is supposed to have

RIVERS OF TABASCO. 149

been the chief brunch when these coasts were surveyed by Grijalva. In the inte-
rior of Tabasco the Grijalva and Usumacin'a present in their numerous ramifying
branches a collective navigable water-system several hundred miles long even in
the dry season. In 1840, 1843, and 1845, Texan, Yucatan, and American flotillas
of war easily penetrated into the Grijalva as far as the landing-stage of San Juan
Bautista, the capital, over 80 miles above the bar. The Usumacinta also is navi-
gabie during the floods for nearly 200 mile, from its mouth, while light river-
craft ascend still farther above the rapids.

In a region of loose, soft soil changes are necessarily frequent, every inundation

Fig. 64.— MourTas or THE GRIJALVA AND UsuMAcINTA.
Sexle 1 : 2.000 000.

al i

RY PaaS À. | e
BG OST ES SS RAVI I DÉS OW:

West of Greenwich

0 to 10 10 Fathoms
Fathoms. and upwerds.
30 Miles.

modifying the aspect of the land. When the streams rise and overflow their banks
a great part of the State of Tabasco is laid under water. A space of about 2,000
square miles within the fixed coastline disappears regularly during the winter
floods. <A first rise caused by the summer rains takes place towards the end of
June, but it is usually of short duration, and is followed after an interval of three
months by the second rise, which usually begins in October and lasts till March,
or for about half the year. During this period all land travelling becomes impos-
sible, and the inhabitants move about by water. But almost every channel and

150 MEXICO, CENTRAL AMERICA, WEST INDIES.

back water offers them a passage through the forests. Thousands of such channels,
flowing now one way, now another, according to the currents of the affluent rivers,
cover the whole country with an endless network of navigable waterways masked
from view by the floating masses of nympheæ and other aquatic plants.

The Terminos lagoon, which receives a portion of the Usumacinta waters through
the branch known as the Rio Palizada, and which is also fed by several other
streams, such as the Chumpan, Candelaria, and Mamantel, is an eastern continua-
tion of the low-lying plains of Tabasco. An upheaval of a few yards would suffice
to expose its sandbinks and change its navigable channels to stagnant waters.
The shore line, which will serve as a rampart for the future lands now being
gradually created by the fluvial deposits, already exists in the chain of the two long
islands, Aguada and Carmen, which close the entrance of the lagoon, leaving only
three passages for vessels of light draught. The Puerto Escondido, or “ Hidden
Port,” as the eastern channel is called, is only a few inches deep on the sill, and
this depth is seldom increased to three or four feet even by the tides, except when
accompanied by strong sea winds. The insular spits are merely sandy beaches
rising scarcely six or seven feet above sea-level, so that a few miles from land
nothing is seen except the continuous line of trees behind which stretch the still
waters of the inland lagoon. On different mips the contour lines of this lagoon
are differently figured ; they differ, in fact, according to the seasons, the winds and
the quantity of sediment washed down by the affluents. On the north side the
sheet of water is continued parallel with the shore for a distance of some 60 miles.
This extension of the lagoon is merely a brackish channel gradually narrowing
towards its northern extremity, where it is nothing more than a feeble seaward
passage occupying the bed of an old inlet on the coast. The lagoon received the
name of Terminos in 1518 from the pilot Antonio de Alaminos, who supposed that
the “island ” of Yucatan ‘terminated ”’ at this point.

Farther north as far as the neighbourhood of Campeachy a few small coast
streams reach the sea. But beyond that place all the rainwater rapidly dis-
appears in the porous limestone soil; not a single rivulet it visible, although there
exist in the interior a few lacustrine basins, formed probably in the depressions
where more close-grained rocks approach the surface. Such is, towards the middle
of the peninsula, the brackish Like Chichankanab, which stretches north and south
a distance of about fifteen miles. Other smaller sheets of water are scattered over
the north-eastern district and, according to native report, lagoons are also numerous
towards the neck of the peninsula west of British Honduras. But neither rivers,
springs, por any surface waters are seen in the more densely- peopled central, north-
western, and northern districts, where nothing oceurs except some morasses tem-
porarily flooded during the rainy season. The moisture, however, is collected in
the bowels of the earth above the impermeable rocks, and, thanks to the natural
galleries occurring here and there, the inhabitants are able to reach these under-
ground reservoirs, from which they draw their supplies.

In these deep cavities the water does not appear to flow as in subterranean rivers,
but rather spreads out in vast basins which communicate with one another through

CENOTE OF VALLADOLID, YUCATAN.

THE CENOTES OF YUCATAN. 151

endless channels, while the whole liquid mass filters slowly in the direction of the
sea. Some of the labyrinthine underground streams are inhabited by crocodiles
as well as by the teh (momotus), a species of bird with silken plumage and tail
made of two long feathers.

The caverns, or cenotes, a word borrowed by the Spaniards from the Maya
language, increase in depth as the land recedes from the coast and rises to a
higher level above the sei. At Merida they lie from 25 to 30 feet below the sur-
face, and each house has its well sunk far enough to tap the reservoir. Farther

Fig. 65.—Trrminos Lacoon.
Scale 1 : 1,400,000.

= de de Cars
Ls . =

. FES TRE;
b/ *+ 00

0 to 10 10 Fathoms
Fathoms. aud upwards.
30 Miles.

north-west of Merida and Valladolid, that is, in the direction of the sea, the basins
lie nearer to the surface, so that the distance from the coast may be estimated by
the depth to which the wells have to be sunk to reach the reservoirs. On the coast
itself the water bubbles up at the shore line, where it mingles with the tides amid
the mangrove bushes. This natural distribution of the water, so different from
what occurs in other regions, is the essential feature in the physical geography of
Yucatan. The fluid is nowhere to be seen, yet its effects are everywhere manifest
in the well-irrigated grounds and the sanitary condition of the houses. Morning
and evening long processions of women pass up and down the steps leading to the

152 MEXICO, CENTRAL AMERICA, WEST INDIES.

cenotes. Through the increasing gloom they follow the inclines excavated obliquely
in the rocky wall until they reach the vaults from which hang stalactites entwined
by long pendent alga. Here they fill their large pitchers with the dark fluid,
which has to be brought laboriously to the surface. The work entailed on the
women is perhaps heaviest at the cenote of Bolonchen, or the “ Nine Springs,” a
ruined village lying north-east of Campeachy on the road to Merida. Here the |
deep cavity is reached through fissures in the rock and spiral stairs forming a
gallery altogether nearly 550 yards long and descending to an absolute depth of
about 410 feet below the surface of the ground.

The form of the coast-line along the northern seaboard of the peninsula may

Fig. 66.—Tum Rio or Yucaran.
Serle 1 : 4,900,000.

nr : : ie Ue =e 7 Per
NV iS Tixkokob "1." Re rf esi oe Sake Re Hu =
wg MERIDA. ARE ramal coe’ i: *Espita rue et
"2 Tocbas* nets Mic rhe
West of. Greenwich ile StS a Oe
Depths.
0 to 50 50 Fathoms
Fathoms. and upwards.

60 Miles.

be partly explained by the pressure of the inland waters spreading out beneath
the surface of the limestone plateau. A strip of land fringes the shore at the
north-east corner of Yucatan, but it has not the free development of the littoral
cordons skirting the Texas and Tamaulipas coasts on the opposite side of the
Gulf. It is disposed in a narrow band near the true shore-line, the outer and
inner beaches presenting the same curves with a surprising parallelism. It
becomes somewhat less regular towards the eastern extremity, where it is inter-
rupted at several points, and even forms the large island of Holbox facing the
Boca del Conil (“ Rabbit's Mouth”), a considerable inlet, where extremely copious
springs bubble up amid the marine waters about a quarter of a mile from the
coast. The normal cordon, beginning west of this inlet, runs for a distance of

THE RIO OF YUCATAN. 153

170 miles, broken only by two narrow passages facing two streamlets—exceptional
phenomena on this part of the seaboard.

The narrow channel separating the mainland from its shifting outer beach
is known by various names, such as laguna, pantano, tierra fangosa, but is more
commonly called the s/o, or river, or even the Rio Lagartos, “ Crocodile River.”
At first sight this term “river’’ would seem to be scarcely justified by a long
channel, which during the dry season is interrupted at several points. It is
crossed not only by fords, but even by tracks and now by roads and railway
embankments, and here and there by a tangle of bushy growths, leaving of the
rio nothing but narrow stretches of meres or lagoons. Numerous springs reappear
in the open sea, but the channel itself receives most of the overflow from the
underground reservoirs, and the sediment brought down from these sources
suffices to maintain the rampart of sands and broken coral reefs by which the
marine waters are kept at some distance from the shore. At the north-west
corner of Yucatan the fringing sandy cordon curves round southwards with
almost geometrical regularity, terminating near a point of the coast known by
the name of Desconocida. This double shore-line coincides with that of the
marine current, which skirts the beach from east to west, and which here meets
a counter-current setting from the coasts of Tabasco and Campeachy under the
action of the northern winds. At the point where they clash the two marine
currents develop a strong whirlpool, by which the shore is eroded. A study of
the Yucatan seaboard gives the impression that the peninsula has been gradually
formed and continues to increase by these outer strips of sand, shells, and coral
reefs successively added to the muinland.

CLIMATE, Frora, Fauna.

As in their relief and hydrographic systems, Chiapas and Yucatan differ also
in their climates, though to a less extent, for both regions are comprised within
the torrid zone with a temperature approaching the equatorial mean. The
Chiupas slope facing the Pacific les entirely within the play of the alternating
monsoons. The north and north-east winds prevail in winter from November to
April, while the vendaval, or south wind, that is, the monsoon proper, dominates
in summer from May to October, when the sun is at the zenith. Nevertheless
the normal atmospheric currents are subject to disturbances, by which they are
frequently replaced by winds blowing from different points of the compass.
Both their direction and force are, in fact, endlessly modified by the inequalities
of relief, the varying trend and outlines of the rising grounds. As a rule, dry
weather and clear skies prevail in winter, while the summer monsoon is accom-
panied by rains, thunderstorms, and tornadoes.

Yucatan is mainly exposed to the action of the north-east trade wind, but
the almost exclusively limestone formation destitute of surface waters becomes
during the hot season a focus of attraction for all the surrounding sea breezes.
Stimulated by the intense solar heat dur ng the day, these winds follow the course

154 MEXICO, CENTRAL AMERICA, WEST INDIES.

of the sun round the horizon. The regular trades are also frequently interrupted
by the fierce gales coming from the north, that is, from the Texan and Mississippi
plains. The driest months are March, April and May, when showers are extremely
rare. But, as in Chiapas, this dry season is immediately followed by torrential
downpours and thunderstorms, lasting till November, when the almost rainless
regular winds again set in. The year might thus be divided into three periods,
a dry, a wet, and a windy season.

For Europeans the Yucatan climate is one of the most dangerous in the Gulf.
Yellow fever often sweeps away numerous victims; but still more dreaded is
consumption, which is both endemic and hereditary, alike fatal to those con-
stitutionally predisposed and to persons enjoying good health and strength.
Mexican soldiers, removed as a punishment to the peninsula, consider themselves
foredoomed to death. In Tabasco, a watery region where the people live as much
afloat as on dry land, the prevailing epidemic is marsh fever. In this moist land
consumption, the scourge of the dry Yucatan plateau, is almost unknown.

Both the flora and the fauna of Chiapas and Yucatan belong to the same zone
as those of south Mexico, with the addition of various forms characteristic of
Central America. This southern region, intermediate between Mexico proper
and the isthmuses, nowhere presents any desert wastes, and the vegetation is
extremely luxuriant in many places, even on the slopes of the Soconusco
Mountains and the neighbouring coastlands, where the rainfall is far from
copious. Tree ferns, the cacao and other plants requiring much moisture and
a constantly humid atmosphere, grow vigorously, while on the lowlands rice
thrives without irrigation. The scanty rainfall is here supplemented by the
moisture percolating below the surface from the rising grounds. Even the arid
limestone plains of Yucatan are clothed with a stunted vegetation ; very different,
however, from the magnificent forest growths festooned with lianas, which cover
the fertile districts of Chiapas and Tabasco. Little is seen except thorny scrub
and cactus or agave thickets, without any of the large species which, on the
Anahuac uplands, grow to a height of over 30 feet. Here the rain-water dis-
appears too rapidly in the porous limestone to nourish a rich vegetation.

Amongst the plants peculiar to Chiapas and Yucatan, and not found in Mexico
proper, there are many trees and dyewoods, such as mahogany and campeachy, or
logwood (hwmatoxrylon campechianum). The former ig even more common in
various parts of Central America than in Tabasco, while the latter is exclusively
confined to the region from which it takes its ordinary name. In favourable
localities this hard-gruined plant sometimes attains a height of from 40 to 45 feet.

Amongst the more remarkable members of the Chiapas fauna is the “snuff-
box ”’ tortoise, which has its lower shell furnished at both ends with two appen-
dices enabling it to shut itself completely up and defy all enemies.

INHABITANTS.

Like that of Anahuac, the population of East Mexico is very mixed, although
the indigenous element is here relatively greater. The Nahuas proper are repre-

THE MAYAS. 155

sented in Soconusco along the historic route by which the Aztecs in comparatively
recent times migrated from Anahuac to Nicaragua. The warlike Chiapanec nation
still survives in the north-west part of the state which from them takes the name
of Chiapas. The more numerous but less cultured Tzendals, Tzotzils, and Quelens
(“Bats”) oceupy the forest regions comprised between the Tehuantepec depression
and the Guatemalan frontier. Lastly, the numerous nomad or settled groups
belong to the same family as those of west Guatemala—Lacandons and Chontals
in the north, Chols and Chañabals in the centre, Mamés in the south. They all
appear to be connected by language, primitive usages, and traditions with the
cultured Mayas of Yucatan, the most advanced representatives of this ethnical
division The Mayas held out more valiantly against the Spaniards than the
Aztecs; they would also appear to have reached a higher degree of civilisation
than the Nahuas in pre-Columbian times. Although never actually visited by
Columbus, he had, nevertheless, heard of their fame. The work of extermination,
as described by Las Casas and Diego de Landa, resulted in the almost total dis-
appearance of the Maya race; which, however, has gradually revived and even
preserved the national speech. Those acquainted with Spanish are said to abstain
from speaking it, and Maya is still generally current in all the rural districts
except in the neighbourhood of Campeachy. In the inland provinces the
descendants of the Spaniards have to a large extent forgotten their mother tongue,
and in Yucatan the conquerors may be said to have themselves been conquered.
Even in Merida everybody is obliged to learn Maya in order to hold inter-
course with the maceguales (mazehuatl), as the natives are called.

The Spaniards and Mestizoes are represented chiefly in the towns and southern
parts of Chiapas which are traversed by the more-frequented highways between
Mexico and Guatemala. The half-caste Maya-Spanish race is one of the finest
in America, and the women especially are remarkable for their personal charms.
It is noteworthy that the Indian type of features is perpetuated from generation
to generation. However white the complexion miy become, the Yucatec Mestizo
always preserves certain Maya traits by which he may be at once recognised.

The range of the Maya language, which embraces the Huaxtec territory in the
State of Vera Cruz, extends far beyond the frontiers of Yucatan, for it comprises
nearly the whole of Tabasco, a part of Chiapas, and about half of the Guatemalan
republic. According to their own traditions the Mayas reached the peninsula
from opposite directions, from east and west, from the sea and the mainland. A
god had guided them across the ocean, and it is certain that they were acquainted
. with navigation. They had even decked vessels, which probably hoisted sails, and
voluntary or involuntary voyages frequently took place between Yucatan and the
island of Cuba. Once established in the peninsula the Mayas long remained its
peaceful rulers. Ina region lying apart from the regular highway of migrations
along the Pacific coast they had nothing to fear from invading hosts. At the time
of its greatest expansion the Aztec empire was conterminous with Mayaland only
at its south east extremity, and the Nahuas had scarcely any knowledge of Yucatan,
where the more cultured part of the nation was settled.

156 MEXICO, CENTRAL AMERICA, WEST INDIES.

The Mayas, properly so called, are of mean stature with robust bony frames,
round head, delicate hands and feet, and great staying power. The branch of the
Maya group dwelling in the Tabasco forests, and known as Chontals, or “ Savages,”
a name implying that they had remained aliens to the civilisation of their Yucatec
kindred, are a remarkably frugal people. A few roots or bananas with a little
maize suffice to maintain them for days together under the hardest work as porters
or buatmen. Their costume is extremely simple, being limited to drawers and a |
shirt worn as a blouse. In Yucatan the dress of the men is the same as that of
the Spaniards; but the Maya women, more faithful to the national usages, have
preserved the pre-Columbian fashions. The Mayas are a gentle, inoffensive
people, and a market-day in a Yucatan town presents an almost unique spectacle :
in the quiet demeanour, courtesy, and mutual goodwill of buyers and sellers.

Like all other cultured Indians, the Mayas call themselves Catholics, though
mingling with their private worship certain rites which they have assuredly not
learnt from the Spaniards. Thus, after burials, they mark with chalk the path
leading from the grave to the house, so that when the time comes to enter the
body of some new-born babe, the deceased may not mistake the way to his former
dwelling. From this it is evident that, despite the teaching of the Church, the
doctrine of metempsychosis still survives amongst them. They have also preserved
the old lore regarding the healing art and the stars. Many astrologers still
observe the conjunctions of the constellations, predicting from them the public and
private events of life, the results of the harvests, and similar forecastings. Every
village has its “cunning man,” who reads the future in a quartz crystal globe.
Before the disastrous war of 1847, nearly every village had also its Chilan-
Balam Book, that is, the “Interpreter of Oracles,” and of this work at least
sixteen copies are still known to exist. Amongst the natives are certain priests,
either very complacent or else very ignorant of the orthodox rites, for they
celebrate with the people the misa milpera, or “ field Mass,” at which a cock is
sacrificed, the four cardinal points being first sprinkled with some fermented
liquor, with invocations both to the Three Persons of the Holy Trinity and to the
Pah ah tun, that is, the four patrons of the rain and the crops. These tutelur
deities have, however, taken Christian names, the Red, or God of the East, having
become St. Dominic; the White, or God of the North, St. Gabriel; the Black,
or God of the West, St. James; and the “ Yellow Goddess ” of the South, Mary
Magdalene.

The Maya language, at once guttural and sonorous, and pleasant, especially in
the mouth of the women, appears to be the purest member of the linguistic family
whose various other branches—Tzendal, Lacandon, Quiché (Kachiquel) —are
spoken between the Gulf of Mexico and the Pacific seaboard. These various
dialects, however, differ from each other merely in the admixture of foreign words
and a certuin variation in the pronunciation and in the final syllables. Pure Maya
is at present spoken only in the north-east part of the country round about
Valladolid and Tizimin.

A striking proof of the persistence of the Maya genius is afforded by the

THE MAYA

157

geographical nomenclature of Yucatan, nearly all the native names having been
preserved despite Spanish influences.

The term Yucatan, which has prevailed

Fig. 67.—Maya Yours.

‘eth

over the Spanish Zs/4 de Santa Maria de los Remedios, is itself of Maya origin,
though its exact meaning is somewhat doubtful.

It probably arose from a mis- |
understanding on the part o: the Spanish navigators when enquiring after the

158 MEXICO, CENTRAL AMERICA, WEST INDIES.

name of the peninsula. According to Bishop Landa, apostle of the Mayas, the
usual description was Ulumit Cuz el Etel Cet, that is, “Turkey and Deer Land.”
Mayapan, the name of the ancient capital, was also frequently applied to the
whole peninsula, and Maya, the name of the people, would appear to have
previously been given to the country, This word, Ma-ay-ha, is said appropriately
enough to mean “ Waterless Land.”

As amongst the Aztecs, the fanatical conquistadores endeavoured to efface
everything recalling the national religion. Manuscripts of priceless value were
thrown to the flames, the idols and sculptures ruthlessly destroyed. Nevertheless,
a few traditions have survived of pre-Columbian times, and by their aid the
learned have endeavoured to reconstitute the political history of the Maya nation
for the two or three hundred years preceding the conquest. The first legendary
personages in Yucatan history, at once gods, heroes, and founders of empires, are
Votan and Zamna, who were partly confused together in the popular imagination,
and to whom were attributed all the national institutions, as well as all inventions
made since the beginning of the world. After them came Cukulcan, another
mythical ruler, identified by archeologists with the Mexican Quetzalcoatl and
with the Guatemalan Gucumatz, the ‘ Feathered Serpent,” whose history coincides,
in fact, with that of this Aztec and Quiché demi-god. Hence there can scarcely
be any doubt that the epoch personified by the Maya hero represents an interval
during which the influence of the Northern Nahuas was dominant in the peninsula,
Then followed other conquerors, apparently from the south, though their very
name, Tutul Xiu, would seem to imply that they also were Nahuas. According
to the national legend, they reigned as many as eleven centuries over Mayaland,
and it was probably under their rule that were erected the remarkable monuments
of Yucatan. Despite incessant wars and local revolutions involving the destruc-
tion of many cities, this dynasty still held sway in a part of the territory at the
time of the Spanish invasion.

The first Spanish navigators had already been struck by the numerous monu-
ments of Maya architecture, which were afterwards mentioned by all writers
speaking of this region. But during the present century no attempt was made
till after 1830 to systematically examine and describe these astonishing ruins.
Uxmal was first visited and described by Zavala in 1835, and its remains were
soon after studied and illustrated by Frederick von Waldeck. But public interest
was first awakened by the traveller, Stephens, and the painter, Catherwood, who
together twice explored the land, and whose writings* may be regarded as the
starting-point for the archæological study of Yucatan.

Since that time the ruined cities have been frequently visited, amongst others,
by M. Charnay, whose work acquired exceptional value from the magnificent
photographs, by which the accuracy of previous drawings could be judged. Over
sixty groups of extensive ruins are already known; but it is impossible to say
how many more may still exist in the unexplored territory of the independent

* Stephens, Incidents of Travel in Yucatan ; Catherwood, Views of Ancient Monuments in Central
America.

THE MONUMENTS OF YUCATAN. 159

Mayas. Certain archzxologist<, proud of being amongst the first to draw attention
to the splendid structures of Chiapas and Yucatan, did not fail to extol their
magnificence, and even to compare them with the temples of Fgypt and Greece.
Such praise was certainly not justified, for the Maya buildings lack elegance
of proportion, sobriety of ornamentation, nobility and perfection in their sculp-
tures. Nevertheless, their vast size, massive character, and lavish wealth of
carvings attest a civilisation fur superior to that of many civilised peoples in the
Old World.

Most of the Yucatan structures stand either on natural eminences or on
artificial terraces. They are usually found in the vicinity of cenotes, or even
built over these underground reservoirs, which were at all times places held in

Fig. 68.—Curer Ruins or Yucatan.

Scale 1 : 4,200,000.

S= sop re
——

sf)

= SClara > Cd Pas 2onot =

PRET Es

sa ©

.Temax LENS
ails Here «Motul! ° Tizimin
ID
(lincs) Aké !zamal .Espita
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ayapan 2
Sih | Ticul 3
= Bokuche, ayaa Chichen-Itza Valladolid |
den = Tabi Cheb Kob
——, Kabah Sa ase Te kax 4 exe
= Féeté *Xiaboak Tulum,
Chunhuhu'Labna oncacab ace ——— _—|
20 Itzimté+ aS 5 SS
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Gamneee Sh SS
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=, Ceibaplaya Jibilnocac’* “Elemax ChanSantacruz

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ai Macanche d

West of Greenwich

60 huiles.

veneration by the surrounding populations. The monuments usually face the
cardinal points, but not with astronomic accuracy, and the parts are rarely disposed
in correct order, having apparently been erected without any general plan. Some
archæologists have assigned a vast antiquity to these remains, attributing them to
peoples who had already disappeared at the time of the conquest. But this
opinion is no longer beld, and is in fact refuted by tradition and internal evidence.
According to the testimony both of the Spanish conquerors and of the national
chronicles, the Mayas continued to use the temples for religious purposes down to
the second half of the sixteenth century. Nearly all the Yucatan buildings affect
the pyramidal form, temples and palaces alike rising from a broad base through
a series of receding steps to the crowning structure on the summit. Such
structures were absent from some of the pyramids, which in that case were

169 MEXICO, CENTRAL AMERICA, WEST INDIES.

truncated, the free space on the upper terrace formiag an altar open to the
heavens, where the sacrificing priests celebrated their rites in the presence of the
assembled multitudes. None of these massive piles were carried to any great
elevations—so as, for instance, to overtop the larg: forest trees. The highest
pyramids fell short of 100 feet; but in some instances the base covered a vast
space, that of Zayi, near Uxmal, presenting a periphery of over 1,500 feet.

According to Viollet le Duc, one of the most remarkable architectural triumphs
of the Maya builders was the employment of mortar to cement the layers of
stone in a solid rock, modelling and carving the cement itself with figures and
ornamental designs. Mortar, cement, plaster, stueco, all was made of sand and
lime mixed in different proportions, but always hard as stone. Made with nearly
pure hydraulic lime, it is so thoroughly adhesive both in the mass and when
applied as a surface coating, that it can scarcely be chipped off by the hammer.

In the Yucatan buildings and round about very little pottery and instruments
have been found, although such objects are usually met in abundance in historic
and prehistoric stations. Idols also have rarely been brought to light, doubtless
because they were mostly hidden away by the natives after the arrival of the
Spaniards, who destroyed all images they could lay their hands upon. But the
walis are sometimes found completely covered with sculptures and figures in bas-
relief. The type of such figures is the same as that of the present natives,
especially the eastern Lacandons, except that it is highly exaggerated, especially
in the temples of Palenque. Receding forehead and arched nose were regarded
as marks of nobility, and such features were naturally given to human or divine
images held up to the veneration of the people. There is in any case reason to
believe that in those times, as well as at present, the heads of the children
were artificially deformed by the Maya women. Symbolic animals, especially the
serpent, embellish the walls, on which are also seen ornaments in the form of
elephants’ trunks. From this it has been hastily concluded that the Maya sculptors
were acquainted with that animal, and consequently that they had received their
first lessons from masters of Asiatic origin. Some of the bas-reliefs represent
social scenes; but nowhere have been discovered warlike subjects, such as those
covering the walls of the Assyrian palaces and Egyptian temples. Hence the
Maya would appear to have been in the enjoyment of profound peace when the
monuments of their great artistic epoch were erected. The almost total absence
of fortifications round their cities and buildings also attests the tranquil condition
of the land, and the peaceful character of its inhabitants. At present all these
grey carvings intermingled on the crumbling walls, such as those of Uxmal some
350 feet long, seem to be merged in a chaos of indistinct forms. But they were
formerly relieved by fresh colours—yellow, red, white, and black—sharply contrast-
ing one with the other, and presenting a mystic or historic subject understood by all.

The “ calculiform ” hieroglyphics, so named from their contours, usually
rounded like those of calculi or pebbles, are all arranged in long lines like the
written characters of a book, and undoubtedly served as the explanatory text of
the associated carvings. These writings still remain undeciphered, but may

TOPOGRAPHY OF CHIAPAS, 161

possibly one day reveal the history of the people by whom the buildings were
erected. At least they may explain the purposes of edifices which are at present
designated under fantastic Spanish names. A clue may also thus be obtained to
determine their date, at present a subject of interminable discussion amongst
archæologists. The same characters were also reproduced on textiles and on bark,
and such manuscripts could be either rolled up or bound together in thin volumes.
But hieroglyphic documents in the Maya language are extremely rare. Four
only are preserved in European collections; nor has their interpretation been yet
facilitated by the discovery of any bilingual inscription, such as the Rosetta stone
and the Bisutun cuneiform tables, which served to unravel the mystery of the
Egyptian hieroglyphics and the Persian and Mesopotamian cuneiform writings. Yet
the Spanish priests were acquainted with a Maya alphabet, and the manuscript
possessed by one of these missionaries has even been recovered * The only infor-
mation still extant on the nature of the Yucatan writing system is contained in
this work, which belonged to the fanatical bishop, Diego de Landa, who threw to
the flames hundreds of manuscripts found in the temples. Landa’s book explains
only some sixty of several thousand signs, and as each sign may be replaced by
others having the same meaning though differently formed, it 1s obvious that no
translation is at present possible.

ToPrpoGRAPHY.

Being separated from the interior of Chiapas by a coast range running close to
the shore, and crossed neither by great trade routes nor by railways, the groups of
habitations situated on the Pacific seaboard naturally possess but slight commer-
cial importance ; nor are there any good harbours on this coast to attract shipping.
Nevertheless such is the fertility of the soil and the excellence of its produce that
Soconusco has already acquired a high reputation in the foreign markets.

Here the most frequented seaports are Tonala and San Benito, or Soconusco, both
accessible to vessels of light draught through dangerous pissages which communi-
cate with long coast lagoons. Although the nearest port to the capital of Chiapas,
Tonala has a yearly trade of less than £40,000 ; in the neighbourhood are two hills
scarcely surpassed in the whole world for their wealth of iron ores. San Benito,
which exports the cacao of Soconusco, has nearly double the trade of Tonala, and
it cannot fail to acquire a rapid development when the railway is opened to
Tapachula, on the slopes of the Soconusco Mountains near the Guatemala frontier.
Union Juarez, founded a few years ago close to the border at an altitude of 4,300
feet, is the centre of the Chiapas coffee plantations ; Chiapa de los Indios, the ancient
capital of the Chiapanec nation, which has given its name to the whole province,
lies on the Atlantic slope in the valley of the Grijalva. Above the present town
and its numerous ruins stands a bluff crowned with the remains of the Chiapa Nan-
. duimé fortress, behind whose ramparts the Chiapance warriors defied the attacks
of the Aztec forces. Here also they long held out against the Spaniards and,

* Daniel G. Brinton, The Books of Chilan-Balam.
44

162 MEXICO, CENTRAL AMERICA, WEST INDIES.

when reduced to the last extremity, the survivors, to the number of 2,000, threw
themselves with their wives and children over the precipice.

A few miles west of Chiapa, in a lateral valley of the Grijalva, lies the little
town of Tuxtia, which was for a few years made the capitai of the state to punish
the rebellious inhabitants of San Cristobal Las Casas, the present capital. This place
stands on the site of the old Indian city of Ghouel or Hue-Zucatlan. Ithas received
its present designation ot Las Casas in honour of the valiant defender of the Indians,
Partholomew de Las Casas, bishop of Chiapas. Beyond the Anahuac plateau San
Cristobal is the highest city in Mexico, though the estimates of its altitude vary
from 6,240 to 7,000 feet.

Sun Juan Bautista, formerly Villa Hermosa, capital of Tabasco, is a small
place occupying an opening in the extensive forest which covers the whole of the
delta region. It is connected by a short railway with the Grijalva, and thus com-
mands the magnificent system of navigable waterways ramifying over a district
many hundred square miles in extent, reaching from the delta to the neck of the
Yucatan peninsula. Though at present destitute even of carriage roads, the capital
is destined in the near future to become a converging-point for the railways running
north, east and south towards Mexico, Yucatan and Guatemala. Its outlet on the
Atlantic is the port of Frontera (Guudalupe), on the right bank of the Grijalva.

The Usumacinta, which joins the Grijalva above Frontera, has no towns in
the part of its vast basin comprised within the Mexican States of Chiapas, Tabasco

and Campeachy. Palenque, or the “ Palisade,” the best-known place in this
region, is a mere village lying at an altitude of about 350 feet on one of the
last slopes of the plateau limited by the alluvial plains of the Usumacinta.
Palenque, founded during the second half of the sixteenth century under the
patronage of Santo Domingo, soon acquired great importance as a centre of the
transit trade and converging-point of the numerous tracks around the low-lying
plains with their ramifying system of countless canals. Despite its isolated
position in the midst of forests, it also became during the last century the chief
station for caravans journeying between Guatemala and Campeachy. But the
shifting of the trade routes has again consigned it to solitude.

About ten miles south-west of Palenque le the imposing ruins of a forest-
grown city whose very name has perished, though supposed to have been either
Nachan or Colhuacan, the “Serpent City.” The inhabitants of Palenque were
unaware of its existence till the middle of the last century, when the ruins were
accidentally discovered in 1746. Their systematic exploration began in 1773,
and since that time they have been frequently visited, described, and reproduced
in drawings and photographs. But great ravages have been made by the damp
climate, the rank vegetation, the fires kindled in the midst of the ruins to clear
the ground for tillage, the eagerness of explorers to enrich public museums or
their private collections, by ignorant travellers carrying off souvenirs of their
visit, and even by the wanton love of destruction. The largest structure, known
as the palacio, appears to have really been a “palace” of some kind, or the
residence of a religious community, but certainly not a temple, for it is divided into

PALENQUE—TULHA. 163

a large number of chambers, passages, and apartments of all kinds. Like all the
other monuments, it stands on a raised platform, which takes the usual shape of
a truncated pyramid. One of the façades shows a row of pillars supporting a
projecting architrave of a highly original design, The walls of this edifice are
covered with sculptures, while in another was found the famous “ Greek cross,”
symbol of the “tree of life,” or of “fecundity,” which has given rise to so much
discussion amongst archeologists. South-west of Palenque, about midway on the
road to San Cristobal, capital of Chiapas, in an upland valley watered by a western
affluent of the Usumacinta, are grouped the houses of Ococingo, whose name has
also been assigned to an ancient city lying five miles farther east. By the Indians

Fig. 69.— Ruins IN THE Lacanpon AND TZENDAL CouNrRIES.
Scale 1 : 2,800.000.

:. °° Balancan.’..

Pa 0 Fi

60 Miles.

this place is called Tonila, that is, ‘Stone Houses,” and the ruins are said, on
pure conjecture, to be those of 7w/ha, ancient capital of the southern Toltecs.
Amongst them was discovered a plaster carving, whose perfectly Egyptian
expression greatly surprised Stephens, Catherwood, and Brasseur de Bourbourg.
It takes the form of a medailion with large wings spread out above the porch of
a palace. In the whole district between Ococingo and Palenque the hills and
mountains are crowned with sepulchral mounds, and according to the inhabitants
of the country, other magnificent structures are hidden away amongst the hills
of Tumbala, and farther south in the direction of San Cristobal and Comitan,

One of these unknown cities in the Lacandon territory was lately discovered
on the left bank of the Usumacinta, in a district which must have been frequently

164 MEXICO, CENTRAL AMERICA, WEST INDIES,

visited by the Guatemalan and Campeachy traders. But all reference to these
ruins of Menche were of the vaguest character till the year 1868, when they
were first distinctly mentioned by Suarez. Since then they have been visited by
Rockstroh in 1881, by Maudslay and Charnay in 1882, and the last-mentioned
traveller gave them the name of Lorillard City, in honour of the American citizen
who defrayed the expenses of his expedition. The ruined city stands on a head-
land encircled by the river below its confluence with the Ococingo, and above
the series of rapids extending all the way to Tenosique. Some heaps of stones
near the shore look like the butment of a broken bridge, but they are merely the
remains of a sustaining wall at the base of the amphitheatre of houses and temples.
To their very summit the escarpments are cut into flights of steps, or else faced
with masonry, with large trees now growing through the cracks and fissures; all
the building materials exactly resemble those of Palenque. The largest temple,
the facade of which is partly overgrown with interlaced branches and foliage, is
disposed in three receding storeys, where traces are still preserved of the original
stucco coating and paintings; the topmost storey is arranged in little regular
square niches, each of which was decorated with sculptures. One of the lintels

? and in the court is seen an

represents two figures supporting “ Latin crosses,’
idol sitting cross-legged, the hands resting on the knees, and the face crowned
with an enormous headdress, which takes the form of a diadem of precious stones
surmounted by huge feathers. This serene and dignified image, absolutely unique
in the New World, recalls the buddhas of the extreme East. The bowls of coarse
clay found close by contained a resinous substance, probably the incense which
the Lacandons even recently still burnt in honour of the deity. :

The little town of Tenosique below the rapids, and at the entrance of the plains
the village of Balancan, are the chief groups of habitations on the lower Usu-
macinta. Carmen, the only town in this part of the delta, lies on a strait through
which the Terminos lagoon communicates with the sea.

The picturesque city of Campeachy (Campeche), with its irregular streets and
houses shaded by cocoanut groves, is surrounded by ramparts and commanded by
forts crowning the encircling hills. Campeachy is still one of the most beautiful
cities in Mexico, but it has lost the relative importance it enjoyed during the
days of commercial monopolies. During the Spanish rule it was one of the three
privileged places on the east coast north of the isthmus of Darien—Vera Cruz and
San Juan de Nicaragua being the other two—which were open to the trade with
Spain, and, thanks to this advantage, it had developed extensive relations with
the interior. At that time Campeachy was not only the emporium for the whole
of Yucatan, but also served as the outlet for the produce of Tabasco, Chiapas, and
even Guatemala. Now, however, these regions have their own direct trade routes,
and even Yucatan itself finds Carmen a more convenient outlet for Campeachy
wood and other exports. If Campeachy possessed a real harbour, it would have
at least attracted to itself a great part of the exchanges of the peninsula, but the
roadstead with its shelving bed is exposed to the full fury of the dreaded nortes ;
the pier projecting seawards does not reach sufficient depths to be accessible at

TOPOGRAPHY OF YUCATAN. 165

all times, so that vessels drawing thirteen or fourteen feet have to anchor at a
distance of five miles from the port. Its trade is consequently limited to cocoa-
nuts, some timber, sugar, hides, and salt.

The scarcity of towns, villages, or even hamlets in the neighbourhood of the
sea, as shown by the blank spaces on the map of Yucatan, is apt to cause surprise
The sparse population on the coastlands is partly explained by the want of shelter
on the seaboard, and the presence of insalubrious coast lagoons or marshes, but
it is also due to the filibustering expeditions to which the people were exposed

Fig. 70.—Merma AND Norru-Westr Yucatan.
Scale 1 : 1,009,600.

SOARES OR = CCL =O Ma AB BAS CAP

REE SDF SIS

| Depths

SS
0 to 5 5 Fathoms
Fathoms, and upwards.
24 Miles.

during the last two centuries. The English corsairs, landing suddenly in some
creek, often penetrated far into the interior, killing the men, carrying off the
children, sacking and burning towns and villages. Although these raids have
long ceased, no special industries have been developed, while the natural resources
of the coastlands have not been sufficient to attract immigrants from the interior.
Hence in this region the population is still mostly concentrated about Merida,
where it was also most dense at the time of the conquest. Merida, capital of the
State of Yucatan, and formerly of the whole peninsula, stands on the site of
the ancient Ho, or Ti-ho6, that is, “ City” in a pre-eminent sense. Most of its

166 MEXICO, CENTRAL AMERICA, WEST INDIES.

monuments were pyramidal structures with their upper terrace crowned by
temples or palaces. All have been destroyed, and the materials used in the
modern buildings, which are consequently here and there embellished with
ancient carvings embedded in the walls. In the outskirts alone are found the
remains of pyramids, one of which, till recently occupied by a community of
Franciscan friars, covers, with its cloisters and gardens, a surface of about five
acres; its picturesque ruins present somewhat the aspect of a citadel. According
to ancient Maya usage, some of the streets traversing the city are still indicated
at either end by the sculptured image of the symbolic animals, such as the flamingo
er hawk, to which the thoroughfare was dedicated. The white terraced houses
with their Moorish courts resemble those of Andalusia, but those of the suburbs,
surrounded by groves and gardens, are still constructed in the Maya style. They
are little houses of stone, or else of plaited bamboo, raised a couple of feet above
the street level, with a porch in front which is enclosed by walls on both sides
and provided with a continuous bench all round. In the central part of the city
is still seen the emblazoned palace built for himself by Montejo, founder of the
new town, in 1542.

Thanks to its trade in henequen, or agave fibre, of which from 40,000 to
60,000 tons are annually exported, Merida has become the converging-point of
several lines which, when completed, will cover the whole peninsula with a net-
work of railways. For the present, however, the capital is connected only by a
road with its ancient port, the little town of Sisa/, at the north-west corner of
Yucatan. From this seaport the henequen takes its English name of Sisal hemp,
by which it is known in the trade. The price of this valuable fibre has increased
sixfold since the middle of the present century. The roadstead of Sisal, being
exposed to the dangerous north winds, was abandoned in 1871, when a new
“ marina’’ was founded on the coast due north of Merida, with which it is con-
nected by a railway 22 miles long. The line is carried over the coast lagoon by
a strong embankment. The new town, which replices the old Indian village of
Tuxulu, has already justified its name of Progreso, although the only advantage it
enjoys over Sisal is its relative proximity to the capital. To shipping it is equally
inaccessible, large vessels having to anchor in an open roadstead from three to six
miles from the port. Fo dangerous is this roadstead that steamers and sailing
vessels are always ready to weigh anchor and escape to the high sea; towards noon
every day communication with the shore becomes almost impossible, owing to the
violence of the surf under the action of the fierce northern gales.

Over 50 miles east of Merida, following the windings of the route, and on the
verge of the more thickly-peopled districts, stands the ancient city of Zzama/,
so named from Itzmatul (Itzenmatul), “God of the Dew.” But this old
capital was already in ruins at the time of the conquest, and was regarded only
as a holy city to which pilgrims flocked from all parts of the four highways
radiating in the direction of the cardinal points. Twelve pyramidal or conic
mounds, each crowned with a temple or palace, rose at that time above the city,
but are now merely shapeless piles of refuse visible above the dense foliage of

|| Ht IT
HULL

RUINS OF UXMAL—THE GOVERNOR'S PALACE,

MAYAPAN—UXMAL. 167

the surrounding gardens. Here M. Charnay discovered certain wall-paintings,
which afford a clue to the decorative system of the Mayas. As usually happens
with most holy cities, Izamal has become a much-frequented market-place, priests
and sacrifices being succeeded by traders and their wares. Between Izamal and
Merida are seen the finest remains of the old causeways, which have been
compared by the archæologists to the Via Appia. These roads were partly
destroyed by the Yucatecs themselves, to arrest the advance of the Spanish
conquerors, and since then they have been utilised as quarries to supply materials
for buildings, enclosures and other highways. Raised above the level of the
plain, which was occasionally flooded, these causeways were slightly arched and
provided with footpaths, and covered to a depth of about sixteen inches with
a layer of cement, which has become as hard as the solid rock. According to
Landa this cement was made of lime hardened with water in which the bark of
some species of tree had been steeped; but the present inhabitants have no know-
ledge of the process. Ruins are numerous in the whole district. One of the
most remarkable is the pyramid of Aké about midway between Merida and
Izamal. This pyramid is one of the oldest Yucatec structures, judging at least
from the surrounding pillars, which are formed of huge rough-hewn blocks put
together without any mortar, and presenting a somewhat cyclopean aspect.

Some twenty miles south of Merida is the site of HMayapan, ‘“ Banner of the
Mayas,” which, as indicated by its name, was long a capital of the Maya nation.
Some traces are still preserved of its temples, notably a cone-shaped pavilion over-
grown with agave and other plants, and enclosed by a ruined rampart three
miles in circuit. After the destruction of Mayaran in the fifteenth century, the
residence of the Maya sovereigns was removed farther south to Mani, which in its
turn was destroyed by the Spaniards, and where appear to have also perished the
Yucatec manuscripts said to have been burnt by order of Bishop Landa. The
most numerous Maya monuments occur south-east and south of Merida, along the
little ridge of low limestone hills running south-east and north-west towarls the
angle of the peninsula. Uwmal, or “ Olden Time,” near the north east extremity
of this ridge and above some underground reservoirs, is the most famous site in
this group, and the richest in remarkable structures. One of these, the so-called

“ Governor’s Palace,”

is one of the best preserved of all the Maya palaces, and
may be considered the type of many similar Yucatec monuments. It forms a
long narrow quadrilateral with a double row of apartments, which are separated
by corridors with walls inclining towards each other and covered by a horizontal
roof. The upper storey is richly embellished with crescents, rhombs and other
ornamental devices attesting a highly inventive faculty. One of the outer decora-
tions has been taken by certain archæologists for an elephant’s trunk. The
“nunnery,” a still larger edifice, is even more sumptuously decorated ; nowhere
else in Yucatan can be seen a greater variety of motives executed with more
success. Innumerable heaps of stones, mounds and pyramids reduced to the
form of wooded knolls, are crowded round the vicinity of Uxmal, Zicul, Tekax,
and along both slopes of the ridge which stretches south-eastwards to Nohpat,

168 MEXICO, CENTRAL AMERICA, WEST INDIES.

Sache, Kabah, Sanacte, Labna and Zayi. The ruins of the latter place are amongst
the finest in Yucatan ; it is looked on as a haunted city of the dead by the natives,
who rarely venture to approach it, declaring that at times a mys‘erious music
is heard vibrating among the stones. The district stretching south of the limestone
hills is strewn with ruins as far as the town of Iturbide, recently founded in the
borderland between civilised Yucatan and the territory held by the independent -
wild tribes. |

In the eastern part of Yucatan the Spanish name of Valladolid has been
given to the chief town, the ancient Zaci, or “ White Clay.” Zaci, which is not
yet connected with Merida by rail, lies in the centre of a tolerably fertile district,
which is so salubrious that consumptive persons resort to it from Campeachy
and Merida. But, like so many other places in Yucatan, it is more interesting
for the surrounding mines than for its modern structures, especially since the
Maya revolt, when it was nearly depopulated and its cotton mills destroyed.
Chichen-Itza, former residence of the Itza dynasty, lies twenty miles west of
Valladolid; it isnow a mere village strewn with ruins which, during the wars
of the conquest, were successively occupied by the Indians and Spaniards as strong-
holds. The pyramid of Chichen-Itza, which is still in a good state of preservation,
is approached by a monumental flight of steps lined with trees and terminating
at the base in two colossal snakes with yawning jaws.

In a building which he called the “ gymnasium,” Stephens discovered some
paintings which he pronounced to be the most precious gems of native art to be
found anywhere on the American continent. Unfortunately, the colours have
been almost completely effaced by the weather and visitors. One of the subjects
represented a lirge vessel with raised prow and poop, tiller and rudder. At
Chichen-Itza, Dr. Le Plongeon also discovered under a heap of rubbish 26 feet
thick the finest statue of Nahua art now preserved in the Museum of Mexico. It
is the effigy of Chac-Mool, the ‘‘ Tiger King,” reclining on his back and looking
towards the right; the features are quite regular and the head is adorned with
fillets in the Egyptin fashion. The simple majesty of this statue stands in
striking contrast to the figures, overcharged with barbaric ornaments, which are
met in so many other temples of Mexico, Tabasco, and Chiapas, The reservoir
from which Chichen-Itza takes its name, meaning “ Mouth of the Springs,” is a
broad gloomy well about 500 feet in cireuit, with circular ledges carried round the
walls by means of projecting layers of masonry. In its deep green water, 65 feet
below the rocky surface, are reflected the overhanging trees and festoons of
pendent creepers. So recently as 1560, human victims were - still cast alive into
this well as sacrifices to the gods.

Farther south follow H/ Meco and Cankun over against Mujeres Island ;
Paalmul and Pamal on the shores of the strait separating Cozumel Island from
the mainland; lastly, 7w/wm crowning a cliff still farther south. The last-
mentioned appears to have been a powerful capital which was defended on the
land side by a solid enclosure still in good repair. The towers flanking this
rampart are also well preserved, and appear to be the same as those mentioned by

COZUMEL.—THE INDEPENDENT MAYAS. 169

the early navigators. The architecture of the Tulum buildings presents some
peculiar features, which seem to point at a mingling of cultures in this remote
region of Mayaland. Some of the temples cause surprise by the Lilliputian
dimensions; pierced by a narrow opening scarcely wide enough for a single man
to creep in, they would seem to have been made for a race of dwarfs. The part of
the seaboard where Tulum is situated belongs at present to the free Indians, and
in the same district stands a ‘“‘ holy rood,” where they gather on solemn occasions
to hear the “ voice of God,” which issues from the cross, appointing the chiefs,
declaring peace or war, condemning or pardoning the guilty. A Catholic priest
who had ventured to penetrate into the country was brought before this cross,
which sentenced him to death.

Mujeres, like all the other islands fringing the coast, has remained in pos-

session of the Yucatecs. Its very name of ‘ Women’s Island” recalls the

special part played by it in the religion of the Mayas at a time when crowds
flocked to its temple to worship the female deities of Yucatan. At present it is
inhabited by a few hundred black and half-caste fishers, who trade directly with
Havana.

Cozumel, a much larger island lying farther south, some twelve miles off the
coast, was also a much-frequented place of pilgrimage. It is the ancient
Aheuzamil, or “ Swailow Island,” whose temple contained the image of a god with
swallow feet. Cozumel, which is densely wooded, has not yet been explored,
although the Spaniards had occupied it even before the conquest of Yucatan, and
had built a church whose ruins are still to be seen. When these ruins were
rediscovered, with the altar and cross in the midst of the bush, it was supposed that
they represented a Christian civilisation dating from pre-Columbian times. There
still remain some traces of the paved highway, crossed by other routes, which
traversed the island from north to south.

The southern part of the coust between Tulum and Chetumal Bay is sparsely
peopled by a few full-blood Indians, who have preserved their language, customs,
and independence. The territory of these free Mayas is bounded on the north by
the so-called “ Southern Line,” that is, the chain of fortified posts which extends
nearly along 20° north latitude through Peto, Ixmul, and Tihosuco. Formerly they
frequently crossed this “pale,” and wasted the land as far as Valladolid and
Tekax, and were even reported to have hacked to pieces two thousand persons in
the latter place with the manchette.* At present the civilised Yucatecs are
separated by a kind of march or borderland from their independent kindred, who
no longer dare to cross over.

These independent Mayas are usually called “ barbarians,” although scarcely
less civilised than the others. They till the land in the same way, and keep their
roads in good repair; they make their own manchettes, shaped like short scimitars,
with iron imported from Belize, and procure their rifles from the same British
settlement. Some of them being well-made stalwart men, they make good soldiers,

* Manchette is the French-Creole form of the Spanish machete, a kind of hooked knife used in tropical
America for clearing the bush.

170 MEXICO, CENTRAL AMERICA, WEST INDIES.

going through their drill with great precision, and keeping their arms in perfect
condition. Nobody can read or write, and the rites of the Catholic religion have
been forgotten, although they build cabins to which they give the name of
churches, and which serve as inns for wayfarers; crosses are also set up at
intervals along the highways. The cacique is at once king and high priest, and
rules more by might than right, or until some other chief becomes strong enough
to seize the supreme authority in his turn. Santa Cruz, which lies on the plains
west of Asencion Bay, is their present capital, and this place was valiantly
defended against the forces sent from Merida in 1871. Bacalar, or rather
Bakhalal, the “ Reed Palisade,” on the swampy margin of a lagoon draining to
Chetumal Bay, was a Spanish settlement founded in 1544 under the name of
Satamanca. Destroyed by the bucaneers in 1633, it was rebuilt and fortified in
1730, and even recently still carried on a brisk trade with British Honduras ; but
the Indian insurgents took it by surprise and massacred the whole population.
The remains of some of the people are still seen piled up in the old church where
they were slain.

LV.—Economtic AND SocrAL Coxpirion oF Mexico.

The growth of the Mexican population has not been so rapid as that of most
other American states. ‘lhe normal rate of increase has been greatly retarded by
the sanguinary war of independence, which lasted two years ; by military con-
spiracies and local revolutions, fomented by personal ambitions, but really due to
class and racial hatreds; by the misery of the peasantry deprived of their lands ;
by the depredations of the wild tribes, Apaches and ‘Comanches on the northern,
Mayas on the southern frontiers; lastly, by two foreign wars, one with the United
States, the other with France. Nevertheless, the population of the Union has
more than doubled since the beginning of the present century. In 1808,
Humboldt, carefully sifting all the statistical reports furnished to the admi-
nistration of New Spain, estimated the whole population at 5,837,000, or
5,767,000 for the part of the territory constituting the present Mexican republic.
In 1888, eighty years after Humboldt’s estimate, the official census returned a
population of 11,396,000, which, according to the rate of annual increase, may be
certainly raised to 11,650,000 for 1891, this increase having been about 2 per cent.
during the last decade. As regards the distribution of the population, Mexico
differs from most other regions, the uplands being far more densely peopled than
the lowlands.

Immigration, which has acquired such great economic importance in the United
States, in Canada and Argentina, has but a secondary influence on the growth of
the Mexican population and the development of its resources. 1t is easy to under-
stand why so few emigrants from the Old World direct their steps towards Mexico.
In this region the only unoccupied lands are the arid northern plains, till recently
exposed to the raids of marauding wild tribes, and the forest regions of the south,
largely under water and much dreaded by the white men for their climate.
Neither in Chihuahua nor in Tabasco can the European working classes hope to

ECONOMIC CONDITION OF MEXICO. Ais!

succeed except under specially favourable circumstances. Even in the provinces
where the soil is already appropriated, European settlers, expecting a relatively
high rate of wages, could never attempt to compete with the pure or half-caste
Indians who are satisfied with the lowest pay, and who, often crushed under the
burden of their debts, have to work almost gratuitously as veritable serfs. The
Mexican territory, already divided into great landed estates, has scarcely any
room for small holders, the very class which elsewhere supplies the bulk of the
colonists. Hence, with rare exceptions, such as that of the French settlement in
Jicaltepec, the various attempts, made either by the government or by private
persons, to colonise the country by Italians or other foreign labourers have failed,

Fig. 71.—DENSITY OF THE POPULATION IN MEXIco.
Seale 1 : 30,090,000,

HE
PLEINE

Bee

wes! [1 Da j LS

=" SR =
ar) aS

West of Greenwich
Inhabitants to the Square Mile.

O isa FE |
0 to 10. 10 to 20. 20 to 40. 40 to 60
and upwards.
© Feder1l district, 780 to the square mile. o Towns of over 50,000 inhabitants.
620 Miles.

and the settlers have, after a time, all been dispersed, leaving the ground to the
natives. In 1888 the twenty “ colonies ” in the republic had a collective popula-
tion of only 6,319, and of these 1,411 were Mexicans. Recently an American
company has been formed to introduce negro settlers into the southern provinces,
while in another direction certain Chinese speculators propose to found colonies of
their fellow-countrymen. But if agricultural interests fail to attract many immi-
grants, foreigners are drawn to Mexico in yearly increasing numbers by the
inducements of trade and the industries. The construction of railways, telegraphs,
and factories of all kinds has brought thousands of mechanics, engineers, and other

172 MEXICO, CENTRAL AMERICA, WEST INDIES.

artisans from North America. Italian craftsmen and petty dealers arrive in con-
stantly increasing numbers, while the community of speech facilitates the settle-
ment of Spaniards in the country discovered by their ancestors. At the end of
1887 the number of Iberians entered on the consular registers exceeded 9,500 ;
next to them the French and Italian settlers are the most numerous.

As in other countries where the population is steadily increasing, agriculture
and the industries have been developed at a still more rapid rate, Maize, which is
the chief crop throughout the temperate zone, and even on the plateaux, is still
the “ corn,” in a pre-eminent sense, for the Hispano-Mexicans, as it formerly was
for the Aztecs; with it is made the fortilla, or hot cake, in the preparation of
which over a million of women are constantly employed. The annual crop ‘is
estimated at from £22,000,000 to £24,000,000, whereas wheat, grown by the side
of maize in the cold zone, is valued at scarcely more than £4,000,000. Barley
represents even a still smaller value, while rice is raised only on the lowlands,
together with manioc on the Pacific and Atlantic slopes.

The frijoles, or haricot beans, form part of the diet of most Mexicans, and are
cultivated with peas, broad beans, and lentils to the extent of over £2,000,000
annually. Potatoes are scarcely appreciated in their original home, and next to
maize and haricots the most important article of food is the banana, a fruit of
Asiatic origin. In the warmer parts of the temperate zone a clump of bananas
with four or five stems yields from 620 to 720 fruits, twelve of which suffice to
sustain a man for one day. Thus a space of about twenty square yards growing
this plant produces enough food to support one person for a twelvemonth ;
whereas, to obtain the same result with wheat, a space of at least 160 square yards
would be needed. Besides the binana, Mexico produces an immense variety of
other fruits, being suitable for the cultivation of almost every plant grown both in
the tropical and temperate zones. The orange is here found associated with the
cocoanut, the grape with the chirimoya, so that no fruit-markets can surpass those
of the capital and the other cities of the plateau for the endless variety of their
produce.

Wine is not the national drink, although the vine might yield excellent results
in various parts of the country, and especially in Chihuahua and the other northern
states from Zacatecas to the American frontier. Its cultivation, already valued at
over 1,000,000 gallons in 1878, is even yearly increasing, but only to meet the
demands of the wealthy classes. The plant which yields the really national beve-
rage is the maguey (agave americana), of which over thirty varieties are known
to agriculturists. It is grown on the upper slopes of the temperate zone and in the
cold regions, especially on the light sandy soils of the plateaux between 6,000 and
8,000 feet above the sea. Between Tlaxcala, Pachuca, and the capital, the maguey
fields cover many thousand square miles of land. The pulquero obtains the
maguey wine by removing the bloom at the moment of its greatest energy. Then
the sap, which would have served to nourish the huge cluster of flowers, fills the
deep cavity caused by the excision, and this cavity is emptied from two to nine
times a day, according to the species and years, during the whole period of efHo-

ECONOMIC CONDITION OF MEXICO. 173

rescence. Certain plants have thus yielded during the season as much as
2,000 or even 4,000 pounds of aguamiel, or sap, which may be drunk at once
slightly diluted with water. But it is usually allowed to ferment, and thus
changed to pu/que, which may also be consumed on the spot, or forwarded while
quite fresh to all the surrounding markets. The trunk line between Orizaba and
Mexico, as well as the other railways on the plateau, have their daily pulque trains,
each often conveying hundreds of tons of the liquor in all directions. The term
pulque is taken from the Araucanian language of Chili, and it has not yet been

Fig. 72.—-PuLQueERo.

Zig.
CZ

made clear why it has been substituted by the Spaniards for the proper Aztec
name, octli. In the Nahua traditions its discovery was attributed to a prince, who,
as a reward, received the king’s daughter in marriage. At first strangers find
pulque somewhat disagreeable, owing to its smell of “high” meat or old cheese ;
but, as a rule, they soon learn to relish this drink, the stomachic qualities of which
are much praised by medical men. In its composition it resembles mare’s milk,
and of all fermented beverages peculiar to the Old World it approaches nearest to
the koumiss of the Kirghiz nomads. Taken in large quantities it intoxicates like

174 MEXICO, CENTRAL AMERICA, WEST INDIES.

wine, and the drunkenness caused by it is said to be provocative of wranglings and
bickerings. Besides pulque, the agave, treated in different ways, yields various
other drinks, sweet or acid, weak or strong, such as the mexcal or lequilu, the
“ Mexican brandy ” of English writers.

Maguey, the planta de las maravillas of the Mexicans, yields other products
besides pulque and mexcal. From it the ancient Aztecs obtained paper, as their
descendants do soap, a species of gum, and especially various kinds of fibre used
according to their quality for making brushes, cordage, yarns, and textiles. The
smaller varieties of maguey known by the names of ixéli and lechuguilla (agave hete-
racantha) contribute largely to the wealth of San Luis Potosi and Valles, while the
Zapotecs of Oaxaca export a variety of articles made from pita fibre (bromelia
silvestris). Henequen (agave sisalensis or Sisal hemp) has done still more for the
prosperity of Yucatan, and, thanks to this cactus, the most arid regions of the
peninsula have become the most productive. The fibre of this plant serves to make
cables, cordage, canvas; which, though not so stout as that of hemp, is none the
less in great demand throughout the industrial centres of North America.

Two of the Mexican articles of export, cochineal and indigo, have ceased to
possess any economic importance, the former having been ruined by the com-
petition of the cochineal produced in the Canary Islands, the latter by the indigo
grown in Bengal, and now also partly replaced by mineral dyes. Oaxaca,
formerly the chief centre of the cochineal industry, and still exporting about 8,000
ewt. in 1870, produced only a fiftieth part of that quantity in 1877, and the outlay
had everywhere exceeded the returns. The nopal (cactus coccinifera), on which
the insect fed, has accordingly been almost universally replaced by other economic
plants, especially the coffee shrub. But there is another variety of cochineal
which yields large profits, and the cultivation of which has already made some
progress. This is the ae or avin (Uaveia avin), that is, the “ fat cochineal,” very
common in all the low-lying and temperate parts of south Mexico. The adult
female of this insect, boiled in a metal vessel, yields about 27 per cent. of its
weight in axine, a fatty substance about the consistency of butter, and the most
siccative oily product known to commerce. The Yucatecs formerly used it for
painting their dwellings, and the North Americans have also begun to employ it.
Every tree peopled by a colony of ajes easily yields 20 to 25 pounds of insects, or
about 6 pounds of grease.

Mexico also takes a certain limited share in the production of the great agri-

cultural industries of the world. Cotton is grown chiefly in the northern provinces

bordering on the United States, as well as in Guerrero and Vera Cruz. The
sugar-cane, introduced by Fernan Cortes, is cultivated in the southern states of
Morelos, Puebla, Campeachy, aad Yucatan, but almost exclusively for the local
consumption; cacao, which thrives well on the lower slopes of the Soconusco
escarpments, and even in the interior of Chiapas, grows in a too thinly-peopled
region to yield large annual crops. Coffee is of far more economic importance,
especially as an item in the foreign trade of the country. In 1887 Oaxaca already
possessed 3,000,000 shrubs; the plantations in the temperate zone of Vera

ECONOMIC CONDITION OF MEXICO. 175

Cruz, under the isothermal lines of 62° to 68° F., are also very extensive, though
less appreciated than the coffee grown in the Uruapan district, Michoacan. The
tobacco raised on the banks of the Papaloapan, about the slopes of the Tuxtla
volcano, and on the spurs of the Tabascan hills, is scarcely inferior in aroma to
that of Cuba itself. Since the insurrection of 1868 on that island, several of the
banished planters have introduced this industry into Mexico. Vanilla also
succeeds perfectly in the hot moist lands about the foot of the eastern Sierra

Fig. 73 —Maceury Prantations, San Francisquiro District, NEAR Mexico.

meyers lege eM oy ee Lemay CHA FRA ETC LIL CIE : 5 Ha
ie : SA “a int je mens LE Ne |

Madre, and especially in the environs of Papantla, and at one time Mexico was
the largest exporter of this fragrant pod. Now, however, it is far outstripped by
the little French colony of Réunion.

Stock-breeding is one of the chief industries of Mexico. In some of the
haciendas in the relatively arid northern provinces, as well as in the moist
savannahs in certain parts of Vera Cruz and Tabasco, the whole population consists

176 MEXICO, CENTRAL AMERICA, WEST INDIES,

of vaqueros, or “ cowboys,” each having in charge hundreds of horned cattle, or else
from eight to ten atajos, or over 200 horses. These herdsmen, employed on farms
of 10,000, 20,000, or even 30,000 cattle, are, for the most part, Indians or half-
eastes differing greatly from other Mexicans. They are a half-savage race of
“‘eentaurs,’’ who capture the untamed horse or overturn the strongest bull with a
throw of the lasso, and whose loves, combats, and heroic adventures are a favourite
subject with romance writers. But generations flow on and industries change.
Formerly the ox and the horse roamed the prairie like the aurochs or bison, and the
cowboys were rather hunters than keepers. After capturing and branding the

Fig. 74.—Cuier AGRICULTURAL PRODUCE IN Mexico.

Scale 1 : 30,v00,000.

Fer

0%
à
III

TS
2.
Era
CE
=",

a! F Sep

Tobacco. Cacao Maize Cereals. Rice. Bananas.

Se ees Pee
Jane, Cottee.
[~~]

Miguey, Cactus. Cochineul. Viue. « olion. Cacutchouc. Forests. Lands little cultivated.

620 Miles.

animal with its owner’s initials, they again released it till it had to be recaptured
for the shambles, or to be transferred to the dealer. Even the breed of ponies
known as mustangs or ladinos had reverted to the wild state, living in the bush far
from running waters, and in summer, when all the meres were dry, slaking their
thirst by chewing the thornless cactus. But at present many farmers have intro-
duced a more orderly system of stock-breeding, developing new breeds by
crossings with European, American, and even Asiatic animals. Thus the Indian
zebu and the carabao, or buffalo of the Philippine Islands, have been introduced
with good results in the Mexican cattle-farms. The Andalusian horses brought

ECONOMIC CONDITION OF MEXICO. 177

over by the conquerors, and endowed with the qualities of mettle, strength, and
endurance, have also been crossed with other breeds, and a more varied choice is
thus daily offered to the gallant Mexican cavaliers, who are so proud of their
horsemanship, their gay trappings and richly-embroidered, gold-fringed costumes.

Smaller animals, such as sheep and goats, find less favour with the stock-
breeders, though numerous herds of swine are reared in the forests and on the
plains, especially in the States of Mexico and Jalisco.

When the Spaniards arrived in the country with their traditional theories of
property, they were unable to understand the communal system prevalent among
the natives. Montezuma himself they looked upon as a sort of ruler like their
own sovereign, and they concluded that the great personages of the empire were
feudatory vassals in the possession of vast domains. Hence they supposed that
they had only to substitute themselves for those Mexican lords, and Fernan
Cortes set the example by seizing vast territories such as the Cuernavaca district
with the populations inhabiting them. Nearly the

’

and the “ Oaxaca valley,’
whole country was thus distributed amongst the conquerors, and the natives,
hitherto unaware that the land could be appropriated, became themselves so much
property, like the soil itself. Still a small plot was usually left for their use
within a radius of a few hundred yards round about the parish church.

Although the Spaniards were driven out by the war of independence, the
system of large domains introduced, by them remained intact. The haciendas
are not so much farms as territorial divisions as extensive as a rural parish or even
a shire. Asa unit of square measure the hacienda has a superficial area of 35
square miles, but some of the northern haciendas are a hundredfold this size,
covering a surface equal to one of the large departments of France. The whole
land between Saltillo and Zacatecas, a distance of over 180 miles, belongs to three
owners. These owners are naturally unable to cultivate more than a relatively
small part of such estates, in the heart of which they erect a fortified dwelling,
and around this stronghold, serving as a sort of citadel during the civil wars, are
grouped the houses of their clients and retainers. All highways converge on the
seignorial mansion ; in the neighbourhood are held the markets, and all travellers
must call on its master either to demand hospitality or procure fresh mounts and
supplies. The vast enclosures in the vicinity are carefully guarded refuges, where
the herds are driven to escape the raids of marauding Indians or predatory ani-
mals. But while a solitude reigns round these isolated centres of life and industry,
the great hacendados left the country open to incursions, and it was owing to this
baneful system that till recently the Apaches and Comanches were able to extend
their daring plundering expeditions far into the interior of the republic. As was
remarked nearly a century ago by Humboldt—“ Mexico is a land of inequality ;
nowhere else does there prevail a more frightful inequality in the distribution of
wealth.” About the middle of the century the official surveys returned over 13,000
ranchos, or small holdings, with one “cabin” as a centre of habitation. But even
were they the indisputable property of the free peasantry, all these ranchos
constituted a scarcely perceptible portion of the national wealth. Since that

178 MEXICO, CENTRAL AMERICA, WEST INDIES.

time vast tracts have been surveyed and either sold or rented. But one-third of
these national lands has been gratuitously given to speculating land companies,
while a large part of the rest has been assigned to other financial societies or
to private persons in lots of 6,250 acres; a single company thus owns no less
than 15,000,000 acres, while very little has been assigned to the peasantry.

The bulk of the Mexican population is dependent on the great mining or land
companies. Of the two classes the miners are by far the more independent, owing
to the neighbourhood of the towns that have sprung up round about the works.
The peasants, poorly paid and kept by the very force of circumstances in the
power of the territorial lords, differ in name only from real serfs. Destitute of

the necessary resources, they are
His Ter NOR EEE or Saye. unable to borrow except from the
proprietor or his steward, and

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debtor to servitude, or sell him to

ee eee se

another owner, in discharge of

\ rue

Frs-—s
Nb
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all or part of any real or fictitious
claim. The son is no longer even
liable for his father’s debts, nor

can the future of minors be

Mexico. Other Countries,
pledged for advances beforehand.

But in many districts remote from the capitul, and especially in the south-eastern
provinces, the law is a dead letter, and the natives are even said to have been
secretly sold to Cuban planters. Practically servitude still exists, as during the
early days of the conquest, for it is the natural consequence of the landed system.
To be enslaved, to die a slave, in a land so fair, is the burden of every song round
the villages of Tabasco. The traveller, passing through the country, cannot fail to
be impressed by the plaintive tone of these songs, which float continually on the
air in the neighbourhood of all human habitations,

At the beginning of the century the chief wealth of Mexico, apart from maize,
maguey and the other alimentary produce of primary necessity, consisted in the
precious metals; the export trade was in fact confined almost exclusively to the
products of the mines. These products represented an enormous value, without

ECONOMIC CONDITION CF MEXICO. 179

even taking into account the vast sums which were smuggled out of the country,
and of which no returns could be made. There are numerous auriferous deposits
in Mexico, but her chief treasures are the silver mines, which since the discovery
of America have yielded fabuious sums to the trade of the world. According to
the researches of Humboldt, the total value of the gold and silver furnished by the
metalliferous veins of New Spain amounted to £425,000,000 from the conquest to
the year 1803. This figure is regarded as somewhat too high by Soetbeer, Del Mar,
Neumann, and other economists, who, however, estimate the value down to the
year 1890 at no less than £300,000,000, or over one-fifth of the total production
of the world during the four centuries since the first voyage of Columbus.
In 1850, before mining oper-
ations had begun in California, Fig. 76.—THE Wortp’s YIELD or THE Precious MeErats.

Arizona and New Mexico, regions

- 1680

formerly belonging to New Spain,

1661
1801 “18

_-|1541-1560
- [1561-1580
_.|[1641 -1660
--|1701 -1720
---|!721-1740
_|1741-1760

-|1761-1780

---|!60! -1626

__- |1621 -1640
__._|1681 1709
___.11861 - 1880

1881 -1890

the proportion yielded by Mexico

Years
__-_--_-11493-1590

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neal

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since the conquest had been much
higher, or about one-third. This
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beans, squares of soap, and simi-

lar objects of daily use were em-
200 ieee te Len

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ployed in Mexico itself for petty
dealings. The yield of the Mexi-
can mines, so far from falling off

200

during the present century, has |,
considerably increased, despite | so
wars and revolutions, and flooded
mines. The improvement in

the highways of communication, ities en the OR ad Si

combined with the introduction

of better mining processes, has more than compensated for the advantages enjoyed
by Mexico at a time when the precious metals possessed a greater relative value
than at present. An oscillation in international trade favourable to the develop-
ment of the mining industries would have the result of increasing to an enormous
extent the production of silver in Mexico, where there are thousands of well-
known deposits still untouched owing to their relative poverty, or to the lack of
communications. Even the slag heaped up about the workshops still contains
from 25 to 20 per cent. of metal, or altogether £240,000,000. In the year 1889
alone, as many as 2,077 declarations were registered respecting new mines. At
present the yearly production exceeds two tons of gold, valued at £300,000, and
600 tons of silver, valued at £5,500,000, and in 1889 the total yield exceeded
£8,000,000.

180 MEXICO, CENTRAL AMERICA, WEST INDIES.

So extensive is the area of the Mexican mineral region that it may be estimated
at four-fifths of the whole territory. The chief metalliferous zone is that of the
western Sierra Madre from the Arizona frontier to the isthmus of Tehuantepec ;
but the other Sierra Madre is also very rich, especially in the States of San Luis
Potosi and Hidalgo. Besides gold and silver the Mexican highlands contain
deposits of platinum, copper, lead, iron, manganese, and quicksilver, the last of

Fig. 77.—Yretp or Gotp AND Sriver IN Various COUNTRIES SINCE 1492.

NEW WORLD.

Trt rr r11 TT
TE

Rs :

PÉRRRRRE
+ HE

United States : £400,000,000. Rest of America : £500,000,900.
OLD WORLD.

ET
.
[

FR SR is nr ts Rein Rs R RS Rs ts Ses Sin ess RN en Sans test

Australia: £300 000,000.

Each square represents £400,000.

great value in the reduction of the ores. Coal has been found in Sonora, on the
banks of the Rio Grande, in the Sierra de Tamaulipas and in the southern
uplands. Sulphur is obtained in the craters both of the active and quiescent
volcanoes ; near Tuxpan are found petroleum springs; by scratching the surface
the sulphates and carbonates of soda, saltpetre, sea salt are turned up; lastly, there
occur quarries of marble, onyx, jasper, basalt, obsidian, while certain rocks abound

in precious stones.

ECONOMIC CONDITION OF MEXICO. 181

The early explorers often speak of the beautiful chalchihuites, jadeites or
emeralds, with which the Mexican nobles adorned themselves and decorated their
idols. Amongst the resources of Mexico must also be included yellow amber,
common in Oaxaca and the neighbouring states, but of an unknown vegetable
origin. It is perfectly transparent, of a lovely golden hue, and, seen in the light,
shines with a fluorescent glow. In certain parts of the interior it is found in such
quantities that the natives use it even for kindling their fires. The specimens of
this substance sent to Europe come from the coast, where it occurs here and there
in the sands. In Mexico there are reckoned altogether about a hundred impor-
tant mineral districts, and in 1888 there were as many as 575 mines at work, to a

Fig. 78.—Cuier Mrverat Recions or Mexico.
Seale 1 : 30,000,000.

("et

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w 3 © 2 a a e . a
Silver. Gold. Platinum. Cinu bar Lead. Tron. Copper. Coal. Salt.
620 Miles.

great extent owned by English capitalists. The total yield of all metals, earths,
stones, and combustibles is valued at nearly £10,000,000 yearly.

To mining, which was already represented in all its branches, such as smelting
and minting, under the Spanish rule, have now been added some of the large
manufacturing industries. Cotton, one of the chief crops in the republic, is
entirely employed in the Mexican spinning and weaving mills, and manufacturers,
moreover, import large quantities of the American staple. Over 50,000 families are
supported by the cotton industry, and about a hundred factories produce a quantity
estimated at 30,000,000 pounds a year. The Statesof Puebla, Mexico, Queretaro,
Guanajuato, Jalisco and Coahuila are the chief producers of cotton textiles, which
take the form of mantas, sarapes, rebozos, and other articles forming part of the

182 MEXICO, CENTRAL AMERICA, WEST INDIES.

national costume. The artisans of the plateau are also skilled in all the crafts
connected with saddlery, leather-dressing, embroidery and other trimmings so
highly appreciated by the Mexican cavaliers. The complete outfit of a regular
dandy is worth some hundred pounds, including the trappings of his mount. All
the large European industries, even those requiring a deep knowledge of scientific
processes, have now been introduced, and are contributing to transform the
economic conditions of the country. Moreover, a large number of the small local
industries stil]l hold their ground. Thus the Indians of Michoacan continue to
produce those articles of featherwork which the conquerors admired in Monte-
zuma’s palaces, and the Mixtec women still weave, with the cocoons of a native
species of bombyx, certain silken stuffs, coarse to the touch but very stout, and
highly prized by the natives.

In most of the provinces the ceramic art has undergone but slight change
since pre-Columbian times. The Indians, as a rule, are excellent craftsmen, as
patient, methodical, and regular in their operations as the machines which they
employ. Nor do they lack the necessary initiative where it is needed by the
character of the work. They display remarkable talent in designing and modelling,
they copy without difficulty all objects presented to them, and knead wax with
rare skill. In them survives the genius of their forefathers, who sculptured the
facades of the temples, carved hieroglyphic inscriptions, designed and painted
topographic charts.

This general increase of culture, shown by a more scientific and a more active
utilisation of the local resources, has at the same time reacted favourably on the
development of foreign commercial relations. At the beginning of the century
under the Spanish régime, the annual movement of the exchanges carried on
exclusively through Vera Cruz was about £%,000,000. At present it has in-
creased more than threefold, while the precious metals, which till recently formed
seven-eighths of the exports, have now fallen to two-thirds or even one-half.
Amongst the more important exports are dyewoods, timber, skins and hides,
besides such colonial produce as coffee, vanilla, tobacco, caoutchoue, sugar and
indigo. Mexico also forwards large quantities of fruits to the United States, but
no manufactured goods are exported. "These industries have not yet acquired
sufficient development, nor are they sufficiently specialised to find an opening in
foreign markets. Of imported goods the chief are, in their order of importance,
textiles, machinery, hardware, paper, chemicals, glass and china ware, besides flour
and other alimentary substances. Thanks to the proximity of the United States
and the connecting lines of railway, the first place in the foreign trade of the
country is taken by the northern republic: hence, in the Mexican ports nearly all
shipping documents are drawn up in the English language. Great Britain comes
next in importance to the United States, France occupying the third place. These
three countries, which collectively possess nine-tenths of all the exchanges, are
followed by Germany, whose relations are increasing, especially along the Pacific
coast; whilst Spain, which formerly monopolised the whole trade of the colony,
now takes only the fifth place. |

ECONOMIC CONDITION OF MEXICO. 183

Like the United States, Mexico has endeavoured to foster her industries by a
system of tariffs affecting most objects imported from abroad. As a rule the duties
levied at the seaports or on the land frontiers amount to 38 per cent. of the
declared value. Hence the contraband trade, especially in American cotton
fabrics, continues to flourish all along the line, but principally in the “ free zone,”
where 850 custom-house officers, distributed over a distance of 1,680 miles, are
supposed to keep effective guard over all the exchanges. Some articles, regarded
as useful for the industrial or scientific development of the land, enter free of duty.
In 1889 only eighty ports were open to foreign trade, exclusive of the “land
ports” on the northern and southern frontiers. In 1889 the Mexican seaports
were regularly visited by twelve lines of steamers, six in direct relation with
Europe, the West Indies, and the Eastern States of the northern republic, two
with California, and four engaged on the coast service. The sea-borne traffic by
steam represents nearly one-half of all the exchanges, although sailing-vessels,
mostly flying the national flag, are four times more numerous than steamers in the
movement of the seaports. The coasting-trade is reserved exclusively to Mexican
shipping.

Mexico has lagged a quarter of a century behind the civilised countries of
West Europe in railway building. The first line, connecting Vera Cruz with a
suburb, was not opened tili 1850. Another line, constructed in 1857 between the
capital and the shrine of Guadalupe, was rather an object of curiosity for pleasure-
seekers or devotees than a means of communication subservient to commercial
interests. But after the collapse of the attempt made to restore the monarchy and
the definite recognition of Mexican independence, a beginning was made with the
various projects that had been long worked out for the development of a regular
railway system between the large centres of population. Thanks to the aid of
British, and to a less extent of United States capital, the work was undertaken and
pushed on so rapidly, soldiers being even employed as navvies, that in the course
of a few years Mexico already compared favourably with several European countries
in the relative extent of her railway system. A great obstacle to the progress of
the new means of communication was the line between Vera Cruz and the capital,
which was the first taken in hand, and which happened to be the most difficult of all.
But before any expansion could be given to the system it was considered essential
to open the great trade route, placing the capital of the republic in direct relation
with the ports of the United States, Great Britain, France, the West Indies, and
South America. To accomplish this result enormous works had to be executed,
works unexampled even in Europe. Mountains had to be scaled to double the
height of the highest Alpine tunnels, the three hot, temperate, and cold zones had
to be successively traversed in a vertical direction, in order to reach the region of
snows without extending the route beyond all reason along the interminable slopes
of the lateral valleys. This colossal work has been successfully executed, and the
Vera Cruz line to the capital now offers an amazing series of stupendous bridges,
viaducts, tunnels, sharp curves, steep gradients, and other engineering triumphs.

The Metlac viaduct between Cordoba and Orizaba is a model of constructive

184 MEXICO, CENTRAL AMERICA, WEST INDIES.

skill, in which lightness and strength are happily combined. But the section
between Maltrata and Boca del Monte, giving direct access to the edge of the
Anahuac plateau, is so precipitous that it never fails to excite the apprehension of
travellers, both ascending and descending this tremendous incline, which has a total
rise of no less than 4,000 feet in a distance of sixteen miles in a bee line. At the
highest pass near the Malinche volcano the line stands at an altitude of 8,420 feet
above sea-level, and to avoid a still more elevated pass over the snowy range, it is
deflected northwards, thus obliquely traversing the Mexican valley in its entire

Fig. 79.—Tue Boca pet Monte ASCENT.
Scale 1 : 90,000.

8 300 Yards.

length. With good reason the Mexicans speak of this great engineering work as
a monument of human genius.

To connect the network with that of the United States was a far easier under-
taking. The Anahuac plateau has a general incline from south to north without
any abrupt declivities, so that throughout most of the section between the capital
and the Rio Grande del Norte heavy engineering operations could be dispensed
with. In 1884. two years after the Americans themselves had reached this river
at Laredo, the Mexicans opened their line to Nuevo Laredo on the opposite bank.
The same year they completed another line running parallel with the western
Sierra Madre all the way to Paso del Norte. Railway communication was
thus henceforth continuous between Mexico and San Francisco, St. Louis and
New York: by the latter route passengers were able, in 1889, to travel from

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ECONOMIC CONDITION OF MEXICO. 185

Mexico in eleven days to the Paris Exhibition. Another line crosses the Rio
Grande at Piedras Negras between El Paso and Laredo, and a fourth traversing
Sonora connects the American frontier with the port of Guaymas. But all
these railways, which give North Americans and their wares easy access to
Central Mexico, and which converge towards the heart of the country, constitute
a serious political danger. They lay open the frontier to a powerful neighbour,
who has already occupied about half of the former territory, and who has more
than once threatened to extend the range of her conquests. Hence it becomes all
the more urgent to increase the lines which descend from the uplands to the sea-
board, and which would afford equal commercial advantages to all countries without
any special privilege to the United States. To the Vera Cruz line on the Atlantic

Fig. 80.—Mexican Rattway Sysrems IN 1890.
Scale 1 : 30 000.000

El Pasd del Norte

H =
5 p \
i Ma oros
tab fie
ontere
Altatay Culiacan e VA À =
~— = :
Linar =

== (Zacatecas

—Héuakcalientek 4 2 gampico ——
San Bla S.Luis Potds —— Progress =
Guadalajara put ee
achu =

Colima 6 exe sie ampeche —

Manzanil MEX100% 0 ÇPWeraCruz =
Puebla —— = —

Coatzacoalcos

West of (Greenwich

620 Miles.

side has already been attached the San Luis Potosi—Tampico line; but on the
Pacific side, where trade is less developed than on the slopes facing towards Europe,
the system is not yet completed which will ultimately extend to the seaports of
Altata, Mazatlan, San Blas, Manzanillo, Sihuantanejo, Acapulco, Huatulco, and
Salina Cruz. On this Pacific side the engineering difficulties are as great as on the
Atlantic slope. Thus the line which runs west of the capital across the Ajusco
crests to the heights of Las Cruces near Salazar, attains an extreme altitude of
10,000 feet, or about 2,600 feet above the city of Mexico; this is the highest
point yet reached by the Mexican system.

In 1774, the engineer Cramer, commissioned to survey the isthmus, reported
that a navigable canal might be cut from ocean to ocean without much difficulty and
expense, and in his report he traced the course of such a canal, But no attempt

186 MEXICO, CENTRAL AMERICA, WEST INDIES.

was ever made to realise the project. In 1811 the Spanish Cortes also decreed
the opening of this line, but their decision could be regarded as little more than an
abstractresolution inspired through the fear of losing the empire of the West, Imme-
diately after the constitution of New Spain as an independent state, the geographical
study of the land was resumed ; but no definite canalising projects were formed
till 1842, when José de Garay offered to take such a work in hand. But he failed
to raise the necessary capital, and a like fate befell the American company which
had obtained the concession, in 1867, after the fall of Maximilian. All these now
abandoned projects of an interoceanic canal have been followed by that of a ship
railway on the same plan as that of the Chignecto isthmus in Nova Scotia, but of
far greater proportions. The importance of such a route, especially for the navi-
gation of the United States, is obvious enough. For the trade of the whole world
the best line across Central America would, doubtless, be that of Panama, which
lies on the direct highway from England to Peru, Chili, Australasia, and Indo-
nesia. But the Americans are naturally most interested in the route lying nearest
to their own territory. Most of their traffic is carried on between New York and
San Francisco, on which highway the Tehuantepec route is 860 and 1,630 miles
shorter than those of Nicaragua and Panama respectively. Planned by Eads, the
same American engineer who opened the South Pass in the Mississippi delta,
the Tehuantepec ship railway would be regarded mainly as an American work,
and the future tariff was even arranged in such a way as to favour the American
quite as much as the Mexican seaports. Mexico was, none the less, ready to grant
great privileges to the promoters, such as exemption from taxes for ninety-nine
years, and the grant of nearly 1,250,000 acres of land. The expenditure was esti-
mated at £15,000,000 for a line 150 miles long, the heaviest engineering work
being a cutting 850 yards long and over 100 deep at the highest point of the
waterparting. This would reduce the steepest gradient to less than two in 100
yards ; but the undertaking was suspended by the death of the engineer.

The Mexican telegraph system has been rapidly developed throughout every
province of the republic, having increased threefold during the last decade. It
is now also completed by the submarine cables connecting Galveston with the
Mexican seaboard, and Vera Cruz with the northern and southern ports. Another
submarine line now also joins Salina Cruz, the port of Tehuantepec, with the
Pacific seaports of the Central American republics. Most of the lines belong to
the federal government, though several are also owned by the different states, railway
companies and private corporations. The telegraph and postal services increased
more than fourfold in the eight years ending in 1888; yet the letters forwarded
are still at the low rate of three per head of the population, showing that, com-
pared with the countries of West Europe, instruction has hitherto been in a back-
ward state.

But education also is at last making rapid progress. Most of the states have
adopted the principle of compulsion and gratuitous public instruction for all chil-
dren; but the official returns make it evident that public opinion has not yet
completely sanctioned such measures. At the same time it is impossible to ascer-

GOVERNMENT OF MEXICO. 187

tain the precise number of children attending schools, owing to the carelessness of
provincial governors in forwarding the yearly reports to the federal administration.
It is certain, however, that from decade to decade great progress is being made,
and the attendance at schools already represents a twentieth of the whole popu-
lation, the proportion being highest in the States of Queretaro, Guanajuato,
and Chiapas. But much still remains to be done in the remote districts, and
especially for the Indian populations. Ignorance and superstition are still so
prevalent amongst the natives that so recently as 1874, two “ sorcerers,”” a mother
aud her son, were burnt alive in a village in the State of Vera Cruz for having
caused the death of a young man by incantations. On the other hand brigandage
has rapidly disappeared with the development of the railway and telegraph ser-
vices, and most of the highwaymen have taken to more legitimate pursuits. The
time has passed when travellers were warned by placards posted at the cross-
roads of the capital to provide themselves with money under the threat of being
beaten, or losing nose or ears.

A taste for reading is not yet very widespread ; hence libraries are few and
poorly equipped, although scientific literature has already acquired a certain
value. . It comprises some standard works on a level with the admirable carto-
graphic undertaking, superior to similar works in the United States, which when
finished will contain the whole topography of Mexico in thousands of well-executed
sheets. Popular literature consists mainly in journals, of which at the end of 1888
as many as 120 were issued in the federal district alone, and 385 in the whole
state. In 1852, all publications taken together comprised only 60 journals.
Mexico is one of the Hispano-American countries which claim to speak the best
Castilian.

V.—GovERNMENT AND ADMINISTRATION.

Constituted on the model of the Anglo-Saxon federation, the republic of
Mexico consists of a certain number of independent or sovereign federal states
united together according to the compact of 1857. ach state is, so to say, a
miniature of the confederation, with its chambers and governor, its laws and local
finance. But its deliberations and jurisdiction are confined within certain limits
laid down by the general constitution of the republic. It can neither declare war
nor conclude peace, and all its relations with foreign powers have to be conducted
by the central government.

But independently of all constitutional formulas, there can be no deubt that
at present the populations of the various states, formerly without cohesion or any
sense of national unity, now form a somewhat compact political body. In 1846,
during the war with the United States, no popular movement was made against
the invaders, and the two States of Vera Cruz and Zacatecas even refused, in
virtue of their autonomous rights, to take any part in the war against the North
American republic. But the national sentiment assumed a far more active cha-
racter at the time of the French invasion and the assumption of the imperial title
by Maximilian. When Mexico at last issued triumphant from this formidable

188 MEXICO, CENTRAL AMERICA, WEST INDIES.

struggle, the exultation of victory and the consciousness of nascent strength tended
‘to create a Mexican nation in the true sense of the term. From that time dates
the real history of modern Mexico.

The annexation of Mexico to its powerful northern neighbour, an event confi-
dently foretold by somany politicians as inevitable, becomes daily more improbable as
the country continues to increase in wealth and population. The centres of gravity
of the Mexican and Anglo-Saxon republics will always be separated by a distance
of at least 1,500 or 1,600 miles, and the intervening space largely consists of arid
regions, where the population must always remain scattered. The zone of dis-
affected states, which American adventurers had endeavoured to constitute in the
north between Sonora and Tamaulipas, with the view of dividing the republic and

Fig. 81.— Porrricar Divisions or Mexico.
Seale 1 : 30,000,000.

S ristobal A aie
L/
ares o 115°
£

West of Greenwich:

620 Miles,

annexing it piecemeal, have resumed their place as integral members of the
political organism. Thus Mexico and the United States seem destined to remain
distinct ethnological domains.

Every Mexican citizen is regarded as a freeman, with the right of choosing
his own domicile, of associating with whomsoever he listeth, of coming and going
whithersoever he pleaseth, of bearing arms and freely expressing his thoughts
either verbally or through the press. No titles of nobility or hereditary preroga-
tives are recognised, and all citizens are considered, in virtue of the constitution,
as equal before the law. All are electors on the single condition of themselves
signing their voting-papers. Even foreigners become citizens on acquiring pro-
perty in the country, or when children are born to them, unless within a period
of eight months they express a formal desire to keep their first nationality.

GOVERNMENT OF MEXICO. 189

The number of parliamentary representatives increases with the population ;
for this purpose each state is divided into as many electoral circles as there are
40,000 inhabitants, and each circle elects a representative from candidates over
twenty-five years old for a period of two years. The senators, who must be at
least thirty, are elected for four years, two for each state, so that they number
fifty-six for the twenty-seven states and two territories; every two years half of
the senate is re-elected. The Congress, that is to say, the two chambers combined,
holds two regular annual sessions, comprising a total of at least forty-five sittings;
both deputies and senators receive a yearly allowance for their services. A
permanent delegation of the Congress sits during the recesses. The capital,
where Congress meets, lies not in any of the states, but in a neutral territory, the
so-called “federal district,’ formed by a circuit of ‘two leagues,” or six miles’
radius round the central spot. The president of the Mexican United States,
chosen in the second degree by popular vote, was, till recently, appointed for a
term of four years, but in virtue of an amendment in the constitution passed in
1887, he may be re-elected for a second term, and the president in whose favour
this law was enacted was in fact so re-elected. In 1890, by another law, he was
made president for life. |

The judiciary power is exercised by district and circuit courts and a supreme
tribunal composed of judges elected for a period of six years. The civil and
criminal code is the same for all the states except those of Vera Cruz and
Tlaxcala. Imprisonment for debt is abolished, and the republic binds itself to
reject all extradition treaties for political offences. The decimal system has been
legalised for weights, measures, and currency.

Under the colonial régime the clergy exercised great power in the government
of the country. Its enormous revenues, combined with the spiritual authority
enabling it to open or close the gates of heaven, ensured it the unquestioned
control of the Indian populations. Some of the prelates had incomes ot £40,000,
and, according to Lucas Alaman, the ecclesiastical estate represented half of the
whole property of Mexico. Although the wealth and power of these high
dignitaries were diminished by the war of independence, the clergy still retained
great influence, for the Creole priests, such as Hidalgo and Morelos, who sided
with the people or even stirred them to revolt against Spain, caused those church-
men to be forgotten who, on the contrary, hurled anathemas against the rebels.
About the middle of the present century Lerdo de Tejada still estimated at one-
third of the national territory the lands owned by the clergy. With the revenues
derived from hypothecated trusts and from tithes still illegally collected, this
vast fortune yielded an annual income of about £4,000,000. But in 1855 the

’

clergy numbered altogether not more than 4,615, some “poor curates,” others
prelates and other dignitaries “rolling in wealth.’ A first blow had been given
to the power of the Church by the Spaniards themselves in 1767, when all the
Jesuits residing in Mexico were imprisoned, deprived of their property and then
banished. The revolution was completed nearly a century afterwards, in 1857,

by the mortmain law ordering the immediate sale of ecclesiastical property. But

190 MEXICO, CENTRAL AMERICA, WEST INDIES.

the struggle for ascendency was none the less continued, and the higher clergy
did not consider themselves vanquished till after the fall of Maximilian, the
withdrawal of the French troops, and the definite triumph of the republican
party. They were then deprived of their effects, and the priests lost the right
of superintending schools and ceiebrating their rites in public. The establish-
ment of religious corporations or communities was forbidden, and since 1873 the
Church has been completely separated from the State, which has proclaimed itself
neutral as regards the various cults. Over a hundred Protestant churches,
belonging to twelve different sects and nearly all founded by American mission-
aries, have been built in the capital and in other parts of the country. In 1866
the capital also contained as many as 37 Protestant schools, attended by 1,340
pupils. On the other hand, in several remote districts where the population is
purely Indian, the old Catholic ceremonies are being rapidly forgotten. Many
parishes remain without priests, and the natives cease to practise any outward
form of worship. In nearly all the towns, except in Michoacan, churches have
been transformed to workshops, barracks, warehouses, even circuses for bull-
fights, for this pastime, after having been interdicted, is again permitted.

Although small, the Mexican army is relatively larger than that of the
United States. In 1889 it comprised altogether over 27,000 men with the
gendarmes and rangers; with the reserves it forms a force of 160,000 of all
arms. Mexico also possesses a flotilla of two corvettes and three gunboats, and
naval schools have been founded at Mazatlan and Campeachy. The Mexican
forces are doubtless insignificant compared with the vast armaments of the great
military powers; nevertheless they suffice to weigh heavily on the federal budget,
the expenditure under this head amounting to from £2,500,000 to £3,000,000,
or over one-third of the national outlay.

The finances of the republic were long in a state of the greatest confusion,
especially at a time when foreign traders were able to employ diplomatic influences
for the purpose of raising fictitious claims, and compelling the Mexican Govern-
ment to pledge the customs as security for their demands. Since that epoch, the
revenues of the republic have rapidly increased. Over half of the receipts
are derived from the duties levied at the seaports almost exclusively on imported
goods. Stamps represent a fourth, and direct contributions not more than a
twentieth of the annual budget. Another resource is the profit on coining, which
has acquired so much importance in Mexico, where the various mints have issued
altogether £720,000,000 in gold and silver since their foundation.

To the federal budget must be added those of the different states, which
average about £2,000,000 yearly, and lastly, those of the municipalities, which
have an estimated collective value of from £200,000 to £250,000.

The national debt, although less in proportion than about the middle of the
century, was estimated in 1890 at £26,500,000.

In the Appendix will be found a table of the several states and territories, with
their areas and approximate populations.

a uh

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CHAPTER III.

BRITISH HONDURAS (BELIZE).

= HIS colonial territory, one of the least important in the vast

British Empire, is, geographically speaking, nothing more than a
section of Yucatan, conventionally severed from the peninsula.
On the north, however, the frontier towards Mexico is distinctly
marked by the southern shores of Chetumal Bay, and by the
course of the Rio Hondo. Southwards the Rio Sarstun (Sarstoon) has been
chosen as the political boundary as far as the so-called Gracias-à-Dios rapids.
From this point an arbitrary parting-line runs nearly north to Garbutt’s Falls on
the Rio Viejo (Mopan, or Belize), and is continued thence to the Rio Hondo.
This line, laid down by the treaty of 1860, but not actually surveyed, is assumed
very nearly to coincide with 89° 30’ west longitude.

Physically an integral part of Yucatan, this region was also politically regarded
as within the Spanish main ever since the year 1506 or 1508, when its shores
were visited by Yañez Pinzon and Juan Dias de Solis. But towards the close of
the seventeenth century, some English corsairs seized the island of Carmen, which
half closes the entrance to the Terminos lagoon on the opposite side of Yucatan.
In 1717 they were driven from their stronghold by a Spanish flotilla, and then
took refuge on the east coast of the peninsula; here they founded a settlement,
which, from the name of their leader, was known as Wallace, a term afterwards
corrupted by the Spaniards to Be/ice or Belize. In this outlying station, far
removed from the centre of Spanish authority, they easily held their ground, and,
with the aid of the Indians and half-caste negroes, even overran the surrounding
districts. But in 1730 an expedition was sent against them, which seized their
boats, and fired their cabins and the piles of logwood collected on the beach.
After the departure of the Spaniards, the English settlers returned from the
forests where they had taken refuge, and reoccupied the place.

Again expelled by a second expedition, they again returned, erected fortified
posts at the entrances of all the rivers, and remained henceforth free from all
attack. By the treaty of Paris of 1765 they acquired the right to hold peaceful
possession of the territory already occupied, but only for the purpose of working
the surrounding forests, and trading in the timber and other natural produce.
Their forts and palisades had to be razed, all permanent agricultural settlements,

192 MEXICO, CENTRAL AMERICA, WEST INDIES.

municipalities, and organised forces were interdicted, and the country remained
a political possession of Spain. These conditions were maintained by the treaty
of Versailles of 1783; which, however, enlarged the area of the forest domain
conceded to the descendants of the English intruders, But England was the
stronger power, and the war

Fig. 82.-—Britisn Honpvuras. that broke out towards the

Seale 1 : 2,800,000. close of the last century,

followed by the naval vic-
tory of 1798, enabled Great
Britain to claim, by right

of conquest, the territory
which she had hitherto oc-
cupied by enforced conces-

sion. Thesovereign dominion
which the English now set

up was never seriously con-

tested, and the protests of

the Spaniards were regarded

as mere formalities. The

settlers even continued from

year to year to encroach on

the territories lying beyond

the stipulated frontiers. Thus

the southern frontier, origi-
nally fixed at the Rio Sibun,
was gradually shifted about
110 miles farther south to
the Amatique inlet, at the
head of the Gulf of Hon-
duras.

British Honduras, whose

superficial area is approxi-
mately estimated at 7,560
square miles, is but thinly

Dente peopled, the whole popula-
= == = tion numbering, in 1887,
0 to 50 50 to 500 500 Fathoms somewhat less than 28,000.
Fathoms. Fathoms. and upwards.

In the sixteen years since
1871, the total increase had
only been 3,000, and at present there cannot be more than about three per-
sons to the square mile. Belize is thus by far the least densely-peopled region

60 Miles.

in Central America, a fact explained by the unfavourable climatic conditions,
which make most of it unsuitable for Anglo-Saxon colonisation. There are
scarcely more than 400 English settlers altogether, a number greatly exceeded by

BRITISH HONDURAS. 193

the Spanish half-castes and the descendants of political refugees from the Central
American republics. In the towns the bulk of the people are Mulattos of all
shades, while the hamlets scattered over the rural districts are occupied chiefly
by the so-called “ Caribs,”’ that is, Indians who have, no doubt, some Carib blood
in their veins, derived from the Caribs removed in 1797 by the English from
St. Vincent to the islands on the Honduras coast.

Some 30 miles above the town of Belize the river is fringed by a large
number of artificial mounds, which have not yet been explored. They appear to
have been either burial-places, or raised camping-grounds, to serve as refuges for
the people during the floods. Anyhow, they show that this region was not always
a solitude.

Although within an eighteen-days’ voyage of England, the interior of Belize
is less known than Central Africa. Yet few regions abound more in natural
resources of all kinds. ‘One of the most remarkable peculiarities of the climate
and soil is that almost all the tropical products of commercial value may be grown
in the same zone. I have frequently seen maize, rice, bananas, pineapples,
oranges, coffee, cacao, cotton, cassava, rubber, and cocoanuts all flourishing on the
same piece of land. Cacao of good quality is found growing wild in the forests ;
there is an abundance of fibre-producing plants, particularly henequen and silk-
grass, varieties of the aloe, and there is a large extent of land suitable for cattle
and mule breeding.”’* In the southern part of the t rritory, the area of drainage
within the British frontier is very narrow; the | ills in this district are, for the
most part, merely the advanced spurs of the Sierra de Chama, which traverses the
Guatemalan province of Alta Vera Paz. In these unexplored regions the
highest summits visible from the sea exceed 1,000 feet, while the little isolated
group of limestone rocks known as the “ Seven Hills,” terminating in a head-
land on Amatique Bay, falls to about half that elevation. Northwards, pine-
clad cliffs skirt the shore at a certain distance inland, forming, so to say, a second
beach rising above the low-lying coast zone.

THe CockscomB MouxTAINs.

In British Honduras the highest mountains are the Cockscomb range,
which are also connected by a lateral ridge with the Guatemalan system. The
loftiest peaks lie within British territory, where the main crest is disposed in the
direction from west to east, while from the northern slopes torrents descend to the
River Belize. These uplands, which are richly wooded on their lower flanks, and
dotted with a few pine-trees on their higher escarpments, consist partly of granite,
as shown by the rolled blocks in the beds of the torrents. Explorers have
specially noticed hard limestones veined with quartz and vertically disposed schists,
which are very difficult to scale. Those are probably the pedernales which Cortes
and his followers took twelve days to cross during his wonderful expedition to
Honduras in 1524. Victoria Peak, the culminating point, ascended for the first

* J. Bellamy, Proc. R. Geo. Soc., September, 1889.
46

194 MEXICO, CENTRAL AMERICA, WEST INDIES.

time during the Goldsworthy expedition of 1888, has an altitude of 3,700 feet.
Other summits, one of which was named, from the geologist of the expedition,
Bellamy Peak (2,700 feet), follow in the direction from west to east, where the
range terminates abruptly in a few hills or low offshoots. Victoria Peak, which
presents the aspect of a sharp and apparently inaccessible needle, was, neverthe-
less, scaled by several members of the expedition, aiding themselves with ropes
and a few gnarled and stunted fig-trees.

“The top of Mount Victori: is a thorough peak, with but little room for
moving about, and an extensive view is obtained on all sides. For some distance
the prospect is nothing but alternate ridge and valley, densely wooded. There
were no higher points north of us, but to the south Montagua and Omoa, in
Spanish Honduras, were seen towering above the rest. No open country was
seen, nor any of the traditional lakes.’ * In the Cockscomb and conterminous
Guatemalan uplands geologists have discovered iron and lead ores as well as traces
of gold and silver. But whenever these highlands become connected with the
neighbouring seaports, they will have the still greater advantages of offering to
agricultural settlers many fertile valleys, and a fur more healthy climate than
that of the surrounding lowlands. Here sooner or later will be established the
health-resort of British Honduras.

Rivers.

The low-lying plains receive an abundant rainfall, the excess finding its way
to the sea through numerous and copious streams. The Sarstun, on the southern
frontier, is 700 yards wide at its mouth, and has nearly seven feet of water at the
bar; within this obstruction vessels ride at anchor in depths of 35 or even 40 feet.
The other rivers, following northwards, although generally rising nearer to the
coast and less voluminous, are all equally navigable. Some even send down
sufficient water to fill the coast lagoons on both sides, and carry far seawards two
banks of alluvial matter. One of the largest is the Sibun, which reaches the sea
a few miles south of the capital, after traversing a region of limestone hills pierced
by underground galleries. It receives some of the waters flowing from the Cocks-
comb range, which however is chiefly drained by the Mopan, or Belize as it is usually
called by the English. This river rises south-east of Lake Itza, or Peten, in Gua-
temala, and after a winding north-easterly course enters British territory at the
Garbutt Falls. Here it is known to the inhabitants by the Spanish name of Rio
Viejo, or “Old River,” probably because before the arrival of the English settlers
it had already been used as a navigable waterway. The Belize deposits a great
quantity of sediment in the shallow waters about its mouth, where a long alluvial
peninsula has thus been formed, which projects beyond the normal shore-line.
North of the Belize no other rivers worthy of the name are met except the Nuevo
and Hondo, which discharge their waters at the south-west corner of Chetumal
Bay. The Hondo, that is, “ Deep,’’ deserves its name, being navigable for a great
part of its course, which forms the frontier-line between British Honduras and

* Bellamy, loc. cit.

BRITISH HONDURAS. 195

that part of Yucatan which is still held by the independent Indians. Both the
Nuevo and Hondo traverse low-lying districts studded with shallow lakes which
communicate with the shifting fluvial channels.

THE SEABOARD.

For a aistance of 155 miles, between the Amatique and Chetumal inlets, the
whole seaboard is fringed by an outer coastline formed by coral reefs, which here
and there develop wooded cays, islands, and inlets, the lines of mangroves grow-
ing even on the still submerged banks. The space between the two coasts, which
is no less than eighteen miles wide, is fur the most part occupied by shoals covered
by only a few yards of water. Nevertheless winding channels sheltered from the
surf run parallel with the seaboard between the coral beds, and thus form a valuable
line of inland navigation available for the coasting trade.

Seen from the high sea, the chain of breakers separating the inner lagoons
from the outer waters seems impassable, nor can they be crossed without a pilot
even by skippers provided with the best charts. Nevertheless some of the passages
are very deep, that of Belize, amongst others, ranging from 50 to 150 feet and
upwards. Others, again, are so shallow that the local fishermen are able to wade
across them. The opening between the Yucatan mainland and Ambergris, largest
of the cays, is accessible only to small craft drawing less than 30 inches.

Chetumal Bay, which is separated from the sea by Ambergris Island, presents
the same general features as the two more northerly bays of Espiritu Santo and
Asencion in Yucatan, but it is far larger, having a superficial area of some 400
square miles. The whole basin teems with coralline life, and the reefs in process
of formation, covered with a mean depth of from 10 to 16 feet of water, are highest
at the entrance of the passage, growing more slowly towards the head of the
inlets, where;depths of 24 to 26 feet are met. The inland basin itself is navi-
gated only by flat-bottomed craft, which are engaged in shipping timber and dye-
woods about thé mouths of the rivers. It is noteworthy that both shore-lines, the
already consolidated beach on the mainland and the outer chain of cays, run nearly
parallel to each other, and that the latter forms the direct southern continuation
of the east Yucatan seaboard. Moreover, the valley traversed by the Belize river
above its great bend round to the east is continued northwards by a series of
lagoons and by another fluvial valley, that of the Rio Nuevo (New River), all of
which are disposed in the same direction, forming with the west side of Chetumal
Bay athird line parallel with that of both shores.

The Rio Hondo also flows in the same direction along the foot of a cliff which
may likewise have been an old shore-line. Lastly, still farther inland, the parallel-
ism is maintained in the interior of Yucatan by the twin Mariscal and Bacalar
lagoons, and if the maps of this part of British Honduras can be trusted, other
lagoons, such as Aguada San Pedro, Aguada Concepcion and Aguada Carolina,
all follow the same general direction, which would appear to be that of successively
developed coastlines. But this hypothesis still awaits confirmation from the

196 MEXICO, CENTRAL AMERICA, WEST INDIES.

geological survey of the interior, which will probably show that the hanks of the
parallel rivers and lagoons are really composed of coralline rocks constituting
west and east a series of terraces with very broad steps. An analogous pheno-

Fig. 83.—PARALLELISM OF THE OLD AND RECENT WATERCOURSES.
Seale 1 : 3,000,009.

=p
82a y

te
=

:: -Beliz

ee
West of Greenwich

0 to 50 50 to 500 500 Fathoms
Fathoms. Fathoms and upwards.
60 Miles.

menon is presented by the concentric shores of Florida, which were successively
formed by the coral-builders during the course of ages.

The islands in the gulf beyond the fringing reefs also follow the general
direction and belong to the same formation. Thus Turneffe, that is, Tierra Nueva,
a verdant group facing Belize, rests on a foundation of reefs whose channels, partly.

BRITISH HONDURAS. 197

obstructed by sand, form natural reservoirs for fish and turtles. Turneffe may
be regarded as a large island disposed in a line with the Chinchorro bank and
Cozumel Island in the Yucatan waters. It looks like a first instalment towards a
future beach, while yet another shore-line in course of development seems to be
indicated by the more distant Glover and Lighthouse rocks.

CLIMATE, FLoRA, Fauna.

British Honduras, a mere political enclave at the neck of the Vucatan peninsula
between Mexico and Guatemala, differs little in its climate from these regions.
At Belize the mean temperature is about 78° or 80° Fahr., and although even
in summer it scarcely rises above 86°, the heat is very difficult to bear, owing to
the humidity of the atmosphere. In the town of Belize, surrounded by rivers,
lagoons and swamps, fogs are frequent and dews abundant; hence the sky is
mostly overcast, and when the west wind blows, the mosquitoes arrive, with
‘intermittent agues caused by the exhalations from the neighbouring marshes.
Winter is the best season, when the northern winds prevail, and when the roar
of the breakers is heard on the chain of islands, under whose shelter the water
remains calm at Belize.

The flora and fauna of British Honduras resemble those of Yucatan, but in
ail the non-calcareous and well-watered valleys the forests are far more extensive
and leafy. In the interior the woodlands alternate with pastures such as those
of Peten, where hundreds of thousands of cattle might be raised, but where the
destructive nigua (pulex penetrans) has been introduced from the east. The
British Honduras waters are well stocked with fish, and here large numbers of
turtles are captured for the London market.

ToPOGRAPHY.

The town, which under the Spanish form of Belize still bears the name of its
founder, the freebooter Wallace, lies on the west side of the inner lagoon, where
the scarcely emerged land is traversed by the Rio Viejo (Mopan, or Belize). The
two quays of the port are connected by a wooden bridge which crosses the
mouth of the river. But the ground is so low that it has had to be artificially
raised with the ballast of vessels frequenting the harbour, with driftwood and
other flotsam Nevertheless a tide a little higher than the usual, which scarcely
exceeds twenty inches, would suffice to flood the houses. Most of these are built
of wood. or rest on piles, for stone or brick would soon sink into the spongy
soil. A few villas stand on the neighbouring islets, these being considered more
salubrious than the town, beyond which extends a marshy tract crossed by embank-
ments. The harbour shoals so gradually that it is accessible only to vessels of
light draught ; it is also exposed to the east winds, though the surf is broken by
the islands fringing the coast and by the more distant reefs. The cnly supplies
procurable on the spot are the fish and other produce of the neighbouring waters ;

198 MEXICO, CENTRAL AMERICA, WEST INDIES.

itis quite impossible to raise any crops on the flooded or swampy ground in the
neighbourhood, and Belize formerly drew nearly all its provisions from Bacalar
in Yucatan, whence they were forwarded by Chetumal Bay. But since the
destruction of that place, supplies are drawn from various parts of the seaboard,
and especially from the United States across the Gulf of Mexico. Although
surrounded by rivers, Belize is unable to procure any water even from the Mopan,
and is supplied by cisterns. But while the neighbouring forests abounded in
mahogany, campeachy wood and cedar, which were easily floated down in the

Fig. 84.—BELIzE AND THE CocxscomB Mounrains.
Scale 1 : 1,600,000.

SS ee

LT 7 FES:

West of Ca 88°: 30

Depths.
O0 tod 5 to 50 50 to 500 500 Fathoms
Fathoms. Fathoms. Fathoms. and upwards.

30 Miles.

form of rafts, the settlers did a flourishing trade, and grew rich despite the many
drawbacks of the position. Now, however, timber of large size has become rare,
and the inhabitants, mostly blacks or people of colour, have been compelled to
engage in other pursuits, and at present the trade of Belize consists chiefly in
produce and wares imported from the United States and Great Britain, which
are redistributed amongst the Atlantic ports of Guatemala and Honduras. The
local exports are chiefly fruits, and most of the traffic is served by a steamer
plying regularly between New Orleans and Belize.

The population of the town has fallen from nearly 11,000 in 1844 to less than
6,000 in 1889, and Belize can scarcely fail to continue to decline whenever more

BELIZE—VIEW TAKEN FROM THE HARBOUR.

SAR OEE GORE MND EEE QUES igs en, | gare LL

’ : A

BRITISH HONDURAS 199

frequent direct communications are established between the Central American ports
and those of Europe and the United States. A revival of prosperity may, however,
be brought about by developing the neighbouring sugar, coffee banana, orange,

Fig 85.—Domarxs or British Honpuras.

Scale 1 : 2,500,000.

yf MKGyy RQ
/ NZ

toe

CRAN 2080

hay otebeierers
sms,

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ORCI OE SO ROROM CCN ECC
pce eo hee

OM eS

LL Purrtas

Westat Greenwich

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Crown Lands. Domain ofthe Other Cuuvessions,
Belize Estate Company.

60 Miles.

caoutchouc and henequen plantations, and by opening new routes or railways with
the inland districts of Peten and Yucatan. But such prospects appear somewhat
remote, at least so long as most of the estates continue to be held by absentee pro-

200 MEXICO, CENTRAL AMERICA, WEST INDIES.

prietors, unwilling or unable to develop the local resources. One land company
alone owns over one-third of the colonial domain, although unable to utilise a
hundredth part of its property.

The port of Corosa/, or Palmeraie, occupies a favourable position at the mouth
of the New River and not far from the Rio Hondo; it is thus the natural outlet for
the timber felled in these two fluvial basins. Corosal has also naturally benefited
by the destruction of Bacalar, which was situated some 30 miles to the north-west,
on the lagoon of like name. Those who escaped the fury of the Indian rebels’
emigrated in mass to British territory, and Corosal is now the second town in
the English colony, with flourishing sugar plantations, and about 5,000 inhabi-
tants, mostly of Spanish speech. The other settlements are mere hamlets or
plantations, or else fishing villages such as San Pedro, on Ambergris Island, which
does some traffic with Belize. The most important ports on the coast are Stann
Creek and Punta Gorda, both occupied by Carib settlers, who have cleared large
tracts and supply Belize with cattle, fruits, and vegetables. About 700 negroes’
from the Southern States have also founded the settlement of Toledo, about ten
miles south of Punta Gorda, where they are chiefly occupied with sugar-growing.
Turneffe has only a single fishing hamlet, though the explorations have shown
that it was formerly far more densely peopled.

ADMINISTRATION,

British Honduras is a Crown Colony, under the direct control of the Home.
Government, and administered by a Governor, with a legislative council of ten
members. The annual budget of over £40,000 consists chiefly of custom-house
dues, supplemented by a grant from Great Britain ; a small sum is also raised by
the sale of lands at the relatively high price of nine shillings an acre. Few
small holders, however, venture to settle in the neighbourhood of the powerful
financial companies. Belize and some other ports are occupied by a few troops
from Jamaica. In 1872, they were called upon to protect the frontier against an
incursion of the Maya Indians. The blacks of Belize enjoy the privilege of self-
government, electing a “queen,” who is enthroned with great pomp, and to whom
they submit all their little differences.

BOQ. Saye

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CHAPTER IV.

CENTRAL AMERICA (GUATEMALA, HONDURAS, SAN SALVADOR, NICARAGUA,
COSTA RICA).

I.— GENERAL SURVEY.

JHE long strip of tropical lands disposed in the direction from north-
west to south-east between the Tehuantepec Isthmus and the Atrato
valley, constitutes a geographical region quite distinct from the
great continental masses of North and South America; they are,

however, usually grouped with the northern section of the New
World, to which they are attached by a broad base gradually narrowing south-
wards. Ina remote geological epoch they were detached from both, constituting
a chain of islands analogous to those of the West Indies. But the exploration of
these lands is still far from complete, except in a few districts separated from each
other by less-known intervening tracts ; hence it is not yet possible to indicate the
exact outlines of this insular chain before the marine channels were filled up, It
seems evident, however, that this process was not accomplished in a single epoch,
and some of the passages still persisted for long ages after others had been changed
to dry land either by eruptive formations or by alluvial deposits.

Some of the ancient interoceanic channels, such as those of Tehuantepec and
Nicaragua, may still be clearly traced along their primitive shores. The Costa
Rica and Panama peninsulas are also now attached to the mainland by isthmuses
whose original marine character is easily determined. The other straits are more
difficult to recognise ; but itis no longer doubtful that the sea formerly occupied
the central depression of Honduras at the Guajoca and Rancho Chiquito passes,
as well as the central plateau of Costa Rica, at that of Ochomogo. Other channels
flowed between Chiriqui and David Bays, while the track of the Panama and
Darien Canals was already indicated by the former marine depressions, one of
which is also now occupied by the valley of the lower Atrato. The narrowest part
of these isthmuses has been attributed politically to the South American State of
Colombia ; but such official awards correspond in no way with the divisions far
more sharply traced by the hand of nature herself. Thus the physical limit of
Central America is still clearly determined in Colombian territory by the course
of the Atrato, the wooded morasses lining its banks and the depression connecting
this fluvial basin with that of the San Juan.

202 MEXICO, CENTRAL AMERICA, WEST INDIES.

Central America, taken in its narrowest political sense, that is, as the region
of isthmuses—excluding Chiapas, which belongs to Mexico, and the double crescent
of Panama, which is included in Colombia—has more than once constituted a single
political dominion. Under the Spanish rule the Royal Audienza of Guatemala,
which also comprised the present Mexican province of Soconusco, extended south-
wards to Chiriqui Bay. Ia 1823, when the independence of Guatemala was pro-
claimed, the southern provinces continued to form part of the new republic, of
which Guatemala was the capital. But in 1838, after much civil strife, this con-
federacy was definitely dissolved, and Central America became decomposed into the

Fig. 86.—Oxp Srrarrs IN CENTRAL AMERICA.
Scale 1 : 215,000,000.

aul

SS
.

West of Greenwich

300 Miles.

five autonomous States of GUATEMALA, Honpuras, SAN Satvapor, Nicaracua and
Costa Rica.

But in 1879, the constitution of Guatemala already anticipated an intimate
political union between the various republics, and engaged on its part to maintain
and cultivate “ mutual family relations” with them. It also expressed the wish
of the people to again form part of a larger Central American nationality. All
natives of the neighbouring republics became by right Guatemalan citizens by
merely expressing a desire to that effect. At the same time, all these acts of
fraternal legislation were accompanied by warlike armaments, to compel the other
states to join the union should they prove refractory. In 1886, on the initiative
of Guatemala, a congress was held for the purpose of preparing a new scheme of

MAL.

Re OR pal F

—— eee ee « " à

CE PA

CENTRAL AMERICAN STATES. 203

federation, and next year it was decided that all disputes between the several
states should be henceforth decided, not by war, but by arbitration. In order to
give practical effect to that principle, Costa Rica and Nicaragua, at that time
at war about a question of frontiers, appealed to the decision of the United States
President. Lastly, the congress assembled in September, 1889, in the city of
San Salvador, concluded a treaty of union between the five states, thereby
constituting themselves a federation under the name of “ Centro-America,” for a
provisional term of ten years. According to this official project, the novitiate

Fig. 87.—Pozrricaz Divisions oF CENTRAL AMERICA.
Scale 1 : 17,500,000.

je)
=

LULU UE UN UMA IL

=, } & a
OR .

S Sa wade

West of Greenwich.

300 Miles.

should be brought to a close in 1900, when the definite federal constitution will
be proclaimed.

But scarcely had this federal compact been signed when disappointed ambi-
tions tore it to shreds. A fierce war broke out between San Sulvador and
Guatemala; Costa Rica and Honduras soon after joined in the fray ; and no sooner
had these troubles been momentarily quelled than Honduras became the scene of
a sanguinary revolution, calling for the active interference of Guatemala. In
the middle of November, 1890, President Bogran, of Honduras, had to fly for his
life, and a de facto government was proclaimed by General Sanchez, leader of the
revolutionary party Sanchez was soon after captured and shot, But towards

204 MEXICO, CENTRAL AMERICA, WEST INDIES.

the close of the year the outlook was extremely gloomy, and all the Central
American states threatened to be involved in a general conflagration.

The great length itself of Central America, which extends south-eastwards
for a distance of about 750 miles, with a comparatively narrow mean breadth,
seemed already to point at a future rupture between the various ethnical groups
in this region. Here the inhabited zone is even considerably narrower than the
strip of land itself. The civilised populations, Spanish or Mestizo, have nearly
all settled along the Pacific coast, so that, on the opposite slope, the great fluvial
basins of Guitemala, the northern forests of Honduras, the almost unexplored
valleys of Mosquitia, are, so to say, so many desert regions, occupied by a few
half-savage scattered tribes. Thus the civilised peoples, those who have con-
stituted themselves in republican states, form little more than a slender cordon
of towns and villages stretching along the west side of Central America. This
ethnical contrast between the two oceanic slopes is in great mzasure explained by
the physical contrasts of soil and climate. On the Pacific side are found nearly
all the more fertile and less humid lands, which offer a more regular alternation
between the dry and the rainy seasons. But other causes also tend to the relative
depopulation of the Atlantic seaboard. Columbus here first began to kidnap the
natives, and his example was followed by the West Indian planters in search of
slaves to cultivate their estates. Thus all the lands accessible by sea, or by the
rivers, were wasted, and the populations that escaped capture by the slave-hunters
took refuge in the remote interior. Then the Spanish settlers were naturally
unable to establish factories and develop plantations in a depopulated and unculti-
vated region. Nevertheless, they needed, at any cost, fortified stations to main-
tain the communications with the mother country ; but when Spanish supremacy
in the West Indian waters was supplanted by that of the buccaneers, these posts
themselves were often attacked and captured. Thus, of the two Central American
seaboards, the eastern, facing towards Europe, was the “dead,” the western,
skirting the boundless waste of Pacific waters, the “ living ” coast.

But the relations have greatly changed since Central America has ceased to
be a remote dependency of Spain. In the first place the population has increased
more than threefold; at the census of 1778 the “kingdom” of Guatemala,
excluding the province of Chiapas, had a total population of 847,000, which had
risen to about a million in 1821, when Guatemala declared its independence of
Spain. Since that time the inhabitants of the five republics have more than
trebled ; the groups of settlers, formerly isolated, have been gradually brought
closer together by the foundation of intermediate colonies, while the Atlantic
slope has been partly reclaimed for cultivation, and already possesses its towns and
seaports.

Before the introduction of steam navigation, the communications were rare
and uncertain, depending on the seasons and the winds, and even under the most
favourable conditions they were always less rapid than at present. The general
service of packets plying between the seaports and on both sides, arriving and
departing with the regularity of clockwork, has reduced by more than nine-tenths

CENTRAL AMERICAN STATES. 205

the dimensions of Central America, measured not by miles, but by hours. More-
over, the interoceanic roads and railways have almost brought into close proximity
coastlands which were formerly separated by journeys of several days, and even
weeks. A project has recently been submitted by the President of the United
States to Congress, having for its object the exploration of the Central Americ in
States preparatory to the construction of a railway to run longitudinally from
Mexico, through Oaxaca, Guatemala, and San Salvador to Panama.

But much preliminary geographical work remains to be done before any such
scheme can be taken in hand. Certain regions, such as the metalliferous districts
of Darien, which were formerly well known, have even fallen into oblivion. In
the uninhabited tracts, so difficult ure the routes across the swamps and densely-
wooded uplands that small exploring parties run great risks, over and above the
exposure to the dangerous hot and moist climate. Paths have to be cut through
the dense tangle of trees and creepers, and the traveller has to avoid the im-
penetrable thickets, precipitous escarpments, slopes liable to frequent landslips,
gorges flooded by rushing torrents, bottomless quagmires, from which escape is
impossible. Explorers provided even with the best guides and porters have
often been unable to advance more than one or two miles a day, and have at times
been fain to give up the struggle and retrace their steps.

The labour already expended during the course of four centuries in discovering
or creating interoceanic highways represents a prodigious outlay of energy,
which would have certainly sufficed to accomplish some one great work had it
not been frittered away in a thousand different essays. The first survey was
made by Columbus himself, who, in 1502-3, skirted the Central American sea-
board from Honduras to Veragua in search of the passage which he hoped would
lead him to the “mouths of the Ganges.” During this voyage he at all events
heard of another sea, which lay a little farther west. Ten years afterwards
Nuiez de Balboa, at the head of nearly 800 Spanish soldiers and native carriers,
forced his way across swamps and rivers, tbrough forests and hostile populations.
In twenty-three days of incessant struggles and hardships he succeeded in crossing
the isthmus, here 40 miles wide, and thus reached the spacious inlet which he
named the Gulf of St. Michael. Advancing fully armed into the rising flood,
he took possession of the new ocean ‘with its lands, its shores, its ports and
islands, from the north to the south pole, within and without both tropics, now
and for ever, so long as the world shall last, and unto the judgment day of all
mortal races.” But the strait still remained undiscovered, and it was being
sought in the waters west of the Antilles, when Magellan had already found it
at the southern extremity of the American continent.

When it became evident that there existed no marine passage between the
Caribbean Sea and the Pacific, the idea naturally occurred of opening such a
passage across one or other of the narrow isthmuses separating the two oceans.
Such an undertaking was beyond the exhausted resources of Spain ; nevertheless
expeditions were made for the purpose of studying the problem at the isthmus
of Tehuantepec, on the banks of the San Juan and Lake Nicaragua, at Panama,

206 MEXICO, CENTRAL AMERICA, WEST INDIES.

and other points. Since the Central American states have asserted their inde-
pendence such projects have followed rapidly one on the other, all based on
individual or collective surveys, and promoted by costly expeditions, official
encouragement and concessions, lastly even by colossal operations actually begun
and actively prosecuted for years. The annals of Central America record no less
than a hundred plans and schemes for cutting the isthmuses since the year 1825,
when the Mexican Congress had the Tehuantepec region again surveyed, and
more accurate information brought to bear on the project brought forward by
Orbegozo in 1771. Panama, like Constantinople and Alexandria, lies at a point
of paramount importance for the growing commerce of the world; if before the
era of universal peace the leading nations agree to proclaim the neutralisation
of certain places essential to the well-being of the human race, assuredly the
American isthmuses will be included in the category of such territories.

IJ.—GuATEMALA.

This republic is by far the most important of the five Central American states,
for it contains nearly one-half of their collective population. Like its Mexican
neighbour, it still bears a name of Aztec origin, the term Guatemala (Quauh-
temallan), according to some interpreters, meaning “ Eagle Land,” though
a less poetic etymology gives it the signification of “Land of the Wooden
Piles.” Others again write, U-ha-tez-ma-la, a group of syllables which would
mean, “ Mountain vomiting water,” the whole region being so named in reference
to the Agua (“ Water”) volcano, one of its loftiest cones.

Guatemala corresponds very nearly to the two former Spanish provinces of
Quezaltenango and Guatemala, though the frontiers have been shifted in many
places, while in others they were never accurately determined. Those at last
officially adopted coincide neither with the natural geographical divisions nor
with the distribution of the ethnical groups. Thus the whole of Soconusco with
a part of Chiapas would seem properly to belong to Guatemala, of which they
form an orographic extension. On the other hand Peten, inhabited, like Yucatan,
by Mayas, and also resembling that region in the nature of its soil and products,
should form a political dependency of that region rather than of Guatemala,
from which it is separated by a steep mountain range. Towards British Honduras
the frontier has been drawn by a straight line across mountains and valleys, from
one torrent to another, the political border coinciding with the natural features
only in the district where it follows the Sarstun river to its mouth in Amatique
Bay. Eastwards the territory of the republic is limited by a meandering line,
which runs north-east and south-west from the mouth of the Rio Tinto on the
Atlantic to that of the Rio Paza on the Pacific. This line follows the crests of
the hills throughout a great part of its course, though here and there the boundary
is purely conventional. Taken as a whole Guatemala, excluding the northern
plains, has the form of a triangle with its base on the Pacific and its apex
projecting towards Honduras Bay.

GUATEMALA. 207

PuysicAL FEATURES.

Tn its main outlines the relief of Guatemala is extremely simple. The more
elevated part of the plateau skirts the Pacific at a mean distance of 50 or 60
miles from the sea, and presents in this direction its more precipitous but also its
more regular escarpments. The slope facing the Atlantic, although much longer
and more gentle, is more difficult to traverse, owing to its abrupt ravines and the
deep gorges excavated by the running waters. The Guatemalan range does not
terminate in a sharp crest, but, on the contrary, is rounded off towards the summit,
where it broadens out in granitic plateaux of various extent, forming, so to say,
so many mesas, or “ tables,” somewhat analogous to those of Anahuac. The great
irregularity of the sierra is due to the volcanoes, which have risen above these

Fig. 88.—TREND oF THE GUATEMALAN RANGES.

Seale 1 : 4,500,00C.

Cos Si
West of Greenwich gg9°

60 Miles.

mountains but which are not disposed in a line with the sierra itself. Towards
the frontier of Chiapas and in the Altos, or uplands, of Quezaltenango, the great
eruptive cones lie exactly on the upper edge of the plateau, their slopes merging
in the escarpments of the pedestal on which they rest. But farther on, that is,
in the direction of Salvador, the axis of the volcanoes running almost due south-
east ceases to coincide with that of the sierra, which trends more to the north,
while the lofty pyramids rise midway on the slope of the range, where they are
enclosed by a rampart of ravines. But to the traveller coasting along the Guate-
malan seaboard, the peaks which he sees rising at intervals above the land horizon
seem to shoot up from the very crest of the mountains.

The elevation of the escarpments rising above the southern shores of Guatemala
falls gradually from the frontiers of Chiapas south-eastwards in the direction of
Salvador. In the Altos or “ Heights,” as the western part of the state is called,

208 MEXICO, CENTRAL AMERICA, WEST INDIES.

the plateaux exceed 6,500 feet ; that of Totonicapam rises even to 8,000 feet, while
the chief summits tower some 3,000 feet still higher. The great central plain of
Guatemala, lying on the waterparting between both oceanic slopes, has a mean
altitude of 5,000 feet, and is dominated by the crater-shaped peaks of the Antigua
district, which reach an elevation of 10,000 feet. Lastly, in the eastern provinces
the uplands do not appear greatly to exceed a mean height of 3,300 feet, with
culminating peaks from 4,000 to 5,000 feet.

South-east of the active Tacana volcano, which has been chosen as the boun-
dary between Mexico and Guatemala, the next igneous cone is Tajomulco, which
also exceeds 11,660 feet; it dominates the plateau under the form of a huge
and perfectly regular cone clothed at its base with dense forests. The Indians
here find large quantities of sulphur, which led Dollfus and Mont-Serrat to sup-
pose that the deposits were constantly renewed by solfataras as fast as they were
cleared away. Here flames were distinctly seen shooting up by Bernouilli in 1863.
Beyond Tajomulco no burning mountains occur till Quezaltenango is reached.
This group comprises three cones disposed north and south, the northern, some
ten miles from the town, being a mere hiilock 600 or 700 feet high. But the
southern, Santa Maria, whose superb peak, 12,400 feet high, is visible from the sea,
is one of the most imposing mountains in Guatemala. Like the other it has been
extinct from time immemorial, and dense forests now clothe both its flanks and
the crater. In most of the Central American eruptive groups the southern
volcanoes have remained longest active; but here it is the central cone, the Cerro
Quemado, called also the Quezaltenango volcano, that still continues in a dis-
turbed state. Less elevated than Santa Maria, the Cerro Quemado (10,250 feet)
in no way presents the aspect of a typical volcano. Its symmetry was doubtless
destroyed during the last eruption of 1785, when the entire terminal cone was
blown away, leaving in the place of the crater a spacious irregular plain covered
with a chaos of boulders, between which fumeroles are now seen to rise. Since
then it has been quiescent.

East of the Quemado and beyond the deep gorge of the Rio Samala rises Mount
Zuiil, or the “ Volcano,” as it is emphatically called by the natives. Yet no
record remains of any eruption, nor has any explorer yet discovered, in the dense
forests clothing its flanks, the aperture through which the lavas were formerly
ejected from this cone, which, like those of the surrounding district, consists of
trachytic porphyry. About eighteen miles farther on, and ina line with the axis of
this igneous system, the extinct San Pedro (8,300 feet) raises its pyramidal peak
near the south-west corner of Lake Atitlan. About ten miles farther east three
other cones, connected at their base, are disposed north and south transversely to
the main chain. The two northern peaks, both about 10,000 feet high, terminate
in small craters already overgrown with vegetation; but the underground forces
are still active in the southern member of the group, which is commonly known as
the Atitlan volcano, and which towers to a height of 11,800 feet. At the time
of the conquest, Atitlan was in a state of commotion, and when the natives heard
the continuous rumblings in the interior of the mountain, they threw a young

PHYSICAL FEATURES OF GUATEMALA. 209

maiden down the crater in order to propitiate the angry demon. It was again
active in 1828 and 1833, and since that time abundant vapours have been con-
stantly emitted by the crevasses near its summit.

But the most famous volcanoes in this region are those which dominate the
central part of the plateau in the vicinity of the successive capitals of Guatemala.
Looking southwards from the pleasant city of Antigua, the eye sweeps over a

Fig. 89.— Car oF THE FuEGo Vorcano.
Scale 1 : 60,000.

Wy
Z

TIRE
LE

SN S
Sassy
D =

AWW

EN
=>

hi iN A
NN SS
2 Ly Hi K { NS
COLLE = A iN
SE NE
Se i)
\ N\ | CPE SF
AS NI
oo 2
+ West of Greenwich 90°45’

2,200 Yards.

magnificent prospect of cultivated plains, where the horizon is bounded on both
sides by the harmonious profile of the mountain ranges, towering 6,000 feet above
the surrounding plateau. On one side is the chain terminating in the Fuego,
or “Fire,” on the other the Agua, or “ Water,” volcano. The eastern sierra,
where one crater is still active, is itself merely an elevated ridge above which
rise nine or ten eruptive cones, all disposed in the direction from north to south.
The northern craters, which are all extinct and overgrown with vegetation,
47

210 MEXICO, CENTRAL AMERICA, WEST INDIES.

culminate in the Acatenango cone, called also Pico Mayor, or Padre del Volcan
(“Father of the Volcano”), because it rises higher than Fuego, and is, in fact,
the loftiest summit in the whole of Central America (13,700 feet). It was
ascended in 1868 by Wyld de Dueñas, who found nothing but three nearly
obliterated craters, although sulphurous vapours were still escaping from a
crevasse in one of them. Acatenango is separated by a deep ravine from the.
southern group, which includes the vast but partly breached Meseta cone.
Beyond it follows Fuego (13,200 feet), whose summit, scaled for the first time
by Schneider and Beschor in 1860, terminates in a narrow bowl about 85 feet
deep; immediately to the south is seen a tremendous chasin, nearly perfectly
round, over 450 yards in diameter and no less than 2 000 feet deep. Fuego was
in full eruption at the time of the Spanish invasion, and the terror it inspired
in the natives seemed to show that they had previous experience of its destructive
energy. Since that time explosions bave been frequent, and the surrounding
districts have often been laid under ashes.

Agua, which corresponds to Fuego on the other side of the valley, although
not quite so lofty (12,360 feet), presents a more majestic appearance due to its
completely isolated position. “Seen from Escuintla, near its southern base, it
seemed “the most lovely sight in the world” to Dollfus and Mont-Serrat, by
whom it has been scaled. The gaze here follows the perfect curve of its escarp-
ments unbroken by any disturbing prominence, while the vegetable zones—
cultivated ground, leafy forests and pine groves—follow with their varying tints
one above the other along its regular slopes. Despite repeated assertions to the
contrary, Agua has never been in eruption since the epoch of the conquest. The
catastrophe to which it owes its name was caused by the bursting of the rim of
the crater, which was flooded by a terminal tarn at the summit of the mountain.
To reach this point travellers usually pass through the breach, and here some
idea may be formed of the liquid mass formerly contained in the basin suspended
thousands of feet above the plains. Assuming that the reservoir, about 230 feet
deep, was entirely filled, it would have been nearly a third of a mile in circum-
ference at its upper rim, and 760 feet round at the bottom; consequently, its
volume could not have been much more than 35,000,000 cubic feet. But when
the side cf the crater gave way on the disastrous day in 1541, the aperture
occurred immediately above the capital, which the Spanish conquerors had just
founded on the site of the present Ciudad Vieja. The avalanche of water rushed
down the mountain, tearing up the ground, sweeping rocks and trees along its
irresistible course, and burying the city beneath heaps of mud and débris.

Agua is separated by the deep valley of the Rio Michatoya from the Pacaya,
a group of igneous peaks so named from a species of palm growing at its base
and producing edible flowers. A near view of Pacaya reveals a cluster of
irregular summits, where the supreme cone seems to have disappeared during
some prehistoric convulsion. The loftiest cone, which is still active, rises to a
height of 8,400 feet, or some 3,000 feet above the surrounding plateau. Close
by 1s a wooded peak, and both of these crests are enclosed within the breached

PHYSICAL FEATURES OF GUATEMALA. 211

margin of an enoimous crater some miles in circumference. On a neighbouring
terrace also stand two other craters, one of which, the Caldera, or ‘“‘ Cauldron,” of
the natives, contains a lake of pure water, while from the other light vapours
are still emitted. According to a local tradition the smoking peak of Pacaya was

|
HHH

Fig. 90.—Antieua: Ruins or CrrisrcHurcx, Agua VoLcANO IN THE BACKGROUND.

the scene of an eruption in 1565, and since that time it has never ceased to eject
ashes, vapours, and even lavas.

None of the other volcanoes in the eastern part of Guatemala have been
disturbed in recent times. Two of these lie a short distance east of Pacaya at

212 MEXICO, CENTRAL AMERICA, WEST INDIES.

the village of Cerro Redondo, or ‘“ Round Hill,” which takes its name from one
of the cones Farther on another is mentioned by travellers, beyond which the
normal igneous chain is cut at right angles by a transverse fissure which extends
for over 60 miles towards the north-east. It begins near the coast, where the
Moyuta or Moyutla peak rises far to the south of the main axis, and it is con-
tinued on the opposite or north side by Amayo, Cuma or Columa, Santa Catarina,
or Suchitepec and Ipala, loftiest peak of this transverse range (5,465 feet).

Ipala terminates in a flooded crater,

Fig. 91.—Pacaya Vorcao. and on one of its flanks is rooted

Serle 1 : 159,000.

another igneous cone called Mount

Rico. The Guaitemalan igneous

system terminates near the frontier,

where the perfectly symmetrical
cone of Chingo rises to a height of
over 6,600 feet above the prolonga-
tion of the main range. Chingo is
said to be extinct, although Dollfus
and Mont-Serrat fancied they saw

some vapours escaping from its
-sumunit.

North of the Guatemalan platean
the regions carved by the run-
ning waters into numerous separate
masses present a chaotic appearance
in many places, especially towards
the diverging sources of the Motagua
and Usumacinta rivers. Here the
highlands form a central nucleus
whence radiate several elevated
chains. The loftiest of these sierras

is probably the Altos Cuchumatanes,
which runs north of Huehuetenango
towards Tabasco; it is also known
as the Sierra Madre, although it is
separated from the other Guatemalan

32 Miles. ranges by the deep valley of the

Usumacinta. East of this copious
stream the ranges are disposed mostly west and east, and gradually diminish
in altitude in the same direction. Taken as a whole, this northern region of
Guatemala drainifg to the Atlantic, and limited southwards by the lofty
rampart of the main range, may be compared to a stormy sea breaking into
parallel billows. One of these great billows, consisting of mica schists, runs
north and parallel to the Motagua under the name of Sierra de las Minas, so desig-
nated from its auriferous deposits. Farther east, where it is known as the Sierra

RIVERS OF GUATEMALA. 213

del Mico, or “ Monkey Range,” it reaches the coast between the Rio Golfete and
St. Thomas’s Bay, where it terminates in the Cerro de San Gil, a conic mountain
said by the natives to be a volcano. At the point where it is crossed by the main
route, about 60 miles from its eastern extremity, the Minas Range is about 3,000
feet high. The ridge running north of the Rio Polochic takes the name of Sierra
Cahabon in the province of Alta Vera Paz. Towards its eastern extremity the
Sierra de Santa Cruz, as it is here called, develops the headland which separates
the Rio Golfete from Amatique Bay.

In the north of Guatemala the last great chain is the Chama, which trends
north-eastwards round the sources of the Rio de la Pasion. Towards the east it is
connected by a few low ridges with the Cockscomb Mountainsin British Honduras.
The passes over this sierra, which have been traversed by few explorers, are
extremely rugged and difficult, not so much because of their elevation as of the
vertical disposition of the rocky crests. North of the Sierra de Chama stretch the
savannas, which are continued northwards in the direction of Yucatan. But
these plains are dotted over with isolated hills, for the most part wooded, rising
like verdant islands in the midst of a verdant sea.

Speaking generally, the southern and central parts of Guatemala are almost
entirely covered with pumice in the form of tufa. The granites, mica schists and
porphyries are only seen here and there, on the more elevated parts of the plateaux
and mountains, or in the depressions eroded by running waters. The quantity
of pumice ejected by the volcanoes was prodigious, the deposits accumulated in
every part of the country having a thickness of 150 and even 200 yards. There
exists scarcely a single valley which has not been partly filled in, or a plateau that
has not been levelled by these deposits.

On the masses of pumice lies a layer of yellowish clay, with a mean thickness
of twelve or fifteen feet, which has probably been formed by the surface decomposi-
tion of the underlying rocks. It is in these clays and in the pumice immediately
below them that are found from time to time the remains of mastodons and of
Elephas Colombi, animals which lived during quaternary times. Hence this was
the epoch during which occurred the prodigious eruptions of the Guatemalan
volcanoes.

Rivers AND LAKESs.

The rainfall is sufficiently abundant in Guatemala to feed a considerable
number of watercourses. But rivers in the strict sense of the term could scarcely
be developed except on the Atlantic slope, where the disposition of the land and its
gradual incline afforded space for the running waters to ramify in extensive fluvial
systems. On the Pacific side, where the escarpments of the plateaux fall abruptly
seawards, the torrents descend rapidly through the parallel ravines furrowing the
flanks of the mountains. Almost waterless during the dry season, but very copious
in winter, these streams for the most part discharge into the coast lagoons. In
fact, they do not communicate at once with the sea, from which they are separated
by sandy strips several miles long, and the seaward chanuels themselves are often

214 MEXICO, CENTRAL AMERICA, WEST INDIES.

shifted by the tides and tempests. One of the largest streams on the Pacific side
is the Suchiate, which forms the common frontier between Guatemala and Mexico.
A still more extensive basin is that of the Samala, which flows from the Quezal-
tenango and Totonicapam heights. The Iztacapa is a smaller river, although it
receives the overflow of Lake Atitlan, not through a surface stream, but through
underground filtrations across the scoriæ covering the plain of San Lucas, on the
southern bank. Lake Atitlan itself, which has an area of 65 square miles,
develops an irregular crescent at an altitude of 5,140 feet, round the spurs of the
Atitlan voleano, which rises on its southern margin, and which created the lake by
damming up the fluvial valleys. The waters thus pent up by the accumulating beds
of ashes and lavas gradually filled the vast Atitlan basin, which is said to have a
depth of over 1,650 feet. The water, being continually renewed, thanks to the
subterranean outflow, is perfectly fresh and limpid.

Farther east the smaller Lake Amatitlan has been formed under analogous
conditions at an altitude of 4,000 feet. Here the waters have been gradually
dammed up by the lavas and scoriæ deposited by the Pacaya voleano on the south
side of the lake. Formerly its basin was even far more extensive than at present,
and traces of its old level are still distinctly visible at distances of several miles
from the present margin. The water of Amatitlan, which exceeds 200 fathoms in
depth, is as fresh as, but less pure than, that of Atitlan, and along the margin its
temperature is raised by thermal springs. Nearly two hundred years ago Thomas
Gage spoke of it as “ somewhat brackish,” adding that salt was collected on its
shores. Such is no longer the case, its flavour being in no way affected by the
slightly purgative salts of soda and magnesia which it contains in solution, though
they give rise to a strong odour during the dry season. It is probably fed by
underground affluents, the few surface streams draining to the basin being
insufficient to create an emissary. The overflow is discharged south-eastwards to
the Michatoya, or “ Fish River,” which escapes from the plateau through a deep |
gorge 600 or 700 feet below an escarpment of the Pacaya volcano. Farther on
the affluent has a clear fall of 200 feet near San Pedro Martir, beyond which
point it loses itself in the coast lagoons a little to the east of the port of San José.

Amatitlan lies about midway between Atitlan and Ayarza (Ayarces), a third
flooded depression at the southern foot of the Mataquezcuintla mountains, which
here rise to a height of over 8,000 feet. But Ayarza already belongs to the San
Salvador hydrographic system, draining through the Ostua to the fluvial basin of
the Rio Lempa, main artery of the neighbouring state. On the Atlantic slope,
also all the western and northern regions, at least one-half of the whole territory
belongs to the Usumacinta basin, which throughout its lower course flows through
Mexican territory. The largest watercourse entirely comprised within the limits
of Guatemala is the Motagua, which, like so many others in Spanish America, is
called also the Rio Grande. It rises in the central mass of the Altos de Totoni-
capam, where its headstreams are intermingled with those of the Usumacinta.
Farther east it collects all the torrents descending from the main Guatemalan
waterparting, which in many places is contracted to a narrow ridge furrowed on

‘NVILILV ANVI NO NAMVL MAIA

RIVERS OF GUATEMALA. 215

both sides by deep ravines. But the Motagua flows, not through one of these
eroded valleys, but through an older fissure belonging to the original structure of
the land. After its confluence with the copious affluent from the Esquipulas and
Chiquimula, the Motagua becomes navigable for small craft. From this point it
follows a north-easterly course, skirted on both sides by picturesque wooded
heights all the way to its mouth in Honduras Bay. During the floods it is a
broad and deep stream, navigable for over 100 miles in a total length of 300 miles.
But the approach is obstructed by a bar at the mouth of the chief branch in the
delta, which has usually scarcely more than three feet of water. The other
branches are also inaccessible to vessels of large draught, and the whole of the low-
lying alluvial tract is a region of swamps and backwaters fringed with mangroves,
almost as dangerous to approach from the land as from the sea. So unhealthy is
the district that the inlet enclosed by the long promontory of Tres Puntas, pro-
jecting north-west towards Amatique Bay, is called Hospital Bay. This inlet
is connected with the main stream by a partly artificial channel ; but the true
port of the fluvial basin lies, not in the delta, but immediately beyond it at the
foot of the last spurs of the Sierra del Mico. Here is St. Thomas’s Bay, the best
haven along the whole Atlantic seaboard of Central America. After rounding
a dangerous sandbank large vessels penetrate through a narrow channel into a
circular basin enclosed by an amphitheatre of wooded hills. Here is ample space
for hundreds of ships in a perfectly sheltered sheet of water with a superficial area
of six square miles and depths ranging from 14 to 30 feet.

Like that of Motagua, the Polochic basin is entirely comprised within
Guatemalan territory. Although a smaller stream, it is navigable by flat-
bottomed boats for about an equal distance from its mouth. Rising in the Coban
mountains, which here form the divide towards the Usumacinta valley, the
Polochic flows almost due east to its junction with the Cahabon, which descends
from the Sierra de Chama to its left bank below Teleman. Like the Motagua it
ramifies through several arms at its mouth, where numerous shoals bar all access
except to light flat-bottomed craft. The delta, however, lies not on the Atlantic,
but on an inland sea known as the Golfo Dulce or Izabal Lagoon. This “ golfo”’
certainly appears to be a lacustrine basin rather than a marine inlet, for it
has not the s'ightest trace of salt, and during the floods its level rises about 40
inches. It has a mean depth of from 35 to 40 feet, and as it has an area of
over 250 miles, it might easily accommodate all the navies of the world but for
the shallow channel through which it communicates with the sea.

Towards its north-east extremity the current, elsewhere imperceptible, begins
to be felt; its banks, here low and swampy, gradually converge, and the Golfo
Dulce becomes the Rio Dulce, whose depth falls in some places to ten or twelve
feet. Lower down the water grows more and more brackish, and the Rio Dulce
enters another basin, whose saline properties betray its marine origin. Below the
Golfete or “ Little Gulf,” as this basin is called, the banks again grow higher,
developing cliffs and escarpments, where the lianas, twining round the branches of
great forest trees, fall in festoons down to the stream. During ebb-tide the water

216 MEXICO, CENTRAL AMERICA, WEST INDIES.

flows in a swift current seawards through a rocky gorge about 600 feet deep,
but with scarcely six feet at the bar. From this bar to the Polochic delta there
is a clear waterway of about 60 miles navigable by schooners.

North of the Golfo Dulce and its straits the only important river is the
Sarstun, whose lower course has been chosen as the frontier towards British
Honduras. Farther north the quadrilateral space comprised between Tabasco,
Yucatan and Belize is drained partly by the Usumacinta, and partly by the Rios
Mopan and Hondo, leaving only a few lakes dotted over the northern savannas
with no outflow. The largest of these is Lake Itzal, so named from the Itzas, a
Yucatan nation which took refuge on its shores in the fifteenth century. It is

Fig. 92.—Gozro Durce AND THe Lower Moracua
Scale 1 : 1,700 009,

==
GO HWESPESS UCD:

SS = = = ——
a= hospiéalBea= <———Puerto=bo

wl
sw

FA £
We st
0 to 10 10 ‘o 50 50 Fathom:
Fathoms. Fathoms. and upwarda
30 Mules.

also called Peten, or the “Island,” from an isolated hill where the immigrants
founded their first settlement. Peten has the form of an irregular crescent, with its
convex side facing north-westwards, and is divided into two basins by a peninsula
projecting from its south side. Enclosed between low limestone banks, the lake
rises several yards during the rains, while in some places it has a normal depth
of over 180 feet. Some of the creeks, however, are shallow enough to develop a
rich growth of waterlilies, whose seeds in times of scarcity are ground and
kneaded to a sort of bread which is astringent but little nutritive. Peten is at
present a closed basin, but other lacustrine depressions scattered over the savannas
appear to have formerly connected it on one side with the San Pedro affluent of
the Usumacinta, on the other with the Rio Hondo, which flows to Honduras Bay.

GUATEMALA. 217

CLIMATE, FLorA, Fauna.

The distribution of the climates in vertical zones of temperature is far more
clearly marked in the southern parts of Guatemala than in Mexico itself.
The regular rampart of mountains which dominate the Guatemalan seaboard
presents almost exactly the same geographical conditions throughout its whole
extent, and here the zones of hot, temperate, and cold lands follow uniformly
from base to summit, each indicated by its special types of vegetation. Above
the cold zone coinciding with the edge of the plateau there is even distinguished
a ‘frozen zone,” that of the higher summits snow-clad for a short period of the
year. This highest zone is uninhabitable, and the same might almost be said of
the lowest, especially for European settlers. Here the mean temperature varies
from 77° to 82° Fahr., while the glass often rises even to 104°.

The two intermediate temperate and cold zones, the former suitable for the
cultivation of the banana, sugar-cane, and coffee, the latter for cereals and
European fruits, comprise by far the greater part of the Guatemalan territory,
and here the populations of European or mixed origin can be acclimatised. The
temperate zone especially, which les mainly between the altitudes of 1,600 and
5,000 feet, occupies a collective area of considerable extent. In other words
Guatemala is, relatively speaking, far more favourably situated than Mexico for
the cultivation of economic plants. Its characteristic growth is the banana, the
alimentary plant in a pre-eminent sense, which here flourishes throughout the
whole of the temperate zone.

Lying, like Mexico, within the range of the trade winds, Guatemala is
exposed especially to the north-east currents, which pass between the cones
of the voleanoes down to the Pacific seaboard. But these regular currents are
frequently deflected from their normal course, and then the fierce nortes sweep
from the uplands down to the low-lying valleys.

The rainfall is very unevenly distributed over the different regions of
Guatemala. The Atlantic slope is naturally the most abundantly watered, the
prevailing wind being charged with the vapours from the Gulf of Mexico and
Caribbean Sea. “It rains thirteen months in the year,” say the inhabitants of
Izabal. But the Pacific seaboard has also its share of humidity, and here the
temperate lands more especially receive copious downpours. ' Here the wet season
lasts six or even seven months, with a short interruption in the month of August,
due to the fact that the cortége of clouds has followed the sun farther north
towards the Tropic of Cancer. Even during the dry season few months pass
without some rain, the effect of which on the growth of vegetation is magical on
these rich voleanic lands. Fogs also are by no means rare at this period, and
contribute to support plant life. The mean rainfall has been recorded only, for
the capital, where it amounts to 54 inches. On the lower slopes of the temperate

zone it certainly exceeds 80 inches, while on the Quezaltenango Altos it must fall
short of 20 inches.
In its natural history Guatemala resembles the conterminous provinces of

218 MEXICO, CENTRAL AMERICA, WEST INDIES.

East Mexico—Chiapas, Tabasco, and Yucatan. In its forests are intermingled
various species of oaks and conifers, some of the latter growing to a height of
150 or 160 feet. In many regions the traveller might fancy himself transported
to the pine-groves of the Landes in Gascony, or else to the Pomeranian woodlands.
On the low-lying Pacific seaboard the bamboo grows in dense thickets to a height
of 100 feet; these thickets, which wave in the breeze like tall cornfields, are
traversed by narrow, gloomy galleries made by wild beasts.

As in Tabasco the giant of the Guatemalan forests is the ceiba, or pyramidal
bombax. In the neighbourhood of their settlements the Indians of the plateaux
and escarpments generally clear a large space round the ceiba to give it ample
room for the development of its wide-spreading branches and rear its majestic
form more imposingly avove the throng of worshippers at its feet. As in south
Mexico the whole surface of the forest is interwoven with the coils of lianas
gliding snake-like from tree to tree.

In Vera Paz the enclosures are often formed by a species of arborescent
thistle, which grows rapidly and interlaces its stems so as to form a compact
greyish wall carpeted with mosses and ferns intermingled with the large foliage
of the plant. The forests of the hot zones near Ratalhulen, as well as those of —
the Polochic, have become famous for their magnificent orchids. Another
remarkable Guatemalan plant is well known to the Indians for the heat emitted
by its efflorescence at the moment of fertilisation. Hence its rame of flor de la
calentura (“fever flower”) given to it by the Spaniards.

The tapir, peccary, and a few other mammals inhabit the Guatemalan forests,
where, however, no special forms have been discovered except amongst the lower
orders of animals. The alligator and some thirty species of fishes in Lake Peten
were unknown before Morelet’s expedition. Here also has been found a species
of trigonocephalus, which completes the series of these dangerous snakes between
South Carolina and Guiana.

Vera Paz is the earthly paradise of ornithologists; here is still met the
wonderful qguezal, or ‘resplendent couroucou”’ (trogon pavorinus, pharomacrus
paradiseus), a member of the gallinaceous family, with an emerald-green silky
plumage dashed with a golden lustre above, with a lovely purple hue below, and
a tail fully three feet long. The Guatemalan republic has chosen this bird as the
national emblem.

INHABITANTS.

The common Guatemalo-Mexican frontier traverses regions whose populations
on both sides have the same origin and speak the same languages. Thus the Mayas
of Yucatan are found also in the Peten district ; east and west of the Usumacinta
the Lacandons have their camping grounds; Chols, Tzendals, and Mamés occupy
the heights and slopes both of the Guatemalan Altos and of Soconusco. But
central and east Guatemala are inhabited by ethnical groups distinct from those
of the Mexican republic. Various attempts have been made to classify these
heterogeneous populations according to their affinities, usages, and languages ; but

NHABITANTS OF GUATEMALA. 219

the work begun by Brinton, Stoll, and others is still far from complete, and

meantime the tribes are disappearing, and several languages spoken down to the

resent century are now extinct. East of the meridian of Lake Amatitlan, nearly
P À ; \

Fig. 93.— Lanpscare 1x Sourn GUATEMALA— BAMBOO JUNGLE.

Na
NS

yy)

all the Indians have already become Ladinos, and no longer speak their primitive
tongues. Nevertheless, according to Stoll, as many as eighteen native languages
were still current within tbe limits of the republic in 1883.

The Aztecs, the dominant indigenous element in Anahuac, are represented in

220 MEXICO, CENTRAL AMERICA, WEST INDIES.

Guatemala only by the single group of the Pipils, who dwell, not in the neigh-
bourhood ef the Mexican frontier as might have been supposed, but in the eastern
provinces near others of the same race, settled in Salvador. At the time of the
conquest the Pipils occupied a far more extensive territory than at present. But
their domain has been gradually encroached upon, not only by Spanish, but also
by the spread of other native tongues, such as the Cakchiquel and Pokoman. At
present the Pipil forms two separate enclaves, one at Salama and on both banks
of the Motagua (Rio Grande), the other at Escuintla and Cuajiniquilapa in the
Guacalate and Michatoya basins.

Some historians regard the Pipils as a branch of the fugitive Toltecs who
migrated southwards after the overthrow of their dominion by the Chichimecs, and
it is probable enough that such a migration may have taken place at some remote
epoch. Juarros tells us that Pipil means “ Children,” and that the people were so
called by the Mexicans because they were unable to speak the Nahuatl language
correctly. But according to another interpretation the Pipils of Guatemala and
of the other Central American republics represent the ancient Pipiltins, that is,
the ‘‘superior”’ or “ better,” the nobler branch of the Aztec family. This name
they are supposed to have themselves assumed when they settled amongst the less
civilised populations south of Mexico.

The great majority of the Guatemalan Indians belong to the same stock as that
of the Huaxtecs in the Vera Cruz uplands, and of the Mayas dominant in Yucatan.
All the populations speaking various forms of the common language are collectively
called Maya-Quiché, from the two most important members of the group, the
Mayas of the Yucatan plains and the Quichés of the Guatemalan plateaux.
Within the limits of the latter state the Mayas, properly so-called, occupy an
extensive territory, comprising the Peten district and uearly the whole region
bounded southwards by the Pasion and Mopan rivers. In this region the Maya
nation is represented by the Itzas, one of the very purest members of the family.
Thanks to their isolation in the peten, or ‘island,’ of the great steppe lake, the
Itzas were long able to preserve both their political independence and the purity of
their race and national usages. The Lacandons, who dwell farther west, between
Lake Peten and the Usumacinta river, are also a pure Maya people, although
frequently called ‘‘ Caribs”” by the Spaniards and even by the Mayas themselves.
Like the Itzas, they have maintained their independence, and although admitting
strangers into their country, they yield obedience to no one, and stillregard them-
selves as masters of the land. However, they are but a small group, scarcely
numbering more than 4,000 or 5,000, according to the estimate of travellers who
have visited them. They are described as an anemic people, “flabby and soft,”
which should perhaps be attributed to their mode of life passed entirely in the .
humid atmosphere of dense forests.

The Mopans, who are met in scattered groups south of Lake Peten and in the
upper valley of the Rio Mopan (Belize river), are also independent Mayas,
although their language is said to differ from that of the Itzas and Lacandons.
Their southern neighbours, the Chols, that is, “Men,” who roam the steppe

INHABITANTS OF GUATEMALA. 221

between the Usumacinta and the Golfo Dulce, belong to the same widespread Maya
family. They were met on his expedition to Honduras by Fernan Cortes, who
was able to converse with them through Doña Marina, she being acquainted with
the Chontal dialect. The Chols appear to have been one of the most civilised
nations in the region now known as Guatemala, for in their territory are situated
the fine ruins of Quirigua. But they are greatly reduced in numbers, and both
people and language seem to be dying out.

Owing to the former slave-raiding expeditions of the Spaniards, the whole
Atlantic seaboard, from Yucatan to Nicaragua, is almost entirely destitute of a
native Indian population. After the extermination of the Española and Cuban
natives, and before their places could be supplied by negroes imported from Africa,
the planters of those islands sought to recruit their gangs by introducing “ Caribs,”
that is, Indians of all races, whether in the islands or on the mainland. These
so-called Caribs were accused of cannibalism and of every other crime under the
sun, and could consequently be enslaved with a free conscience. Man-hunting
expeditions were undertaken, especially along the coast between Capes Catoche and
Gracias-à-Dios ; these lands were completely depopulated in a very few decades,
and when no more victims remained, the raiders had to ascend the rivers and lay
waste their valleys in search of fresh captives. It is evident from Bernal Diaz’
descriptions that at the time of Cortes’ expedition to Honduras the shores of the
Golfo Dulce were, in many places, lined with settlements and plantations.

South of the Chol camping-grounds, which are still met in the upper valley of
the Rio de la Pasion, the district about the headwaters of the Polochic is occupied
by the Quekchi and Pokonchi, who form a special branch of the Maya family.
Their territory was formerly known by the name of Tezulutlan, that is, “‘ Land of
War,” because the Spaniirds made frequent expeditions against the natives;
without, however, succeeding in reducing them. Their submission was, in fact,
brought about by the celebrated Bishop of Chiapas, Bartholomew de las Casas,
and the Dominican missionaries who soon acquired unlimited power over the
people. Then the territory changed its name from “ Land of War” to Vera Paz,
“True Peace.’ But although they thus became the voluntary serfs of the Domi-
nican friars, the Quekchi and Pokonchi were, after all, but outward converts, and
their usages still recall those of pagan times.

One of the chief indigenous nations is that of the Pokomans, in whose territory
the present capital of the state has been founded. They are also one of the best-
known Guatemalan tribes, for the Indians of the large settlement cf Mixco, who
supply the capital with fuel and provisions, are all Pokomans. They are of Maya
stock, and display the same remarkable power of passive resistance and tenacity
as other branches of that race. They have gradually encroached on the Pipil
domain, dividing that nation into two separate sections by conquering the region
of the main Guatemalan waterparting.

The Quichés were, with the Aztecs and the Mayas, the most cultured inhabi-
tants of Central America at the time of the conquest. At that epoch they were
also a very numerous nation, the chronicles speaking of “several millions.” They

222 MEXICO, CENTRAL AMERICA, WEST INDIES.

are now greatly reduced, though still occupying nearly the same territory as
when Alvarado first attempted to subdue them. In certain districts, notably in
that of Totonicapam, they still energetically resist the intrusion of the Spanish
tongue, which, however, as the official language, cannot fail, sooner or later, to
prevail in the towns, if not in the rural districts. The Quiché linguistic domain
comprises especially the region of the Quezaltenango and Totonicapam Altos ;
but it also extends north and north-east towards the upper Usumacinta and
Motagua basins, while southwards it reaches the sea along the Pacific slope of the
main range. For over sixty miles it holds the seaboard south of Retalulheu and
Mazatenango. Quiché, the language of the old rulers of the land, is one of the
few American idioms which possess, if not a literature, at least some original
documents. The Popol-Vuh, or “ Book of History,” written by an unknown
native soon after the conquest, to replace another national history which had been
lost, possesses great value for the study of Central American myths and legends.
It was translated into Spanish at the beginning of the eighteenth century by the
Dominican friar, Ximenes, and afterwards edited, with a French translation, by
Brasseur de Bourbourg.

Cakchiquel, which is spoken on the plateau from Solola to Chimaltenango and
Antigua, that is, in the zone comprised between the Quiché and Pokoman domains,
is, like Quiché, also a literary language. Brasseur de Bourbourg has described a
document containing the history of the Cakchiquel nation from the creation of
the world, and in several passages harmonising with the Popol-Vuh. Cakchiquel,
Quiché, and Tzutujil, which last is spoken in a small enclave south of Lake Atit-
lan, are described by Spanish grammarians as the “ three metropolitan languages,”
because each was at one time a court idiom current in a royal residence. All
closely resemble each other, while the Mem, or Mamé, differs greatly from Quiché,
although also belonging to the same linguistic stock. This language of “ Stam-
merers,” as it was called by the Quichés and Gakchiquels, because of the difficulty
they had in understanding it, prevails throughout all the western districts of
Huehuetenango and San Marcos, as well as in the Mexican provinces of Soconusco
and Chiapas; it forms a distinct group with Ixil, Aguacatan, and perhaps some
other dialects spoken by the little-known tribes of the upper Usumacinta basin.

Nearly all the native languages current within the limits of Guatemala belong
to the Maya stock. Besides those already mentioned, almost the only other
exception is the Carib, which still survives amongst the fishers and woodmen, who
are descended from the West Indian Caribs removed by the English to the main-
land at the close of the last century. Stoll has endeavoured to draw up a
genealogical tree of the Maya languages, which is intended to show the order of
succession in which the various members branched off from the parent stem The
Huaxtecan of Vera Cruz would appear to have become first detached, and it has
diverged all the more that to the modifications introduced by time have been
added those derived from a totally different environment surrounded by popula-
tions of totally distinct speech and usages. Then the parent stem split into the
two great Maya and Quiché divisioris, the former subsequently throwing off the

INHABITANTS OF GUATEMALA. 223

Mexican branches (Tzendal, Tzotzil and Chol), while Quiché ramified into the
various Guatemalan subdivisions of Pokoman, Pokonchi, Cakchiquel and modern
Quiché with Ixil and Mamé.

The pure Indians, who constitute over two-thirds of the whole population,
differ little in their physical appearance, to whatever linguistic group they may
belong. The Cakchiquels, who may be taken as typical Guatemalan Indians, are
of average or low stature, but stoutly built, with clear eye, prominent cheekbones,
large nose, firm mouth, black, lank hair, thick eyebrows, low forehead, somewhat
depressed by the strap passed round the head to support their loads. They never
grow grey, and preserve to old age their well-set dazzling white teeth and muscular
frames, which never put on too much flesh. They are indefatigable walkers, and
the women may be daily seen trudging to market, doing their three and a half
miles an hour under loads of 90 to 110 pounds, with the baby perched on the hip.
The Guatemalan Indians are much addicted to the practice of eating an edible
earth of volcanic origin, of a yellowish-grey colour and strong smell, which is
taken as an accompaniment or appetiser. Reference is already made to this habit
in the Popol-Vuh. Christians going on pilgrimages also eat little earthen figures,
which they obtain at the holy shrines, and which are supposed to heal all mala-
dies. Gage was acquainted with two Creole ladies, who ate ‘ handfuls of earth ”
to brighten the countenance. The natives age rapidly, doubtless owing to their
extremely monotonous existence, unrelieved by any incidents which might stimu-
late curiosity or afford food for reflection. After the age of thirty they have
passed through all their experiences, and nothing further remains to be learned.

Musical gatherings are greatly enjoyed ; the least pretext, such as the death
of a child, which has become an angelin heaven, serves to get up festivities, to
which everybody is invited. The natives, and especially the Mayas of Peten, have
a delicate ear for music, and in this respect are said to be superior to the Spaniards.
The Itzas sing in perfect tune, and even vary their parts with much originality ;
according to Morelet their songs are lively and bright, very different from the
plaintive melody of the Ladinos. The same traveller believed in the native origin
of several musical instruments, such as the chirimiya, somewhat like a clarionet,
and the marimba, a series of vertical wooden tubes formed of uneven calabashes,
which are disposed like those of a reed-pipe, pierced at the lower extremity and half
shut by a thin membrane ; its notes are said to be more powerful than those of the
piano. The marimba, however, is not an Indian but an African invention; it is
widely known in the Niger and Congo basins and as far south as Kaffraria. Its
name is or Bantu origin, and it was doubtless introduced into Central America by
the African slaves.

Although more fervent Catholics than the Ladinos, the Indians have none the
less preserved the old religion under a new form. In many places dolls repre-
senting the gods of their forefathers are hidden under the altars of the churches,
and by this device both divinities are simultaneously worshipped. When kneeling
before Saint Michael they light two tapers, one for the dragon, the other for the
archangel. An old deity corresponds to each personage of the Christian religion,

224 MEXICO, CENTRAL AMERICA, WEST INDIES.

the sun to God the Father, the moon to the Madonna, the stars to the tutelar
saints. Most of the Indians think there are two gods, one of whom, the Dios de
la Montana, ‘“ God of the Forest,’ attends specially to the aborigines, taking no
notice either of the Ladinos or of the whites. He is often called Dueno del Palo,
“Tord of the Tree,” because he dwells in the ceibas, and to the foot of these
gigantic trees in the forest clearings are brought the firstfruits of the harvest

Fig. 94.—Nattve POPULATIONS oF GUATEMALA.
Scale 1 : 4,500,000

L./¢z@ oo

. iesaltens gon CE
Pape 4 GUATEMALA
fe Z Schi Hepis

\S SALVADOR —

ESA län)/

West ile Greenwich

60 Miles.

and the chase. The earth also is worshipped, but feared as representing the prin-
ciple of evil.

In every village the natives are grouped in confradias, or “ brotherhoods,”
which are evidently organised on the model of the old Aztec calpulli. Each has
its tutelar saint, wno is féted with much pomp, the male and female “ captains ”
collecting the money required for the costumes, music, tapers and decorations.
Sometimes this costly worship plunges the whole community into debt for months

together, but the saint is only all the more highly esteemed.
Mimetic dances represent mythological or historical dramas of Indian origin,

TOPOGRAPHY OF GUATEMALA. 225

but since the arrival of the Spaniards more or less modified by the addition of new
legends. Thus in the ‘“ Moors’ dance ” the chief personages are Charlemagne and
Tamerlane. There are also the ‘negroes’ ball,” and even the “dance of the
conquest,” the performers on these occasions wearing wooden masks and fantastic
garbs of leaves or herbage, and exciting themselves to a pitch of frenzy. Such
is the passion and fury of these Bacchanalian dancers that one easily realises the
ancient religious ceremonies, when the devotees fell on the palpitating bodies of
the victims and devoured their flesh.

Conscious of the strength derived from numbers, and even mindful of the evils
brought on them by servitude, the Indians have kept aloof from the Ladinos, and
have often taken advantage of the local revolutions to rise in revolt against their
oppressors. In 1838, an Indian army, under Rafael Carrera, penetrated victoriously
into the capital, proclaiming that they had been “raised up by the Virgin Mary
to kill the whites, foreigners and heretics.’’ But in their very triumphs they had to
feel the ascendency of the more civilised Ladinos, with whom they are brought
yearly more and more into contact. As the term “white” is sometimes applied
to the Ladinos, who are all of mixed origin, many of the rural populations are in
the same way regarded as pure Indians though they also have a strain of foreign
blood. On the plantations crossings continually take place between the ruling class
and their serfs and the black slaves originally introduced by the Dominican friars
to cultivate their lands have also contributed to this mixture of races. Pure
negroes can scarcely any longer be found in Guatemala, although their more or
jess modified features may be recognised in whole populations.

ToPoGRAPHY.

The Guatemalan population is grouped chiefly in the cold and temperate lands
of the Pacific coast range. All towns of any importance are situated on the high
grounds between the coastlands and the upper Motagua and Usumacinta valleys.
Near the Mexican frontier the first town on the plateau is Sax Marcos, which lies
in the cold zone on an eminence whence is commanded a wide prospect of the sur-
rounding coffee plantations. Ona neighbouring plain stands the native town of
San Pedro Sacatepeques, whose inhabitants no longer speak Mamé, the old language
of West Guatemala. By a recent decree they have been declared Ladinos, which
has the consequence of allowing them more freedom in the administration of their
local affairs. The natural outlet of San Marcos and its plantations is the Ocos
estuary some 50 miles towards the south-west. On this part of the coast the plains
are vast low-lying savannas, often under water, dotted over with permanent
lagoons and forest tracts. In April the traders and planters from Soconusco, in
Mexico, and from west Guatemala assemble at this place for the transaction of
business. The Ocos estuary was long regarded as the frontier between Mexico
and Guatemala. West of the port, which is open to foreign trade, the frontier
station has been fixed at the village of Ayutla, a place of pilgrimage much fre-
quented by the Soconusco Indians.

226 MEXICO, CENTRAL AMERICA, WEST INDIES.

About 30 miles south-east of San Marcos, Quesaltenango, second capital cf the
republic and chief town of the Altos, occupies an extensive space, 7,740 feet above
the sea, on a hilly plateau south of which rises the still smoking Cerro Quemado.
In 1838 this place was the capital of a state which comprised the three eastern
provinces of Totonicapam, Quezaltenango, and Solola. The houses are built of
lava blocks quarried at the foot of the volcano. The small industries are repre-
sented by woollen and cotton weavers, dyers and leather-dressers. A speciality
of the Quiché artisans is the preparation of gold-embroidered mantles, feather hats
and the masks used bw the natives in their dances, processions, and scenic per-

Fig. 95.—Tur Aztos REGION.
Scale 1 : 1,100,000.

SN
Ne,

rN fe
ja yt Vi NAS

i oat
VASE

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Au

Ÿ a
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ts

TASS

7h
West of Greenwich

18 Miles.

formances Probably from this feather industry the city took its Mexican name of
Quezaltenango, which means “ Green-Feather Town,” not, as is often asserted,
“Town of the Quezal Birds,” a species which is net found in the district. In the
capital of the Altos region reside most of the great landowners, whose estates
cover the Costa Cuca slopes facing the Pacific; here also dwell the traders and the
moneylenders, who are the real masters of the land.

They prefer this salubrious place to Retalhuleu, which, although lying much
nearer to the zone of plantations, is one of the most unhealthy towns in Guatemala.
Retalhuleu, that is, the “ Signal,” stands at an elevation of not more than 1,360
feet, that is, in the very heart of the hot lands under a climate with a mean tem-
perature of 82° to 84° Fahr. It is a very ancient market, probably founded by the
Quiché kings to procure a sufficient supply of cacao and cotton. Cacao, which

aye #

TOPOGRAPHY OF GUATEMALA. 227

was formerly the chief crop, has recently been replaced by coffee and the alimen-
tary plants required by the hands employed on the plantations. Hence the neigh-
bouring port of Champerico, which is connected by rail with Retalhuleu, now exports
little except coffee. Being a hotbed of fever in the rainy season, Champerico is
scarcely inhabited except in the dry period, and especially in April and November,
when the skippers, nearly all from the United States, come for their cargoes of
coffee.

Totonicapam stands on the same plateau as Quezaltenango, twelve miles more
to the north-east, but in a colder climate, at an altitude of 8,200 feet, that is, 460
higher than its neighbour and 660 higher than Mexico. Its inhabitants are chiefly
Quiché Indians, who still mostly speak the national language, and who, so far from
considering themselves inferior to the Ladinos, constitute, on the contrary, a sort of
local aristocracy. Many, in fact, descend from the old “ caciques ”’ of Tlaxcala who
accompanied Alvarado on his expedition, and who in return for their services
received special class privileges together with exemption from taxation. The best
dwellings in the town belong to these Tlaxcalans. Like the neighbouring capital,
Totonicapam is an industrial centre, producing textiles, earthenware, furniture,
guitars, marimbas, and other musical instruments, Sahcaja, a few miles to the
south-west, although now an obscure village, was at one time a place of some note.
It was the first settlement founded by Alvarado in 1524, and its churh, dedicated
to the Virgin of Victory, became a famous place of pilgrimage. Afterwards most
of its inhabitants removed to Quezaltenango. Between these two towns flows the
Olintepec brook, called by the natives Xiquigil, or “ Bloody River,” to comme-
morate the day when it flowed with the blood of thousands of Quichés massacred
by Alvarado in the decisive battle which made him master of the land.

Another historic place is Santa Cruz Quiché, or simply Quiché, which still bears
the name of the nation whose capital it was, but which is now almost exclusively
inhabited by Ladinos. It stands at an altitude of 6,220 feet, about 25 miles north-
east of Totonicapam on a plain of the temperate zone watered by the headstreams
of the Rio Grande (Motagua). This plain is enclosed by deep barrancas separat-
ing it from the terraces on which stood the monuments of Utatlan, residence of the
ancient Quiché kings. Surrounded by precipices over 1,300 feet high on the south
side, the terrace of the Acropolis presents a nearly level surface for about a third
of a mile in all directions, and is connected with the neighbouring heights by a
precipitous track which was formerly defended by strong fortresses. The palace
of Utatlan, said by the chroniclers to have rivalled that of Montezuma in size,
was spacious enough to contain a whole population of women, servants and
soldiers ; the school contained over 5,000 children educated at the charge of the
sovereign, and when this potentate mustered his forces on the terrace to oppose
the advance of the Spaniards, he is said to have passed in review as many as 12,000
combatants. The pyramid known as the Sacrificatorio still presents a somewhat
regular contour, and preserves the traces of steps. Beyond the citadel, the slopes
of the hills, the surrounding heights and plains are strewn for a vast space with the
ruins of edifices now for the most part overgrown with vegetation. The excava-

228 MEXICO, CENTRAL AMERICA, WEST INDIES.

tions made at various times have brought to light statues, bas-reliefs, and much
decorative work. South-eastwards on the verge of the plateau stands the healthy
town of San Tomas Chichicastenango, which is still inhabited by the descendants
of the ancient Quiché nobility: it was here that the Dominican, Ximenez, made
the lucky find of the Popol- Vuh, or “ Book of Myths.”

West of Quiché, the chief headstreams of the Motagua intermingle with those
of the Usumacinta, in the department of Huehuetenango, one of the most sparsely
peopled in the republic. Huehuetenango (Gueguetenango), that is, * City of the
Ancients,’ has also replaced an old Indian town, Zakuleu, or “ White Earth,”
which is said to have been the capital of the Mamé nation. The modern town
lies in the temperate zone, and in a fertile district yielding both European and
tropical fruits, and watered by a stream descending from the north-west to the
Grijalva. In the neighbourhood is the flourishing town of Chiantla, whose
convent, enriched by the offerings of multitudes of pilgrims, was formerly one of
the wealthiest in the New World. Argentiferous lead-mines, now no longer
worked, also contributed to the opulence of the Dominican friars of this district.

On the upper Chixoy, which is the main headstream of the Usumacinta, the
only town is the Quiché settlement of Sacapulas, which crowns an eminence 3,840
feet high, on the right bank, a short distance below the Rio Negro and Rio Blanco
confluence. Immediately below the town numerous thermal springs flow directly
from the granite cliffs, at temperatures varying from 104° to 158° Fahr. They
are both saline and bitter, somewhat like seawater in taste, which is due to the
simultaneous presence of sodium chloride and sulphate of magnesia. Other
springs flowing farther east, although less saline, are more utilised by the natives
in the preparation of salt. The chief salt pan is at present that of Magdalena,
about ten miles north-west of Sacapulas, beyond some steep intervening cliffs.
Here two copious streams, one yielding over twenty gallons a second, and contain-
ing four per cent. of pure salt, flow from the foot of a hill, which was formerly
forest-clad, but which, since the opening of the works, has become completely
treeless. ‘

Salama, capital of the department of Baja Vera Paz, is also situated in the
upper Usumacinta basin, on an eastern tributary of the Chixoy, 2,865 feet
above sea-level, consequently quite within the tropical zone. San Geronimo, an
old Dominican establishment a few miles east of Salama, has become the centre
of a flourishing sugar plantation, the produce of which is exported far and wide,
despite the difficult communications. This Vera Paz region, which, for several
years after the arrival of the Spaniards was known as the ‘ Land of War,’ contains
numerous ruins of large cities, now overgrown with rank vegetation. Pueblo
Viejo, or the “Old Town,” which stands on the slopes above San Geronimo,
occupies the site of the ancient Xubabai. Rabinal lies farther west on an affluent
of the Chixoy, surrounded by banana, orange, and sugar plantations, in a district
dotted over with numerous old sepulchral mounds. Northwards are seen the
ruins of a fortress, and about six miles to the north-west the remains of Nim-
Pokom, formerly a capital of the Pokoman nation, and traditionally said to have

TOPOGRAPHY OF GUATEMALA. 229

contained 100,000 inhabitants. The ruins occupy a considerable space on the
crest of a hill; but the Pokoman language has been driven farther east by Quiché,
the idiom of the people who, before the arrival of the Spaniards, had gradually
acquired the political ascendency. Nearly all the summits in the Rabinal
district are crowned with ancient strongholds, now overgrown by a luxuriant
vegetation, while the Pakalah valley, facing the confluence of the Rabinal and
Chixoy rivers, is occupied by the temples, palaces, and citadels of Cahuinal, form-
ing the finest group of ruins in Vera Paz.

The towns situated on the plateaux and heights to the east of Quezaltenango
and Totonicapam, although still standing at a great elevation above the sea, are
‘not regarded as belonging to the region of the Altos. Solola, which has given

Fig. 96.—Soroza AND LAKE ATITLAN.
Scale 1 : 550,000.

S-1t AS
PRES AU
S{TACPANATLTLAN \

91°107 West on Greenwich

12 Miles.

its name to one of the departments of the republic, lies at an elevation of 7,000
feet on a terrace terminating towards Lake Atitlan in a rucky peak which rises
to a height of nearly 2,000 feet. Two deep ravines on the right and left sides
give to the terrace the aspect of a superb promontory, entirely detached from
the rest of the plateau except on the north side. Beyond the last houses of
Solola is seen the rampart of walls and huge blocks piled up and cemented with
an argillaceous mortar without apparent tenacity. Thus the vast ruin seems as
if about to fall with a crash into the blue lake, which is enclosed on the north by
steep cliffs, on the south by gently-sloping green banks, rising in a succession of
graceful curves towards the Atitlan voleano. A path cut at sharp angles in the
tufas and rocks of the escarpment leads from Solola to the margin of the lake,
and to the village of Panajachel, whose name is sometimes extended to tho basin

230 MEXICO, CENTRAL AMERICA, WEST INDIES.

itself. Solola, ancient capital of the Cakchiquels, and still inhabited by the
descendants of these proud and industrious Indians, bears also the name of Tecpan-
Atitlan, or “Communal Palace of Atitlan,” in contradistinction to the Atitlan of
the Ladinos. This place lies on the opposite or south side of the lake, and was
formerly capital of the Tzutujil nation, whose language still survives in the
district.

An easy pass, lying between the Atitlan and San Pedro voleanves, leads down
to the rich plantations of Costa Grande, which cover the lower slopes of the
mountains. But Zecojaté, the nearest seaport, being too dangerous for shipping,
the produce is mostly exported through Champerico. A road partly accessible
to wheeled traffic runs from the shores of Lake Atitlan through Muzatenango to
Retalhuleu. The coffee grown in the Mazatenango district is one of the most
appreciated in the European market.

On the lofty plateaux separating the basin of Lake Atitlan from that of the
Rio Motagua are seen the remains of one of the numerous cities which bore the
name of Quauhtemalan, or Guatemala, a name afterwards extended to the whole
region. The city, which was the capital of the Cakchiquels, and which they
called Ivimché, has a circumference of “three leagues.” It stood on a terrace
encircled on all sides by precipices, and accessible only by one approach, whose
two gateways were each closed by a single block of obsidian. The Spanish
conqueror Alvarado made it his residence in 1524, and gave it the name of
Santiago. A second Guatemala, standing on a terrace near the Iximché plateau,
is distinguished by the epithet of Tecpan-Guatemala, or “Communal Palace of
Guatemala.” About eighteen miles farther east, on a terrace overlooking the
Motagua valley, are seen the still more famous ruins of Mixco.

Chimaltenango is at present the capital of the department of like name, a region
roughly coinciding with the ancient domain of the Cakchiquels. It stands at a height
of about 6,000 feet exactly on the waterparting between the Atlantic and Pacitic
near the northern extremity of the chain of voleanoes which terminates southwards
in the Fuego peak. For trading purposes, it liesin the zone served by the railway
which runs from Guatemala to Escuintla and San José. Between Chimaltenango
and Guatemala, but nearer to the latter place, is situated the present Indian
village of Mirco, to which were removed the captives taken at the surrender of the
old city of this name. The first Guatemala of Spanish foundation, which succeeded
the two others of Cakchiquel origin, is the place now known as Ciudad Vieja, or
“Old Town.” It was founded in 1527 by Alvarado, in the picturesque Almolonga
valley on the banks of the Rio Pensativo, which flows through the Guacalate to
the Pacific. It would have been difficult to choose a more delightful situation
with a more equable and milder climate, a more fertile and better-watered soil,
or more romantic scenery, than this upland valley between the Fuego and Agua
volcanoes. Yet the city lasted only seventeen years. In 1541, after long rains,
the edge of the flooded crater of Mount Agua, dominating the rising town, suddenly
gave way, and nearly all the inhabitants, amongst whom was Alvarado’s wife, Dona
Beatriz Sim Ventura, the “ Hapless,” were either drowned or crushed beneath the

TOPOGRAPHY OF GUATEMALA. 261

ruins; Nothing remained except a magnificent tree, under whose shade the
Spaniards had assembled before the building of the city. Its site is at present
occupied by a few little houses lost amid the surrounding plantations. To avoid
another such disaster—which, however, could not have been repeated in the same
way—it was decided to remove the town farther north, and in 1542 Alvarado
supervised the foundation of a second capital—Santiago de los Caballeros la Nueva,
the “new,” but now called Antigua, the “ancient,” to distinguish it from the
modern Guatemala. The city flourished to such an extent that in a few years it
became the most populous place in Central America, and this despite a succession

Fig. 97.—Succrsstve DISPLACEMENTS OF GUATEMALA
Seale 1 : 750,000.

MS
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A ey SiN
UE NN RUN]

iy
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12 Miles,

of storms, floods, earthquakes, and epidemics. Its inhabitants, remarked Gage,
dwell between “two mountains which hold their ruin in suspense: the Agua
voleano threatens them with the deluge, and Fuego opens to them one of hell’s
gates.” The people had many a time made every preparation for flight, and
then, the danger over, had done nothing but repair their dwellings, when nearly
all the buildings were overthrown by the terrific earthquakes of 1773.

At last it was decided to select a third site for the capital, and choice was
made of the hamlet of Hrmita on the eievated Las Vacas plateau, about 25 miles
farther to the north-east. The work of reconstruction began immediately after
the disaster that had overtaken Antigua, but the official transfer was not made till
the year 1779. The first house of Guatemala, the hacienda de la Virgen, still
exists, and is pointed out to strangers as a historic monument. Nevertheless,

232 MEXICO, CENTRAL AMERICA, WEST INDIES.

Antigua was never completely abandoned, and it now ranks for size as the fifth
city of the republic. The population even continues to increase, its thermal waters
attract numerous invalids, the inhabitants of Guatemala have their country resi-
dences here, and many of the demolished structures have been rebuilt.

This third Guatemala, at present the largest city of Central America, lies on a
gentle slope in a depression of the plateau about 5,000 feet above the sea on the
divide between the two oceans. Guatemala is dominated by a little porphyry
eminence, the Cerro del Carmen, where stands the old hermitage, whence the place
takes the nam? of Ermita still in use amongst the Cakchiquels. From this knoll
a view is commanded of tke whole city, which covers a considerable space. The
surrounding landscape is unattractive owing to the absence of trees on the scrubby
watershed of Las Vacas, or the “ Cows,’

which throughout the Spanish occupation
has been used as a cittle ranche. But the vast panorama stretching beyond this
district, and limited southwards by the two lofty volcanic cones, presents a superb.
prospect : no other c rpital occupies a more marked central and commanding position
over the region sloping in all directions at its feet. Guatemala, which is laid out
with the perfect regularity of a model city, presents in the interior a somewhat
monotonous aspect. According to the original municipal regulations, inspired by
the memory of the disasters that had overtaken Antigua, the builders were for-
bidden to erect any houses exceeding 20 feet in height, and although this law is
no longer observed, the churches having here as elsewhere their domes and bel fries,
most of the structures are very low, gaining horizontally what they lose vertically.
Hence the population is somewhat scattered, except in the suburbs, where every
narrow cabin is occupied by an Indian family. Towards the middle of the century,
when it was scarcely half its present size, travellers were wont to compare Guate-
mala to a city of tombstones. Formerly all the large buildings were convents or
churches. Now the Jesuits’ establishment has been transformed to a national
institution with an observatory. The city also possesses a polytechnic and other
schools, learned societies, libraries and a museum. But the industries only suffice
to supply the local wants, and provisions are mostly brought from the surrounding
villages and plantations on the Pacific slope. Water is also brought from a con-
siderable distance by the two aqueducts of Mixco and Pinula. On the plateau
itself, covered with volcanic scoriz in some places to the depth of 600 or 700 feet,
the rain water is rapidly absorbed, reappearing lower down in remote valleys.
But to this very circumstance, preventing the accumulation of stagnant waters,
Guatemala probably owes its complete immunity from the ravages of typhus.
Still the place is not very healthy, and all maladies affecting the respiratory organs
are aggravated by the clouds of dust raised by every breeze from the loose igneous
soil. Hence most of the well-to-do citizens remove during the dry season to some
umbrageous rural retreat the most fashionable places at present are the towns and
villages situated farther south in the neighbourhood of Antigua.

The railway descending from Guatemala towards the Pacific branches off from
the valley of Antigua southwards in the direction of Lake Amatitlan, which it
skirts on the west side. The town of Amatitlan, situated on the lake at the outlet

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Fr

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“"MAIA TVAANHIO— V'ILNINOSA

TOPOGRAPHY OF GUATEMALA. 233

of the Rio Michatoya, was formerly a large hacienda belonging to the Dominican
friars, whose estate has become a vast plantation. During the flourishing days of
the cocbineal industry Amatitlan was a large place, with a population of 15,000 in
1865. But the ruin of the old dyeing processes was fatal to the prosperity of the
district.

Escuintla, the ancient Itzcuintlan of the Nahuas, is the chief station between
Amatitlan and the sea. This place, which before the Spanish conquest was a capital
of the Pipil nation, lies quite within the hot zone at an altitude of not more
than 1,450 feet above sea-level. The well-watered volcanic district dominated
by the Agua volcano is covered with an exuberant tropical vegetation, and before

Fig. 98.—Tuicxiy-Innasitep REGION OF GUATEMALA.

Scale 1 : 3,500,000.

D PES a

West of Gree

nwich

60 Miles.

the opening of the railway the wealthy citizens of Guatemala usually resorted
during the winter months from December to February to Escuintla, which enjoys
a milder climate than that of the plateaux. But its reputation as a rural retreat
has been impaired by the occasional outbursts of malignant fevers. In the same
climatic and vegetable zone, and some 25 miles farther west, lies the large town of
Santa Lucia Cozumathuapa, which has become famous for the discovery of statues
and curious bas-reliefs representing the “ King of the Vultures” (sarcoramphus
papa), in which the local Nahua artists display a talent at least equal to that of
the Aztec and Maya sculptors. San José, terminal station of the railway on the
Pacific, boasts of an iron pier projecting 1,000 fet seawards and provided with

234 MEXICO, CENTRAL AMERICA, WEST INDIES.

rails and cranes for the convenience of barges in connection with the shipping
which has to ride at anchor over half a mile from the port.

The department of Santa Rosa, conterminous on the east with Amatitlan
and Escuintla, has no large towns; its only trading station is Cuajiniquilapa,
which lies on the highway from San Salvador on the west side of the deep
valley of the Rio de los Esclavos, so called from the “Slaves,” that is, the Sinca
people occupying its banks. The broad stream is here crossed by an eleven-arched
bridge, built in the sevent:enth century by the Spaniards, and regarded as the
finest monument of Central America. At the south-east extremity of the republic
stretches the pastoral and agricultural department of Jud¢iapa, with chief town of
like name. This region is yearly increasing in importance for its exports of live
stock, indigo, and other produce to the neighbouring state. A few other centres
of population have assumed a somewhat urban aspect in the eastern districts of
Guatemala comprised within the Motagua basin. Such is Jalapa, which stands
at an altitude of 5,600 feet in an upland valley of great fertility. The town of
Esquipulas, also on an affluent of the Motagua, but near a pass leading down to the
sources of the Lempa in San Salvador, is for the greater part of the year almost
deserted, except by a scattered community of about 2,000 Indians. But on
January 15th, feast of Nuestro Señor de Esquipulas, a vast crowd throngs the
streets and squares lined with temporary huts. The sick and afflicted bend the
knee before a black effigy of Christ, with votive offerings of silver, carved
wooden objects, feather and straw work. With the religious feast is combined a
fair, which down to the middle of the century, before the construction of the
Panama railway, was frequented by pilgrim traders from Guatemala, ‘Salvador,
and even Mexico. As many as 80,000 persons, we are told by Juarros, were at
times assembled on the plain of Esquipulas. Near the town stands one of the
most magnificent churches in Central America. In a neighbouring southern
valley are worked the A/otepeque silver mines, the most productive in the state.

On the stream flowing from Esquipulas northwards to the Rio Motagua lie the
towns of Chiquimala and Zacapa, both capitals of departments of like name, and
destined to acquire considerable importance in the future development of the
country. They stand on the route to be followed by one of the projected railways
between Guatemala and Puerto Barrios on the Atlantic. About midway between
the two the Copan River joins that of Esquipulas after watering the plains of
Comotan and Jocotan, formerly centres of the cochineal and indigo industries, now
surrounded by rich tobacco plantations. About six miles below Zacapa the united
streams fall into the Rio Motagua, which a little farther down becomes navigable
for steamers, the heads of navigation being Guadan during the floods and Barbasco
in the dry season. In the forests of the Sierra del Mico north-east of the latter
place, the site of an Indian city, whose very name has perished, is indicated
by numerous pyramids and some fine ruins, especially carved monoliths, covered
with hieroglyphics, human figures, turtles, armadillos and other animals. This
group of monuments takes at present the name of Quirigua, from a village five
miles off. In 1839, when Stephens and Catherwood began their archeological

TOPOGRAPHY OF GUATEMALA. 235

exploration of Central America, the very existence of these ruins was unknown,
and travellers passed within a few miles of the place without hearing of them.
At that time nothing was known of any abandoned Indian city in this district
except Copan, which lay just beyond the Guatemalan frontier towards the source
of the Comotan. According to Stoll, the Quirigua remains strike the spectator
especially for their remarkable state of preservation, although not built of particu-
larly hard materials and exposed to a destructive climate at once very damp and
very hot; moreover, the inundations of the Motagua occasionally reach the site
of the ruins, and furrow the surface with ravines. Hence he infers that the
monuments cannot date from any remote period, and perhaps were even in a
perfect condition when the Spaniards made their appearance in the country.
The slave-hunters, who wasted the land in quest of labourers for the Cuban and
St. Domingo plantations, may have been the destroyers of these Indian cities,
although Maudslay thinks they must have already been in ruins at the time
of Cortes’ expedition. Being everywhere in search of provisions for his starving
followers, the conquercr would certainly have applied to Quirigua for succour had
such a large city been in existence at that time. The ruins of Chapulco, which are
said to lie on the south side of the Motagua valley over against Quirigua, have
not yet been explored. Paved causeways and sepulchral mounds occur here and
there in the surrounding forests.

The present route from Guatemala to the Atlintic diverges from the Motagua
valley at Barbasco, and after crossing the Mico range a little to the east of
Quirigua, leads down to Jzaba/, an unhealthy place on the south side of the Golfo
Dulce. Under the Spanish rule this port, which has the immense advantage of
lying some 60 miles inland, bat which is inaccessible to vessels of deep draught,
was unable to develop any trade, owing to the corsairs at that time infesting the
surrounding waters. But after the declaration of independence, Izabal almost
entirely monopolised the foreign trade of Guatemala, such as it was. Then the
discovery of the Californian goldfields, and the establishment of regular lines of
steamers between Panama and San Francisco, had the result of diverting the whole
life of Guatemala from the Atlantic to the Pacific seaboard. Thus Izabal found
itself abandoned, and its silent streets are now overgrown with the sensitive
mimosa. But the improvement of the communications, and peopling, or rather
repeopling of the land facing the Atlantic, cannot fail to revive and even increase
the trade of Izabal.

At the mouth of the Rio Dulce, on the Gulf of Amatique, stands the seaport of
Livingston, so named in honour of a jurist who drew up the legal code of Guate-
mala. The first colonists settled herein 1806, and the place is at present inhabited
by Caribs, agriculturists, fishers, and seafarers, who carry on a coasting trade with
Belize and Honduras, Livingston has recently been declared a free port, and is
already much frequented by American skippers, who here ship bananas and other
fruits in exchange for spirits. This port is the third in Guatemala, ranking next
in importance to San José and Champerico.

On the east bank of the neighbouring Rio Dulce, and near the present village

236 ù MEXICO, CENTRAL AMERICA, WEST INDIES.

of San Gil, stood the great city of Mito, which was captured by Cortes’ lieutenant,
Olid, and which he wished to make the capital of an independent state. The
eastern headland, at the issue of the Rio Dulce on the margin of the lake, is
crowned by the citadel of Sun Felipe, one of the most unhealthy places on the
seaboard. It has accordingly been chosen by the Government as a state prison.
Coban, capital of Alta Vera Paz, stands 4,330 feet above the sea in the
healthiest and one of the most fertile districts of Guatemala. It is a flourishing
place, with an increasing population of over 18,000, mostly industrious Quekchi
Indians, who raise considerable crops of mize and beans. Coffee, cinchona,
and the wax plant (myrica cerifera) are also successfully cultivated. The
neighbouring rocks are pierced by numerous caves, and the whole region may be
said to rest on limestone vaults, the most remarkable of which is that of San

Fig. 99.—Laxre PETEN.
Scale 1 : 720,000,

LAS ete

- 0°

12 Miles.

Agostin Lanquin, where a little affluent of the Polochic has its source. A good
carriage-road running south-east and east through the villages of Tactic, Tamahu,
Tucuru, and Teleman, leads to the riverain port of Panzos, where the local produce
is forwarded by a small steamer down the Polochic to the Golfo Dulce. No trace
now remains of the Nueva Sevilla, founded in 1544 near the mouth of the Polochic ;
but in 1825 the English established in the district the colony of <Abbotsville (Boca
Nueva), which was not more successful than its Spanish predecessor.

Libertad, capital of the department of Peten, better known by its Indian name
of Sacluc, lies on an affluent of the Pasion, a main branch of the Usumacinta.
The few inhabitants of the surrounding savannas are occupied chiefly in stock-
breeding. Excellent pasturage is afforded by the whole of this lake-studded
region stretching northwards in the direction of Yucatan. An island in the

dt a Los

PTIT 7

—— dun oué

TOPOGRAPHY OF GUATEMALA. 937

neighbouring Lake Peten is occupied by the ancient city of Tuyasal, now re-named
Flores in honour of a victim of the civil war of 1826. A steep road leads from
the place to the crest of a hill, whence a fine prospect is commanded of the
islands, headlands, wooded heights, and blue waters of the lake. On the opposite
shore are seen the two large Indian settlements of San Andres and San José dis-
posed along the slopes of the encircling hills. The whole territory of Peten is

Fig. 100.—DENSITY OF THE POPULATION 1x GUATEMALA.

Seale 1: 4,500,000.

a | aj
er a
+ Ie
ee
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ir L 7 S
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ee tien
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Inhabitan’s to the Square Mile

0 to 2. 2 to 20. 20 to 40. 40 to 60. 60 to 100. 100 and
upwards.

+ Towns of ove: 25,000 inhibitants.

ios 60 Miles.

surprisingly fertile, maize yielding two hundredfold without manure, while the
cacao, coffee, tobacco, and vanilla of the surrounding plantations are of the best
quality. The fishes inhabiting the lake are said to be all of distinct species.
According to the legend they were formerly of larger size than at present, being
fed in pre-Columbian times on the bodies of the dead. Of the ruined cities that are
scattered over the clearings north of the lake, in the direction of Yucatan, 7ihkal
alone has been explored. It lies 20 miles to the north-east of Peten, and is noted

238 MEXICO, CENTRAL AMERICA, WEST INDIES.

for its lofty verdure-clad pyramid, the most majestic Maya structure seen by
Maudslay during his explorations of Central America. Here Bernoulli found
about a dozen hieroglyphical tablets of sapota wood, which are now preserved in
the Museum of Basle.

Economic CoxXDITION oF GUATEMALA.

The population of Guatemala is steadily increasing almost exciusively by the
natural excess of births over the mortality. Foreign immigration is so slight that
not more than 2,000 strangers are settled in the republic. Of these the most
numerous are the “ Tiroleses,” a term applied generally to all North Italians, whose
industrious habits have earned for them the contempt of the Indians, hitherto
accustomed to regard their white masters as a superior race above the necessity of
manual labour. Since 1778 the population has grown from 260,000 to 1,450,000,
and the increase has been uniform in all the departments, except in some of the
northern districts on the Atlantic coast. At the same time illegitimacy is exces-
sive, especially amongst the Ladinos, or “civilised” Indians, nearly one-half of
whom are returned as born out of wedlock.

With the exception of wheat grown with potatoes on the Altos (uplands), the
agricultural produce amply suffices for the iocal demand. Like those of Mexico,
the Indians of the temperate zone live almost exclusively on maize, beans, and
bananas ; even tasajo, or jerked meat, is a rare delicacy, and pork is eaten only on
feast-days. Water is their usual drink, except on pay-day, when they get drunk
on a fiery brandy here bearing the Peruvian name of “ chicha,” or on other fermented
liquors such as fisté and pulique, which, like the poso/a of Tabasco, is food and
drink combined.

When Guatemala proclaimed her independence, next to nothing was raised for
the foreign markets ; but cochineal, for which the country is as well suited as Oaxaca _
itself, soon became a lucrative industry, especially in the Amatitlan and neigh-
bouring districts. The export rose from 16,000 pounds in 1827 to nearly 2,250,000
in the middle of the century. But the cochineal industry was ruined by the dis-.
covery of dyes extracted from coal, and nopal-fields are now rarely seen. They
have been replaced by coffee, which:is now the staple of the export trade. In the
districts where it is cultivated—Boca Costa, between Retalhuleu and Escuintla,
Antigua, Petapa, Amatitlan—the shrub thrives in the shade of leafy trees from
2,000 to 3,000 feet above the sea, and on open plantations up to 4,000 and even
5,000 feet. The Guatemalan coffee is highly esteemed, and the plant has hitherto
escaped the ravages of parasites. The crop of 1890, yielded by over 50,000,000
shrubs, was estimated at 30,000 tons, worth £3,000,000.

The temperate zone is also suited for sugar-growing, although, for want of
capital, Guatemala is unable to compete with the wealthy planters of Cuba, Louis-
iana, and Brazil. Nevertheless, from 5,000 to 6,000 tons are raised in the Costa
Cuca and Costa Grande districts, for the local wants and for the production of rum.
But distillers are so heavily taxed that little profit is made, except by smugglers.
The cultivation of cacao (theobroma) has been almost abandoned, although the

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ECONOMIC CONDITION OF GUATEMALA. 239

local varieties are of exquisite flavour. During the Spanish rule the cacao of
West Guatemala and Soconusco was reserved for the Court of Madrid; now it is
no longer exported, though it commands a higher price in the country than tke
best varieties exported to Europe. Indigo, formerly raised in the Retalhulcu
district, is also now neglected, but, being a vigorous plant, it continues to grow wi'd
and in many places has invaded the sugar and other plantations. Cotton is scarcely

Fig. 101.—Cuter Propucts oF GUATEMALA.
Scale 1: 4,500,000.

Ffures

Forests
Cedar

Forests
Cedar Forests

$ India rubbcr
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60 Miles.

ultivated, except by the Indians of the hot zone. The competition of foreign
importers has also nearly ruined the native weavers.

Unsuccessful attempts have been made to introduce caoutchouc (castilloa
elastica) into the temperate zone, but it is still collected in the forests, although
the wild plant yields an inferior gum. The cocoanut palm has been planted
round most of the coast towns and farmsteads, but more for ornament than use.
On the other hand, cinchona is extensively cultivated, especially in the Coban
district and on the Pacific slope; as many as 1,550,000 trees had already been
planted in the year 1884.

240 MEXICO, CENTRAL AMERICA, WEST INDIES.

Vast tracts, formerly under primeval forest, have been cleared, and mostly
converted into savannas for stock-breeding. Even in the districts under cultiva-
tion, the planters have their pofreros, or sacatales, little plots reserved for pasturage.
Nevertheless, the stock is insufficient for the local demand, and cattle have to be
imported at high rates from Mexico and Honduras. Sheep are confined chiefly
to the Altos, where the wool is used in the manufacture of coarse fabrics.

As in Mexico, most of the Indians employed on the plantations are held in a
state of real bondage by ‘the habilitaciones, or advances in money, which they are
unable to refund, and for which the produce of their future labour becomes
pledged. Hence, as in the days of slavery, the planters keep overseers to prevent
the men from escaping. Statute labour, and even the lash, flourish in spite of the
law, and the magistrates themselves supply the landowners with “hands” for a small
consideration. Nevertheless, in many districts the Indians are still free, and own
the land they till. In virtue of a recent law, all mayors, or the jefes politic
(political agents), of the Alta Vera Paz communes, where the civilised Indians
are most numerous, are required to allot to each native as his share of the public
domain a plot of about 4,400 square yards with free title, but on condition of
neither selling, letting, nor mortgaging the concession for the first ten years. Vast
spaces are still unoccupied, and these daldios, as they are called, all belong to the
State, which sells or leases them at pleasure. In order to safeguard what remains of
the vacant lands it has been decided to make no grants of more thin 3,400 acres
to a single person, who must be a native or naturalised citizen.

Although, compared to Mexico, Guatemala possesses little mineral wealth,
the Izabal district, on the Atlantic seaboard, was said to abound in auriferous
deposits, hence the expression “ Gold Coast” often applied to it in official documents
of the seventeenth century. These treasures were worked exclusively by English
miners, who, according to the tradition, extracted enough gold to purchase “a
kingdom of Spain.” In recent times they have been succeeded by Americans,
who have at least discovered gold washings, though the yield is valued at no more
than £6,000 a year. Quicksilver mines exist on the Huehuetenango plateaux ; but
the Indians, who from time to time offer the pure metal for sale, have hitherto
refused to reveal the locality. A mountain in the Cumbre de Chixoy is also said to
contain over 35,000,000 cubic feet of lead ore, three-fourths of which is pure metal.

The foreign trade of Guatemala, although steadily increasing, is still less than
£2,000,000, including all the exchanges. About nine-tenths of the total exports
are represented by coffee, the other articles in order of importance being sugar,
skins and hides, caoutchouc, silver, and bananas. Great Britain has the largest
share of the foreign traffic, the United States, France, and Germany ranking next
in importance.

The railway system is little developed, the only important lines being those
from San José to Guatemala, and from Champerico to Retalhuleu. It is now
proposed to continue these lines to the Atlantic, and Puerto Barrios, on St.
Thomas Bay, has been chosen as the eastern terminus of the transoceanic railway.
A few miles have already been constructed at the Atlantic end, but the ascent to

ECONOMIC CONDITION OF GUATEMALA. 241

the plateaux, the bridging of the Motagua, and other difficulties, have arrested
the progress of the line, the total length of which is estimated at 186 miles.
Even good carriage-roads are still rare, and the only bridge crossing the Motagur

Fig. 102.—GUATEMALAN ALCALDES, Attos REGION.

Eh,

has been swept away by the floods. Meanwhile, all merchandise destined for the
Atlantic has to be transported by pack mules. In the thinly-peopled regions of
the interior the postal service is still carried on, as in the time of Montezuma, by

242 MEXICO, CENTRAL AMERICA, WEST INDIES.

relays of couriers, by means of whom letters and verbal messages are transmitted
with great rapidity. But the development of the telegraph, and even of the
telephone, must soon supersede this antiquated system.

Education is still in a backward state, and in 1890 there were only 1,200
schools, with an attendance of 53,000, in the whole republic. The three colleges
for secondary instruction are frequented by about 1,200 students, and in all the
higher schools English is obligatory.

The Guatemalan constitution has undergone many changes. At one time part
of a larger state, at another an independent republic, alternately ruled by the
“ Serviles ” and the “ Liberals,” exposed to the tyranny of a Carrera or the
cruelty of a Barrios, the nation has had to modify its political charter with every
fresh revolution. The last constitution was that of 1879, completed in 1889,
though fresh changes will have still to be made if Guatemala is eventually to
become a member of the contemplated Central American Confederacy.

The legislative power is vested in a chamber of deputies, in the proportion
of one to 20,000 inhabitants, elected by all citizens capable of reading and writing.
The deputies, half of whom retire by rotation every two years, number at present
69, and are returned by electoral districts, which are represented by one,
two, or three members, according to their population. The executive is entrusted
to a president elected for six months, assisted by a state council, and six ministers
having charge of foreign affairs, the interior, publie works, war, finance, and
public instruction. Lastly, the judicial functions are exercised by a high court of
final appeal, and lower courts, all judges being appointed by election. Imprison-
ment for debt is abolished, and the domicile, as well as private correspondence, is
held to be inviolate, except in time of war or invasion, when all rights are
suspended. |

In the departments and communes, the ayuntamientos are constituted by
popular suffrage, although the Government reserves the right of dissolving these
assemblies, and replacing them by a judge. It also appoints to each department
a jefe politico, who is always a military officer, although charged with civil func-
tions. His power over the Indians is almost unlimited, and in each commune
a comisionado politico or gobernador, often chosen amongst the descendants of the
ancient caciques, transmits his orders to the alcaldes, of whom there are two or
three, according to the population of the district. The “ first alealde”’ has special
charge of the Ladinos, the “ second”’ of the Indians, and both wear the traditional
hat and band as the badge of their authority, besides tle cruciform or silver-
mounted rod.

The Church, long supreme in Guatemala, has no longer any recognized privi-
leges. According to the constitution, no cult enjoys any pre-eminence, and the
free exercise of all religions is authorised, although in 1890 there was only one
Protestant church in the capital. The Jesuits had already been expelled in 1767,
and in 1871 their establishments were finally suppressed and their property con-
fiscated. The same fate had befallen the other religious communities in 1829,
although they subsequently recovered part of their effects. But the property of

ECONOMIC CONDITION OF GUATEMALA, 243

all religious orders was “nationalised” in 1872, and in 1874 all nunneries were
suppressed except one. Some of the convents were used as schools or depôts ; but
most of the ecclesiastical domains benefited the “ politicians ’’ alone, many of whom
suddenly found themselves in possession of vast fortunes.

Officially all citizens between the ages of 18 and 50 are bound to military
service ; but the law exempts the only sons of widows, professors, officials, and all
capable of purchasing exemption by an annual payment of 50 dollars. Pure

Fig. 105.—Porrricaz Divisions oF GUATEMALA.
Scale 1 : 4.500.000.

“la Libertad
(Sacluc)

‘ ! SC: =.
Fetonicgpat| ="

| EB) ae A GUADEMALA FS
2 3 RY CHimalténan o Pome

99° West of Greenwich as

120 Miles,

Indians are not enrolled, but in time of war they are pressed into the transport
service.

The yearly budget varies from £800,000 to over £1,000,000, mostly raised
from the customs levied on nearly all foreign imports, or derived from the excise
on the manufacture and sale of spirits. Most of the revenue is absorbed by the
army, thougha yearly sum of £80,000 to £100,000 is devoted to public instruction.

In 1890 the national debt was about £4,200,000, over half of which was due to
English capitalists.

244 MEXICO, CENTRAL AMERICA, WEST INDIES.

The republic is divided into 23 administrative departments, all of which are
less than 3,000 square miles in extent, except the three great divisions of Huehue-
tenango (6,000), Alta Vera Paz (7,000), and Peten (10,000). The chief towns,
mostly bearing the same names as the departments, have all populations of less
than 20,000, except Totonicapam (20,000), Quezaltenango (24,000), and the state
capital, Guatemala (66,000).

III.— San SALVADOR.

San Salvador, or simply Salvador, smallest of tbe Central American states, is
the richest and relatively the most densely peopled. Its area is estimated at
about 7,250 square miles, or less than that of British Honduras, though its popula-
tion is at least twenty times greater than that colony. It forms a narrow zone of
quadrilateral shape on the Pacific slope, 156 miles long and with a mean breadth of
not more than 50 miles. The landward frontiers are mostly conventional lines, or
else indicated by streams both banks of which are inhabited by peoples of the same
origin. Towards Guatemala the line follows the course of the little river Paza to
the Chingo volcano, beyond which it intersects Lake Guija and trends round east-
wards to Honduras, where it traverses mountains and valleys with equal disregard
of the physical and ethnical relations. Northwards the frontier isnot indicated by
the crest of the sierra, but by the river Sumpul, a tributary of the Lempa, then by
the Lempa itself below the confluence, and lastly by another stream belonging
to the same basin. On the east it follows the course of the Goascoran, which
leaves to Salvador only a small part of the margin of Fonseca Bay.

The main range and the volcanic chain, which had already ramified in Guate-
mala, continue to diverge to a considerable distance eastwards, so that the former
belongs entirely to Honduras, the latter to Silvador. Here the prevailing rocks
are undoubtedly of eruptive origin, although many volcanic cones are no longer
easily recognised, their craters having been obliterated, and their slopes covered
with the same grey, white or yellowish clay which also overlay the Mexican and
Guatemalan mountains. The plains encircling the volcanoes consist to a great
depth of ashes and pumice, the upper crust of which, when decomposed, yields a
soil of extraordinary fertility.

East of Guatemala the chief range is that of the steep Matapan Mountains
(5,000 feet), which rise to the north-east of Lake Guija, and which from a distance
seein quite inaccessible. But noigneous cones are here visible, and most of the
active craters lie nearer to the Pacific coast, between Ahuachapam and the village
of San Juan de Dios, where is developed a line of the so-called ausoles disposed
transversely to the volcanic axis. At many points along this line gases are emitted
in abundance, but all the most remarkable ausoles, presenting every transition
from the mud volcano and gas jet to the hot spring, are concentrated close to
Ahuachapam, on the main route between the cities of Guatemala and San Salvador.
Over the plain are scattered large mud lakes, kept in a state of ebullition by the
underground vapours, and the clays deposited by the ausoles present every shade
of colour—blue, green, yellow or red, evidently due to the disintegration of ferru-

SAN SALVADOR 245

ginous rocks interspersed with alum and sulphur. To judge from the accounts
of early writers, all the ausoles would appear to have diminished in temperature
and activity during the. present century.

Farther east is developed an igneous svstem, the Madre del Volcan, with peaks
from 5,500 to 6,500 feet high, all of which—Apaneca, Launita (Lagunita), San
Juan, Aguila, Naranjo and others—are said by the inhabitants of Sonsonate to be
true volcanoes. But according to Dollfus and Mont-Serrat they are rather masses
of trachytic porphyry, covered with yellow clays and ashes ejected by distant
volcanoes. One, however, the Santa Ana (6,650 feet), appears to be a real crater,
which has been recently even in eruption. ;

A far more celebrated, though less elevated, volcano is that of Izalco, which

Fig. 104.—Ausor at AHUACHAPAM. .

belongs to the same system, and which, like the Jorullo of Mexico, has made its
appearance since the arrival of the Spaniards in the New World. At the beginning
of the seventeenth century, its site, or at least the district near Sonsonate, was
occupied by ausoles like those of Ahuachapam, which, however, appear to have after-
wards become extinct. But on February 23, 1770, the ground suddenly opened
and ejected copious lava streams. Then the cone began to rise above the surface,
and has ever since continued to expand ; but since the first eruption it has ejected
nothing but ashes. Formerly the explosions were almost incessant, and the
volumes of fiery vapour rolling up from the crater at night earned for Izalco the
title of the Faro del Salvador (‘Salvador Lighthouse”). Dollfus and Mont-
Serrat, who ascended it during a skort pericd of repose in 1866, estimated its height

246 MEXICO, CENTRAL AMERICA, WEST INDIES.

at a little over 6,000 feet, and found the summit pierced by three craters, one of
which emitted vapours with hissing and rumbling noises. Izalco is a perfect cone,
‘as regular as if turned out bya lathe.” rts j

San Salvador, a volcano rising to a height of 6,200 feet, about six miles north
of the capital, appears to have been quiescent since pre-Columbian times. From

a distance it presents none of the distinctive features of an igneous cone, being an _

elongated mass with irregular base, and wooded nearly to the summit. But it
terminates in the so-called bogueron, an immense crater nearly round, about three
miles in circuit and flooded by a green transparent lake 650 feet deep. On the
flanks is an ausol constantly discharging vapours, and near the north base are some

Fig. 105.—Vorcaxoes or Wesr SALVADOR.
Scale 1 : 1,200,000.

West of Greenwich

18 Miles.

parasitic cones, one of which, the Quezaltepec volcano, was the scene of a small
eruption at the beginning of the century. ©

But although the volcanoes in the neighbourhood of the capital have not been
the scene of any important eruptions during the historic period, earthquakes have
been frequent and almost as disastrous as in any region of the globe. They are
all the more dangerous that the ground on which San Salvador is built consists of a
whitish tufaceous rock, light and unstable, “ floating,” so to say, in the depressions
of the solid crust without coalescing with it. The city has been overthrown and
rebuilt on the same site no less than seven times during the last three centuries.
The sudden catastrophe of 1854 swallowed up many victims, while that of 1873
was even still more destructive to the buildings.

This disturbance appears to have radiated from Lake Ilopango (Apulo), a deep

ILOPANGO VOLCANO.

SAN SALVADOR. 247

basin six miles east of the capital, about 1,600 feet above the sea, encireled by steep
rocky shores. The lake, which has an area of 24 square miles, has frequently
changed its level, and towards the middle of the eighteenth century it was much
lower than at present. But after a series of landslips its eastern emissary, which
flows in a deep barranca to the Jiboa, a direct affluent of the Pacific, was dammed
up, thus causing a considerable rise in the level. In 1873, the lake was
violently agitated and raised about three feet above its normal level, and in 1879,
a fresh disturbance was followed by another rise of four feet.

Then the waters overflowed their banks, and rapidly excavated a channel,

Fig. 106.— Lake ILorAxGo.
Scale 1 : 170,000.

TEE Catal 7

= PTE Lena —

Dents

0 to 50 : 50 to 100 100 Fathoms
Fathoms. Fathoms. and upwards.

3 Miles.

whereby a subsidence of eight feet was effected in three hours. In 54 days there
was a total fall of 35 feet, the volume discharged being estimated at over 20,320
million cubic feet. The noxious vapours which at first accompanied these convul-
sions were followed by discharges of lava, and islets composed of eruptive matter
rose gradually above the surface of the seething waters. But when all was over
nothing remained except an island of hard lava 160 feet high, in the immediate
vicinity of which the sounding-line revealed a depth of over 100 fathoms.
During the eruption the geologist Goodyear recorded no less than 440 violent
shocks.

248 MEXICO, CENTRAL AMERICA, WEST INDIES.

North-east of Lake Ilopango rise the spurs of the Cojutepec volcano (3,400
feet), whose crater, though still visible, has been quiescent throughout the historic
period. Farther on follows Chichontépec, the “ Twin-peaked,” now known by
the name of San Vicente, highest volcano in Salvador (7,920 feet). Like Agua,
in Guatemala, its terminal cone formerly contained a tarn, which after a long
rainy season, burst its margin and rushed down to the plains through barrancas
scored in the flank of the mountain. The summit of San Vicente presents the
finest panoramic view in Salvador, embracing Lake Tlopango, the richly culti-

Fig. 107.—Votcanors or East SALYADOR.
Seale 1 : 600.000.

iquilisco,

SRE
slucuaram

ER NY
ZN” MA

West of G reenwich

12 Miles

vated slopes descending towards the Pacific, and the deep valley of the Rio
Lempa.

Beyond the gap caused by this fluvial valley the chain of igneous cones is
continued by the Tecapa volcano, also containing a lake of considerable extent,
whose waters, according to the natives, “are cold on one side and hot on the
other.” Farther on follow the mountains of Usulutan and the four-crested
Chinameca (5,000 feet). None of these have been the scene of recent disturbances,
while Chinameca’s vast crater, nearly a mile in circumference, is completely

closed. :
San Miguel, one of the loftiest summits in Salvador (7,i00 feet), which, thanks

——- =

RIVERS OF SALVADOR. 249

to its isolation, its rugged slopes, and sharply-truncated upper crest, presents an
aspect of unrivalled grandeur, offers a superb prospect of the surrounding plains
and river valleys away to the Pacific and ramifying inlets of Fonseca Bay. San
Miguel has been in eruption several times during the historic period, and in 1844
as many as fourteen fissures on its flanks discharged diverging streams of lava, one
of which flowed ten miles northwards to the outskirts of the city of San Miguel.
The terminal crater is one of the largest in Central America, being nearly two
miles in circuit and 500 feet deep.

Farther east the volcanic chain terminates in the twin crested Conchagua,
whose gently-inclined wooded slopes project into Fonseca Bay. Conchagua, whose
chief summit, the Cerro del Ocote, rises to a height of 4,100 feet, was supposed to
be extinct till the year 1868, when a fissure was opened on its flanks, whence
issued dense volumes of vapours, accompanied by violent earthquakes and avalanches
of rocks.

The lava streams which have been discharged parallel with the Pacific coast
have certainly contributed to modify the hydrographic system of Salvador by
damming up the streams and compelling them either to excavate fresh channels or
to fill vast lacustrine depressions. A distinct waterparting has been formed by
the volcanic range, whence on one side flow rapid torrents seawards, while, on the
other, the running waters converge in the great valley of the Rio Lempa, running
parallel with the igneous axis and the main Honduras range.

The Lempa, one of the chief rivers of Central America, rises in Guatemala, one
of its headstreams descending from the famous shrine of Esquipulas. After
crossing the frontier it receives the overflow of the great Lake Guija, which is
itself fed by the Ostua and numerous torrents from the surrounding mountains.

Below the confluence the Lempa continues to flow parallel with the Pacific
coast, receiving on both banks numerous tributaries from the northern and southern
ranges. Beyond its junction with its largest affluent, the Sumpul from the
Honduras mountains, it is joined from the east by the Tonola. Beyond this point
the mainstream forces a passage through the escarpments of the plateau down to
the plains, where its yellow waters, scarcely 10 feet deep in the dry season, flow
with a sluggish current a few yards above the level of the Pacific. During the
floods its lower course has a depth of from 20 to 26 feet, but at its mouth it is
obstructed by a bar never more than six or seven feet deep. Thus the Lempa, with
a course of about 185 miles, a catchment basin 6,000 square miles in extent, and a
mean discharge of from 16,000 to 24,000 cubic feet per second, is inaccessible to
marine navigation, though river steamers can ascend its lower reaches to the
great southern bend at the Tonola confluence. The San Miguel, which flows in a
nearly parallel channel farther east, enters the sea at the Estero de Jiquilisco, an
inlet which might easily be connected with the Lempa.

The Salvador coast, like that of Guatemala, has been subject to numerous
changes of level in past times. Banks of recent shells lying some distance inland
show that the beach has been upheaved, or else that the neighbouring waters have
subsided.

250 MEXICO, CENTRAL AMERICA, WEST INDIES.

CLIMATE, Frora, Fauna.

Being intersected by 13° 30’ north latitude, with a general southern incline, the
Salvador coastlands are exposed to great heats which, despite the refreshing sea-
breezes, range normally from about 78° to 83° Fahr. But the coastlands are the
least inhabited part of the country, most of the population being concentrated in
the elevated volcanic zone between 2,000 and 3,000 feet above sea-level, where the
mean temperature falls to 74° and even 70° Fahr. Farther north, in the low-lying
valley of the Lempa, which is inaccessible to the sea-breezes, the climate again
becomes hot and insalubrious; hence this district also is but sparsely peopled.

The rains, which are more copious on the seaward slopes of the mountains,
begin to fall about the middle of May, and last, with a short interruption towards
the end of June, till the month of September. They are always brought by the
vendavales, or southern winds, and are at times accompanied by storms, and even by
chubascos, or cyclones. © During the dry season, when the north winds prevail, the
coastlands are also exposed to storms, the so-called ferrales, which are much dreaded
by the fishing populations, especially in the months of February and March.

In its flora and fauna Salvador differs little from Guatemala. A characteristic
species is the balsam (myrospermum salvatorense), which has given its name to the
section of the coast between Acajutla and Libertad, and which was formerly called
‘ Peruvian Balsam,” because forwarded to Spain by the Callao route. Salvador is
especially rich in medicinal plants, gums, and resins. Of late years the planta-
tions have been somewhat frequently visited by clouds of locusts.

INHABITANTS.

The Pipils, that is, the Aztecs of Guatemala, were also in possession of west
Salvador at the time of the Spanish Conquest, as is attested by the local nomen-
clature. The centre of their power was at Suchitoto, north of the present capital,
and Bernal Diaz tells us that their social, religious and political institutions were
identical with those of the Mexican Aztecs. Their territory was limited north
and east by the Rio Lempa, which river long arrested the advance of the Spaniards.
The very name of the river is a corruption of Lempira, chief of the Chontal
Indians, who offered the stoutest resistance to the invaders.

After the conquest, the Pipils, like their Mexican kindred, were reduced to a
state of abject servitude; yet they became gradually assimilated to their masters
by crossings, and at the time of the declaration of independence in 1821, the
Salvador half-breeds greatly outnumbered the whites. At present, about four-
fifths of the population are of mixed Hispano-Indian descent. But there still
survive some nearly if not quite full-blood Indian communities, such as the Pipils
of Izalco, who still speak a Mexican dialect.

But the native customs and language are best preserved by the people of the
Balsam coast, south of the volcanic range. These Indians, who dwell in low huts
covered with foliage, cultivate a little maize, and do some trade in bananas with

TOPOGRAPHY CF SALVADOR. 251

the seaports. The money derived from this traffic is spent in decorating their -
churches and feasting their patron saints, all being now at least nominal Catholics.
Physically, they differ little from their Guatemalan neighbours, except in their
darker complexion, and the much smaller stature of their women.

ToroGRAPHY.

Ahuachapam, the first town near the Guatemalan, is perhaps the city of Paza
(Pazaeo), whence was named the Rio Paza, forming the present political frontier
between Guatemala and Salvador. Ahuachapam, with the neighbouring towns of
Atiquisaya, Chalchuapa, and Santa Ana, lies in a marvellously fertile district, on
which sugar and coffee are largely grown, but which has often been a battle-field

Fig. 108.—San SALVADOR AND 178 Environs.

Scale 1 : 230,000.

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in the wars between Guatemala and Salvador. It was at Chalchuapa that the
dictator, Rufino Barrios, was overthrown in the sanguinary engagement of 1885,
which put an end to the hegemony of Guatemala over the other Central American
states.

Sonsonate, or the “ Four Hundred Springs,” also lies in a rich and well-watered
plain, which is often illumined at night by the fires of Izalco. Formerly the most
important place in west Salvador, Sonsonate has now been eclipsed by Santa Ana,
which lies to the north of the volcano of like name on the main route between
Salvador and Guatemala. Since the earthquakes by which the capital has been
twice destroyed, Santa Ana has become the largest city in the republic; it is an
important agricultural centre, and the neighbouring district of J/etapan, on

252 MEXICO, CENTRAL AMERICA, WEST INDIES.

the north side of Lake Guija, abounds in productive iron, copper, silver, and
zinc mines.

Acajutla, the outlet of this western division of Salvador, lies on the west side
of a spacious bay, open to the western and southern winds. Despite its exposed
position, Acajutla has become the largest seaport in the state, shipping coffee and
other produce in exchange for foreign manufactured wares. It is the seaward
terminus of the first railway built in Salvador, which runs north to Sonsonate and
Armenia, the ancient Guaymoco, and which is ultimately to effect a junction with
the projected trunk line from Mexico to Panama. A branch in course of con-
struction runs through the Guarumal towards the flourishing coffee plantations of
Santa Ana, whence the main highway leads to San Salvador, capital of the
republic.

This place was originally founded in 1525 in the Suchitoto valley, much
farther north than its present position in the fertile plain, 2,300 feet above the
sea, at the east foot of the San Salvador volcano. The district, covered with coffee
and other plantations, is watered by the Aselguate, a southern affluent of the Rio
Lempa, while immediately to the south other streams flow in parallel channels
down to the Pacific. The city thus stands on the waterparting, and has the
further advantage of occupying a strong central position, defended by wide and
deep barrancas of extremely difficult access. But the district is exposed to
frequent and violent earthquakes, by which San Salvador has been twice destroyed —
during the present century. On these occasions, many of the inhabitants sought
refuge elsewhere, and especially at Santa Tecla, nine miles to the north-west.

Santa Tecla thus became the temporary capital, and even received the name of
Nuevo San Salvador, but being equally exposed to underground disturbances, as
well as to volcanic eruptions, it scarcely offered much more security than the first
place, which has been rebuilt of wood, on a principle of elastic frames calculated
to resist sudden shocks. San Salvador has now resumed its position as seat of
the administration, but has not yet recovered the population of 30,000 which it
possessed about the middle of the century. It communicates by a well-kept road
with its seaport of La Libertad, an exposed roadstead, where the shipping rides at
anchor in the surf over half a mile from the shore.

East of the capital the main route passes north of Lake Ilopango to Coju-
tepeque, an Indian town, followed successively by Jihoa and San Vicente, the
latter founded in 1638 on a western affluent of the lower Lempa on the site of the
ancient Aztee city of Tehuacan. The ruins of this place, known by the name of
Opico, stand on a lateral terrace of the San Vicente voleano. The route leads
thence through Sacatecoluca to the port of Concordia, at the mouth of the Rio
Jiboa.

In the marshy and insalubrious valley of the Lempa there are no centres of
population, the nearest towns being Suchitoto, I/obasco, and Sensuntepeque, which
stand on breezy headlands, where the temperature is lower than in the low-lying
fluvial basin. Chalatenango, the only town in the northern district between the
Lempa and the Sumpul, lies also at some distance from the mainstream.

TOPOGRAPHY OF SALVADOR. 253

East of the Lempa the largest place is Chinameca, which is inhabited by
Indians and half-castes. San Miguel, lying farther east on the river of that
name, derives some importance from its fairs, which are frequented by traders

Fig. 109.—La Ligerran, Port or San SALVADOR.

Yaga.

from all parts of Central America and Mexico. Its seaport of La Union stands on
one of the numerous sheltered inlets of Fonseca Bay where excellent anchorage is
afforded at about a mile from the shore.

254 : MEXICO, CENTRAL AMERICA, WEST INDIES.

Economic Conprrion oF SALVADOR.

Despite its foreign wars and civil strife, Salvador is a prosperous country, as
shown by the rapid increase of population unaided by any foreign immigration.
Since 1778, when it was originally returned at 117,436, the population has
certainly more than quadrupled, the census of 1886 yielding over 651,000, and the
estimate for 1890 being at least 675,000, or about 70 inhabitants per square mile.
At the same proportion the United States would have a population of from
340,000,000 to 350,000,000, instead of 63,000,000 according to the census of
1890.

Recently Salvador has given a striking proof of its vitality by the ease with
which it has accomplished a great economic revolution. ‘Till lately its revenue

Fig. 110 —Densrty OF THE POPULATION OF SALVADOR.
Seale 1 : 2,700.000.

oo AE TE

West of Greenwich
Inhabitants to the Square Mile.
0 to 40. 40 to 60. 60 to 80. 80 to 120. 120 and upwa ds.

Each square represents a popula’ion of 500.
e Towns of over 20,000 inhabitants.

60 Miles.

depended mainly on indigo, its only article of export. But since the discovery of
‘the various coal-tar dyes superseding the use of indigo, the Salvador planters have
had to abandon its cultivation and replace it chiefly by coffee and sugar. The
yield of the silver mines has also contributed to pay for the textiles, hardware,
corn, and other articles imported from abroad. The total value of the exchanges
is about £4 per head of the population, amounting in 1890 to over £2,250,000.
Inland traffic is facilitated by carriage-roads with a total length of 2,700
miles in 1890, but in the same year there were only 36 miles of railways. The
telegraph and postal services are also in a backward state, though education, now
gratuitous and obligatory, is making considerable progress. In 1889 the schools
were attended by over 40,000 scholars, or one-eighteenth of the whole population,

HONDURAS. 255

exclusive of 1,300 frequenting the high schools and 180 following the courses of
the national university in the capital.

Salvador has been an independent state only since 1859, and even since then
its constitution, which should be representative, has been frequently modified an
superseded by a military government tempered by insurrections. In theory the
legislative power is vested in a national assembly of 42 members, elected for
one year by popular suffrage, while the executive is exercised by a president, who
is also elected by the people, but for four years, and who chooses his own ministry,
consisting of four secretaries of state.

The standing army comprises about 2,000 of all arms, with a militia nominally
40,000 strong. The administration of justice is entrusted to a supreme court
situated in the capital, with courts of appeal at Santa Ana, Cojutepeque, and San
Miguel, tribunals of first instance for each of the three judiciary districts, and
justices of the peace for the towns and communes.

As in most American states, the revenue is mainly derived from the customs,
about one-third being contributed by monopolies on tobacco and spirits. Not
more than a fourth of the national income is absorbed by the army, a proportion
less than that expended on education and public works. In 1890 the debt
amounted to £1,300,000.

Under the Spanish régime Salvador formed part of the viceroyalty of Guate-
mala, comprising the four provinces of Sonsonate, San Salvador, San Vicente,
and San Miguel. At present the republic is divided into fourteen adminis-
trative departments, grouped under three divisions, for which see Appendix.

TV.—Honpvuras.

The very name of Honduras recalls the times of the discovery, when the
Spanish pilots, advancing cautiously along the.coasts, reported shallow soundings
(honduras) in the waters at the head of Honduras Bay. Columbus, who in 1502
first explored these waters between Capes Caxinas (Honduras) and Gracias-à-Dios,
ran great risks amid the surrounding reefs and shoals. But its present name was
given to the seaboard not by Columbus, but by Bartholomew de las Casas, who in
his Discovery of the West Indies by the Spaniards, speaks of the land of
“ Hondure,” as if this name were of Indian origin. Twenty-two years later, at
the time of Fernan Cortes’ famous expedition across Yucatan, the country was
known to the Spaniards by the name of Hibueras or Higueras, and it has also been
called ‘‘ New Estremadura.”’

After forming part of the Guatemalan viceroyalty, Honduras was separated
from the mother country with the rest of Central America, and at present forms
one of the five sister republics. But despite its natural advantages of climate,
central position and excellent harbours on both oceans, its progress has been
relatively slow. Under the Spanish rule the seaports and cultivated plains on
the Atlantic side attracted the attention of the corsairs by whom these coast-
lands were ravaged for a great distance inland. The country has, doubtless,

256 MEXICO, CENTRAL AMERICA, WEST INDIES.

been gradually resettled, but the highest estimates assign it a population of not
more than six persons to the square mile.

PuysicaL Fratu RES,

Like Guatemala, Honduras is of triangular shape, but its position is reversed,
so that its base rests on the Atlantic, and its apex reaches the Pacific at Fonseca Bay.
The limits of the state are, how-

Fig. 111.—INTEROCEANIC TERPAR : =. £39
8 Warenpantine, Hompunas ever, almost everywhere indi-

Seale 1 : 480,000. 3 ;
cated, not by conventional lines as

my elsewhere, but by such natural
7)
ND features as mountains and river

AD valleys. Jn the north-west it is
ees separated from Guatemala by a
winding frontier, which, while
assigning to Honduras the Guate-
malan valley of Copan, coincides
in a general way with the crests
agent 20 of the Merendon, Espiritu Santo
“an and Grita ranges, beyond which
it follows the course of the Rio
Tinto to a secondary inlet of
Honduras Bay.
Towards Salvador the frontier
3 is formed mainly by the Rivers
Ui Pager Xe yi N Sumpul, Lempa, Tonola and Goas-
LE “ Wise MG \iga | coran, and towards Nicaragua by
oon the Rio Negro on the Pacific side,
and by the Ocotal and Segovia
on the Atlantic slope, the common
waterparting being indicated by
the Dipilto range.
The interior is still imperfectly
known, but the country may, in

a general way, be said to be di-

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rene Peut Create vided into two unequal slopes by
a sierra madre disposed parallel

7) mt
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12 Miles.

with, and at a mean distance ot
about 60 miles from, the Pacific coast. This range is much more precipitous on
the Pacific than on the Atlantic side, so that the south side should be regarded
rather as the escarpment of a plateau carved into distinct masses by streams
flowing north to the Caribbean Sea.
Towards the west or Guatemalan frontier the Sierra de Pacaya (6,600 feet)
branches off from the Merendon range and farther on merges in the Sierra de
Selaque, round which the running waters diverge in all directions. Here the

PHYSICAL FEATURES OF HONDURAS. 257

Honduras orographic system appears to culminate in several peaks exceeding 10,000
feet in height. Farther on the uplands fall and again rise in the direction of the
east, where they develop the Opalaca and San Juan ranges. At the extremity of
this chain is opened the great depression forming the natural highway of communi-
cation between the two fluvial basins of Humuya on the north, and Goascoran on
the south. Here the waterparting is indicated only by the relatively low passes
of Guajoca (2,300 feet) and Rancho Chiquito (2,400), which are already traversed
by a road, and which will probably soon be crossed by a railway of easy ascent and
free from tunnels.

Rocks of tertiary formation overlying the older strata recall the epoch when
this depression was still flooded by a channel flowing between the two oceans when
Central America formed a chain of islands, not, as at present, a continuous
isthmus.

Beyond the depression the main range, here called the Sierra Lepaterique,
soon ramifies into a northern and a southern chain, the former running north-east
to Cape Gracias-à-Dios, the latter southwards to the main range of Nicaragua.

The igneous system, which in Salvador and Nicaragua runs between the main
range and the Pacific coast, disappears altogether on the Honduras mainland, but
is represented in the islets of Fonseca Bay. A slight upheaval of the marine hed
would suffice to connect Sacate Grande and the other volcanoes in this bay with
the opposite coast. Sacate Grande, largest of the group, rises to a height of 2,000
feet, while the neighbouring Tiger Island is 600 feet higher.

On the Atlantic side the Merendon main range is continued north-westwards
by the long crest of the Espiritu Santo and Grita chains, which run at a mean
altitude of over 6,700 feet between the valleys of the Guatemalan Rio Motagua and
the Honduras Rio Chamelicon. The system rises probably to 10,000 feet in the Omoa
group, which forms its seaward terminus near the port of Omoa. A northern
spur of the Opalaca hills terminates in the huge and nearly isolated bluff of
Mount Puca, while the San Juan crags, dominating the interoceanic depression,
are continued in the same northerly direction by the Montecillos and the Sierra de
Canchia, which confront the Comayagua Mountains on the opposite side of the
depression.

Eastwards the Lepaterique hills are ccnnected with the central mass of the
Sierra de Chile, whence various ridges ramify between deep valleys in different
directions. Lastly, the parting-line between Honduras and Nicaragua is formed
by the Cordillera de Dipilto, which is continued seawards to the converging point
of the rectilinear Honduras and Mosquitia shore-lines.

In the interior of the state the Sierra Misoco runs due north-east nearly
parallel with the Sulaco and Pija ridges, and Mount Paya, rising to a height of
3,730 feet, near Cape Cameron, probably belongs to a branch of the same system.
On the northern edge of the Honduras plateau the Congrehoy ridge, which cul-
minates in a peak 8,206 feet high, seems to form a distinct chain disposed parallel
with the neighbouring Bay Islands.

Some of the mountains of the interior have been spoken of as volcanoes, but

258 MEXICO, CENTRAL AMERICA, WEST INDIES.

they have never been seen in eruption, nor have they yet been ascended by any
scientific explorer. Such pretended volcanoes are Teapasemi (3,000 feet), in the
Dipilto range, about midway between the two oceans, the Guaymaca and Boqueron
heights in the Misoco chain.

Rivers, ISLANDS, INLETS.

Honduras, being well exposed to the Atlantic rains, is traversed by numerous
watercourses, nor are there any closed basins, as in Mexico and Guatemala. In
the west the first copious stream is the Chamelicon (Chamlico), which flows from
the Merendon Hills parallel with the Motagua of Guatemala, terminating, after a
rapid course of over 160 miles, in a delta connected by one branch with the
Puerto-Caballos lagoon. The Chamelicon might almost be regarded as an
affluent of the Ulua, its lower course running for 30 miles. parallel with that
stream through the same low-lying plain, where their waters are intermingled
during the floods.

But apart from the Chamelicon, the Ulua is the largest river in Honduras, its
catchment basin comprising about a third of the whole state, and occupying all
the space between the Merendon and Chile ranges. From the west it is joined
by the Santiago (Venta), swollen by the Rio Santa Barbara, and various emissaries
from the great Lake Yojoa. From the south comes the Humuya, which may be
regarded as the main branch ; from the east, the Sulaco.

Lake Yojoa (Taulebé) has the form of an upland valley disposed crescent-shape
from south to north, and without any visible affluent at low water. But during
the floods it rises to a great height, sending its overflow through the Jaitique at
its south-eastern extremity to the Santa Barbara. But there are other outlets by
which its waters also escape, disappearing in the pozos or cavities of the sur-
rounding fossiliferous limestone rocks and reappearing lower down as tributaries
of the Santa Barbara. According to Stanton and Edwards, there are no less than
nine of these underground emissaries all flowing during the rainy season to the
headstreams of the Ulua.

During the floods the Ulua is accessible to small steamers as far as the Sulaco
confluence; but the bar at its mouth has scarcely more than three feet of water,
so that shipping is obliged to anchor at some distance from the estuary.

The next large river going east from the Ulua is the Aguan or Romano, which
enters the sea through two channels between Capes Honduras (Caxinas) and
Cameron. The Romano, which is said to have a course of over 120 miles, traverses
a forest region of great sylvan beauty abounding in auriferous sands. But it is
a less copious stream than the Patuca, whose various sources flow from the Misoco
and Chile ranges and unite in a single channel above the formidable gorge of the
Portal del Infierno, or “ Hell-gate.’’ From this point the Patuca is navigable for
the rest of its course to its mouth, which presents the same difficulties as those of
all the other estuaries along this coast.

The abundant alluvia of the Rio Patuca have advanced in a sharp point beyond
the normal shore-iine, enclosing right and left shallow marine lagoons, which

THE BAY ISLANDS. 259

communicate through several channels with the open sea. On the west is the
Brus (Brewer) lagoon; on the east the much larger Caratasca (Cartago) basin,
with a depth of 16 feet in the centre. The grassy shores of these inlets are dotted
over with clumps of fir and other trees, giving the landscape the aspect cf an
English park.

Although everywhere navigable, the Honduras waters rest on a submarine
bed scarcely more than 50 fathoms deep, with banks, reefs, and islets rising
above the surface. This plateau extends seawards for a mean distance of about
18 or 20 miles, when the sounding-line plunges suddenly into depths of

Fig. 112.—Bay ISLANDS.
Scale 1 : 1,500,000.

Depths.
0 to 100 100 Fathoms

Fathoms and upwards.

30 Miles.

500 fathoms. Beyond Cape Cameron the shallows extend to Mosquito Bank,
which projects for nearly 130 miles in the direction of Jamaica, The plateau,
which has an average depth of about 20 fathoms, reproduces east of Honduras
the same limestone formation as the submerged terrace encircling the Yucatan
seaboard.

Above the submarine bed rises a long line of coralline islets, which are
collectively called the Bay Islands, but of which one alone, Utila, deserves the
name of island. Utila stands at the western extremity of the group, at the very
edge of the plateau, where the soundings suddenly reveal depths of over 200 fathoms

260 MEXICO, CENTRAL AMERICA, WEST INDIES.

on the north side. Roatan, Elena, Barbareta (Borburata), Bonaca and the other
members of the group all lie in deep water, and are disposed in the direction from
west-south-west to east-north-east. Roatan, which is by far the largest, is 30
miles long, and is continued eastwards by Elena and Barbareta. Although
scarcely a mile wide, Roatan has a few hills, culminating westwards in an eminence
800 feet high. Bonaca (Guanaja), the Isla de Pinos of Columbus, which lies at
the eastern extremity of the group, is still more elevated, its pine-clad granite
peak rising to a height of 1,200 feet.

On the southern slope of Honduras, the two most copious streams are the
Goascoran, the lower course of which forms the boundary-line towards Salvador,
and the Choluteca, whose basin is entirely comprised within Honduras territory.

The Choluteca flows from the Lepaterique hills to the marine inlet, to which,
in 1522, Gil Gonzalez de Avila gave the name of Fonseca, in honour of Cortes’
relentless enemy, Bishop Fonseca. This vast basin has a superficial area of over
800 square miles, with.a breadth of 22 miles between the two outer headlands of
Coseguina and Amapala. The narrowest of the four navigable passages by which
it communicates with the sea is about two miles wide between the Conchagua
and Conchaguita volcanoes, with a mean depth of about 40 feet. Within these
passages the gulf develops several secondary inlets, such as those of L’Estero Real
and La Union, the former penetrating south-eastwards into Nicaragua, the latter
north-westwards into Salvador. Above the surface rise several reefs and islands,
conspicuous amongst which is the symmetrical cone of Tiger Island. Notwith-
standing its great extent, the Gulf of Fonseca is too shallow to be regarded as a
marine basin ; it is probably little more than a flooded depression, nowhere more
than ten fathoms deep, and navigable only by vessels of moderate draught.

CLIMATE, FLORA, Fauna.

Owing to its mean elevation of at least 3,000 feet above the sea, Honduras
enjoys a comparatively temperate climate, though the low-lying coastlands are
oppressively hot and insalubrious. The Atlantic seaboard especially suffers from
the excess of moisture brought by the vapour-charged trade winds. Here the
mean temperature ranges from 75° to 82° Fahr., whereas it is scarcely more than
68° at the capital, Tegucigalpa, which stands at an altitude of 3,320 feet. Accord-
ing to Squier, the annual rainfall on the Atlantic slope is about 120 inches.

The Central American flora and fauna differ in details only at their two
extremities, the isthmuses of Tehuantepec and Darien. But here and there sharp
transitions occur between the species, and in certain regions the secondary
differences between the various organic forms are more numerous than elsewhere.
Such is the case in central Honduras, where the Humuya and Goascoran valleys
with the intermediate depression constitute a natural biological parting-line. Here
the flora and fauna on either side often present remarkable contrasts. One of the
characteristic Honduras trees is the pine, which occurs in all the upland districts,
and even on both slopes down to the vicinity of the Pacific coast. But here it

SCENERY,

HONDURAS

INHABITANTS OF HONDURAS. 261

does not reach lower than an altitude of about 1,250 feet, whereas on the Atlantic
slopes, especially on the plains of Sula, it descends as low as 250 feet, while along
the watercourses of Truxillo it is dotted over the savannas like the clumps of trees
characteristic of English scenery.

INHABITANTS.

About three-fourths of the population of Honduras appear to be Ladinos, or
more or less civilised Hispano-American half-castes. The pure Indian element
scarcely numbers 70,000 altogether, and even these “ wild tribes ” now live at
peace with their Spanish-speaking rulers, and recognise their authority. To the
Spanish conquerors their forefathers had offered a brave and steadfast resistance,
and those of the interior at least escaped extermination, whereas most of those
dwelling on the coastlands, or along the navigable rivers, were carried away by the
corsairs, to perish on the plantations of the West Indies.

In the western parts of the republic the natives are of the same speech as those
of Guatemala. Such are the Chorti of Copan, kinsmen of the Pokoman Mayas.
The most remarkable historic ruins of Honduras have been discovered in their
territory, and the builders of these monuments are supposed to have been the
ancestors of the Indians still inhabiting the district. Hence the Chorti were
probably fully as civilised as the Aztecs and Mayas, and even if the other natives
of Honduras have left no such monuments, they were all at least settled agricul-
turists and skilled artisans. Various Aztec geographical terms occurring in south
Honduras show that Aztec was regarded as the language of culture in a pre-
eminent sense.

At present the Honduras Indians are collectively designated by the name of
Lencas. Villages exclusively inhabited by them are scattered over the plateau, and
are met even in the neighbourhood of the two capitals, Comayagua and Teguci-
galpa. To the same stock belong the Xicacs (Hicacos), the Payas and the Toacas
of the northern slopes and Atlantic coastlands.

All resemble each other in their low stature, thickset frames, and extraordinary
staying power as carriers of heavy loads. The Toacas, who occupy the upper
affluents of the Patuca, and who shoot the dangerous rapids of that river in their
light but firm pipantes of cedar-wood, also produce excellent cotton or wild silk
fabrics interwoven with the down of birds. They speak a dialect different from
that of the other Lencas, as do also the Xicacs, who number about 5,000 and keep
quite aloof from the Ladinos.

The Payas or Poyas of the Rio Negro near Cape Cameron have preserved their
patriarchal customs ; like the Pueblo Indians of New Mexico and Arizona. they still
dweilin large oval houses about 80 feet long by 30 feet broad, in which each family
has its own apartments. The Payas, like all the other natives, call themselves
Catholics, but this formal profession of faith is merely an act of submissicn to the
dominant white race.

After the extermination of the coast Indians negroes became numerous along
the seaboard. About the beginning of the seventeenth century a large slaver was

262 MEXICO, CENTRAL AMERICA, WEST INDIES.

said to have been stranded near Cape Gracias-à-Dios, and the Africans, escaping
from the wreck, founded a petty republican state in the district. Later they were
joined by other fugitives from the West Indies; then some English planters
introduced slaves and founded settlements in the hope of conquering the country.
Gradually transformed by interminglings, the whole of this black population
consisted at the end of the last century mainly of Sambos, that is, negro and
Indian half-breeds. They were numerous, especially about the lower Patuca and
the neighbouring Brus and Caratasca lagoons; but a great invasion drove most of
them southwards to the Mosquito Coast in Nicaragua.

The invaders were themselves exiles, some 9,000 Carib Indians removed in
1796 by the English from St. Vincent to Roatan, one of the Bay Islands. Many
remained as fishers and gardeners on this and other members of the group, but the
majority accepted the offer made them by the Spanish Government of some lands
near Truxillo on the Honduras coast. These Carib exiles from St. Vincent have
gradually become the dominant race, not only in the Bay Islands, but along the
whole of the Honduras and Guatemalan seaboard, as well as throughout the
southern part of British Honduras. They are at present estimated at about
20,000, and are a thriving industrious people, many already owning sugar and
tobacco plantations besides local factories.

Nearly all are more or less familiar with three languages, English, Spanish,
and their West Indian mother-tongue, which, however, appears to be dying out.
But while these communities are being gradually assimilated to the surrounding
Europeanised populations, there are many other Honduras Caribs who, while
calling themselves “ Cristianos,” still retain many of the usages of their pagan
ancestors. They practise polygamy on the condition of assigning to each wife
her separate establishment, cottage, and garden, and treating all exactly alike.

On the Atlantic coast of Honduras, the English and Indian half-castes are the
most numerous element, and a more or less corrupt form of English is the
dominant language in many districts. This is partly due to the neighbourhood
of Belize, partly also to the repeated attempts made by the English Government to
acquire formal possession of the whole seaboard. In the last century the Jamaica
freebooters had become masters of the Rio Negro (Tinto or Poya), where their
plantations were protected by a fort, which, however, they had to evacuate in
virtue of the treaty of Versailles.

But they attempted to return, as they had returned to Belize, and after seizing
the Bay Islands, spoke of Roatan as a “new Gibraltar,” the ‘key to Spanish
America,” and so forth. In 1819 Sir Gregor Macgregor, who had become cacique
of the Payas, settled on the Rio Negro and founded a paper kingdom embracing a
great part of Honduras and Nicaragua. Again in 1839 an English company, heirs
to the Scottish cacique, endeavoured to appropriate the Atlantic slope of Honduras
by founding the new province of “ Victoria,” with its capital, Fort William, over
against the Bay Islands. But all these attempts at gaining a footing in Honduras
were brought to a close by the intervention of the United States in 1850, when the
disputed territories were restored to Honduras. ;

TOPOGRAPHY OF HONDURAS. 263

ToroGRAPHY.

Copan, which has given its name to the westernmost department of the
republic, has become famous for the surrounding ruins, which were first described
in 1576 by Palacio in a report to Philip II. They were then forgotten till the
present century, when they were again visited and described by Galindo, Stephens,
aud Catherwood. The chief building rises to a height of 60, and in some parts
even 100 feet on the banks of the River Copan, three-quarters of a mile to the east
of the village. Since its erection the river has evidently shifted its bed farther
south, where it has eroded the base of the edifice. Trees also spring from the
fissures in the masonry, while the summits are entirely clothed in vegetation.
An opening, to which the pile is indebted for its Spanish name of Las Ventanas,
the “ Windows,” reveals the dense thicket now filling the inner courts of the temple.

The irregular enclosing walls on the sides away from the river are flanked by
pyramids, and interrupted by broad flights of steps, mostly forced upwards by the
roots of trees. The numerous idols, which have also been displaced or else half
buried in foliage, consist of sandstone monoliths, carved with a profusion of details
unsurpassed by those of the Hindu temples. The central figure, of colossal size,
but carefully modelled, is surrounded by reliefs of all kinds, ornaments, symbols,
and hieroglyphics, differing little from those covering the Maya monuments.
The huge blocks described as altars are for the most part less elaborately
embellished than the vertical steles of the idols; but most of them reproduce the
type of high heads, prominent jaws, and receding foreheads figured on the temples
of Tabasco and Yucatan.

Still more remarkable is a semicircular altar, exactly like the fai-kr of the
Chinese, symbolising the “great vault,” the “ pole of the world,” the union of
force and matter, the principle without beginning or end.

The whole group of ruins stretches for some miles along the river, and an
eminence 2,000 feet high on the opposite side is also crowned with crumbling
walls, while huge blocks, intended for fresh structures, have been left unfinished
in the surrounding quarries. The village of Cachapa, seven miles above Copan,
also occupies the site of a ruined city.

Santa Rosa, capital of the department of Copa lies in the fertile district of
Sensenti, which is watered by the Santiago branch of the Ulua, and which yields
the best tobacco in Honduras. The Majocote affluent of the same river traverses
Gracias, which is also the capital of a department abounding in mineral wealth.
Gracias was founded by Alvarado’s lieutenant, Chavez, in 1536.

Santa Barbara, on a lateral tributary of the Santiago, is the chief town of the
favoured department which comprises the rich plain of Sula, the alluvial lands
of the lower Ulua and Chamelicon, and the best ports on the Atlantic coast. But
the Sula district, densely peopled before the conquest, is now almost deserted,
though the town of San Pedro de Sula, on the west side of the plain, is the most
important agricultural centre in the state.

The chief seaports in the department of Santa Barbara, and on the whole sea-

264 MEXICO, CENTRAL AMERICA, WEST INDIES.

board on the Atlantic side, are Puerto Cortes and Omoa, both of which lie to the
west of the Ulua and Chamelicon estuaries. Puerto Cortes owes its name to the
Mexican conqueror, who founded it at the time of his Honduras expedition ; but
it is now more commonly known as Puerto Cuballos. The harbour is enclosed by
a tongue of land projecting westwards, and sheltering it from the winds and surf
of the high seas. This spacious and deep basin might easily be greatly enlarged

Fig. 113.—Purrro Corres AND LAKE ALVARADo.
Scale 1 : 50,000.

CAE COPA SO QE
ed
——— [Puerto Corte Ene

Depths.
Sands exposed 0 to 5 5 ba nous '
at low water. Fathoms. and upwaris.
1,100 Yards.

by the Alvarado lagoon, with which it already communicates through a channel
about six feet deep.

But despite its manifold advantages, Puerto Caballos, being exposed to the attacks
of the buccaneers, was long abandoned for the more easily protected port of Omoa,
which is approached by a narrow passage six miles farther west. N ow, however,
Puerto Caballos has resumed its former importance as the terminus of a railway run-
ning sout!.wards to San Pedro de Sula for Comayagua, and eventually for the Pacific
coast. Naco, famous at the time of the conquest, has disappeared, but it probably
stood at the mouth of the Chamelicon.

TOPOGRAPHY OF HONDURAS. 26

Puerto Sal and Triunfo, lying east of the Ulua, are merely exposed roadsteads,
followed by the much more frequented port of Progreso, which is formed by an
indentation on the south side of Roatan Island, perfectly sheltered from all
winds, but a hotbed of deadly fevers.

Truxillo, founded in 1524, and chosen as the capital of the new department of
Colon, is also well protected from the trade winds by a promontory disposed, lke
that of Puerto Caballos, from east to west, and enclosing a basin accessible to the
largest vessels. But the town is a mere collection of huts, inhabited by a few
hundred Caribs, who are engaged in the export trade of mahogany, sarsaparilla,
cattle, hides, and other produce brought down by convoys of mules from the mag-
nificent province of Olancho.

This highly-favoured upland region, watered by the headstreams of the Patuca
and Romano rivers, enjoys a perfectly salubrious climate; its soil is extremely
fertile, forest glades and woodlands alternating with rich arable tracts and
savannus under succulent herbage, while copious streams flow through every
valley, washing down auriferous sands from the wooded and picturesque slopes of
the encircling heights. On an affluent of the Patuca stands the little town of
Jutigalpa, and in the neighbourhood the Indian village of Catacamas, the products
of whose industry might be forwarded northwards by the Romano Valley to
Truxillo, south-westwards by the mountain passes leading down to the Choluteca
Valley, and north-westwards by the Patuca river, accessible to the Carib canoes
to the port of Delon, within a few leagues of Jutigalpa. Yet, with all its
exceptional advantages, this glorious region is still almost deserted. For the whole
of the extensive department of Olancho, the last census returned a population of
little over 30,000, while that of Colon, comprising all the north-west corner of
Honduras, is occupied by less than 3,000 natives ; altogether scarcely 35,000 in
a region where millions might easily be supported without any overcrowding, as
in some of the West India Islands under the same latitude.

Comayagua, chief town of the department of like name, and former capital of
the republic, stands at an altitude of 2,000 feet on an extensive plain about mide
way between the two oceans. Founded in 1540 by Alonzo Caceres, Nueva Valla-
dolid, as it was formerly called, was a prosperous city of nearly 20,000 inhabitants
before the year 1827, when it was besieged, taken, and sacked by the Guatemalan
“ Serviles.” It never recovered from that blow, and at present its chief attractions
are the numerous ruins of ancient cities by which it is everywhere surrounded.
Of these the most remarkable is Tenampua. (Pucblo Viejo), standing on a lofty
eminence nearly 20 miles south-east of Comayagua, and comprising within its
enclosures a number of apparently religious edifices, pyramids, terraces, sculptures,
and much painted pottery.

West of the department of La Paz, whose present capital, La Paz, stands on the
site of the ancient city of Las Piedras, the chief place towards the Salvador frontier
is Esperanza, not far from the famous Ærandique opal mines. Near Virtud, in the
same hilly district of Intibucat, is seen the remarkable cave of the “ Agua de
Sangre,” a red fluid which coagulates as it falls and then putrefies, emitting an

256 MEXICO, CENTRAL AMERICA, WEST INDIES.

odour of blood. The liquid, which owes its colour and peculiar properties to the
living organisms contained in it, affords a certain nourishment to birds and other
animals.

The most densely-peopled part of Honduras is the basin of the Choluteca river,
which descends to the Pacific at the Gulf of Fonseca. The upper portion of the
basin, which forms a natural transition between Salvador and Nicaragua west and
east, comprises the department of Tegucigalpa, which gives its name to the present
capital of the republic. This place almost suddenly acquired great importance in
the year 1762 as the centre of a region abounding in gold and silver mines.
Between 1778 and 1819 the Tegucigalpa district yielded nearly £40,000,000 to
the trade of the world, and mining operations, interrupted by wars, revolutions,
and oscillations in the value of the precious metals, have in recent times again
been actively resumed.

Tegucigalpa, chosen in 1880 as the seat of congress, and even designated as a
future capital of the Central American Confederation, is by far the largest place in
the republic, and is increasing from year to year. It rises in amphitheatrical form
at the foot of a steep mountain on the right bank of the Choluteca, which is here
crossed by a ten-arched bridge. Concepcion, on the opposite side of the river,
forms an integral part of the city.

Two other departments, also abounding in mineral resources, are comprised
within the Choluteca basin. One of these, whose capital, Yuscaran, dates from the
middle of the eighteenth century, has received the well-merited designation of
Paraiso, or “ Paradise,” while the other takes the name of the river and of the
Indian nation dwelling on its banks; Choluteca, its capital, on the left side of
the estuary, was the Xeres de la Frontera of the early settlers.

Nacaome, on the river of like name, which also flows into the Gulf of Fonseca,
but much farther west, is noted for its mineral waters. Its port of San Lorenzo
stands at the northern extremity of the inlet of like name, where shipping finds
good anchorage in depths of 22 to 24 feet close to theshore. One of the projected
interoceanic railways has its terminus at this port; another is carried over the Rio
Nacaome near its mouth, and, after crossing the marshy backwaters between
Guegensi and Sacate Grande and the mainland, terminates on the west side of the
latter island over against a vast roadstead some 20 square miles in extent, and
from 30 to 50 feet deep, close to the future terminus.

Pending the construction of this important line, Amapala, the seaport of
Honduras on the Pacific, stands on the north-west side of Tiger Island, at one time
a stronghold of the buccaneers. Sacate Grande and Tiger Islands both belonged
formerly to Salvador, which allowed Honduras to occupy them in 1833 in return
for her co-operation in the local wars.

Economic Conpition oF HONDURAS.
Although fully one-half of Honduras is still almost a vast solitude, its popu-
lation has increased at least threefold since the beginning of the century. The
first census, taken in 1791, gave a population of 95,500, while the last (June,

HT Hi
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TAKEN FROM LA CONCEPTION.

TEGUCIGALPA— VIEW

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ECONOMIC CONDITION OF HONDURAS. 267

1887) returned a total of 332,000, of whom nearly three-fourths were Ladinos.
The stream of immigration has not yet been directed to the state, and in the
whole country there are scarcely 500 foreigners, apart from the so-called “English”
immigrants from Belize and Jamaica.

Honduras has developed no industries, and even its agricultural produce
scarcely suffices for more than the local demand. The banana, caoutchouc and
coffee plantations have, however, in recent years acquired some importance, while
the tobacco of Copan and Santa Rosa has long been appreciated. Next to gold
and silver, the chief staple of the export trade was timber, especially the

Fig. 114.—Fonsrca Bay.
Scale 1 : 1,000,000.

BD TS) it) NS 7
7 AGE en

VC LS

res & ata

== AI
= Ti = = hy?)
£ = LS

=Farallon

West of Greenwich «i

Depths.
== = —
===
Oto 5 5 to 12 12 Fathoms
Fathoms. Fathoms. and upwards.

18 Miles. .

mahogany, which reaches its greatest perfection in the forests of Honduras.
But the finest trees have been recklessly felled without any attempt at replanting,
and as mahogany takes three hundred years to arrive at maturity, the sources of
supply threaten to be soon exhausted.

The Honduras exchanges are estimated at a yearly value of about £1,200,000,
the exports consisting of minerals, cattle, and products of the soil, the imports
almost exclusively of manufactured goods. Five-sixths of the foreign trade is
carried on with the United States.

Owing to the reckless speculations connected with railway projects the name
of Honduras has become one of the most notorious in the financial world. Of

268 MEXICO, CENTRAL AMERICA, WEST INDIES.

£5,200,000 borrowed in recent years ostensibly to construct interoceanic and
other lines, not more than £700,000 were actually expended on railway works.
Hence Honduras is naturally unable to meet her engagements, however reluctant
she may be to repudiate them. No doubt the revenue continues to increase, but
it is drawn chiefly from the customs and monopolies on gunpowder, spirits, and
tobacco, which do not admit of rapid expansion. The public debt with arrears of
interest amounted in 1890 to £7,645,000, representing over forty years of normal

Fig: 115.—Comparative Drsrs oF VARIOUS STATES.

nil
Liberia ave heresies A Tr re £200,000
Hawaii ; : 7 384,000
S. African Rep. ........... Rte . ; PRESS 440,000
Nicaragua ........ PAS Cr ee arr TC CEE j ; Bee 600,000
Switzerlund .. Petar y coon Paaainnrdeste de eh à 3 ROK 1,240,000
Salvador ..... or Asfepegstanpctsseanince Mencaac 1,400,000

Costa-Rica : 5 : Sco rad rs api eeanteceeney pee 000! 000!
Haies ARE RE : “ire ; ee toe 007 00000
SSD O TEM EO NN Lacie set ssvagevenstcosece ee : Rate rurteee A EU.
Bolivia ......... PR EE RTS seepteeved . 2,960,000
Ecuador ............:- PE rea PES Oe se ae ; asset LOS 0DIGDD
Guutemala .. D en TL AL PE PAPERS < ss 4,200,000

TEP SAVE Rare ere Diner ee ee eee BE PR Tes 4,760,000
CHINA 0.0... ceece cece tees ests ers este nen eesteecececneaeees Ne RS RTL EE 5,000,000

NOW AT an ner ee uss fe ess eumenes EE PE EL LEP ER DE EL LS 5,880,000
TNT. one tepoture: © CAamcePOCco-creCnCoN Docc es Tendre re 200 EE 000 000
ET VALE edie en nee M nec ckonetse cy to's ARR rte se 11200000
Colombia : ; | : SES 12,480,000
Hcnduras À : ss. 13,040,000
Sweden Lx ne a LO, OOO:
Uruguay ........... 3 Sr eden ne ne oh tie: MNT)
CRT Le acs AR Re met tempo 020 000
Venezlels 2... HR RTL De ee B ead ... 20,520,000
GLOBE hin ti IN NA an eee nett MIA Noten ne nay eee 24,960,000
Mexico .. EERE PECE PCR CPC TES e 100 tente Dee Ps ten tort ; …… 26,120,000
ROUTE A PP = nee restent suseenartneneniecees ES 3 woe 84,040,000
TDR cer ne a Pence Oona LRO Ceo : wo. 58,640,000
ENT OMEN © beast Pr scorers ee cece / ... 56,960,000
Japan 5 Ole vases ces : 62,000,000
Germany i care : Cate ee 66,560,000
OA SP os oc, tsvavasseeeteeciatonse Ui as NOTE : ... 93,480,000
RÉCENTS RES AL PE RE 100,000,000
HV CN PRO PAT Reise hE ISERE Eee 106,440,000
Portugal A PT PU YG de veveeeceeceeseee 422,640,000
Brazil 22 & 7 123,080,000

United States .... f WMT À SO ... 224,000,000

. 268,000,000

RUSSIE ne cereeeveo™ l y rm cum 478,080,000
Austria-Hungary re l y Ly) cece. 600,000,000

revenue and about £40 per head of the population. As no interest has been paid
since 1872, the state is virtually bankrupt.

The interoceanic railway, which served as the pretext for this formidable debt,
is far from being finished. The only completed section, about 56 miles, or one-
fourth of the whole length, runs from Puerto Caballos across the Sula plain, where
no heavy engineering works had to be executed. To finish the whole line a new
company had to be formed, fresh surveys taken, and attempts made to raise
more money. But the £8,000,000 required to complete this and other lines
from Puerto Caballos to Truxillo, and thence to Jutigalpa, have not yet been sub-
scribed.

Meanwhile carriage-roads are projected for the transport of heavy goods

ECONOMIC CONDITION OF HONDURAS. 269

over the mountain passes between the Atlantic and Pacific slopes. The
two main highways are the interoceanic route through Comayagua, and
that running from Sensenti through Intibucat, La Paz, and Tegucigalpa to
Jutigalpa.

The postal and telegraph services are still in their infancy compared with
those of Mexico, as might be expected in a country where the great mass of the
population is still absolutely unlettered. In 1887 not more than 19,000 adults

Fig. 116.—Drsr per Heap or PoPULATION IN VARIOUS COUNTRIES.

Onin Smic tonton not
DIDELIR 2er mere =
SWACZOLIMMO EEE EE L

INCOR WE Mrs sens nt esse ans
GARMIN een des ksspen see mntnt
Japan

Nicaragua .............-.

Salvador

Mexico

BOLLVEA Eee rene eee

SWETON <iccsvecesece-ccenrcreont :
MAD ane stestaccesasord ters
Guatemala... '

GUO OR rare reereneeres
Colombia Rares PA OCDE
MULK@ Yih. rrrea rennes des enmente ess sesammtess sense
United States

S. African Rep. ......

Russia ....

S. Domingo............

DQ WAÏL EE

Roumania ...........

Denmark

Servia

CMU ees cote ee

C9 ID © C9 O0. ©

tet

=
SOW SP D100 w ©

—

ei pi mi
DS MON © © 0 CG Æ -J G O ND NN = Hi ae

D O1 O1 Où O1 He He He OÙ O9 C9 GO GO C9 C9 O9 9 D) Hi Hi Hi hi © © ©

SMMNAHOSOMOBRNH AH AH

Venezuela

Greece me
Austria-Hungary
Argentine 5
Paraguay ......
SAINS TN
Belgium
Hollande. sss:
United Kingdom

Uruguay
Portugal
France............
Henduras

could read and write, and only 74,000 children were receiving any kind of
education. In the same year the periodical press was limited to four journals.

The government of Honduras differs only in a few minor details from those
of the other Central American republics. The constitution has been frequently
modified between the years 1824 and 1883, during which period as many as forty-
eight rulers have succeeded under various titles to the supreme power. In normal
times the president is elected for four years by universal suffrage, and is assisted
by a council of seven ministers for foreign affairs, the interior, public works, war,
finance, public instruction, and justice. The legislative functions are discharged
by a congress of 37 members returned by the various departments in proportion
to the population. |

270 MEXICO, CENTRAL AMERICA, WEST INDIES.

The army consists legally of all able-bodied unmarried men between the ages
of twenty and twenty-five, regulars and reserves comprising altogether about
25,000 of all arms. Usually, however, there are scarcely more than 500 engaged
in garrison duty.

For administrative purposes the republic is divided into thirteen departments,
for which see Appendix.

V.—NIcaRacua.
Nicaragua is the largest, but relatively the least densely-peopled, of all the

Central American states. Yet within its limits is found the true centre of the :

Fig. 117.—Trrrirory cLAIMED at Various Times By GREAT BRITAIN.
Scale 1 : 17,000,090.

EOF) zz le “Sante

C2 CBAV ABTS
:

SS Cara Frovrder

LS Anores:

*FS-Juan del Norte
Soe Greytown}—

In te Sn 7 k
West of Greenwich.

310 Miles.

isthmian region, and one of the cardinal points in the history of the New World.
This privileged region is the narrow strip of territory comprised between the
Pacific and the shores of Lakes Managua and Nicaragua. Here reigned the famous
cacique, Nicarao, whose name has been perpetuated in a Spanish form as that of
the Hispano-American republic.

Like Honduras, Nicaragua suffered much from the incursions of the corsairs
on its Atlantic side, and here, also, Great Britain long sought to secure a perma-
nent footing. The section of the seaboard known as Mosquitia, or the Mosquito
Coast, was even claimed by the English Government, and but for the intervention
of the United States, the whole space comprised between the Nicaragua River and
Honduras Bay would have become British territory. In virtue of the Monroe
doctrine, “ America for the Americans,” this territory was restored to the republic

NICARAGUA. 271

of Nicaragua, though its independence was again threatened in 1855 by the
American National party itself. In that year the American adventurer, Walker,
one of those men “who have all the qualities required for the throne or the
gibbet,’’ came to the aid of one of the native factions with over 12,000 filibusters,
who were to be rewarded with extensive grants of land for their future victories.

After a first repulse at the town of Rivas, Walker seized Granada, the chief
city of the republic, and secured the election of his nominee to the presidential
chair. Slavery was then revived, and an attempt made to attract capitalists with
the view of converting Nicaragua into one vast plantation, on the model of the
“ Cotton States,” such as Mississippi and South Carolina. But all the peoples of
Central America had already taken the alarm, and a league was formed against
the filibusters. From the south came the Costa Ricans, from the north the
Guatemalans, and the Nicaraguans themselves having also revolted, the adventurer
was driven from port to port, and at last compelled to take refuge in Rivas, where,
after a four-months’ siege, he had to capitulate in 1857. Though his life was
spared, he twice attempted to return to Central America, but having fallen into
the hands of the Hondurans, he was executed as a filibuster at Truxillo, in the
year 1860.

This failure was of more than local importance; it was the first success of the
abolitionist party in America itself. “I have defended the cause of the slave-
holders abroad,” said Walker when dying; “they will soon have to defend it
themselves in their own sugar and cotton fields.”

Since that critical epoch, Nicaragua has pursued a more tranquil course of
development than the sister states. There has been a general increase of popula-
tion and wealth without involving the usual consequences of civil discord and
revolutions. Even the troublesome questions of boundaries have led to nothing
more serious than diplomatic discussions with Honduras and Costa Rica, discus-
sions which were finally settled by the mediation of the United States Government,
appealed to as arbitrator.

Apart from a few slight deviations, the two bold lines traced on the map, on
one side by the course of the Rio Segovia, on the other by the southern shore of
Lake Nicaragua and the bed of the Rio San Juan, are regarded as the frontiers
of Nicaragua towards Honduras on the north and Costa Rica on the south.

PuysicaAL FEATURES.

The Nicaraguan main range forms a south-eastern continuation of tke Chile
Mountains in Honduras, running parallel with the Pacific coast, with peaks
ranging from over 3,000 to 4,000 feet in height. The chain falls gradually
southwards, rising to a mean altitude of scarcely more than 650 or 700 feet along
the east side of Lake Nicaragua. This irregular system may be roughly regarded
as the escarpment of an ancient plateau falling abruptly westwards, and inclining
eastwards to the Atlantic through a long declivity disposed by the running waters
in numerous divergent valleys. Those of north Nicaragua run north-east

272 MEXICO, CENTRAL AMERICA, WEST INDIES.

parallel with the Rio Segovia, and those of the centre due east, while those of the
south, as, for instance, the valley traversed by the Rio San Juan, have a south-
easterly trend.

In several places these fragmentary sections of the plateau present the aspect
of distinct sierras. Such are, in the north, the Sierra de Yeluca, and in the
south that of Yolaina, which terminates seawards in the Punta Mico, the Monkey
Point of English writers. Amongst the various foot-hills of the main range,
there is one ridge which had passed unnoticed by all geographers till indicated
for the first time by the naturalist Belt, in 1874, when it attracted universal
attention owing to the curious resemblance of its name to that of the New World
itself. This is the little Sierra d’Amerrique, near Libertad, otherwise remarkable
for its sheer rocky walls, its obelisks and huge isolated crags. The name of the
continent has now been connected by M. Marcou with these hitherto unknown
rugged heights, the theory being that Amerigo Vespucci and other early naviga-
tors heard the natives speak of the hills in question as abounding in treasures, and
then applied the term to the whole region ; thereupon it occurred to Amerigo to
turn to his personal glory the accidental resemblance of this name to his own.

The Sierra d’Amerrique, called also Amerisque and Amerrisque from a local
tribe said to have been formerly powerful, lies in the territory of the ancient
Lencas, as is shown by the ending rique generally occurring in the Honduras
regions inhabited by these Indians.

West of the Nicaraguan main range, the region facing the Pacific was originally
an extensive low-lying plain, where the underground forces have raised two lines
of eminences, or even mountains, some isolated, others forming veritable chains.
The first of these ranges is so inconspicuous that, when seen from the plain, it seems
merged in the chain disposed immediately to the east of it. Its indistinct cha-
racter is due to the fact that the voleanoes have been upheaved on the very flanks
of the plateau. Thus Guisisil (4,550 feet) rises in close proximity to the Mata-
galpa Mountains, and by damming up the waters formerly descending to the
Pacific, has deflected them through the Rio Grande eastwards to the Atlantic.

South-west of Guisisil, loftiest of these volcanoes, other:cones have emerged
along the depression which is flooded by the two Lakes Managua and Nicaragua ;
here the Cerro de la Palma, Cuisaltepe, Juigalpa, Platotepe, Pan de Azucar, Jaén,
Picara and the Ventanillas are all disposed in a line running close to the east side
of the great reservoir.

But far more important in the geological history of the country are the peaks
of the main range, which forms a continuation of the Salvador volcanic system.
The truncated cone of Coseguina, at the southern entrance of the Gulf of Fonseca
opposite Conchagua, is the first link in this igneous chain ; it still rises 3,860 feet
above the sea, but according to Belcher, the regular cone must have been at least
double that height. Before the Krakatau explosion, Coseguina was usually referred
to with Timboro, of Sumbawa Island, as a typical example of the tremendous catas-
trophes caused by the sudden escape of gases pent up in the bowels of the earth.
On January 20, 1835, the summit of Coseguina was blown to atoms, day was

PHYSICAT, FEATURES OF NICARAGUA. 273

changed to night for a space of several hundred square miles, the sea was covered
with a dense layer of ashes and scoriæ arresting the progress of ships for a distance
of over 25 miles from the volcano, all verdure disappeared under a bed of dust at
least 16 feet thick, and the very shoreline encroached on the ocean and on the Gulf
of Fonseca. Westwards the trade winds wafted the dust 1,380 miles across the sea,
eastwards the counter-current precipitated it on Honduras, Yucatan, and Jamaica,

Fig. 118.—Mompacno Vorcano AND SHORES OF Lake NICARAGUA.

while the aérial eddies carried the ashes southwards to New Grenada. The crash
of the ruptured mountain was heard on the Bogota uplands, a distance of over
1,000 miles as the crow flies. Altogether the ashes fell on a space of about
1,600,000 square miles, while the erupted matter was estimated at 1,750 billions of
cubic feet. The explosion lasted forty-three hours, but the people of the sur-
rounding plains had time to escape, with their domestic animals, followed by
wild beasts, birds and reptiles, beyond the reach of the stifling gases.

Some 30 miles south-east of Coseguina rises the twin-crested mass of the

274 MEXICO, CENTRAL AMERICA, WEST INDIES.

extinct Chonco and Viejo (6,300 feet) cones, beyond which follows the Marrabios
range of peaks, mostly little over 3,000 feet, but culminating about the centre of
the system in Telica, 4,200 feet high. Somewhat east of the Marrabios the series
of volcanoes is continued by the majestic Momotombo (6,150 feet), whose base
forms a promontory in Lake Managua, and which has been in eruption so recently
as 1852. Formerly the missionaries baptised the burning mountains, but some
monks who had undertaken to plant the cross on Momotombo never returned.

Chiltepee (2,800 feet), which rises out of the very waters of Managua, is
followed by some less elevated cones on the mainland, where they are in close
proximity to lagoons evidently at one time forming part of the lake. About
midway between the two basins stands the famous Masaya (2,800 feet), which was
formerly known to the Spaniards by the name of Infierno, “ Hell,” and which in
pre-Columbian times was said to have borne the name of Popocatepetl, like the
Mexican giant.

Masaya, that is, the “ Burning Mountain,” was first ascended by Oviedo, who
saw its crater filled with boiling lavas. At that time slight eruptions occurred
at almost regular intervals of fifteen minutes, and the yellow fluid bubbling up on
the bed of the crater was supposed to be molten gold. Two Spanish monks, accom-
panied by three fellow-countrymen and many Indians, having failed to secure any
of the precious liquid, it occurred to Juan Alvarez, dean of the chapter of Leon,
to tap the perennial stream by means of a tunnel driven through the flank of the
mountain. But before the work could be seriously taken in hand, Masaya boiled
over of its own accord in 1772, and since then it has been quiescent, except in 1852
when it ejected a few jets of vapour. But in 1856, Nindiri, a parasitic crater on
its flank, discharged large quantities of vapour.

Mombacho (4,600 feet), which stands on the same pedestal as Masaya, but on
the north-west shore of Lake Nicaragua, has long been extinct. But its former
energy is attested by the surrounding lava streams and by the Corales, a cluster of
eruptive islets encircling its submerged base.

South-west of Mombacho the voleanic chain is continued in the lake itself, first
by Zapatera (2,000 feet), and then by the large twin-crested island of Ometepe
that is, the Mexican-Aztec Ome-tepetl, “Two Mountains,” 5,360 and 4,200 feet
respectively. The summit of Ometepe is crowned by a flooded crater, and on the
flank of the mountain is a still larger crater overgrown with dense vegetation.
From the top of the mountain a wide prospect is commanded of the whole lake,
the narrow isthmus separating it from the Pacific, and the amphitheatre of hills
sweeping round the eastern horizon.

West of the two lakes the isthmus constituting Nicaragua proper has also its
little coast-range, of moderate elevation and interrupted by numerous gaps.
Venturon, the culminating crest, is only 800 feet high, while the lowest pass
scarcely stands more than 25 or 26 feet above the level of the lake, which at the
narrowest point is rather less than 13 miles from the Pacific. In many places,
the isthmian region is entirely covered by the so-called ta/petate or tepetate, that is,
eruptive matter deposited under the influence of the prevailing south-west trade

RIVERS OF NICARAGUA. TS

winds. The consequence is that this region is destitute of springs or streams,
all the rain water disappearing in the porous masses of scoriæ and ashes,

Rivers AND LAKEs.

Although the Nicaraguan backbone is developed east of the lacustrine depres-
sion, the narrow strip of land limiting Lake Nicaragua on the west side is the
true waterparting of the whole region. The streams descending from the western

Fig. 119.—Isramus or Rivas.
Seale 1 : 1,200,000.

Ni
ww
ll iy
7 =A

——————
a

0 to 5 5 Fathoms
Fathoms. and upwards.
18 Miles.

slopes of the Chontal Mountains do not flow to the Pacific, but after a winding
course find their way to the Caribbean Sea. The pretended law that makes
watersheds coincide with mountain ranges is nowhere more clearly contradicted.
The parting-line, however, which is formed by the isthmus sends down
nothing but rivulets on its west slope. The only Nicaraguan rivers that reach the
Pacific have their sources on the opposite flank of the Marrabios hills, and flow to
the Gulf of Fonseca. Such are the Estero Real, rising in the neighbourhood of

276 MEXICO, CENTRAL AMERICA, WEST INDIES.

Lake Managua, and, farther north, the Rio Negro, which has become the frontier
towards Honduras.

Both of these watercourses have frequently shifted their beds, owing partly to
the erupted matter damming up their channels, and forming islands and peninsulas,
partly also, perhaps, to seismic disturbances. Since the eruption of Coseguina
in 1835 the Rio Negro has changed its course no less than four times, and at

Fig. i20.—-Tus Nicaragua WATERPARTING.

Seale J : 5,000.000.

<I
Îm
4

A Dp
IT

À
il

ll?

pan

itt

| |

PET

Sep FLY
€

BAT L TI) Fe

West of Greenwich

60 Miles.

present it intermingles its waters with those of the Estero Real in a common
delta. i‘

The most copious river in north Nicaragua flows, under a great diversity of
names, from the Matagalpa mountains through the broadest part of the state down
to the Atlantic near Cape Gracias-à-Dios. About its sources, within 50 miles of
the Pacific, it is known as the Somoro, and lower down successively as the Cabrugal
(Cabullal), the Coco (Cocos), Oro (Yoro, Yare), Portillo Liso, Tapacac, Encuentro,
Pantasma, Segovia, from a town on its banks, and Gracias, or Cape River, from
the low peninsula it has formed where it reaches the coast. It also takes the name

OO _ À

RIVERS OF NICARAGUA. 277

of Herbias, while the English call it Wanks or Yankes, this confusing nomenclature
being due partly to the different languages current along its banks, partly to the
lack of historic unity of the fluvial basin. While the Spanish colonists were
settling in the upper valleys of the Rio Segovia, foreign corsairs of every nation
were infesting its lower course.

Pent in between mountain ranges, the Wanks drains a relatively narrow basin,
but, being exposed to the moist east winds, it is a copious stream accessible to small
eraft for a distance of about 170 miles below the rapids. At its mouth it projects
its delta far seawards between banks of a reddish alluvium washed down from
the upper valleys. The Wanks drains an area of nearly 12,000 square miles,
has a course of 400 miles, and a mean discharge of 17,000 cubic feet per
second.

Between this river and the San Juan, the largest watercourse is the Rio
Grande, whose main branch, the Matagalpa, probably at one time flowed west to
Lake Managua. But having been dammed up by the heaps of scoriz ejected
from Guisisil, its course was deflected southwards and eastwards to the Atlantic.
In one part of its valley it takes the name of Bulbul, while the Sambos of
Mosquitia call it Awaltara. At its mouth it communicates through lateral
channels with other watercourses, and according to Levy’s chart there is a con-
tinuous series of backwaters, false rivers, and passages extending for about 250
miles from Cape Gracias-à-Dios to the Blewfields lagoon, separated from the sea
by a strip of sandy beaches and mangrove thickets. Most of these waters are
narrow and obstructed by islands; but the Pearl Cay and Blewfields lagoons are
veritable inland seas, in parts overgrown by mangroves, but still leaving vast
spaces open to navigation. The Blewfields basin, said to be so named from a Dutch
corsair, Blieveldt, receives a river of like name, called also the Rio Escondido
about its middle course.

From the geological standpoint the present coast between Cape Gracias.a-Dios
and Monkey Point indicates a state of transition between the old shoreline, that
is, the west side of the lagoons, and the great Mosquito Bank, which advances
seawards for a variable distance of from 30 to 100 miles and which comprises
numerous submerged and upheaved cays. One of these reefs is the Mosquito Cay,
which has given its name to the whole bank, a name afterwards extended to the
east coast itself and its inhabitants Some of the islands on or near the outer
margin of the banks are large and elevated enough to support a few settlements.
Such are Vieja Providencia and San Andres, which belong politically to the
Republic of Colombia, the little Corn Islands and Pearl Cays, dependent on
Nicaragua.

South of Monkey Point the Rio Indio reaches the coast just above the delta
of the San Juan, which is the most copious of all the Nicaraguan rivers, but which
only partly belongs to the republic. Most of its basin is, in fact, comprised
within the neighbouring state of Costa Rica, though its farthest headstream rises
in the great lacustrine depression west of the Nicaraguan main range. Although
the San Juan at present drains this depression to the Atlantic, there was a time

278 EXICO, CENTRAL AMERICA, WEST INDIES.

when Lakes Nicaragua and Managua formed a continuous basin which sent its
overflow to the Pacific at the Gulf of Fonseca. From that epoch dates the intro-
duction of the marine species, which have gradually adapted themselves to the
fresh waters of Lake Nicaragua.

Gil Gonzalez de Avila was assured by the natives that Lake Xolotlan (Man-
agua) had an emissary flowing directly to the “Gulf of Chorotega ”’ (Fonseca),
but that the outflow was arrested by a lava stream from Momotombo. The
emissary is now represented by the Estero Real, while Managua sought another
issue southwards to Lake Nicaragua, and thus became a tributary of the Atlantic.

A slight upheaval would still suffice to convert Managua into a closed basin.

Fig. 121.—Marrasios RANGE AND LAKE Managua.
Scale 1 : 1,400,000.

de ‘ i
PP nee

WS
> -

Dre

tee

1) WA
A7)

\
J

30 Miles.

During the rains it feeds an emissary which at the Tipitapa sa/fo has a picturesque
fall of 17 or 18 feet; but in the dry season there is no continuous current, the
water slowly percolating through the sands and fissures of the rocks. A dry
space of over four miles separates the outflow from the estero of Panaloya, which,
although presenting the appearance of a river, is merely a tranquil backwater
communicating with Lake Nicaragua.

Even during the rains Tipitapa is completely obstructed by reefs, and in 1836
Belcher had to transport a boat from one lake to the other. Hence it is all the
more surprising that projectors of interoceanic canals should represent Tipitapa as
the natural prolongation of a great transisthmian canal, Managua itself, although
over 400 square miles in extent, is obstructed by shoals, which render it

RIVERS AND LAKES OF NICARAGUA. 279

unnavigable by vessels drawing more than five or six feet of water. It stands at
a mean altitude of 140 feet above the sea.

Nicaragua, the Cocibolco of the natives, stands some 30 feet lower, or about 110
feet above sea-level. It has a mean area of 3,600 square miles; but there are no
abysses as in the Alpine lakes, the deepest cavity being scarcely 280 feet deep.
Some parts, especially near the San Juan outlet, are very shallow, and the general
level varies with the seasons little more than seven or eight feet. But there can
be no doubt that it formerly stood at a much higher level, for the islets south of
Zapatera are covered with scoriz containing freshwater shells, like those still
found on the neighbouring shores.

During the rains vast spaces round the lake are transformed to absolutely
impassable cienagas (quagmires), the waters from the surrounding heights pene-
trating to a great depth into the pasty soil and converting the plains into a sea of
mud. In the dry season the moisture evaporates, and the baked ground becomes
fissured without anywhere clothing itself with vegetation.

Nicaragua is fed by numerous affluents, some of which have acquired a certain
celebrity in connection with various schemes of interoceanic canalisation ; such
are the Rios Sapoa and de las Lajasin the isthmus of Rivas. But the most copious
tributary is the Rio Frio descending from the Costa Rica uplands, and washing
down vast quantities of volcanic sediment, which is gradually filling up the
southern part of the basin, and raising its bed above the surface, as the neighbour-
ing Solentiname archipelago has already been raised. Then the Rio Frio will
become a tributary, not of the lake, but of the San Juan, and this river, thus
charged with sedimentary matter, will form a chief obstacle to the proposed
interoceanic canal,

The San Juan, which escapes from the lake just below the mouth of ihe Frio,
flows in a very sluggish stream till it approaches the Castillo, a little fort on the
right bank 40 miles below the outlet. Here the river has forced a passage through
the schistose ridge connecting the Chontal mountains with the Costa Rican Cerros
de San Carlos. The rapids thus formed are followed some 12 miles lower down by
another series of erosions, the raudal de Machuca, so named from the first Euro-
pean explorer of the San Juan. Farther on the mainstream is joined by the San
Carlos, which sends down from the Costa Rican uplands a volume almost equal to
that of the San Juan itself. A little above the delta follows the still more copious
Sarapiqui affluent, which also descends from the Costa Rican mountains, but which
is so charged with alluvial matter that the idea of utilising the lower course of
the San Juan for the proposed canal has been abandoned.

In the delta itself the shifting branches of the mainstream are joined by
the Rio Colorado, a third affluent from Costa Rica. About the middle of the
century nearly all the united waters of the San Juan basin entered the sea at
Graytown (San Juan del Norte), where the powerful current had excavated a
spacious harbour accessible to vessels of average draught. But most of this
current was deflected by the opening of the Jimenez, a branch of the San Juan,
which now joins the Colorado and which usually bears the same name. Other

280 MEXICO, CENTRAL AMERICA, WEST INDIES.

channels at times carried off all the rest, leaving the harbour half choked with
sands and almost cut off from communication with the river. Hence it has
been proposed to remove the port to the mouth of the Colorado; but the bar,
with from 10 to 16 feet of water, varies frequently in depth, while the road-
stead is exposed to the dangerous north winds.*

CLIMATE, Fiora, Fauna.

Nicaragua is divided by the nature of its soil and climate into three distinct
zones, an eastern, central, and western, each presenting special features in its
vegetation, inhabitants, social condition, and history.

The old schistose quartz and dolerite rocks of the plateaux and mountains on
the Atlantic slope are watered by copious rains and vapours brought by the north-
east trade winds. Hence these regions are covered with forests interrupted only
by river beds, swamps, and marshy savannas. Here are found all the varieties of
timber, cabinet and dye woods of the Honduras and South Mexican floras—cedars,
mahogany, gayac, besides the characteristic cortes (tecoma sideroxylon), which is
hard as ebony and remarkable for the dazzling golden blossom with which it is
entirely clothed towards the end of March, after the fall of the green foliage.
Owing to the superabundance of moisture this region is necessarily unhealthy and
sparsely inhabited, the few Indian or half-caste natives ‘being chiefly confined to
narrow glades in the dense woodlands.

The range of the Atlantic rains and rank forest-growths is sharply limited by
the crest of the main Nicaraguan chain, so that it may rain for weeks or months
together at Libertad on the east slope, while Juigalpa, on the Pacific side, enjoys
cloudless skies. The eastern rains last from May to January, with occasional
intervals of fine weather, especially in October and November.

Immediately beyond the forest region begins the central zone of savannas,
varied here and there by a giant ceiba, which affords a grateful shade to numerous
flocks and herds. Here the work of man in clearing the woodlands has been
aided by the occodoma, a species of ant, which spares the herbage and confines its
attacks to the sprouts and saplings growing on the verge of the forest. According
to Belt, these ants are veritable agriculturists. They cut the tender leaves in
squares, not for food, as was formerly supposed, but for manure to enrich the
underground plantations of fungi on which they chiefly live. The eciton hamata,
another species of ant in the same region, is placed by the same naturalist in the
first rank for its intelligence. When a brook is bridged by a single branch too
narrow to allow a horde to cross except in Indian file, a number of the insects
cluster on both sides of the natural causeway in such a way as to double or treble
its width.

Amongst the remarkable phenomena presented by the fauna of this upland

* Hydrology of the San Juan :—From the source of the Rio San Rafael to Lake Managua, 94 miles ;
Lake Managua, 28 miles; Rio Tipitapa, 18 miles; Lake Nicaragua, 88 miles; Desaguadero (San Juan),
125 miles; total. 353 miles. Extent of the basin, including the Colorado, 16,000 square miles; discharge
at the Lake Nicaragua outlet, 12,000 cubic feet ; at the fork of the delta, 25,000 cubic feet ; during the
floods, 52,000 cubic feet per second.

CEIBA.

WE) ee ee "TS id #7 (LMP - Ee ee ee ee Ae iG
tee i pl Ve Lu AA Lio amin (Lu: DEP 7
CDR TOR DTA MAC réa dc a AN À

‘

INHABITANTS OF NICARAGUA. 281

zone Belt also mentions the timetes chiron, a species ot butterfly, which moves in
countless multitudes over hill and dale, always in the direction of the south-east
towards the Mosquito Coast. They come, probably, from the remote Honduras or
Guatemalan forests, but never return.

The third zone comprises the lacustrine plains and Pacific seaboard, that is,
Nicaragua in the narrower sense—the “ Paradise of Mohammed,” in the language
of the Spanish conquerors—the privileged region on which the other two zones
naturally depend. It is at once the most fertile and healthiest region of the
republic, though exposed to the fierce westerly gales here known as papagayos,
from the Gulf of Papagayo, at the south-western extremity of Nicaragua. Here
the native populations were formerly crowded together in vast cities “ four leagues
long,” and the whole isthmus between the lakes and the sea was transformed to a
vast plantation. Hence the local flora chiefly consists of cultivated plants, and
others associated wifh them.

INHABITANTS.

In Nicaragua the aborigines were exterminated, if not more ruthlessly, at all
events, to a greater extent than elsewhere in Central America. There being no
escape between the ocean and the lakes, the more numerous were the native com-
munities, the more wholesale were the massacres. Even in east Nicaragua, near
the Caribbean Sea, many districts, formerly covered with Indian villages, were
completely depopulated by the buccaneers. Thus between Monkey Point and the
Blewfields estuary, old cemeteries, heaps of potsherds, carved stones, and even
human effigies are found in a region which is now a wilderness. The Spanish
dwellings met along the course of the Mico are built with materials taken from
older Indian structures.

At present all the native populations of west Nicaragua are half-caste Ladinos.
The Mangues, Nagrandans, Dirians, and Orotiñans of the north-west are collectively
grouped as Chorotegas, or Choroteganos, which is merely another form of Cholu-
teca, the collective name of the neighbouring Honduras Indians, to whom they are
related. Some ethnologists affiliate the Chorotegas to the Chiapanecs of east
Mexico, while others regard them as Mayas expelled from Cholula in pre-Aztec
times. They bore the name of Olmecs, like the predecessors of the Nahuas on
the Anahuac tableland, and probably belonged to the same stock.

The final syllables of local names in various parts of Nicaragua certainly indi-
cate the presence of different peoples at different epochs. The ending, galpa, is
Aztec, while rique denotes towns and heights on both sides of the Honduras fron-
tier. In the valley of the Rio Segovia the names of places end in / or guina, and
in Chontales apo or apa is most common.

Fully a century before the arrival of the Spaniards, the Nahuas had advanced
as conquerors through Guatemala, Salvador, and Honduras into Nicaragua. Here
they were known by the name of Niquiran or Nicarao, which some etymologists
identify with the term Nicaragua itself. Like their Mexican kinsmen they had
their city of Tola or Tula, and like them also practised the art of writing, carved

282 MEXICO, CENTRAL AMERICA, WEST INDIES.

statues, and erected temples scarcely inferior to those of Mexico and Yucatan.

The local topographic nomenclature shows that the Aztec rule extended over
nearly the whole of Nicaragua, although their language has ceased to be current even
in the isthmus of Rivas, where they at one time existed in multitudes. Spanish,
enriched by numerous Mexican expressions, has become the common speech of all.
In their stage-pieces, representing myths, historic events, or religious dramas, the
language employed is a jargon called by Brinton the “ Nahuatl-Spanish dialect of

Fig. 122.—Popunation or Honpuras AND NicaRacua.

Scale 1 : 7,000,000.

=/ SET L2 7e

iB P=

CzpEe-Carmarorn.
7

Rue

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[>

aus

à}

124 Miles.

Nicaragua.” Most of these plays are accompanied by baïles, or dances, and nearly
all the old musical instruments are still in use. |

As in Mexico, the conquistadores endeavoured to destroy all memorials of the
old culture. In 1524 the missionary Bobadilla raised a huge pyre at Managua, on
which a bonfire was made of the religious and historical paintings, calendars,
maps, and all other Nahua and Chorotegan documents that he could lay his hands
on. The temples were razed to the ground, the idols overthrown, the cemeteries
desecrated; nevertheless, down to the present century there still survived nume-
rous sculptured stones, especially in the islands of Lake Nicaragua, which the
Spaniards had ceased to visit after exterminating their inhabitants. In the
island of Momotombito alone Squier saw over fifty colossal basalt monoliths

INHABITANTS OF NICARAGUA. | 283

representing human figures and recalling the monstrous statues of Easter Island,
Polynesia.

Numerous antiquities, such as carved stones and rock inscriptions, were also
found in the islands of Ceiba, Pensacola, and Zapatera. From the cemeteries of
Ometepe, where the Nahua population has preserved its primitive purity, Brans-
ford removed to the Washington Museum some eight hundred precious objects
especially huge sepulchral urns containing seated bodies still decked with their
ornaments. Another curious find made by Flint was the traces of thousands of
human feet left on the yellow ashes ejected by Masaya and afterwards covered by
subsequent eruptions.

The uplands between the lacustrine and Atlantic basins are inhabited by abori-
gines designated, like those of south-east Mexico, by the general name of Chontals,
that is, “ barbarians.” Before the conquest they were already held in contempt
by the civilised Nahuas of the plains ; nevertheless the ruins of cities and numerous
vestiges of buildings and causeways show that these so-called barbarians had made
considerable progress in the arts of civilisation. Gradually driven eastwards by
the Ladinos, the Chontals have largely merged with the Zumas (Sooms, or Simus),
the Popolacas or Waiknas, that is, “Men,” or else have altogether disappeared.
In many districts nothing is now seen except their graves, usually disposed in a
vast circle round the habitations.

The Chontals appear to be related to the Lencas of Honduras; their language
is distinct both from Aztec and Maya, and they still number about 30,000, mostly
designated by the names of the rivers inhabited by them. Some, however, bear
distinct names, such as the Pantasmas of the upper Segovia, the Cucras following
lower down, the Carcas, Wulwas (Uluas), Lamans, Melchoras, Siquias, and the
Ramas of the Rio Mico, rudest of all the aborigines.

One of the tribes on the Rio Grande has assumed the title of Montezuma, which
for the populations of Mexico and Central America has become synonymous with
the old national independence. This tribe, however, seems more akin to the Carib
than to the Lenca stock. The word Carib itself, under the form of Carabisi, was
current in this region long before the arrival of the Caribs from St. Vincent.
When speaking of the local idioms, Herrera mentions in the first place that of the
Carabisi ; they have been identified with the present Zumas and Waiknas.

On the other hand the so-called “ Caribs ” of the seaboard, more generally
called Moscos or Mosquitos, are really Sambos, that is, half-caste Indians and
negroes, with a strain of European blood, due to the buccaneers who infested these
shores. Many of the natives in the provinces of Segovia and Matagalpa have fair
hair and blue eyes, which Belt attributes to the intermingling that took place in
‘the sixteenth and seventeenth centuries between the local creoles and the French
and English corsairs. In 1687 the 280 rovers commanded by Ravenau de Lussan,
having abandoned their vessels in the Gulf of Fonseca, crossed the continent, here
310 miles wide, and reached the Atlantic by the valley of the Segovia. Others
ascended the same river, which had become “ the great highway from ocean to
ocean.”

284 MEXICO, CENTRAL AMERICA, WEST INDIES.

Nearly all the whites who settled in the favoured isthmian regions belonged to
the vigorous Galician race, and the Gallego type may still be recognised, though
their Spanish patois contains but few words borrowed from the Galician dialect.
Non-Spanish immigrants, French, Italians, English, or North Americans, are very
few, and their arrival dates only from the middle of the present century. Yet
European artisans and labourers might easily adapt themselves to the climate,
especially in the Matagalpa province.

ToPpoGRAPHY.

Chinandega, the chief place in the north-west on the Honduras route, comprises
two distinct townships, £7 Viejo, on the slope of the mountain of like name, and
the new town a few miles to the south-east, to which the name of Chinandega is
now exclusively applied. It was at one time a flourishing place, but it has lost
its trade since the encroachments of the land on its ports of Tempisque in the north
and Realejo inthe west. The present harbour of Corinto is sheltered by the island
of Cardon, and affords excellent anchorage in 22 feet of water at ebb and 40 at
flow. Corinto, which exports large quantities of dyewoods, is by far the busiest
seaport on the Pacific side.

Leon, the chief city of the republic, lies between Lake Managua and the two
estuaries of Corinto and the Estero Real. At the time of the conquest its pre-
decessor, the Indian city of Subtiaba, contained a population of about 100,000.
But the first Spanish town of the district was founded in 1523, not on the plain
dominated eastwards by the Marrabios chain, but at Zmbita, on the south-west side
of Lake Nicaragua. Owing to various disasters, the settlement was afterwards
removed to the vicinity of Subtiaba, capital of the Nagrandan nation. The new
city, seat of the administration, soon became a flourishing place, and the English
buccaneers who sacked it in 1680 carried off a vast amount of booty.

At the close of the eighteenth century, Leon and Subtiaba were said to have
a colleetive population of 50,000; but during the present century this number has
been greatly reduced, especially by wars and civil strife. In recent yeirs Leon
has somewhat recovered its losses, and it is now connected by rail with Corinto
and the other isthmian towns. The neighbouring thermal waters are little fre-
quented, the whole region round about the city being still almost a wilderness.
During the rainy season Leon is exposed to frequent inundations, and the rudely
paved streets at times resemble mountain torrents, the water surging up to the
very eaves of the houses.

Managua, the present capital of the state, was till the middle of the century a
mere hamlet standing on the site of an Indian city some 60 feet above the level of
Lake Managua. In the neighbourhood are the little closed basins or tarns of
Tiscapa, Nejapa, Asososca, and Apoyo, old craters which, after bursting, were
flooded with a brackish water, differing in its saline properties according to the
nature of the surrounding soil and lavas. The neighbouring plains, formerly
under cotton, are now covered with coffee plantations.

Beyond Tipitapa and the intermittent stream bearing its name, stretch the

‘HAVAHONOHOHL NIVN AHL NI NHHVL MHIA—NO4T

Pre
= Doe =.

7 À

r
|

—s : - : SSE

TOPOGRAPHY OF NICARAGUA. 285

forests abounding in Brazil wood (cæsalpinia crispa). The black marshy lands
on the east side of the lake take the name of jicarales from the jicaro, or calabash-
tree, which is here the prevailing species, and whose fruit supplies the natives
with nearly all their domestic utensils.

Granada, like Leon, is one of the oldest places in Nicaragua, having been
founded in 1523 by Francisco de Cordoba, near the Indian city of Salteba (Jalteba),
now one of its suburbs. The fame of its wealth and of the great fertility of the
district more than once attracted the attention of the corsairs, who, in 1665. and
again in 1670, ascended the San Juan and crossed Lake Nicaragua to sack and

Fig. 123.— DENSITY OF THE Porunation oF Honpuras AND NICARAGUA.
Seale 1 : 7,500,000

pe
/

|
|

ï
mi

=|
LE
i

L}
tp

[

a
fi

]

\ D

ñ
\

1
0
e 1
Et

West of Greenwic

inhabitants per square mile.

L] Fi F5 fs ES 5

Under 2. 2 to 10. 10 to 20. 20 to 30. 30 to 40. 40 to 60. Go and upwards.
124 Miles.

burn the city. Some fifteen years afterwards another band of English and French
buccaneers attacked it from the Pacific side; but before its capture most of the
inhabitants had time to escape with their valuables to the archipelagoes of Lake
Nicaragua. It again suffered during the expedition of the filibuster, William
Walker, who set fire to it before abandoning it in 1856.

Granada lies on the scarp of the plateau on the north-west side of Lake
Nicaragua. Its buildings lay no claim to architectural beauty, and it owes its chief
importance to its schools, its trade and industries. Several landing-places follow
along the neighbouring shore; but Chareo Muerto is the only town possessing a

286 MEXICO, CENTRAL AMERICA, WEST INDIES.

good haven. It lies far to the south, and is sheltered by Zapatera Island from
the trade winds.

The department of Granada is by far the most densely peopled in the state,
and here several important towns and communes are scattered over the fertile
plains. The most flourishing place is Masaya, which has a population of some
15,000 mestizoes. It stands north-west of Granada on the plateau commanded on
the west by the volcano of like name, not far from the lovely Nindiri, a true
“garden of the Hesperides.” The surrounding farmers and peasantry are a
prosperous and industrious people, engaged in various crafts, such as weaving,
pottery, leather dressing, saddlery, and producing a thousand objects of local
consumption.

Jinotepe, south-west of Masaya, stands at an elevation of 2,520 feet amid
productive coffee plantations, while Nandaimé, in a rich valley sloping towards
the bay of Charco Muerto, is surrounded by thriving cacao farms; in the neigh-
bourhood is the famous Val Menier domain, the produce of which commands too
high a price to serve for the preparation of ordinary chocolate. About five miles
west of Nandaimé are the ruins of Mandaimé Viejo, supposed to have been des-
troyed by an earthquake.

Rivas, standing at the narrowest part of the isthmus between Lake Nicaragua
and the Pacific, might claim to be regarded as the “ metropolis” of the republic.
Here resided the Niquiran chief, Nicarao, who, according to most of the chroni-
clers, gave his name to the state; here began the work of conversion and of con-
quest, and here Bobadilla baptized over 29,000 persons in the space of nine days.
Yet no Spanish settlement has been made in this favoured district, and the Indian
village of Micarao-calli was not raised to the rank of a town till the year 1720,
greatly to the disgust of its rival, Granada. It long bore the name of “ Nicaragua,”
but since the beginning of the present century that of Rivas has prevailed. The
town is continued for miles through a highly-productive district by the scattered
villages of Obrage, Potosi, Buenayre, while eastwards it descends to its port of San
Jorgé on Lake Nicaragua.

On the Pacific coast the hamlets of Brito and San Juan del Sur (Concordia) are
names associated with the engineering projects for piercing the isthmus by a
navigable canal, and sooner or later the opening of this interoceanic highway will
confer on Brito the celebrity now enjoyed by Suez and Panama; yet its harbour,
scarcely 70 acres in extent, is so exposed that it will have to be sheltered by costly
breakwaters. On the other hand the magnificent haven of Salinas Bay, common
to Nicaragua and Costa Rica, has no settlements on its shores, and is entirely
neglected except for the exploitation of the Bolanos salt-pans. The haven is an
almost circular basin, over 20 square miles in extent, sheltered from the surf and
ranging in depth from 40 to 80 feet. A cutting across an intervening sandy
isthmus might connect it with the equally safe bay of Santa Elena.

Compared with the western seaboard, the Atlantic coastlands might almost be
called uninhabited, all the civilised populations being concentrated on the uplands
near the waterparting between the lacustrine and Atlantic basins. Throughout

TOPOGRAPHY OF NICARAGUA. 287

its whole extent the great valley of the Rio Segovia has only one town, Ocotal, capital
of the department of Segovia. The first Segovia, founded in 1524, soon became a
flourishing place as a centre of the gold washings in all the surrounding valleys,
but it was destroyed in 1854 by Morgan, most famous of all the West Indian buc-
caneers. Rebuilt in a more protected position, it was again attacked by the Mos-
quitos corsairs, and had to be shifted a third and a fourth time to sites farther and
farther removed from the coast.

The present “ Segovia,” better known by the name of Ocotal, stands at an
altitude of over 2,000 feet on the left bank of the Wanks (Coco), in a mineral dis-
trict abounding in gold, silver, copper, iron and tin. Further down, nothing is
met except a few Indian camping-grounds, one of which, oom, near the estuary
at Cape Gracias-à-Dios, was formerly the residence of a Sambo “ king.”

The upper valley is somewhat more settled than that of the Wanks. ata-
galpa, capital of the department of like name, has the advantage of easy access to
Lake Nicaragua, although its waters drain to the Atlantic. It is a thriving place,
surrounded by rapidly-spreading coffee plantations.

Jinotega, on the opposite side of an intervening ridge, is also a prosperous town,
whose cultivated lands are steadily encroaching on the neighbouring pine forests.
The uplands of this region are also rich in the precious metals, and near the Indian
village of Sebaco are seen numerous galleries, whence the natives drew large
quantities of gold. The auriferous sands of Principolca have also attracted many
immigrauts from the Zamba territory.

Acoyapa, or San Sebastian, capital of the department of Chontales, stands on
the site of a formerly populous city, but is itself a mere village near the east shore
of Lake Nicaragua, where it possesses the port of San Ubaldo. In the same dis-
trict, but farther north at the foot of the Sierra Amerrique, stands the town of
Juigalpa—in Aztec, the “ Great City ”’—which appears to have been a large centre
of population, to judge, at least, from the numerous ruins, the disinterred idols, and
still undeciphered inscriptions covering the surrounding rocks.

Libertad, on the opposite or Atlantic side of the sierra, is the capital of a pro-
ductive mining district, but the excessive moisture renders its climate highly
insalubrious. Farther east the basin:of the Blewfields is almost uninhabited as
far as the great lagoon of like name. Here stands the village of Blewfields, a
former nest of pirates, and residence of the Mosquitos chief, who takes the redun-
dant Anglo-Spanish title of “ Rey-King.” This potentate, formerly protected by
Great Britain, but now a pensioner of Nicaragua, administers all the villages of
_ the Mosquitos Cvast for a space of about 150 miles between the Hueso and Rama
Rivers north and south.

Blewfields is also the centre of the Protestant missions and English schools
along the seaboard. It is surrounded by extensive banana and other plantations,
and since 1883 it has developed a considerable trade in cocoanuts, pineapples,
oranges, and other fruits with New Orleans.

The shores of the Pearl Lagoon as well as the neighbouring Corn Islands have
also become busy agricultural centres. Oysters abound along the coast lagoons,

288 MEXICO, CENTRAL AMERICA, WEST INDIES.

although the vast kitchen-middens of the surrounding forests contain none of these
bivalves. Potsherds and little human figures have been found in the refuse.

San Carlos, on the left bank of the San Juan where it escapes from the lake, is
a mere group of cabins, commanded by a ruined fort. But according to Belly,
this is the site of the future Constantinople of the American Bosphorus. Castillo,
a little farther down, is the most important station between the lake and San Juan
del Norte, often called Greytown since the time of its occupation by the English.
This town, famous in the history of the wars between the Spaniards and bucca-

Fig. 124.—San Juan DEL Norte BEFORE THE CONSTRUCTION OF THE PIER.
Scale 1 : 85,000.

27 +2 +8 JUAN DEL NORTE 3
12... (Greytown). *

se + ©
BR chests Pogo

West of Greenwich

Depths.
9 to 16 16 to 32 32 Feet and
Feet. Feet. upwards.

3,300 Yards.

neers, and long the scene of English and American rivalries, is the only seaport of
Nicaragua on the Atlantic side. Its little white wooden houses, with their smiling
garden plots, trailing plants, and shady palm-groves, are surrounded by swampy
tracts, backwaters and channels, alternately flooded and filled with mud, which should
make Greytown a hotbed of fever. Yet according to the testimony, not merely of
engineering speculators, bat of disinterested travellers, it is really one of the least
insalubrious places along the whole seaboard. This is mainly due to the porous
nature of the volcanic matter washed down by the river, so that the surface waters

ECONOMIC CONDITION OF NICARAGUA. 289

rapidly disappear, carrying with them all the impurities of the soil, while the
exhalations are continually dissipated by the prevailing north-east trade winds.

The absence of a port at Greytown has obliged the promoters of the Nicara-
guan interoceanic canal to construct an artificial harbour on the north-west side
of the delta, A jetty projecting 1,440 yards seawards has enabled the stream to
sweep away the sands and gradually scour the channel to a depth of seven or eight
feet. A few structures on the beach mark the site of the future ‘ City of America,”
solemnly founded on January 1, 1890. North of this place, the best roadstead is
at Monkey Point between the Blewfields and Rama rivers, and it was here that
Bedford Pim proposed to establish the Atlantic terminus of his transcontinental
railway, crossing the waterparting at a height of 760 feet. The promoters of the
canal are now connecting the Rama valley with the harbour of San Juan. They
will thus have the advantage of two seaports with an intervening territory suitable
for European colonisation.

Economic Conpirion oF NICARAGUA.

Although sparsely peopled relatively to the vast spaces capable of settlement,
Nicaragua, like the sister states, is steadily increasing in population, which
advanced from nearly 132,000 in 1778 to 160,000 in 1813. Since then, despite
civil strife and invasions, progress has been even more rapid, the returns for 1846
showing 257,000, while the total population was estimated in 1890 at 575,000, or
nearly six to the square mile. The birth-rate is at present on an average double
that of the mortality.

The chief products of Nicaragua are agricultural, and these might be indefinitely
increased by bringing the vacant lands under tillage. Coffee, which ferms the
staple of the export trade, comes almost exclusively from the province of Granada.
Next in importance is caoutchouc, collected, not from cultivated plants, but from
forest growths felled by the Caribs of the Atlantic coastlands. Bananas are yearly
becoming more abundant, thanks to the increasing demand in the United States.
The Nicaraguan planters also export cacao and sugar, but have almost ceased to
cultivate indigo, driven from the markets by the new chemical dyes.

A great resource of the republic are horned cattle, exported both to Costa Rica
and Honduras. Many million head might be raised on the grassy plateaux of
Chontales, where the herds number at present scarcely more than 1,200,000.

Nicaragua also possesses considerable mineral wealth, though mining operations
are still mostly carried of in a primitive way. The best-worked mines are those of
Chontales, which have long been owned by English proprietors. The gold washings
of the streams flowing to the Atlantic are almost entirely in the hands of the

Indians and Sambos of the coastlands. Mining, such as it is, is almost the only

g,
local industry, and all manufactured wares, except some coarse textiles and furni-
ture, are imported from Europe or the States. The chief products of the native
craftsmen are the earthenware of Somotillo, the hammocks of Subtiaba and Masaya,
and the calabashes of Rivas embellished with designs in relief.

Foreign trade is scarcely developed, amounting to scarcely more than £2 per

290 MEXICO, CENTRAL AMERICA, WEST INDIES.

head of the population. The total exchanges amounted in 1890 to little over
£800,000, most of the traffic being with the United States and Great Britain.

Tue NicaraGua CANAL.

But trade and the industries will be powerfully stimulated by the completion of
the interoceanic canal which has been so long projected. There can be no doubt
that the isthmus of Nicaragua is by far the most suitable region for a canal with
locks, the line to be followed being already indicated by the depression of Lake
Nicaragua and its emissary.

It has even been proposed to cut a navigable way free of locks, a scheme by

Fig. 125.— PROJECTED INTEROCEANIC CANALS across NICARAGUA.
£cale 1 5,200,000.

erun

BSL err

:
TMNT
\|| [I

| Ill

Greenwich

Oto5 5 Fathoms
Fathoms. and upwards.
nme _ Das Lin à à ss
Projected Canal. Canalised River. Railways opened and projected.
124 Miles.

which the great basin would be more than half emptied and many hundred thousand
acres of arable land reclaimed in the very heart of the country. But a cutting
over 220 miles long, under such a climate and without slave labour, would appear
to be beyond the power of modern industrial resources.

Projects of a more practical nature were spoken of so early as the time of the
conquest, and even under the Spanish rule the buccaneer, Edwards David, con-
ceived the idea of a cutting between the lake and the Pacific. In 1780, the
engineer, Martin de la Bastide, proposed such a canal, and the next year the
Madrid Government undertook a first survey of the ground with a view to its
construction.

THE NICARAGUA CANAL. 291

Immediately after the declaration of independence, the new republic decreed
the accomplishment of this work, but failed to supply the means for its execution,
After the discussion of various plans and counter-plans, a first scheme for a canal
terminating at San Juan del Sur (Concordia), on the Pacific, was propounded by
John Bailey in 1845.

Since that time various other schemes have followed, but without obtaining the
necessary capital. The failure, however, of the Panama undertaking has revived
the hopes of speculators, who propose to carry the interoceanic route through the
Lake of Nicaragua. The works were, in fact, actually commenced at the end of
the year 1889, though not, as the financial world expected, at the expense of the
United States Government. The estimated cost is fixed at £15,000,000, and a
period of six years assigned for the completion of the work, which will have a total

Fig. 126.—Lower San Juan Canat.
Seale 1 : 600 ON,

Depths
Oto 5 5 Fathoms
Fathoms. and upwards.

12 Miles.

length of 170 miles, of which 140 of open navigation through the lake, and not
more than 30 through ship canals. We are assured that vessels of the heaviest
draught will take only 30 hours to pass from ocean to ocean, and that the cutting
will admit 32 such vessels per day, or 11,680, of about 12,000,000 tons, a year.
The San Juan discharges a volume sufficient for hundreds of canals, but its

course is too shifting, its current too irregular and too charged with alluvia to

g
allow of its being canalised and adapted for the navigation of large vessels.
Hence it will be necessary to keep the canal quite distinct from the river through-
out its lower course, where it receives the great tributaries from Costa Rica. This
cutting, joining the river in its tranquil upper course, will be supplied with three
locks, each 550 feet long, by means of which the vessels will be brought to the
level of the lake, which stands over 110 feet above the Atlantic at low water. It

292 MEXICO, CENTRAL AMERICA, WEST INDIES.

will bave a depth of 29 or 30 feet, and a minimum breadth of 80 feet on its bed,
with sidings at the narrowest parts.

Above the upper lock, which will have to be separated by an embankment
from the mouth of the San Carlos, the ships will pass into the lake and traverse
it obliquely to a second canal, whence they will descend to the Pacific through an
artificial lake and the Rio Grande. But Lake Nicaragua itself will have to be
deepened in its south-eastern section, where its bed has been raised by the alluvial

Fig. 127.—Porxricar Divisions or NicaRacva.
Scale 1 : 5,000,000.

Lil

A
EE 0
Hes

VA iil

Leon, Granada. Rivas.

QT
Chontales. Matagalpa. Segovia. Mosquitia.
94 Miles.

matter washed down by the Rio Frio from the Costa Rica highlands. The Pacific

Canal will be partly transformed by huge dykes to lakes at different levels
terminating at the port of Brito.

Such is the magnificent project first conceived by Thomé de Gamond in 1858,
then adopted with modifications by other engineers, especially Menocal, and now
in process of realisation. But will the estimated sum suffice for the construction

COSTA RICA. 293

, gigantic locks, large harbours in stormy seas, channels

maintained at a constant depth, despite the invasions of sedimentary matter brought

of such prodigious works

down by impetuous mountain streams ? On the other hand, the annual increase of
the world’s trade, and the necessity of opening a navigable highway by which
thousands of vessels will be spared a voyage of over 9,000 miles round Cape
Horn, render the execution of this gigantic work more and more probable.

But its successful completion is full of dangers for the republic itself. When
the canal has become the great highway between New York and San Francisco,
and the all-powerful company finds itself mistress of the route with a vast army
of employes at its disposal, how can the feeble and sparsely-peopled state hope to
maintain its independence against the “ manifest destinies” of the North American
Anglo-Saxon nation ?

ADMINISTRATION.

In her political institutions, Nicaragua differs little from the other Central
American states. By universal suffrage are erected two chambers, a senate of
18 members for six years, and a lower house of 21 representatives for four
years. ‘The president is also nominated for the same period, and is assisted by a
council of four ministers, or secretaries, for foreign affairs, finance, public works,
and the interior.

The standing army comprises a few hundred men, with 1,200 custom house
officers, and a reserve of over 15,000 liable to serve in case of civil or foreign war.
The revenue, like tnat of the neighbouring states, is largely derived from tobacco,
spirits, and gunpowder monopolies, supplemented by the customs and some minor
imposts. Most of the expenditure is absorbed by public works, instruction, postal
and telegraph services, Nicaragua, unlike Honduras, has hitherto escaped the
financial speculators, and the public debt amounted in 1890 to about £600,000, with
a mortgage on the 93 miles of railway, altogether little more than one year’s income.

In the Appendix are given the eight administrative divisions with their areas
and populations.

Wile——_Cosra Rica.

Next to Salvador, Costa Rica is the smallest of the Central American states in
extent, while its population is absolutely the smallest. It may be described as
little more than a narrow strip of territory forming a terrace or plateau between
the two oceans at a mean elevation of 3,500 feet, and intersected by a volcanic
range double that height. But it is occupied by a somewhat homogeneous people,
who present a certain originality amongst Hispano-American communities, and
whose progress has been less interrupted than that of the sister states by foreign
wars and civil strife.

In some respects, Costa Rica is the model republic of Central America, as well
as one of the most prosperous, not so much on account of its mineral wealth, as
might be supposed from its name, as of its agricultural resources. This term

294 MEXICO, CENTRAL AMERICA, WEST INDIES.

“Rich Coast,” given formerly to the whole of the south-western shores of the
Caribbean Sea, that is, to the Gulf of Columbus taken in its widest sense, was
later restricted mainly to the district of Veragua in Colombia, where gold had been
discovered. But the present Costa Rica, at first known as Nueva Cartago, was
found so little productive by its first white settlers, that, according to some writers,
the name of “ Rich Coast” was retained by a sort of antiphrasis.

Like the other Central American republics, Costa Rica has scarcely ceased to

Fig. 128.—Guzr or CoLUMBUS.
Scale 1 : 5,000,000.

: a
EEE Albuquerque EE

SDE EFS =
= ——

= t == =
~$:\egS- Juan del Norte—>

nep = ——

SBS SS

West of Gree

Depths.
0 to 50 50 to 1,000 1,000 to 1,500 1.500 Fathoms
Fathoms. Fathoms. Fathoms. and upwards.

124 Miles.

be troubled with frontier questions, which, especially with Nicaragua, have at
times led to sanguinary conflicts. The Nicoya and Guanacaste districts, at present
the most important region of the state on the Pacific side, formed at one time a
part of the province of Nicaragua, the natural limit between the two countries
being the Gulf of Nicoya. But during the first years of independence, political
discussions waxed so furious in Nicaragua, that those more peacefully-disposed

COSTA RICA. 295

districts petitioned the Central American Government to be annexed to Costa Rica
until order could be restored. But the arrangement has been maintained, and is
now officially confirmed by treaty between the conterminous states.

But in the San Juan basin on the Atlantic side, the conflict became more
serious; here the river is a natural highway of trade between the two republics,
so that any frontier excluding Costa Rica from this outlet for her produce would
have deeply affected her interests. The treaty of 1858, ratified in 1888 by the
arbitration of the United States president, definitely settled this question, assign-
ing to Costa Rica the right bank from the delta to within three miles of the

Fig. 129.—OxE or THe Turee Craters oF Poas.

fortifications of Castillo; then the line is deflected eight miles south and east of
this place, beyond which it follows all the windings of the river and of Lake
Nicaragua at a distance of two miles to the mouth of the Rio de la Flor, which
enters the Pacific a little north of Salinas Bay.

On the side of Colombia the southern frontier is clearly indicated by the long
promontory of Punta Burica projecting into the Pacific, while on the north or
Atlantic coast, Costa Rica claims Chiriqui Bay and its islands, including the
Escudo de Veragua off the coast. On the other hand, Colombia claims not only
the whole of Chiriqui Bay, but even that of the Almirante as far as the Boca del
Drago. The question has been submitted to the arbitration of Spain; but in such
matters diplomatic records are of less consequence than the wish of the people.

296 MEXICO, CENTRAL AMERICA, WEST INDIES.

PuysicaAL FEATURES.

Taken as a whole Costa Rica may be regarded as an elevated tableland domi-
nating the flooded Nicaraguan depression. Immediately to the south of this vast
basin, the hills rise from tier to tier to the crest of the igneous cordillera which
is disposed north-west and south-east. Within some 20 miles to the south of
the narrow zone between Salinas Bay and Lake Nicaragua, the Orosi volcano,
which still emits a few jets of vapour from its verdure-clad crater, rises to a
height of 8,700 feet.

Beyond it follows the almost isolated four-crested Rincon de la Vieja, and
still in the same south-easterly direction the Miravalles peak (4,720 feet),
crowned with an extinct forest-clad crater. Miravalles and its neighbour,
Tenorio, are continued south-eastwards by the Cerros de los Guatusos, which for
about 60 miles are destitute of a single igneous cone. But towards the centre
of the isthmus the Poas volcano rises to a height of 8,700 feet, and terminates
in three craters, one flooded with a lake which drains through the Rio Angel to
the Sarapiqui, and another filled with hot water from which vapours are still
occasionally emitted to a great height. In 1834 it was the scene of a violent
eruption; but Barba, its eastern neighbour, has long been quiescent, its terminal
crater (9,000 feet) being also flooded, like so many others in this region.

Farther on stands Irazu, giant of the Costa Rican volcanoes, which rises to
the north of Cartago, and from whose summit a wide prospect is commanded of
both oceans, and of the whole of Costa Rica from the Orosi peak to Mount Rovalo.
Yet it slopes so gently that the traveller may reach its culminating point, a little
over 11,200 feet, mounted on a mule. The lower flanks are covered with maize,
tobacco, and other plantations, diversified with pasturage and terminating with
oak forests. The hamlet of Birris, highest inhabited spot in the republic, stands
at an altitude of 9,400 feet.

Turialba (11,000 feet), last cone going eastwards, has greatly contributed by
its explosions to modify the general relief of the land. Since the eruption of
1866 it has never ceased to eject copious vapours, accompanied now and then with
some ashes. Its name is said to be a corrupt form of the Latin furris alba,
“White Tower,” though Thiel and Pittier have shown that the word is of Indian
origin.

The Costa Rican igneous chain does not run parallel with the Pacific, but
trends in aslightly oblique direction to the general axis of this part of the penin-
sula, even developing a gentle curve with its convex side facing southwards
and its more lofty section disposed transversely towards the Atlantic. It appears
from Pittier’s observations that the older cones began their eruptions early in
secondary times, when the range stood in the midst of the sea, running in the
same way as the insular volcanoes of the Hawaii archipelago. The former
existence of such an archipelago is shown by the sedimentary matter now filling
the intervals between the igneous crests.

According to the same authority some of the Costa Rican cones have ejected

Fig. 130.—Summrr or Mount Irazv.

PHYSICAL FEATURES OF COSTA RICA. 297

no lavas during the historic period, although both Turialba and Irazu have dis-
charged vast quantities of ashes, which, under the influence of the trade winds,
have been deposited on their south-west slopes.

The plateaux stretching south ef the volcanic system, and eroded‘ on both

MHI INI I A | Hy} |
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sides by running waters, formerly contained lakes in their cavities. The Alajuela,
San José and Cartago depressions had also their lacustrine basins, which were
gradually emptied by the erosion of the encircling walls.

Earthquakes are very frequent, but are seldom violent, and the vibrations

298 MEXICO, CENTRAL AMERICA, WEST INDIES.

are rarely felt at any great distance from the base of the volcanoes. But at
the end of the year 1888 several severe shocks, coinciding with the discharges of
mud and water from Poas and Irazu, damaged the buildings of the neighbouring
towns and overthrew some villages. A comparative study of the local seismic
phenomena and of the rainfall during seventeen consecutive years has led Pittier
to the conclusion that the return of igneous activity and of underground dis-
turbances is a direct consequence of the tropical rains penetrating to the caver-
nous recesses under the volcanoes.

South of the igneous system the Costa Rican uplands are interrupted by the
valleys of the Rio Grande de Tarcoles flowing to the Pacific, and of the Reven-

Fig. 131.—PLATEAU AND Votcanors oF Costa Rica.

Seale 1 : 1,200,000.

RAT =

West of Greenwich

MPO ase

18 Miles.

{azon descending to the Caribbean Sea. The sources of these streams are inter-
mingled about the Ochomogo Pass (1,100 feet), which, at a former geological
epoch, was flooded by one of the marine channels connecting the two oceans.
South of this depression stretches an almost unknown region of wooded uplands
some 8,000 square miles in extent, but apparently without any igneous cones.
According to the natives, Mount Herradura (Turubales), at the southern entrance
to the Gulf of Nicoya, has occasionally emitted some light vapours; rumbling
sounds are even said to be heard at regular intervals in the interior of the moun-
tain, but these statements are doubted by Pittier, who denies that Herradura is a
volcano at all. It is connected by a lateral ridge with the Dota mountains, a
section of the main range traversing the isthmus midway between the two

PHYSICAL FEATURES OF COSTA RICA, 299

oceans. Above the ridge rise at intervals a number of lofty summits, such as
the Cerro Chiripo, in the Cabecar district, Mount Ujum (9,700 feet), Nemur,
Kamuk, or Pico Blanco (9,600), and lastly, Rovalo (7,000), close to the Colombian
frontier.

A striking resemblance in their general outline is presented by the two penin-
sular masses of Nicoya and the Golfo Dulce on the Pacific seaboard. Both consist

Fig. 132 —Guzr or Nicoya.
Scale 1 : 750,000.

TAN

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= Los

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S/S Webrita
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——

West of Greenwich

Depths.
0 to 5 5 to 25 25 to 50 5(0 Fathoms
Fathoms. Fathoms. Fathoms. and upwards,

12 Miles.

of a mountain range disposed parallel with the mainland, with which they are
connected by narrow strips of lowlands. The Punta Burica, at the Colombian
frontier, belongs to the same line of promontories, which is continued south of the
province of Panama by the island of Coiba, the large peninsula of Azuero and
the Pearl Islands.

These chains and detached insular or peninsular masses describe collectively a
regular curve of about 550 miles, which is perfectly concentric with the curve

300 MEXICO, CENTRAL AMERICA, WEST INDIES.

presented by the mainland itself between Lake Nicaragua and the Gulf of Panama.
The highest crest of this outer Costa Rican coast-range appears to culminate
towards its southern extremity in a peak not more than 2,000 feet high.

RIvers.

The strips of coastlands on both sides of the central uplands are too narrow
for the development of any large fluvial basins. Even the most copious streams,
the San Carlos and Sarapiqui, become merged in the San Juan before reaching the
Caribbean Sea. The Colorado, which, on the contrary, now receives nearly the
whole discharge of the San Juan, flows entirely in Costa Rican territory, where its
waters are intermingled by lateral channels with those of the Sarapiqui. From
the north-east slopes of the uplands, exposed to the moist trade winds, flows the
Parismina, or Reventazon, which has a much larger volume than might be supposed
from the length of its course. On the same side follow several other rios, such as
the Sicsola, and the Tilorio, or Changuinola, which Peralta identifies with the old
Rio de la Estrella, famous in the local legends for its auriferous sands. The same
name of Estrella has also been given to another less copious stream, which flows
farther north near Cahuita Point, and where the alluvia are still washed for
gold.

On the drier Pacific slopes the watercourses are less copious in proportion to
their length. Nevertheless three of them bear the name of Rio Grande: the Rio
Grande de Terraba, which reaches the coast at the head of the Golfo Dulce ; the
Rio Grande de Pirris, which flows south of the mountains terminating in the
western headland of Herradura, and the Rio Grande de Tarcoles, which rises at
the Ochomogo Pass, and which, after its junction with the Tiribi, the more copious
of the two, enters the sea opposite the southern extremity of the Nicoya peninsula.
Farther north the Tempisque flows to the head of the Gulf of Nicoya after travers-
ing the low-lying isthmus which was formerly a marine channel between the
Nicoya peninsula and the mainland.

All these streams tend by their alluvia to raise the bed of the gulf; but a more
potent cause is the south-east marine current which sweeps into the basin all the
organic refuse collected on the neighbouring coast.

The Gulf of Nicoya, so named from a chief whom the Spaniards converted
with 6,000 of his subjects, rivals the Bay of Naples, the Bosphorus, or the
Strait of Simonosaki in the rhythmical contour of its shores and encircling hills.
Its waters are studded with islands of all sizes, whose deep green forest vegetation
contrasts with the azure hue of the distant mountains. San Lucas, one of these
islands, resembling Capri in outline, is famous throughout Central America for
the legendary reports of the vast treasures here deposited by shipwrecked corsairs.
But nothing has ever been brought to light, oi the numerous expeditions
equipped to discover these treasures.

The Golfo Dulce, that is, “Freshwater Gulf,” is much deeper than Nicoya,
and entirely destitute of islands.

CLIMATE OF COSTA RICA. 301

CLIMATE, Frora, Fauna.

Like Mexico and Guatemala, Costa Rica offers a vertical succession of the three
“hot,” “ temperate,” and “cold” zones. But here the local climates and the
distribution of the vegetable species are endlessly modified by the varying condi-
tions of altitude, aspect, and general environment. In general the climate is
essentially oceanic, and well regulated by the winds prevailing on both seaboards.
At San José, the mean annual temperature exceeds 68° Fahr., rising gradually
to 78° towards the low-lying coastlands, and falling considerably towards the

Fig. 133.—GuLr or DuLce.

Scale 1 : 950.000.

ou Dh SANS ATA TS Uwe 27)
D A NN
ULES

£ RS
BG) WN
tj S

SAINS

= =
Se ah ———

Fal

=O Wa zoel

83°40’ . West of Greenwich

Depths.
0 to 25 25 Fathoms
Fathows. and upwards,

12 Miles.

crests of the mountains. At an altitude of 9,000 feet Pittier observed films of
ice on the margin of the streams, and on the summit of Irazu he found the surface
covered with hoar-frost.

At the same elevation the temperature is lower on the Atlantic than on the
Pacific slope, but it is more oppressive, the atmosphere being more charged with
moisture from the prevailing trade winds. On the west side the seasons follow
very regularly, the rains falling almost exclusively from May to November, whercas

302 MEXICO, CENTRAL AMERICA, WEST INDIES.

on the east side wet weather may be said to last throughout the year. The annual
rainfall rises to at least 130 inches in the Reventazon and Colorado basins.

Nevertheless the Costa Rican climate is one of the most salubrious in Central
America, both for natives and foreign settlers. Consumption is very rare, though
the uplands have at times been ravaged by cholera, smallpox, and other epidemics.
Fevers also prevail in the low-lying coast districts, while on the plateau strangers
are subject to rheumatism from the excessive moisture.

In general the flora resembles that of the other Central American regions,
though botanists have been struck by the contrasts often presented between the
Nicaraguan depressions and the Costa Rica uplands. Thus of the 100 ferns
collected by Levy in Nicaragua, only three or four are found in the 36 Costa Rican
varieties in Polakowsky’s collection. The cactuses, also, which in many parts of
the Mexican plateau ccver vast spaces, are scarcely represented at all on the San
José uplands. In the forests occur numerous Colombian forms, especially several
false cinchonas, which might easily be replaced by the valuable medicinal species.
Tree-ferns grow to an altitude of nearly 7,000 feet, and the banana to about
6,000.

Notwithstanding the reckless destruction of timber in many districts, more
than half of the Atlantic slopes are still covered with primeval forests, containing
an amazing variety of forms. In a space of 100 square yards, more types are here
met than in 100 square miles in north Canada. The streams flow beneath avenues
of overhanging foliage bound together from bank to bank by wreaths of flowers
and festoons of trailing plants. A characteristic form in the clumps of trees dotted
over many of the savannas is a species of mimosa, from which the province: of
Guanacaste takes its name. The widespreading branches of this tree are a favourite
resort of the monkey tribe. According to Pittier the Costa Rican flora comprises
altogether at least 2,200 species.

The fauna, also, is exceptionally rich compared with that of other tropical regions.
In general Brazilian and other southern types prevail over those of the northern
continent. But Costa Rica also possesses several indigenous species, such as a
howling monkey distinct from that of Guiana, a tapir (e/asmognathus), somewhat
different from the Colombian species, besides several kinds of bats and vampires
dangerous to cattle, whose blood they suck. One migrating species appears sud-
denly on the plains of Pirris, south of Mount Herradura, and falls on the domestic
animals, poultry, cats, dogs, as well as horsesand oxen. Although often regarded
as fables, the reports of vampires sucking the blood of human beings, lulling their
victims with their long wings, are by no means questioned by travellers and
naturalists who have visited Central America. Whole villages have had to be
abandoned to escape their attacks, and the engineer, Brooks, one of the surveyors
of the Panama Canal, died from the bites of a vampire.

But the Costa Rican fauna reveals its marvellous wealth especially in the
feathered tribe. In 1885, the catalogue of the Washington National Museum
already enumerated 692 species, distributed in 394 genera, and two years later, six
new species were discovered, altogether twice the number possessed by the whole

FAUNA OF COSTA RICA. 303

of Europe. The parrot and gallinaceous families are both represented by an
extraordinary number of different forms, as well as by the multitude of individuals
comprised in many of the groups.

In the reptile order, as many as 132 species have already been recorded, and
great discoveries still remain to be made on the marshy seaboard and in the
dense primeval woodlands. The surrounding marine waters also abound in animal
life, and the manatee, which has disappeared from most of the West Indian coast-
lands, still frequents the Costa Rican streams. Like Tehuantepec Bay, the Gulf of
Nicoya has its purple-yielding murex, and like the Gulf of California, its pearl and
mother: of-pearl oysters.

INHABITANTS.

In Costa Rica the aborigines have been almost entirely supplanted by a civi-
lised population of Spanish culture. The first European settlement, which, however,
was not permanent, was founded in 1524 by Hernandez de Cordova on the Gulf
of Nicoya. Badajoz, founded in 1540, on the opposite coast at the mouth of the
Sicsola, in the Talamanca territory, also disappeared, and in 1544 took place the
first conflict between the Indians of the plateau and the Spaniards in the neigh-
bourhood of the present Cartago.

In 1563 began the systematic conquest of the country by Vasquez de Coronado,
who secured a firm footing on the plateau, where nearly all the population of
Spanish speech is at present concentrated. Vasquez penetrated to within a short
distance of the Golfo Dulce, reducing the warlike Coto Indians, and afterwards
exploring the Talamanca territory on the eastern slope, the district about Almi-
rante Bay, the Guaymi country and the auriferous region of the Rio de la
Estrella.

At that time the aborigines must have numbered at least 60,000, the Talamancas
alone being estimated at 25,000, and the Indians of Coto at from 12,000 to 15,000.
In 1675, over 100 years after the conquest, there were still scarcely more than
500 Spanish settlers in the country, nearly all grouped round the two towns of
Cartago and Esparza on the plateau. The Indians employed on their plantations
were gradually reduced to a few hundreds, and the colony itself made so little
progress that even so late as 1718, there was not a single place of business on the
plateau, and all the traffic was in the hands of packmen.

During the seventeenth century the seaboard was frequently attacked by the
corsairs, but the country was too poor to attract them to the plateau. Despite its
strategic importance Costa Rica, towards the end of the colonial régime, when it
formed a province of the Guatemalan viceroyalty, had only a population of 47,000,
mainly Mestizoes. The people are usually spoken of as full-blood Spaniards,
mostly from Galicia; but they are really Ladinos, assimilated to the white race
in speech, usages, and national sentiment. The negro element is very slight,
there having been only 200 blacks in the province at the time of the official
abolition of slavery in 1824.

The bravos, or “ wild”’ Indians, variously estimated at from 3,500 to 6,000,

304 MEXICO, CENTRAL AMERICA, WEST INDIES

were quite recently still living entirely aloof from the civilised populations. In
the forests of the northern slopes draining to Lake Nicaragua and the San Juan,
and especially in the Rio Frio basin, dwell the Guatusos, who at present visit the
market of San José, and bring offerings to the Catholic priests, “ brothers of the
sun.” They were formerly said to have fair hair and blue eyes, which Gabb
attributed to contact with the English buccaneers. Others pretended that the

Fig. 134.—Guatuso INDIA.

fugitives from the town of Esparza, sacked by the corsairs, had merged in a
single nation with the Indians.

But all the Guatusos seen at San Carlos of Nicaragua, or at the markets of the
Costa Rican plateau, have black hair, a dark complexion, and prominent cheek-
bones, like the Nicaraguan Chontals, to whom they are probably related. They
are excellent husbandmen, cultivating their banana, cacao and other plantations with
great care. Nor are the Guatusos ferocious savages, as formerly asserted; on the
contrary, most of them have been exterminated by the Nicaraguan and Costa
Rican Ladinos engaged in collecting rubber in the northern forests. According

INHABITANTS OF COSTA RICA. 805

to Thiel hundreds are still kept in a state cf servitude in Nicaragua, where the
price of a Guatuso was recently fifty dollars.

The natives of the southern districts are generally grouped under the collective
name of Talamancas, although each tribe has its special designation. Such are

135. —Youne Tatamancas INDIANS.

the Chirripos, the Cabecars, Viceitas, Bribri and Tiribiés, who still decorate them-
selves with plumes, strings of teeth or pearl necklaces, and dwell in palenques with
thatched roof reaching to the ground.

On the Pacific coast live other tribes. the Borucas or Bruncas, the Terrebas and
others, who have given their names to the neighbouring villages. The Chirripos

and Cabecars near the Cartago district have already been baptised. The other
53

306 MEXICO, CENTRAL AMERICA, WEST INDIES.

Talamancas of the seaboard between Puerto Limon and Almirante Bay appear to
have also been formerly converted, for many of their ceremonies are of Spanish
origin. But they still worship the sun and stars, the rocks and winds, the running
waters and the sea.

The Blancos, a people of Cabecar or Bribri origin, expose the bodies of their
dead on palm-stands one or two yards above the ground, and bury them after
three years, when they are perfectly dry. Some food and precious objects are
at the same time placed in the grave.

In these graves have been found some remarkable little gola figures, which
attest the ancient civilisation of the natives, and their lamentable degradation
under their white rulers. Many of these artistic objects have unfortunately been
melted down and coined at the Costa Rican mint. The jadeites and other green
stones known by the Mexican name of chalchihuites come chiefly from Guanacaste
and the Nicoya peninsula. Objects of pre-Columbian culture, formerly supposed
to be rare in the northern provinces, are now found in thousands, especially about
the environs of Cartago, where stood the ancient city of Purapura.

TopoGRAPHY.

Since the middle of the present century the population of the formerly almost
uninhabited Guanacaste region has increased fourfold. Its vast savannas, where
millions of cattle might be raised ; its forests, abounding in valuable timber and
cabinet woods; its gulf and harbours; lastly, its convenient position between the
Nicaraguan peninsula and the Costa Rican plateau—give promise of a great future
for this hitherto neglected province. Its capital, Liberia, formerly Guanacaste,
lies at the south foot of the Orosi volcanoes towards the middle of the fertile
depression at the neck of the Nicoya peninsula.

In the interior of the peninsula are situated the populous towns of Santa Cruz
and Nicoya, the latter the larger of the two and formerly residence of the
friendly chief who welcomed the Spanish conquerors, and was baptised with all
his people. On the shores of the gulf are obtained both peari and edible oysters,
said to be the best on the whole west coast of America.

Puntarenas (Punta Arenas, or “Sandy Point”) stands on a tongue of sand at
the mouth of the little River Barranca, which has deposited vast quantities of
eruptive matter in the Gulf of Nicoya: The inlet is too shallow for large vessels,
which have to ride at anchor in the roadstead. Yet Puntarenas has since 1814
been the outlet for all the foreign trade of Costa Rica on the Pacific side.

Before that year the Pacific seaport of the province stood some six miles
farther south, near the thermal springs of La Caldera, between the Barranca and
Jesus-Maria estuaries. Before the opening of the railway, which has-its terminus
at Puntarenas, it was proposed to establish the port south of the Rio Grande, in the
picturesque bay of Tarcoles, at the foot of Mount Herradura. But the project was
never realised owing to the dangers of the bar and unhealthy climate of Tarcoles.
In the neighbourhood are some extremely thick beds of anthracite.

From Puntarenas the railway ascends the scarp of the plateau to Æsparza

xD jv 7 ‘
ALT
0e

I
HTH
HAH

PORT LIMON AND UVAS ISLAND.

TOPOGRAPHY OF COSTA RICA. 307

(725 feet), so named in 1578 by its Navarrese founder from his native village
near Pampeluna, but now officially changed to Æsparta. Another station higher
up (2,400 feet) has similarly taken the name of Atenas (Athens), and three miles
farther on stands Za Garita, on the edge of the plateau, whence a view is com-
manded of the plains watered by the Rio Grande. Here have been opened the
most productive gold and silver mines of the republic, which are said to have
yielded an annual output of £40,000 since the year 1821. The gold is coined at
the San José mint.

Alajuela, the ‘ Jewel” (3,000 feet), dates from the end of the last century, but
has already outstripped some of its older rivals, thanks to the fertility of its
voleanic soil. It is the capital of a province which ranks next to that of San
José for population. Here are also the thriving towns of Grecia and San Ramon.

Heredia, east of Alajuela, lies at the foot of the Barba voleano, near the
Desengano Pass (6,000 feet), leading by a difficult route down to the San Juan
valley. It is the Cubujuqui of the Indians, one of the oldest places in the state.

San José, the present capital, was a mere hamlet known by the name of La
Villita at the middle of the last century. But it enjoyed the advantage of a
more central position than Cartago, being admirably situated in the middle
of the plateau, 3,750 feet above sea-level. On the cessation of Spanish rule it was
chosen as the seat of government, and here have been founded the chief learned
and literary institutions of the country — university, normal school, museum,
meteorological observatory. Electricity was introduced in 1887, and San José is
now connected by rail with the Atlantic seaboard.

Cartago, formerly the capital, was founded in 1564 by Vasquez de Coronado,
and is the oldest of still-existing settlements in the country. It was several times
attacked by the buccaneers, partly ruined by the eruption of Irazu in 1723, and
levelled to the ground by the earthquake of 1841. One of the stations on the
railway connecting Cartago with the port of Limon on the Atlantic takes the
name of Angostura from the “narrows” of the Rio Reventazon. | This place is
known in Europe in connection with the disastrous failure of a German agricul-
tural colony founded in the district.

Limon, last of the chain of settlements which follow across the Costa Rican
isthmus, is of recent foundation. Despite the advantages of its harbour, the best
on the Atlantic side of the republic, no seaport could be established here until
access was given to the plateau by practicable routes. Thanks to the railway,
Limon has suddenly developed a foreign trade equal to that of Puntarenas. It not
only exports the coffee raised on the plateau, but also forwards to the United States
vast quantities of bananas from the new plantations in the neighbouring district.

The construction of the railway has necessitated the addition of several other
important works, such as viaducts and embankments across the swamps and
channels on the coast. Such works were needed, especially near J/oin, where a
contraband trade was formerly carried on in English goods.

South of Limon, the only civilised Costa Rican settlement on the Atlantic slope
is San Bernardo, in the territory of the Talamancas, near the Puerto Viejo. But,

308 MEXICO, CENTRAL AMERICA, WEST INDIES.

like the station of Chirripo, it failed to prosper owing to its isolation. The
so-called “city” of Santiago de Talamanca, founded on the banks of the Sicsola,
was burnt in 1610 by the revolted Indians.

The constant reports of rich gold-fields in the valley of the Estrella (Chan-
guinola) rest on a mistake made by Alcedo in his famous Diccionario Geografico-
Historico de las Indias Occidentales. Alcedo had given to these mines of the
Estrella the name of Tisingal (Tinsigal, Tisiugal), which happens to be an abbre-

viated form of Tegucigalpa, as shown
Fig. 136.—Purrro Luton. by the corsair Ravenau de Lussan’s
Scales1 : 50,000. excursion to the Rio Segovia in Nica-
ragua.

This “gold coast,” where no tra-

dition survives of a pretended town of

Estrella, attracted scarcely any settlers.

It was, in fact, rather avoided, owing

to its reefs and inhospitable shores.

Ecoxomic Conpirion oF Costa Rica.

Although not so rapid as that of

other Spanish-American communities,

Depths. the material progress of Costa Rica has

= = = at least been steady and regular. The
ee ne ete RU pao population advanced from 80,000 in
1,100 Yards. 1844 to 120,500 in 1864, and to over

182,000 in 1883, and was estimated at
220,000 in 1890. The number of immigrants is still very small, and of the 4,672
returned in 1883, nearly 2,000 were from the conterminous states of Nicaragua
and Colombia.

In the trade of the world Costa Rica derives its importance almost exclusively
from its coffee, which, in prosperous years, has been exported to the extent of
15,000 tons, chiefly to Great Britain.

Costa Rica also exports sugar, rubber, cacao, hides, and timber ; but in recent
years all these wares are exceeded in value by the bananas forwarded to the
United States, which in 1889 amounted to 40,000 tons, worth over £80,000.
The so-called quiquisque, that is, the taro of Polynesia (edible colocasia), is also
cultivated, in some districts even by Indians.

The planters on the uplands, directing their attention almost exclusively to
coffee-growing, do not produce sufficient supplies for the local demand, and are
consequently obliged to import farinaceous products from Chile. Even the live-
stock is insufficient for the wants of the people, despite the vast extent of their
grazing-grounds. Of sheep and goats there were scarcely more than 2,000, and of
horses and horned cattle, 353,000 in 1888, when all the live-stock was valued at
not more than £80,000.

ECONOMIC CONDITION OF COSTA RICA. 309

But Costa Rica enjoys the advantage over Nicaragua, Guatemala, and Mexico
that about one-half of the agricultural population are everywhere landowners,
except in the province of Guanacaste. The territory which, even under the Spanish
rule, was almost exclusively cultivated by free labour, is, for the most part, divided
into small holdings, which give to the peasantry a direct interest in its improvement.
In 1886 there were enumerated altogether 57,639 such holdings (fincas), with a
total value of £7,760,000, but mortgaged to the extent of £1,600,000. Not more
than one-twentieth part of the whole land has yet been brought under cultivation.

Since the middle of the century trade increased fourfold, from about £400,000
to from £1,400,000 to £1,600,000, or in the proportion of from £6 to £8 per

Fig. 137.—Mnz ror Husxine Correr.

‘aun ai

head of the population. Great Britain, the United States, France, and Germany,
in the order here given, are the chief customers of Costa Rica. The great high-
way of the traffic is the railway by which the capital has been completely connected
with the seaport of Limon on the Atlantic side since the year 1890. The railway
company, besides government advances, has received a grant of many hundred
thousand acres of land on the condition of selling or renting it within a period of
twenty years. <A portion of this vast domain has already been ceded to settlers,
either for tillage or stock-breeding.

Other railways are also projected, to connect Costa Rica with Nicaragua and
its future canal, and plans and estimates have been prepared for regulating the
discharge of the Rivers Frio, San Carlos, Sarapiqui, and Sucio, with a view to

310 MEXICO, CENTRAL AMERICA, WEST INDIES.

making them accessible to steamers. An embankment, forming part of the
Nicaragua Canal scheme, would have the effect of raising the level of the Rio San
Carlos about 50 feet, thus rendering it navigable by vessels of heavy draught to
the foot of the mountain.

On the other hand, the interoceanic route between the ports of Chiriqui and
the Golfo Dulce, for which a concession was granted so far back as 1849, has not
even been begun, although the company received a guarantee of 244 square
leagues “ with streams, rivers, mountains, and mines.”

Fig. 138.—HicHways or Communication 1N Costa Rica.
Seale 1 : 4,500,000.

QUE,
ANG
ory

85° West of Greenwich

— =sc-=se

—

Railways. Projected Railways. . Roads. Navigable Rivers.

50 Miles.

Apart from a few minor details, the political institutions of the republic are
modeiled on those of the other Hispano-American states. The legislative power is
exercised by a congress, whose members are elected for four years, one-half
retiring every two years. À president, also nominated for four years, and not re-
eligible, is charged with the executive functions. He chooses his own secretaries
of state, and appoints the provincial governors, the military commanders, and the
political chiefs of the cantons. The municipalities are elected by popular suffrage,
which is not universal, but restricted to all who are able to live “‘ respectably.”

The laws are administered by justices of the peace, cantonal alcaldes, provincial
tribunes and a court of appeal. Criminal cases are tried before juries, and capital
punishment is abolished as well as all degrading penalties. Freedom of worship,

ECONOMIC CONDITION OF COSTA RICA. 911

decreed in 1870, already existed de facto, and tithes had already been abolished
soon after the declaration of independence. Convents and religious orders are
interdicted throughout the republic.

Public instruction had formerly been much neglected, and even in 1883 not
more than 12 per cent. of the population could read and write. But primary
instruction for both sexes is now obligatory and gratuitous, and in 1886 as many
as 20,000 scholars were already attending the 260 public schools. Under the
Spanish ruie, and down to 1830, Costa Rica had not a single printing-press ; there
are now over ten, and the number of letters forwarded through the post increased
from 600 in 1811 to nearly 3,000,000 in 1890.

Costa Rica was free of liabilities till 1871-2, when loans of £3,100,000

Fig. 139.—ApministrativE Divisions oF Costa Rica.
Scale 1 : 5,000,000.

Se
“ee

Guanacaste. Alajuela. Heredia. San José,

Comarca of Puntarenas.

124 Miles.

were raised on the security of the customs and railway debentures. In 1888 the
public debt was converted into a total amount of £2,000,000 at 5 per cent., and
taken over by the Costa Rica Railway Company. The yearly budget is generally
balanced with an income and expenditure of from £600,000 to £800,000. Most
of the revenue is derived from the customs and spirits and tobacco monopolies.
The army comprises a standing corps of 1,000 men.

Costa Rica is divided into five administrative provinces and two comarcas, with
areas and populations, tabulated in the Appendix.

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CHAPTER V.

PANAMA.

—q LTHOUGH politically forming an integral part of Colombia, the
yf) province of Panama belongs geographically to Central America,
of which it is even a typical section in its serpentine isthmian
contours. The political frontier towards Costa Rica has not yet

been definitely settled; but in estimating the extent of the pro-
vince, the nearly straight line may be provisionally accepted which is traced on
the Colombian maps from the extremity of Burica Point in the Pacific to the
western headland of the Boca del Drago (‘‘ Dragon’s Mouth ”), at the entrance of
Almirante Bay, in the Caribbean Sea. The greater part of “ducal” Veragua
granted to Luiz Colon is thus included in Colombia, while “ royal” Veragua,
stretching thence northwards, is assigned to Costa Rica.

The administrative limits of the province towards South America pass far to
the north of the natural boundary, which is here so clearly indicated, between the
isthmian region and the southern continent. Within these somewhat conventional
frontiers the province of Panama comprises an area of about 32,000 square miles,

with a population estimated at 300,000.

PuysicAL FEATURES.

The main Costa Rican range is continued through Panama by mountains of
great elevation. Picacho, near the frontier, over 7,000 feet, is greatly exceeded
by its eastern neighbour, the extinct Chiriqui volcano, a perfect cone, nearly
11,400 feet high. At its eastern base the range is crossed by a pass which falls
to 3,600 feet, and still farther east by another about 4,000 feet, mentioned by the
traveller Morel. The crest rising between these two depressions to a height of
nearly 7,000 feet takes the name of Cerro de Horqueta, that is, “Mountain of the
Pass.” Wheelwright and other explorers speak of even still less elevated saddle-
backs, falling even to less than 200 feet; but their statements are not supported
by accurate surveys.

Farther on the cordillera maintains a normal altitude of over 8,000 feet, and
here runs much nearer to the northern or Atlantic than to the Pacifie coast,
where space is left for the vast plain of David. To this corresponds on the
opposite side the extensive inlet of the Chiriqui “lagoon,” which gives its name

PHYSICAL FEATURES OF PANAMA. 313

to this section of the cordillera. Farther on it takes the name of the Veragua
range, which begins on the west side with the superb Mount Santiago (6,300
feet), followed by several others over 4,000 feet high.

In this region, the whole of the isthmus, from ocean to ocean, is filled with
mountains or hills, with spurs projecting northwards to the Atlantic coast, and
penetrating southwards through the massive peninsula of Las Palmas, west of
Montijo Bay, far into the Pacific. But the quadrangular peninsula of Azuero,
which limits the Gulf of Panama on the south-west, is physically distinct from
the Veragua range, from which it is separated by depressions and grassy rising
grounds about 500 feet high, culminating south-westwards in a headland exceeding
3,000 feet. The Azuero peninsula, in fact, forms part of an almost completely
submerged chain, which is disposed parallel with the winding isthmian cordilleras,
and which embraces the Nicoya peninsula, with those of the Golfo Dulce and
Burica, besides Coiba Island and the Pearl Archipelago in Panama Bay.

North-west of the Veragua range the orographie system becomes very
irregular in direction and altitude, being broken into several fragments, whose
original trend it is now difficult to determine. Capira, the culminating mass
(5,000 feet), les beyond the line of the main axis, its escarpments plunging
southwards into Panama Bay, and even projecting seawards in the little Cerro
Chame. The main axis itself appears to be continued in the Ahoga-Yeguas
hills, which are crossed by a pass only 380 feet high, and which nowhere exceed
700 feet. Farther on is opened the still lower Culebra Pass (290 feet), which is
distant about 34 miles in a straight line from both oceans.

The geological constitution of the isthmian heights shows that their various
sections belong to no single homogeneous system. The Veragua range consists
mainly of granites and syenites, gneiss and schists, whereas the Panama hills are
chiefly weathered dolerites and trachites, which may be cut with a spade like
cheese.” But these igneous heights nowhere present the aspect of erupted cones.
Hence the eruptions must have taken place at a time when the waters of the two
oceans communicated through channels, The limestone banks occurring in cer-
tain parts of the isthmus are also filled with fossils, dating, probably, from early
tertiary times, and mostly resembling the forms still living in the neighbouring
waters. The channel, in fact, is scarcely completely closed, though the attempts
of engineers to reopen it have hitherto failed. The depression, however, is traversed.
by an interoceanic road and railway.

Beyond the Culebra sill the mountains again gradually rise eastwards, the Maria
Enriquez (1,340 feet) being followed by those of Pacora, which are nearly 1,700
feet high. Then in the neighbourhood of San Blas Bay is developed a coast-
range disposed west and east along the Atlantic, and in one of its crests just east
of Puerto Belo attaining an elevation of over 3,000 feet. The system is continued by
a steep ridge from 500 to 2,700 feet, which here forms the waterparting between
the two oceans at the very narrowest part of the isthmus. The distance between
San Blas Bay and the head of the Pacific tidal wave in the Rio Bayano scarcely
exceeds 17 miles. But the crest where the Bayano has its source is over 1,000

314 MEXICO, CENTRAL AMERICA, WEST INDIES.

feet high, so that for an interoceanic canal it would have to be pierced by a
tunnel at least seven miles long and high enough to admit the tallest vessels.

The San Blas (Chepo) cordillera, consisting of gneiss and metamorphic schists,
is continued under various names as the Atlantic coast-range as far as the entrance
to Uraba Bay, where the isthmus takes the name of Darien. The hilly mass of
Gandi (3,000 feet) and Turganti farther on mark the point where the system bends
round to the south along the west side of the Rio Atrato. At the Tihule Pass it
falls as low as 420 feet, and this site has also been proposed for an interoceanic

canal, which would replace an ancient marine strait along the valleys of the Rio
Atrato in the east and Rio Tuyra in the west.

Farther on the cordillera is connected by lateral des with the Baudo range,

which runs close to the Pacific coast in the direction from north to south for a

Fig. 140.—Course or THE River CHAGRES.

From a Spanish Map of the first half of the Eighteenth Century.

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distance of about 124 miles, The sierra culminates in the Baudo peak (6,000 feet),
but it is interrupted by broad depressions, one of which, the Cupica Pass, is only
1,000 feet high. The last rising grounds of the plateau die out north of the San

\
Juan estuary.
Rivers, Bays, ISLANDS.

Apart from the Atrato, only a few lateral affluents of which are comprised in
the province of Panama, the isthmus has no large rivers, or, at least, none that
send down a large volume except after heavy rains. Many have a considerable
course owing to the disposition of their valleys, which run parallel with, and not
transversely to, the seaboard. But their basins are too narrow to collect any great
quantity of surface waters.

Even the Chagres, a term which, according to Pinart, means “ Great River”
in the Muoi language, is in ordinary times an insignificant tributary of the Carib-
bean Sea. It rises about the centre of the isthmus of Panama, and flows first in

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PANAMA SCENERY ;

RIVERS OF PANAMA. 315

the direction of the south-west parallel with the shores of both oceans. At Cruces,
where it has already collected all its headstreams, it is accessible to small river
craft. At Matachin, a little farther down, where at low water it is only 46 feet
above the level of the Atlantic, it is joined by the Obispo, which descends from
the Culebra heights. Judging from the direction of its valley, the Obispo is the
main branch, for below the confluence the united waters flow transversely to
the coast-ranges to the Caribbean Sea, where they are obstructed by a bar with a

Fig. 141.—Gutr or San Micuet.
Scale 1 ; 500,000.

[l
IL

An
|

= :
EE =

6
4, 5 Mare

Depths
———
2 == =
Beach exposed 0 to 16 16 Feet and
at low water. Feet. upwards.

6 Miles

mean depth of little over 10 feet. The river itself varies from about 14 to 40
feet with the seasons, but unusually heavy rains will sometimes cause a sudden
rise of 40 feet. Rapid changes of level of 20 feet are frequent, and the railway
bridges have been flooded to depths of 14 or even 20 feet. The discharge varies
enormously, from 850 to as much as 70,000 cubic feet per second; but the normal
difference is not more than 700 cubic feet in the dry season and 2,600 during the
floods. Compared with that of European rivers, the mean discharge is very high,

316 MEXICO, CENTRAL AMERICA, WEST INDIES.

the catchment basin not being more than about 1,000 square miles in extent and
75 miles long.

The Chagres is exceeded both in length and the extent of its basin by the Rio
Bayano, which, however, has a smaller volume because it belongs to the drier
Pacific slope. It enters the sea through a broad estuary, which is closed by
_a bar with scarcely two feet at low water. In the Gulf of Panama itself no
anchorage is afforded to large vessels for a long distance from the shore. The
five-fathom line lies nearly six miles from the mouth of the Bayano, and this is
itself one of the greatest objections to an interoceanic canal across the San Blas
isthmus.

Of all the isthmian rivers the Tuyra, flowing also to the Pacific, has the largest
basin and longest course. It flews for nearly 100 miles parallel with the cordillera
of Darien, and after escaping from the densely-wooded uplands, it is joined by
the Chucunaque from the north-west, the united stream being 1,000 feet wide
and over 30 feet deep, with a mean discharge of 1,100 cubic feet per second.
Farther on the river merges gradually in its estuary, and its estuary in the mag-
nificent Darien Harbour, which communicates with San Miguel Bay through the
two channels of Boca Grande and Boca Chica. The encircling heights are clothed
with a glorious forest vegetation, where the tall white stems, 100 feet high,
support a continuous canopy of dark verdure.

On the Atlantic side the largest inlet is that formed by the two bays or lagoons
of the Almirante and Chiriqui, which communicate with the open sea through the
three deep passages of the Boca del Drago, Boca del Toro, and Boca del Tigre, all
accessible to the largest vessels. The Almirante Bay is so named from “ Admiral”
Columbus, who visited these waters in 1503; from him also the wooded island
between the Drago and Toro passages has been named Colon, while another islet
in the bay takes his Christian name, Cristobal (Christopher).

Almirante is a vast aggregate of creeks and havens, like the neighbouring
Chiriqui, which has an area of no less than 320 square miles. The chain of islets
at the entrance is so disposed as to continue the continental coast-line as if they
represented a former shore eroded by the waves.

East of Chiriqui Bay the coast is continued several miles seawards by a marine
bank scarcely 25 fathoms deep and strewn with shoals, reefs, and islets. One of
these is the famous Escudo de Veragua, often referred to in diplomatic documents
as a debatable land between Costa Rica and Colombia.

San Blas Bay, which lies at the narrowest part of the isthmus, presents, like
Chiriqui, somewhat the appearance of an indentation made by marine erosion in
an old rectilinear strip of coastlands. The San Blas peninsula, enclosing the bay
on the north side, is a fragment of the primitive shore, and is continued eastwards
by hundreds of reefs and islets forming the Muletas or Mulatas archipelago.
None of these cays have any hills or cliffs, being merely sandy stretches resting
on a coralline base and rising a few feet or perhaps yards above the surface. The
intervening channels are deep enough to admit large vessels, to which they afford
safe anchorage in smooth water. All are covered with forests or cocoanut groves,

ISLANDS OF SAN BLAS BAY.

INDIAN SETTLEMENTS ON THE

GULF OF DARIEN. 317

and several, with springs of good water, have been occupied by a few Indian
communities.

Beyond the Muletas the cays are scattered in disorder along the coast, forming
an outer barrier reef as far as the Puerto Escocés. Farther on the sea becomes
quite free of these obstructions in the direction of the Gulf of Darien (Uraba),
where, however, begins a fresh formation, that of the alluvial matter deposited by
the mouths of the Atrato. Here the sands and shore-line are continually shifting
with the current, so that the-marine charts should be revised every year.

In the Gulf of Darien the same process of silting, but on a much larger scale,
is going on as in that of Smyrna in Asia Minor. The potent current of the
Atrato is continually impelling the alluvial banks in the direction of the South

Fig. 142.—Guzr or San Bras.
Scale 1 ; 600,000,

Depths.
16 to 32 32 Feet and
Feet. upwards.

12 Miles.

American side, so that the southern part of the bay cannot fail, sooner or later, to
be cut off from the open sea.

The contrast between the Atlantic and Pacific seaboards is primarily due to
the tides, which vary far more on one side than the other. At the mouth of the
Chagres river and in Colon Bay there is a mean rise of 15 inches, and of one foot
in Chiriqui Bay, but this difference between ebb and flow is not constant, being
greatly modified according to the force and direction of the winds. At times the
surface remains at the same level for days together; but as a rule the two
diurnal tides neutralise each other so far as to produce only a single rise and a
single fall in the twenty-four hours.

On the Pacific coast, on the contrary, ebb and flow follow the normal course.

518 MEXICO, CENTRAL AMERICA, WEST INDIES.

In Panama Bay the lowest rise in May and June is about eight feet, whereas it
amounts, in November and December, to 23 feet, the yearly average heing about
13 feet. Owing to these discrepancies the level of the Pacific is scmetimes
higher, sometimes lower than that of the Atlantic, the greatest possible difference
between the two being 10 or 11 feet. Hence in an open canal across the isthmus
of Panama, there would be an alternating current, shifting with the respective
levels and giving to the canal a constantly varying inflow and outflow. Nor
would the movement balance itself, or produce equilibrium, for the average of the
oscillations gives to the Pacific a level a few inches higher than that of the

Fig. 143.— CarenonrA Bay.

Scale 1 : 400,000.

of Greenwich

Depths.
0 to 250 259 Fathoms
Fathoms. and upwards.

6 Miles.

Atlantic in Colon and Caledonia Bays. Moreover, the rise and fall takes place at
different hours in the two oceans, the station in the port of Colon being nine hours
behind that of the Pacific.

Another result of these tidal discrepancies is the different aspects presented by
the opposite seaboards. While the Atlantic coastlands are narrow, those of the
Pacific develop in some places broad stretches of beach, and are also less rich in
coral reefs than the Caribbean Sea, high tides being fatal to most species of
polyps.

Coiba, Cebaco, and the smaller islands on the Pacific side between Burica
Point and the Azuero peninsula, all belong geographically to the mainland.

—_ sn

CLIMATE OF PANAMA. 319

Those in the vast semicircular Gulf of Panama also rest, like the isthmus itself,
on a marine bed less than 25 fathoms deep. Here the larger islands form with
over 100 islets the so-called Pearl Archipelago, although their pearl fisheries have
long been exhausted,

CLIMATE.

The climate of the province of Panama presents some slight transitions
between those of the north-western isthmuses and the neighbouring South
American continent. The mean annual temperature of 78° to 80° Fahr. is some-
what higher on the Atlantic side, which is due to the warmer marine currents of

Fig. 144.—Gutr or Panama.
Scale 1 ; 3,500,000.

| E =
| West of Greenwich +. 80°
Depihs. ’
0 to 10 10 to 50 50 to 500 500 Fathoms
Fathoms. Fathoms. Fathoms. and upwards.

60 Miles.

the Caribbean Sea. But throughout the year the extreme range of temperature
never exceeds 30°, the limits being 65° and 95° Fahr.

Under the infiuence of the neighbouring continent the prevailing trade winds
set regularly rather from the north than the north-east. They daily increase in
force with the heat of the sun, then gradually fall, and often leave the nights
perfectly calm. Between May and November these northern currents are replaced
by the vendavales, or south-eastern monsoons.

The Atlantic seaboard is exposed to the sudden squalls which are so dangerous
to shipping in the Gulf of Mexico. The isthmian region is also occasionally
visited by cyclones, such as that of October, 1865, which swept over Colon, the

20 MEXICO, CENTRAL AMERICA, WEST INDIES.

isthmus of Panama and Mosquito Coast; in 1885 eighteen sailing-vessels were
wrecked by a norte in the port of Colon.

As in so many other respects, the opposite seaboards present a contrast in the
distribution of the rainfall, the northern slopes exposed to the moist trade winds
receiving at least twice as much as the Pacific coast facing the southern monsoon ;
the former is estimated at over 120, the Jatter at about 60 inches during the year.
At the Gamboa observatory, standing 100 feet above sea-level, the average in the
rainy season is 38, in the so-called “dry ”’ season 35 inches.

Being almost constautly saturated with vapour and charged with exhalations
from the marshy tracts, the hot atmosphere of the isthmus is necessarily danger-
ous to Europeans. The first Spanish settlers in Panama gave it the name of
Sepultura de Vivos, or “ Living Grave.” Immigrants from Europe and the United
States connected with the railway and canal works have specially to dread affec-
tions of the skin, of the liver and kidneys, and yellow fever, during the eight first
months of their residence; after that period of probation they enjoy as much
immunity from this scourge as the natives, who suffer most from consumption.
Four-fifths of the hands employed on the international works have been half-
castes either from Colombia or Jamaica, and when all allowances are made, these
works have cost far more lives than similar operations in temperate lands. The
mortality during a period of two years and three months in the Panama works
amounted to 98 per 1,000.

FLorA AND FAUNA.

In the province of Panama, and especially in the isthmus of Darien, the Central
American flora reaches its highest development. Here the South Mexican and
Colombian types are intermingled and associated with a local flora which, according
to Scherzer, represents over one-fifth of the whole. This diversified vegetation
covers the surface with such a tangle of stems, branches, foliage, creepers, parasites
that the traveller finds his progress blocked in every direction. The headlands
along the seaboard nowhere present the aspect of rocky bluffs, being so completely
clothed with verdure that they often look like a single gigantic plant with its roots
in the deep and its superb pyramidal crest towering to a height of 600 or 700 feet.

In the interior the brooks and rivers flow beneath sombre avenues of matted
foliage, the water disappearing in one place under a mass of drifting snags, in
another carpeted with confervals and other aquatic plants. The chamedorea
pacaya, a species of palm, grows to an altitude of 7,000 feet in association with the
oak and alder. Owing to the less copious rainfall the vegetation is somewhat less
exuberant on the Pacific than on the Atlantic side.

A remarkable contrast between both coasts is presented by the oceanic fauna,
although in the early tertiary epoch the two basins were connected by marine
channels. But although the numerous echinidæ, for instance, differ specifically,
nearly all belong to the same genera on both seaboards. It is evident that the
divergence is comparatively recent, and must have taken place since the channels
were closed.

INHABITANTS OF PANAMA. 321

Of the 1,500 and 1,340 species of molluscs belonging respectively to the
Caribbean Sea and Panama waters, less than 60 are common to both groups. Even
the land animals differ in the same way. The chrysothrix, a species of monkey
peculiar to the Chiriqui district, will not even live on the opposite coast.

INHABITANTS.

Most of the inhabitants of Panama, like their Central American neighbours,
are a mixed people, the various elements being the Spanish, Indian, and Negro.
Since the abolition of slavery Jamaica has never ceased to send blacks and mulattos
to the isthmus, where many have settled as petty dealers and farmers, In several
villages on the Atlantic side they are in a majority, and to them is due the spread
of the Anglo-Spanish jargon now current along the seaboard.

Some of the aborigines have preserved their physical type, customs, and speech.
Thus the Guaymi, that is “ Men,” keep somewhat aloof, mostly in the upper
Miranda volley, in the western part of the province. These Indians, whose chief
tribe bears the name of Valientes, belong to the same family as the Costa Rican
Talamancas, and were certainly at one time more civilised than at present. They
are probably the direct descendants of those natives who before the conquest
carved symbolic figures on the face of the rocks, and deposited gold ornaments in
their guacas or graves. One of their chiefs pretends to descend from Montezuma,
a name which they have evidently learned from the whites, and to which they
now attach a certain national sentiment.

The religion of the Guaymi is a pure system of terrorism. Every sudden noise
startles him, and is attributed to some wicked demon, who has to be conjured by
the wizard and propitiated by offerings. When the sick seem to be past recovery
they are taken to the forest and abandoned with a calabash of water and a few
bananas. After death the body is exposed on a platform for a year, when the
remains are cleansed and deposited in a bundle in the “ family vault.”

According to Pinart the Guaymi still number about 4,000, although in 1883
the Muoi tribe had been reduced to three persons. On the southern slope of the
chain lived the Dorasques, a distinct tribe with a different language, but now all
but extinct. The Seguas, called Mexicans or Chichimecs by the early Spanish
writers, were, in fact, more or less barbarous Nahuas met by Vasquez de Coronado
on an affluent of the Chiriqui lagoon; but the locality can no longer be identified.

East of the Chiriqui range, and thence to the San Blas isthmus, all the abori-
gines have disappeared, either extirpated or absorbed in the surrounding Mestizo
populations. But native tribes still survive in the eastern districts, on the shores
and islands of San Blas Bay, and in the Bayano, Tuyra and Atrato basins. But
these Indians have not preserved the tribal traditions, and they no longer
remember the sway of the ancient Paparos or Darienes, whose name survives in
the eastern part of the isthmus, and who were probably related to the Quevas or
Cuevas mentioned by Obido y Valdes and other early writers.

Apart from the southern Chocos, whose affinities are with the Colombian
populations, the various Indian peoples of Darien, despite differences of speech.

322 MEXICO, CENTRAL AMERICA, WEST INDIES.

belong to a single stock, that of the Cunas (Cuna-Cuna), called also 7%, or “ River
People,” from their aquatic dwellings along the banks of the streams. In the
same way the Chocos of the Atrato basin are called Do, a word of precisely the

same meaning.
The Cunas, who call themselves Tule, or ‘“ Men,” are supposed to be of Carib

Fig. 145.—Isramus or CHrriavt.
Seale 1 : 1,500,000.

Vee: > 2
MANS. S = = =
Wa 5 ARE CE —
NA EE 0a
G 4 SK f= Ag Qu
QE PTE + ——

Ss —— == ™ = oe
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R° SSS ; Se
82°40 West of Greenwich SAS
Depths.
0 to 10 10 to 100 100 Fathoms
Fathoms. Fathoms. and upwards.
18 Miles.

stock. They are in general a small-sized, thickset people, with a great tendencv
to corpulence. Albinos are by no means rare, while the fair complexion and red
hair occurring here and there would seem to suggest long contact with the bucca-
neers. They formerly practised tattooing, but now smear the doby with the blackish

TOPOGRAPHY OF PANAMA 323

sap of the jagua (garripa americana), which keeps the skin cool. Their language
is a sort of singsong, in which each sentence is followed by a long pause. The
numerical system is vigesimal, as in Aztec, and may possibly be due to Nahua

influences.

TorpoGRAPHY.

The “city” of Castillo de Austria, founded on the Rio Chiriqui-mula (Crica-
maula), or Rio de Guaymi, during the first years of the conquest, soon disappeared
without leaving a trace of its former existence. The district continued to be
inhabited exclusively by Indians till the beginning of the present century, when
some negroes from the Vieja Providencia and San Andrés islands settled on the
Chiriqui coast and neighbouring islands and gradually spread round the whole
islet. Boca del Toro, their largest station, had in 1883 a thriving population of
about 500, almost exclusively coloured. It lies in Colon Island over against the
Isla Bastimentos, the Provision Island of the English, where passing vessels call for
bananas, yams, and other supplies.

On the mainland the chief trading-place is Gobrante, at the head of the navi-
gation of the Chiriqui-mula, whence a difficult track leads through the Miranda
valley over the cordillera down to the plains of David. An easier route runs
farther west from French Bay through a pass near the Cerro Horqueta. David,
capital of the Chiriqui department, stands within 12 miles of the Pacific on a
grassy plain flanked on the north by the superb cone of Chiriqui. Some twelve
miles farther west the hamlet of A/anje is all that remains of the ancient capital of
the country, a famous market-place on the trade route between Guatemala and
Panama.

Farther on Bugabita, near the village of Bugaba, is noted for the discovery of
numerous guacas, old graves full of gold ornaments, which in 1860 gave the Chi-
riqui district a temporary renown as a new Eldorado scarcely inferior to that of
California. But it was soon found that of every twenty or twenty-five graves not
more than one contained gold or copper objects, chiefly figures of animals, especi-
ally frogs, evidently amulets worn by the natives. Treasures to the value of about
£40,000 were unearthed by some 1,500 searchers, who, after exhausting the supply,
quitted the district.

Nata, or Santiago de los Caballeros, is one of the oldest settlements in America,
dating from the year 1512, some time before the very name of Mexico was known
in Europe. It lies on the Rio Chico near its mouth in Parita Bay, at the western
extremity of the Gulf of Panama.

The famous city of Panama, which gives its name to this gulf, to the isthmus
and the whole province, was not originally founded on its present site. In
1518, when Pedrarias de Avila transferred the capital from the Atlantic to the
Pacific side, he selected a spot at the mouth of the little Rio Algarrobo, which
enters the bay or inner basin at the point where the gulf develops its extreme
convex curve towards the north. For 150 years this first Panama, founded on
the site of an Indian village of that name, enjoyed a monopoly of the trade of the

324 MEXICO, CENTRAL AMERICA, WEST INDIES.

isthmus. Here the Spanish flotillas landed the merchandise and all the gold of
Peru, and over 2,000 mules were employed in transporting the precious metal from
Panama to Puerto Belo, where they were shipped for Spain: But these treasures
could not escape the attacks of the buccaneers. In 1670 Morgan, at the head of
1,100 men, crossed the isthmus and captured Panama, which was sacked and burnt.
Fearing renewed attacks, the Spaniards never rebuilt it, and nothing remains to
mark its site except the shapeless ruins of two churches overgrown with brush-
wood.

The present city stands some six miles farther west, at the foot of Ancon Hill
(560 feet), and near the mouth of a rivulet called “Rio Grande.” Solid walls 10
feet thick still enclose San Felipe, the city proper, and form towards the sea the

Fig. 146.—Panama.
Scale 1 : 57,000.

Boa)

why 71
SALE

ent DS: Le
(PANAMA Siret |
nt Se

Ji est £ Se
SADE, ‘| $ à 7. cee

West of Greenwich

Depths.
Sands exnozed at 0 to 7 7 to 16 16 Feet and
low water. Feet. Feet. upwards.

2,200 Yards.

magnificent promenade of Las Bovedas, Beyond the ramparts the suburbs are
continued along the beach and neighbouring slopes, Conspicuous amongst its
monuments is the cathedral, whose two towers serve as beacons and lighthouses.

Although chosen es the seat of a Spanish American Congress in 1824, and
raised to the rank of a capital when Colombia formed a confederacy of states, now
reduced to the position of provinces, Panama is a place of slight importance as a
centre of population and local trade. The so-called “Panama” hats, at one time
so fashionable in Europe, are not made in the town whose name they bear.

In fact, this place owes all its celebrity to its vital position at the narrowest
part of the isthmus, and its chequered history presents a remarkable alternation
of rapid progressand decline according to the routes followed by international
trade Hence it flourished when it commanded the traffic of Peru and Chile:

Fig. 147.—PANAMA, VIEW TAKEN FROM Mount Ancon.

TOPOGRAPHY OF PANAMA.

and was almost abandoned when it lost that monopoly. It again became a busy
place during the rush of miners to the Californian goldfields, until the stream of
trade and travellers was deflected by the opening of the American railways
from ocean to ocean. Its prosperity was again revived when nearly 20,000 hands

were engaged on the interoceanic canal, and now it has entered on a third period
of decline. It must always, however, retain some importance, thanks to the rail-
way here crossing the isthmus, and to th= lines of steamers converging in its gulf,
from Polynesia, North and South America.

326 MEXICO, CENTRAL AMERICA, WEST INDIES.

Unfortunately, the roadstead offers bad anchorage during the prevalence of
the north winds, when large vessels prefer the more sheltered waters under
Taboga Island 11 miles farther south. According to the general plan, the
interoceanic canal was to be continued between embankments or sea-walls as far
as the little group of islets where begins the five-fathom line. This anchorage
is already connected by a deep channel with the mainland.

Fig. 148.—Coton.
Seale 1 : 46,000.

KOs

= M STE à tlle.
= —— =

Aj ore

—"

=(ASPINWALL)—+#:
<<

Reefs exposed at 0 to 16 16 to 32 32 Feet and
low water. Feet. Feet. upwards.
1,100 Yards.

During the Spanish régime the only line of communication between the two
oceans was a simple mule-track crossing the isthmus northwards to Puerto Belo
on the Atlantic side. This old seaport, whose fortifications are now overgrown
with a forest vegetation, has sunk to the position of an obscure hamlet oceupied by
a few hundred negroes who do a little trade with Colon, Colombia and Jamaiea.
The harbour is commodious, deep and well sheltered, but the district is extremely
unhealthy owing to the want of circulation caused by the surrounding heights.

TOPOGRAPHY OF PANAMA. 327

Here Drake died suddenly in 1595, when about to sack the town after ravaging
the mainland.

Puerto Belo was succeeded by Ohagres, on the right side of the Chagres estuary,
as the Atlantic terminus of the isthmian route from Panama. The river from
this point was navigable for boats to Matachin, within 14 miles of the Pacific as
the crow flies. But Chagres, like Puerto Belo, isa hotbed of ague, the marsh
fevers raging on this coast being commonly known as ‘“ Chagres fevers.” Hence
the population rapidly disappeared as soon as another station was chosen at the
little coralline island of Manzanillo, north-east of Limon Bay, between Chagres
and Puerto Belo.

Here was founded the new port, which was named Colon, in honour of Colum-
bus, who discovered the bay in 1502. It also took the name of Aspinwall from one
of the chief promoters of the isthmian railway, and both names are still in current
use. Colon is a town of wood and iron, with colonnades and verandahs brought
ready-made from the States, docks and depots relieved by a few clumps of cocoa-
nut palms round about the railway-station, and adorned by a statue of Columbus
facing seawards, executed by Carrier-Belleuse.

Colon, having been recently burnt, bas been rebuilt on a larger plan and on
better-drained ground. Some of the building materials have been supplied from
the porphyry quarries at the neighbouring village of Bohio Soldado. It is almost
exclusively a place of transit for goods and passengers, nearly all brought by
regular lines of Atlantic steamers communicating by the isthmian railway with
corresponding lines in the Pacific, Some bananas are also exported to the States
from the plantations on the Rio Chagres. Although sheltered by a recently-con-
structed embankment, the shipping is still insufficiently sheltered at the mouth
of the canal, and sailing-vessels have occasionally to take refuge in the harbour
of Puerto Belo.

So early as 1835 the American, Biddle, was already exploring the isthmus of
Panama with a view to the construction of an interoceanic railway. But the work
was not begun till the year 1850, when the fame of the Californian Eldorado was
attracting thousands of goldseekers from all parts. The line, which was opened
in 1855, was carried across swamps and forests, rivers and mountain passes, under
a dangerous climate, at the cost of many lives, while the outlay, nearly £40,000
per mile, was five times more than the average expenditure in the States.

But this line, nearly 100 miles long, was from the first of great commercial
importance in forwarding goods and passengers between the two oceans. Its
historic importance is also incalculable. Thanks to this route the west coast of
America was suddenly brought some thousands of miles nearer to Europe. Thus
its far-reaching consequences extended to the trade of the world and the whole
system of international communications.

Nevertheless a railway, however useful, especially before the opening of the
United States and Canadian transcontinental lines, could be regarded only as a
sort of “stop-gap” pending the reopening of the marine communication between
the two oceans, the existence of which, though closed since tertiary times, was still

328 MEXICO, CENTRAL AMERICA, WEST INDIES.

suspected long after the exploration of the Caribbean Sea. Columbus himself,
even after coasting the seaboard from north to south, died in the belief that such
a passage would still be found through the region visited by him.

So deep-rooted was the conviction that the strait must exist that it was figured
on all maps down to the year 1540. The illusion spread even to the extreme east,

Fig. 149.—Tue ‘Mystery or THE Srrarr”? AT THE BEGINNING OF THE SIXTEENTH CENTURY.

A «Septer: Jormgse
AS 1 avila

and was embodied in a Chinese map of 1820, which represents the two American
continents as separated by no less than three interoceanic channels. The
“mystery of the strait,” which Charles V. recommended Cortes to solve in 1534,
shows that he also believed in this navigable highway.

But as it could not be found, men’s thoughts turned to the idea of opening it by
sheer force, and schemes of canalisation were proposed before the region itself had

THE PANAMA CANAL. 329

been even roughly explored. Philip IT., however, forbade the presentation of any
new plans, since “the will of God had clearly manifested itself by the creation
of a continuous isthmus.” But when Latin America was finally emancipated from
Spanish leading-strings, the undertaking began again to attract attention. So
early as 1825 Bolivar took steps to have the isthmus of Panama surveyed with a

Fig. 150.—Docxs AND COURSE OF THE Panama Canat.
Scale 1 : 540,000.

cee SL ER RSR 12 Miles.

view to the construction of an interoceanie canal. Scientific exploration had
thus already begun.

Amongst the projects based upon local research, the most important in the
history of Panama were those of Garella in 1843, and of Lull in 1875. But both
of these engineers admitted the possibility only of a canal with locks to ascend the
slopes on one side and descend on the other. But in 1879, a more detailed study
of the ground enabled MM. Wyse and A. Reclus to present a plan with estimates
for a cutting at sea-level, and these propositions were accepted by a congress of
engineers, men of science, and capitalists assembled in Paris. The prodigious
success of the Suez Canal and the yearly growth of navigation between Europe und

330 MEXICO, CENTRAL AMERICA, WEST INDIES.

the west coast of America, tended to overrule objections and dispose the public in
favour of the magnificent undertaking. The movement between the two oceans

was estimated at from 3 to 5 per cent. of the world’s trade, or altogether nearly
5,000,000 tons.

According to the original plan the cutting was to be 44 miles long, following

Fig. 151.—Sm or tar Lock Cana.

Scale 1 : 130,000.

PME ie. Se ANT
SE iy D p (+

Ada UG
Sy)

We
\

a
VEG
SANTE
ys

NBA
SNS)
AK

= a § 08

«ZA
Cr Shek
2

a TERN

A AR
AA it Dy N

| West ae Ce

6 Miles.

the valleys of the Chagres on the Atlantic and of the Rio Grande on the Pacific side.
The crest of the range was to be crossed at Mount Culebra, either by a tunnel 130
feet high or by a tremendous open cutting. Reservoirs were to be constructed by
means of dams to control the flood waters of the Chagres and its affluents, the
displacement of matter being estimated at first at 1,645 millions of cubic feet, and
afterwards at 2,520 millions, to allow for a tunnel nearly four miles long. But the

THE PANAMA CANAL—VIEW TAKEN AT SAN PABLO.

a is
44 F1
au 8 T1 2

ANA ae) ee ‘al NON, AT On ns à 7 aa Foe Le AT RS NS és D D ÉTS PONT eee A | mf

THÉ PANAMA CANAL. 991

outlay, including interest till the opening of the canal in 1888, was fixed under
either alternative at £26,000,000.

This scheme, entrusted to the person whose name was so happily associated with
the Suez work, has ended in financial disaster. So far from being completed, the
works along the greater part of the line are still at the initial stage of projects and
counter-projects. The part actually finished is variously estimated at from one-
third to one-fifth of the whole; officially it is put at one-third, the Colombian
Government having surrendered to the company the 375,000 acres of land agreed
to on completion of so much. Small steamers can ply on the canal for a distance
of 10 miles, and rowing-boats nearly four miles farther. About 1,050 million
cubic feet of matter have been removed, while what remains represents at least a
total of 5,250 millions, for the original plan has had to be modified to lengthen the
curves and give the banks a more gentle slope than had been provided for in
the first estimates.

The outlay already incurred aniounts to £60,000,000, of which, however, not
more than £18,000,000 have been expended on the actual works. But experts
now estimate at £120,000,000 the sum still needed, including £18,000,000 for the
purchase of the works already finished, quays, piers, sections of the canal, various
cuttings, embankments and buildings. The main cutting itself represents an
expenditure of probably £52,000,000.

Ten years have passed from the date of the concession to that of the catastrophe,
and it is calculated that the completion of the work would take at least another
twenty years of continuous labour. The date fixed by the Colombian Government for
the opening of the canal was January 31, 1893, while the company promised to have
everything finished by the year 1887.

Such an enterprise would, no doubt, be a mere trifle for a comity of nations
working in harmony for the common good. But under the actual conditions, where
the civilised nations of the earth incur a yearly expenditure for military purposes
of twice the sum needed for this enterprise, international rivulries naturally prevent
the interested Powers from making a collective outlay which might benefit one
more than another.

Hence the latest and relatively less ambitious projects contemplate a navigable
way in successive stages, each stage being regulated by a system of locks. But
a tremendous difficulty still remains, that of the excessive flood waters, which wash
down vast quantities of alluvial matter equally dangerous to any canal, whether at
sea-level or with locks. According to a plan proposed «by the first engineers and
since diversely modified, it will be necessary to store the overflow by vast dams
capable of retaining as much as ten or eleven billion cubic feet. These embank-
ments will transform to a chain of lakes the whole middle course of the Chagres as
far as a point above Cruces.

To protect the canal from the floods, it has even been proposed to deflect the
course of the river itself, and send it through some tunnel not yet planned to the
Gulf of Panama. Thus, even for a simple canal with locks, enormous works have
still to beexecuted. And when all is done, the economic value of the undertaking

IN)

MEXICO, CENTRAL AMERICA, WEST INDIES.

will be seriously affected by the competition of the future Nicaraguan canal carried
at a height of not more than 110 feet above sea-level.

But despite ofeverything, the work will sooner or later be resumed, unless the
cutting of the navigable way is rendered useless by some fresh discovery. One would
fain hope that so many lives, so much energy and devotion may not have been
sacrificed in vain. The prodigious quantity of machinery accumulated at this vital
point of the globe must be utilised ; the astounding cuttings which the traveller
contemplates with amazement will one day give free passage to the mingled waters
of two oceans ; the ever-growing power of human industry and the yearly progress
of international trade surging round the portals of this isthmian barrier, will all

Fig. 152.—Proyeoren Artirictat Lakes on THE Panama Divine.

Seale 1 : 240,000.

WZ VE

a,
SRC

3 Miles.

combine to open a navigable highway between the neighbouring marine basins.
But its completion must necessarily be delayed for years.

East of Puerto Belo, on the Atlantic side, the Indians largely predominate in
all the settlements. Nombre de Dios, founded by Nicuesa in 1510, has left no
vestige of its existence, and its very site can no longer be determined. The
spacious and deep basin of San Blas Bay, where 10,000 vessels might easily ride
at anchor, is occupied only by a few scattered hamlets of the Cuna Indians.

But schemes have also been proposed for piercing the isthmus at this its
narrowest part. The country was surveyed first by MacDougal in 1864, and since
then by Selfridge, Wyse, and A. Reclus, and from their reports it appears that
here the cutting would be only 32 miles long, of which 6 would follow the deep
bed of the Rio Bayano. But the cordillera at this point is over 1,000 feet high
at the lowest passes, so that the canal would have to be cut through a tunnel
variously estimated at from 6 to 9 miles in length.

CALEDONIA BAY.

Caledonia Bay, about 120 miles south-east of San Blas Bay, and not far from
Putricanti, largest village of the Cuna Indians, revives the memory of earlier
attempts at colonisation. An inlet in the bay bears the name of Puerto Escocès,
“Scotch Port,” so named, like the bay itself, from a group of Scottish immigrants
who settled in this district under the financier, Patterson, in 1698. For Patterson
this was the “ key of the world,” and Puerto Escocès might well have become
one of the world’s portals had the British Government come to his aid against the

Fig. 153.—Prosecrep CUTTINGS ACROSS THE ISTHMUSES OF PANAMA AND DARIEN.
Seale 1 : 3,800.0(0.

=}
PCAPL=T1S/S-=

0 to 100 100 Fathoms
Fathoms. and upwards.
60 Miles.

Spaniards and Indians, and constructed a road across the isthmus at this point.
But tne climate and homesickness soon decimated the Scotch settlers, and the
survivors were dispersed in 1700 by a Spanish squadron; in 1827 the ruins of
Patterson’s fort were still visible.

The neighbouring port, Carreto, had in 1513 witnessed the departure of more
illustrious pioneers, Nuiiez de Balboa and his followers, who in that year started
to discover the South Sea, which they happily reached in twenty-three days. At

994 MEXICO, CENTRAL AMERICA, WEST INDIES.

that time the Spanish station on this coast was Santa Maria, founded as a future
“ metropolis ” on the Gulf of Darien (Uraba), just north of the Atrato delta. But
in 1526 the settlement was removed to Panama, and Santa Maria, gradually
invaded by the forest, received the epithet of Antigua.

Darien was in those early days known by the name of “Castille d’Or,” and
auriferous deposits had already been worked at Cana towards the sources of the Tuyra
in the Choco territory. Till the end of the seventeenth century a certain quantity
of gold continued to be extracted from this “ Eldorado ;” but the buccaneers had
found the way to the mines, and to get rid of these troublesome visitors the
government could think of nothing better than closing the works. Its policy
was based on the principle of ruining its subjects to divert foreign rivals.

Fig. 154.—Progectep CANAL BETWEEN Urasa AND San Micuer Bays.

Scale 1 : 1,900,000.

30 Miles.

The Atlantic slope of Darien, with its abrupt declivities facing the sea, scarcely
affords much facility for canalisation. Nevertheless, numerous surveys have been
made by prospectors, and some of the early travellers reported the existence of
very low depressions where real mountains raised their wooded slopes high above
sea-level. In 1854 the American, Lieutenant Strain, landing at Caledonia Bay,
with a party of twenty-eight men, made his way across the isthmus down to the
Pacific in sixty-three days; but several of his followers had perished of hunger
and hardships. é

MM. Wyse, A. Reclus and Soso also studied a projected scheme of canalisation
for this region, having a total length of 78 miles, including a tunnel over 10
miles long. The Atlantic terminus would have been at the port of Acanti, the
first place north of the muddy mouths of the Atrato where vessels can anchor in
clear water. At the other side of the tunnel the cutting was to descend through
the valley of the Tupisa down to the Tuyra estuary, which penetrates far inland,

DARIEN HARBOUR. 835

and communicates with the ocean by the Darien Harbour, one of the largest and
safest in the world. This commodious inlet is continued seawards by the spacious
Gulf of San Miguel. Along the banks of the streams and estuary are a number of
villages— Vavisa, Pinogana, Chepigana—with an aggregate population of about
2,000. In the neighbouring forests grows the pAytelaphas palm, which yields the
vegetable ivory of commerce.

Another interoceanic cutting, proposed by MM. de Gogorza and Lacharme,
who fancied they had here found a pass not more than 180 feet high, would also
have utilised Darien Harbour; but it took a much more southerly course along the

Fig. 155.—Cuprca Bay.
Seale 1 : 180,000.

West of Greenwich

Depths.
Sands exposed at Oto5 5 to 25 95 to 50 50 Fathoms
low water. Fathoms. Fathoms. Fathoms. and upwards.

3 Miles.

upper Tuyra and lower Atrato valleys. Wyse, however, has shown that this
depression hus no existence, and that the Tihule Pass, lowest of the range, is
nearly 540 feet high. The canal, 140 miles long, would have required 22 locks,
a tunnel 2,200 yards in length and much dredging about the Atrato estuary.

All the other schemes of canalisation in this region suffer from the same
inconvenience of having to enter the Atlantic by the Atrato, which is certainly
deep enough for the largest vessels, but which is separated from the sea by muddy
bars. One of the plans, studied by Trautwine in 1852, and again by Porter,
Kennish, Michler, Craven, and other engineers, follows the course of the Truando,

336 MEXICO, CENTRAL AMERICA, WEST INDIES.

a western affluent of the Atrato, crossing the cordillera by two tunnels and
terminating at the little inlet of Paracuchichi.

According to an analogous project suggested by Selfridge, Lull, and Collins,
the canal would ascend the Atrato, the Napipi, and its Doguado affluent, also
crossing the cordillera by locks and a tunnel at an elevation of 650 feet ; thence

Fig. 156.—Tue Raspapura Drvine.
Scale 1 : 750,000.

ie
Lt O fev

(

|
>

10
Sa
No
+

CA
RAT
a

Le
Fe

r\Surueol §. =>

wich

12 Miles.

it would reach the Pacific at Chiri-chiri Bay, an inlet of Cupica Bay, where
extensive silting has already taken place. Another line studied by the same
American engineers reduces the number of locks. Lastly, the so-called Raspadura
Canal, lying farther south, and called also the ‘“ Priest’s Canal,” first mentioned by
Humboldt as an interoceanic highway opened in 1788, is not a canal at all.
A. Reclus even asserts that it has no existence. Anyhow, it is nothing more than
a simple depression about three miles long, standing on the parting line between

ADMINISTRATION OF PANAMA. 337

the little Raspadura affluent of the Atrato and the Rio Perico, which flows
through the San Juan to the Pacific. During the rainy season the cutting is at
times completely flooded, so that boats are able to utilise it in crossing from slope
to slope. But such a casual transit cannot be spoken of as offering a navigable
highway from ocean to ocean ; no serious study has yet been made for a cutting
across the parting-line at this point. From the mouths of the Atrato on the
Atlantic to those of the San Juan on the Pacific the total distance is 220 miles.

ADMINISTRATION,

The province of Panama, which till the year 1885 ranked as one of the con-
federate states of Colombia, is now nothing more than one of the nine departments
of the centralised republic. Its governor, formerly elected by universal suffrage,
is at present directly nominated by the president of Colombia. In its political,
administrative, and judiciary institutions Panama differs in no respect from the
other Colombian departments. It comprises the six subdivisions of David or
Chiriqui, Coclé or Penonomé, Colon, Panama, Los Santos, and Veragua. The
three districts of Balboa, Darien, and the Canal are specially administered.
Panama, the capital, had an estimated population of 15,000 in 1890.

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A se fe
Jah ih

CHAPTER VI.

THE AMERICAN MEDITERRANEAN (GULF OF MEXICO AND CARIBBEAN SEA).

LTHOUGH far more open to the ocean than the Mediterranean
| between Europe and Africa, the inland sea separating the two
American continents is none the less a well-defined marine basin,
presenting a group of phenomena which constitute it a separate
natural region on the surface of the globe. The parting-line
between the inner waters of the New World and the Atlantic Ocean is even more
sharply indicated than might appear at first sight to be the case. Thus the chain
of islands which describes a vast semicircle round the east side of the Caribbean
Sea, as well as those almost closing the entrance to the Gulf of Mexico, rest on a
common submarine bed, whose scarps sink abruptly towards the Atlantic to depths
of over 2,000 fathoms. The Bahamas and Lesser Antilles represent plateaux
rising here and there above the surface between two profound chasms. The only
passages which attain a depth of 500 fathoms between the inner and outer waters
are the Windward Channel, between Cuba and Haiti, and a few openings in the
chain of the Lesser Antilles.

Taken as a whole, the inland sea is divided into two natural basins, whose limits
are indicated by the Yucatan peninsula and theisland of Cuba. To the north-west
lies the Gulf of Mexico, to the south-east the Caribbean Sea, each of which is again
divided into two distinct sections. The Gulf, so remarkable for the regularity of
its contour lines and the uniform level of its bed, presents on its east side an outer
basin of triangular shape comprised between Cuba, the Florida peninsula, and the
Bahama Islands. Similarly, the Caribbean Sea, enclosed south-eastwards by the
deep oval amphitheatre stretching from Jamaica through the Antilles round to the
Venezuelan mainland, develops north-westwards towards the Gulf an extremely
irregular secondary basin between Cuba, Honduras, and Yucatan, a basin of vary-
ing depths, intersected by submarine banks, and presenting several profound
cavities. The main axis of both seas is disposed in the direction from north-west
to south-east between the parallel lines of Central America and the Lesser

Antilles.

PROGRESS oF ExPLORATIONS—SOUNDINGS.

These American waters are amongst the best known on the surface of the globe.
Their systematic exploration began in 1872 on the west side of Florida under the

THE WEST INDIAN WATERS. 339

direction of the American officers attached to the Coast Survey. Howell, Pour-
talés, Alexander Agassiz, Bartlett, Sigsbee, Baird, and others, have studied this
maritime region from every point of view, and their labours are still continued in
constantly-increasing detail. Not only have careful soundings been everywhere
taken, but the most sensitive instruments have been used to determine the varying
temperature at different depths, the course of the upper and lower currents, their
saline properties, thermometric deviations, and soforth. Special attention has been
paid to the marine fauna down to the darkest recesses of the abyss, and thus have

Fig. 157.—Guzr or Mexico.
Scale 1 : 18,500,000.

*Merida

ec:

West of CR

Depths.
0 to 250 250 to 500 500 to 1,000 1,000 to 1,750 1,750 Fathoms
Fathoms. Fathoms. Fathoms. Fathoms. and upwards.

300 Miles.

been made many startling discoveries, which open marvellous vistas into the past
evolution of life on the globe.

The outer basin between Cuba, the Bahamas, and Florida, through which the
Gulf Stream escapes northwards, is comparatively shallow, being almost entirely
occupied by banks, with intervening channels 200 to 300 fathoms deep. South-
eastwards, however, the deeper Old Bahama Channel skirts the north side of Cuba
to a great distance, in several places presenting cavities of over 1,000 fathoms.
At the entrance of the New Bahama Channel, due north of Havana, the soundings
have revealed an abyss of 850 fathoms.

But the circular inner basin of the Gulf is much deeper, the whole of the

340 MEXICO, CENTRAL AMERICA, WEST INDIES.

central part having an average depth of 1,500 fathoms for a space that may be
estimated at nearly one half of the entire area. Towards the centre a vast plain
runs north-east and south-west for nearly 15 miles, at a depth of nearly 2,000
fathoms.

The Yucatan channel between the Gulf and the Caribbean Sea sinks to 1,000
fathoms off the west point of Cuba, but elsewhere it is much shallower. At its
southern entrance, another secondary triangular basin, the “ Yucatan Pit,”
between Cuba, Yucatan, and Honduras, has a nearly uniform depth of 2,250
fathoms, falling in one place to 2,300. But it is limited southwards by the shallow
bank whose crest is indicated by the chain of the Cayman and Misteriosa islets
stretching from Cape Cruz in Cuba westwards towards British Honduras. South

Fig. 158.—CARIBBEAN SEA.
Scale 1 : 3,000,900.

West of Greenwich

Depths.
0 to 100 100 to 1,250 1,250 to 2,500 2,500 Fathoms
Fathoms. Fathoms. Fathoms. and upwards.

60 Miles.

of the Cayman ridge is developed the “ Bartlett Pit,” a much larger basin extend-
ing from the Bay Islands near the Honduras coast for about 950 miles to the
Windward Channel between Cuba and Haiti. Here occurs the greatest depth
yet recorded in the American Mediterranean, a chasm of 3,430 fathoms, 21 miles
south of Great Cayman, terminal crest of a vast sabmarine mountain. No other
example is found in the whole world of such an enormous difference of level
within such a narrow space. The submerged range of the Caymans is skirted on
its south side by a depression with a mean depth of 3,000 fathoms.

South of this depression the Caribbean Sea between Jamaica and Cape Gracias-
à-Dios on the mainland is again half-closed by a submarine ridge rising to the
surface at the Pedro, Rosalind, and Mosquitos banks. About 124 miles south-west

THE WEST INDIAN WATERS. 341

of Jamaica the section thus closed has an extreme depth of over 600 fathoms.
Beyond the Serranilla, Bajo Nuevo, Combey, and a few other cays, the vast expanse
of the Caribbean waters gradually deepens eastwards to abysses of 1,000, 1,500,
2,000, and 2,500 fathoms; north of the Dutch Islands on the Venezuelan coast it
falls even to 2,600 fathoms, but again shoals in the direction of the Bird or Aves
islets.

The islands which form the outer rampart of the Caribbean Sea rise like the
ruined piers of a bridge, between which flow the currents and counter-currents of
the Atlantic waters. Most of the Antilles are connected by submerged sills, none

Fig. 159.—Tne Purrto Rico Abyss.
Scale 1 : 600,000.

LS Domino ==

— —

Virgin 15

West of Greenwich

Depths.
= = = == =| =
9 to 2,000 2,000 to 2,500 2.500 to 3,000 3,000 to 3 500 3,500 to 4,000 4,000 Fathoms
Fathoms. Fathoms. Fathoms. Fathoms. Fathoms. and upwards.

12 Miles.

of which exceed 500 fathoms except the passage between the Virgin Islands and
Sombrero, and the two channels north and south of Martinique. But the sub-
marine bank on which the islands rest falls rapidly towards the Atlantic, where
the 2,000-fathom line is scarcely anywhere more than 20 miles from the insular
groups. The deepest cavity yet revealed in the whole of the Atlantic occurs at a
point due north of Puerto Rico, where the soundings have recorded a depth of
4,560 fathoms.
CATCHMENT Basins.

Of the two great inland basins, the Gulf is about one-sixth smaller and very
much shallower than the Caribbean Sea. Were its level to be suddenly lowered

342 MEXICO, CENTRAL AMERICA, WEST INDIES.

about 100 fathoms, a space of some 200,000 square miles, or more than one-third
of the whole area, would form continuous land with the surrounding shores.

But if account be taken of their respective areas of drainage, the relations
will be reversed, greatly to the advantage of the Gulf. Thus while this inland
sea has an extent of only 615,000 square miles, compared with the 750,000 of the
Caribbean Sea, the catchment basin of the former is about six times more extensive

Fig. 160.—SLOPES DRAINING TO THE AMERICAN MEDITERRANEAN.
Seale 1 : 50,000,000.

SN
CSS
LEK.
LR
SG eel,

{
x

Depths.

= — =
Fluvial basin of the 0 to 2,000 2,000 to 4,000 4,000 Fathoms
American Mediterranean. Fathoms. Fathoms. and upwards.

1,250 Miles.

than that of the latter—2,250,000 and 360,000 square miles respectively. Owing
to the peculiar conformation of the North American continent, with its two outer
escarpments and great central depression, most of its surface waters are discharged
along the line of the meridian, north to the Arctic Océan and Hudson Bay, south
to the Gulf of Mexico, which receives the Mississippi, most copious of all North
American rivers. Thanks to this single affluent, the area of the Gulf catchment

MARINE CURRENTS. 343

basin is at once more than doubled. This basin also comprises all the streams of
the southern states from West Florida to Texas, besides the Rio Grande del Norte
and the rivers of East Mexico and of South Yucatan as far as the Terminos lagoon.

On the other hand the Caribbean Sea receives no contributions except from the
eastern slopes of the comparatively narrow isthmian region, and from the north-
west corner of the South American continent, whence come the Atrato, the
Magdalena and the Zulia.

MARINE CURRENTS.

In the American Mediterranean the tidal currents are profoundly modified by
the insular barriers developed round a great part of its periphery. As in the
Mediterranean of the eastern hemisphere, the difference between high and low
water is very slight, the highest tides in the Gulf near Apalachicola, in Florida,
averaging rather less than 4 feet, and at the harbour of Roatan Island, in the
Caribbean Sea, a little over 5 feet. But the phenomenon presents great irregu-
larities according to the shifting character of the marine and atmospheric currents.
In some places the two semi-diurnal tidal waves are merged in one, and such
discrepancies often occur in bays or inlets lying close together. Thus on the west
coast of Florida the flow lasts six hours, and twelve in Apalachicola Bay on the
opposite side of the peninsula, while it resumes its normal period on the Texan
seaboard.

Both the Gulf and the Caribbean Sea are sufficiently open to admit the regular
flow of the great oceanic streams; but numerous counter-currents and eddies are
caused by the irregular coast-lines. The vast volume of the equatorial stream,
which sets steadily westwards at a mean velocity of from 23 to 3 miles an
hour, and which impinges on the coasts of Brazil, Guiana and the West Indies,
is not entirely deflected northwards, for a considerable portion is still able to
continue its westerly course between the islands. The current penetrating into
the Gulf of Paria, between Trinidad and Venezuela, is strong enough to neutralise
the ebb and give the flow a velocity of nearly 6 miles an hour. Thus are pro-
duced formidable bores, while the conflicting currents churn up the sands and
mud of the bay, giving the water a ruddy tinge for vast spaces. The name of
Boca del Drago, “ Dragon’s Mouth,” given by Columbus to the strait between
the north-west extremity of Trinidad and the Paria peninsula, is confirmed by all
mariners navigating that dangerous passage. North of Trinidad the equatorial
stream flows through the strait of Tobago at a less rapid rate, averaging 14
mile an hour, but sometimes attaining double or treble that speed. Farther north
access is given to the great ocean stream through other passages, and especially
through the channel, over 500 fathoms deep, between St. Lucia and Martinique.

These various branches of the equatorial current, converging in the Caribbean
Sea, lose in velocity what they gain in expansion. Their united waters broaden
out to such an extent northwards that a portion returns to the Atlantic through
Mona Passage between Puerto Rico and St. Domingo. The normal westerly
movement through the Caribbean Sea is estimated at from 10 to 20 cubic miles

344 MEXICO, CENTRAL AMERICA, WEST INDIES.

per day. But the whole basin is not filled by this vast body, which in some places
gives rise to lateral counter-currents and backwaters, as between Colon and Carta-
gena, where the reflux has a velocity of 1 mile an hour.

After passing at an accelerated speed through the Banks Strait, between
Jamaica and the Mosquitos reefs, the main stream is joined by an affluent setting
from the Atlantic through the Windward Channel. Hence an enormous liquid .
mass passes at a velocity of from 2 to 3 miles through the Strait of Yucatan
into the Gulf of Mexico, where it takes the name of the ‘ Gulf Stream.”’

At first it ramifies into two branches, one of which, following the north coast
of Cuba, sets towards Florida Strait, while the other broadens out in the spacious
basin of the Gulf and develops an intricate system of counter-currents. Towards

Fig. 161.—Main Currents OF THE AMERICAN MEDITERRANEAN.
Scale 1 : 45,000,000.

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Chief submarine banks,

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620 Miles.

the centre of this nearly circular sea the waters seem to be in a state of equili-
brium, while at the periphery they move parallel with, but at some distance from,
the surrounding coasts. South of the Mississippi delta the turbid fluid of the
great river is impelled in a straight line eastwards by the blue waters of the Gulf
Stream. Thus a junction is effected of the two branches about the southern
entrance of Florida Strait, through which the whole mass disembogues like a
mighty river in the broad Atlantic. At the narrowest part, between Jupiter
Inlet on the Florida side and Memory Rock in the Bahamas, the streain is con-
tracted to a width of 56 miles, with an extreme depth of 450 fathoms. In this
contracted channel the velocity varies from 2 to 6 miles, the average being
about 3, and the discharge, according to Bartlett, 175 billions of cubic feet
per second, or 15,260 trillions per day.

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WEST INDIAN HURRICANES. 345

Such. proportions are difficult to grasp, for they represent a moving mass equal
to about 300,000 rivers such as the Mississippi. Yet they are still far inferior
to the prodigious volume of relatively tepid water spread over the surface of the
North Atlantic and Arctic Oceans. In fact, the Gulf Stream issuing from Florida
Strait supplies only a small portion of those tepid waters whose influence is felt
as far east as Novaya Zemlia. The main supply comes from that portion of the
equatorial current which is deflected northwards by the barrier of the West India
Islands, and which is joined by the Gulf Stream south of the Bermudas.

ATMOSPHERIC CURRENTS—HURRICANES.

Where they enter the Caribbean Sea the atmospheric have not quite the same
mean direction as the marine currents. These set mainly from south-east to
north-west, whereas the trade winds blow nearly always from the east or north-
east. The deviations occur especially in the neighbourhood of the coasts. The
north-east trade, which on the Venezuelan mainland maintains its normal course,
veers round to the east along the Central American seaboard, and reaches the
shores of Jamaica and Cuba from the south-east. But the greatest disturbance
in the regular aérial system is caused by the sudden squalls from the north, which
sweep from the Polar regions down the Mississippi valley to the Gulf.

The American Mediterranean is also exposed to hurricanes, whose very Carib
name (hurakan, huiranvucan) shows that the European navigators regarded these
atmospheric disturbances as peculiar to the West Indian waters. Their main
direction about coincides with the insular chain of the Lesser Antilles and
Bahamas; but after reaching the extreme convexity of their curvature in the
south-eastern region of the United States, they are deflected north-eastwards,
arriving in a somewhat exhausted state on the European seaboard.

In the West Indian waters their normal direction is merged in that of the
magnetic needle without declination, passing from the Guianas through St.
Vincent and Puerto Rico towards South Carolina, and crossing the Caribbean
Sea in a period varying from two to four days. The parts of the American
Mediterranean most remote from this main axis are also the least exposed to the
fury of the hurricanes. But the oft-repeated statement that Trinidad, the
southern Dutch islands, the mainland and isthmian inlets from Honduras to
Vera Cruz lie beyond the cyclonic zone is not correct, as shown by the wreckage
strewn over the roadsteads of Panama and Colon, and the destruction of Blew-
fields, though these disasters are certainly rare.

The hurricanes are also said to occur only at the end of summer or beginning
of autumn, when the heated surface of South America attracts the cooler and
denser air of the northern continent. But although most frequent in August,
and generally between July and October, such disturbances have also been
recorded at other times. Few years pass without some disaster taking place at
one point or another of the normal storm zone. Houses have been uprooted like
trees, fortresses have been demolished, ships carried far inland, plantations strewn

346 MEXICO, CENTRAL AMERICA, WEST INDIES.

with huge blocks, islands broken into reefs, reefs piled up into islands, The
“ great hurricane ” of October 10, 1786, levelled cities, wrecked fleets, and—

‘ Amid the common woe,
Reconciled the French and English foe’’—

who were preparing to cut each others’ throats.

TEMPERATURE, MARINE FLORA AND Fauna.
Swirling round the West Indian basin, as in a seething cauldron, the inner

waters are necessarily warmer, and, owing to the greater evaporation, also

Fig. 162.—Drrp-Sea TEMPERATURES IN THE ATLANTIC AND West Inpra WATERS.
Scale 1 : 27.600 000.

On
©

AE à 9 Es ;
ie Br) ‘=

of Greenwich

620 Miles.

relatively more saline than those of the open sea. But the contrast in tempera-
ture is observed chiefly at the lower depths, as is also the case in the European
Mediterranean. At depths of 700 or 800 fathoms the Atlantic has a temperature
of about 40° Fahr., which is the same as that of Bartlett’s trough in the Caribbean
Sea at over 3,000 fathoms. But at such a depth in the Atlantic the temperature
descends to 37°, 35°, and even 33° Fahr.

The West Indian waters are remarkable for the extreme abundance of the
species of sargasso known by the name of “tropical grapes.” It drifts for

ee ——<—— fs SS ee à

WEST INDIAN MARINE FAUNA. 347

interminable distances with the ebb and flow, and in certain places, such as the
trough north of Puerto Rico, it covers spaces vast enough to merit the name of
“marine prairies.” This plant is not entirely of pelagic origin, for it grows
also on the rocks of the Antilles and Bahamas and on the reefs of Florida.
But botanists who have explored the Sargasso Sea have been unable to determine
the process of reproduction, which seems to be effected by the continuous growth
of fresh shoots or sprouts, which become detached from the parent stém by the
action of the waves.

Till recently it was supposed that the marine fauna was confined to the
surface or shallow waters, and that the stillness of death reigned in the gloomy

Fig. 163.—Deprostts on THE BED oF THE ATLANTIC AND West Inp1a Waters.
Scale 1 : 45,000,000.

90° West of Greenwich 70° Le à
TITI GZ
= QD /
Globigerine Red clay. Corals, Silicious Earthy deposits, Pteropod
mud. Coralline mud. sinds. tellurian mud. mud.
620 Miles.

recesses of the deep. But the dredgings of the Blake and of other exploring
vessels in depths of over 2,000 fathoms have already increased the number of
crustacean forms from 20 to 150 species grouped under 40 new genera. The
deep waters of Florida, studied by Pourtales, are also found to be extremely rich
in forms resembling the fossils of former geological epochs, and comprising
numerous phosphorescent species. Jn certain places the marine bed is covered
with living organisms, and in the channels of the Lesser Antilles, near Guadeloupe,
and the Saintes, about St. Vincent and Barbadoes, dense forests of pentacrini
undulate on the bottom like aquatic plants on stagnant waters.

The geological character of these marine beds and of the surrounding shores is
far more varied than in the Atlantic Ocean. The muddy deposits in the central

348 MEXICO, CENTRAL AMERICA, WEST INDIES.

parts of the Gulf and of the Caribbean Sea are derived chiefly from the remains of
pteropods, while mineral formations prevail round the seaboard. Silicious sands
also cover the beach in some places, and coralline muds or calcareous formations
surround the reefs and continue far seawards several peninsulas, amongst others
those of Yucatan and Florida.

The coral builders are at work over a vast range, which may be estimated at
one-fourth of the marine surface; to their incessant toil must be attributed the

Fig. 164.—ANEGADA AND THE HORSESHOE REEF.
Scale 1 : 380,000.

SM a5 Fai t6 5
= as = =

== = = Wecke (=

=== ?

0 to 16 16 to 80 80 to 320 320 Feet
Feet. Feet. Feet. and upwards.
6 Miles.

formation of those calcareous plateaux by which the straits are contracted on both
sides, as well as of those rocky ledges which are washed by high tides, and which
are revealed only by sandy dunes, such as the Salt Cay, or by their fringe of
mangroves, such as the Anegada, and its prolongation—the dreaded Horseshoe
reef—connecting it with the Virgin Islands. More than half of the Cuban sea-
board, the various groups of the Bahamas, the eastern members of the Lesser
Antilles, and the Bermudas are all of coralline origin.

sé th dt ie.

WEST INDIAN LAND PLANTS AND ANIMAIS. 349

Lanp FLORA AND Fauna.

The land floras and faunas of the Great and Lesser Antilles are of extreme
interest to naturalists, owing to the endless contrasts and resemblances that they
present from island to island, and to the means thus offered of determining the
original continuity or geological independence of the several groups. The great
diversity of forms in the different islands has been regarded as a proof of long
isolation. Each island has forms peculiar to itself, and if the various types from
the mainland speak of communications through isthmuses at remote epochs, it is
evident that such migrations must date from pre-tertiary times, and that the
postulated West Indian isthmus, if it ever directly connected the northern and
southern continents, has ceased for many ages to offer a free passage to plants
and animals.

The special faunas are most pronounced in the land shells, the Antilles occupy-
ing in this respect a unique position. For these organisms each island may be
said to constitute an independent centre of evolution. Nevertheless, the Great
Antilles as far as the Virgin group must at some remote epoch have been
attached to Mexico, the Lesser Antilles on the one hand to Venezuela, on the
other to the Guianas.

The birds, which, for the most part, easily cross intervening straits, have
spread from island to island over vast spaces. Certain species have even been
wafted by hurricanes across broad marine channels; the pelican appears to have
been first introduced into Guadeloupe in this way in the year 1685.

The West Indies possess fifteen distinct species of the humming-bird, grouped
in eight genera, of which five are unknown on the neighbouring mainland. On
the whole the avifauna seems more related to that of the southern than of the
northern continent, while the reptile order has greater affinities with those of
Central America and Mexico. But some remarkable instances of specialisation
have been observed ; such are an iguana peculiar to Haiti and the islet of Navaza,
and a trigonocephalus confined to St. Lucia, St. Vincent, and Martinique. The
Cuban ant-eaters belong to a group found elsewhere only in Madagascar.

In general the insular faunas and floras belong to the same zone as South
Florida as far as the marshy everglades, but have little affinity with those of
the United States proper. Analogies occur most frequently with Mexico, Honduras
and the other Central American regions. The deep-sea fauna, also, is more akin
to that of the Pacific than of the Atlantic Ocean, proving that before the chalk
period the Central American isthmuses formed a chain of islands with broad
intervening marine channels.

The term Antilles, applied to the West Indian insular world, dates from a
period anterior to the discovery itself. Antilia was one of the islands of the
Gloomy Ocean, figuring on the maps at one time as an archipelago, at another
as continuous land and wandering up and down the seas between the Canaries and
East India. With the progress of discovery Antilia continually retreated more
towards the setting sun, until it was at last identified with the ‘ West Indies”
discovered by Columbus.

350 MEXICO, CENTRAL AMERICA, WEST INDIES.

INHABITANTS.

Like the animal species, the inhabitants of the Antilles at the arrival of
Columbus in 1492 represented immigrants from the three continental regions of
North, Central, and South America. Although these populations have all
disappeared, with the exception of a few half-caste Caribs removed to the Hon-
duras mainland, the accounts of the early Spanish chroniclers, the traditions and
usages of the natives, the little that has been preserved of their languages, have
enabled ethnologists to reconstruct the history of their migrations to some, at least,
of the insular groups.

The present inhabitants are mainly of mixed origin, Europe, Africa, and even
Asia having contributed even more than America to the re-peopling of the
archipelagoes. The Chinese and Hindus are found in almost every island, while
the Africans, numerically the dominant element, have come from every part of
the Dark Continent, introduced as slaves before the abolition of the traffic in human
. flesh. The whites also come from almost every country in Europe. The Casti-
lians and Andalusians, descendants of the first conquerors and settlers, are still
numerous by the side of Catalonians, Basques, Galicians, and other later arrivals
from the Iberian peninsula. English, Scotch, and Irish settlers from the United
Kingdom here meet their kinsmen from the United States. French, Dutchmen,
Danes, are also numerously represented, and to all these European elements must
be added the so-called “engaged,” that is, whites formerly purchased for a
temporary period of servitude, besides the descendants of the buccaneers and
filibusters.

For the three centuries following the discovery the political and social rela-
tions in the West Indies were in a state of chaos. A ruthless spirit of rivalry
prevailed amongst traders, planters, and other adventurers; life and liberty were
at a discount; on the same island neighbouring promontories were occupied by
hostile communities, who went about armed to the teeth, watching each other,
and ever on the look out for an opportunity of falling upon and murdering their
chronic enemies. Trading vessels lay concealed during the day in some secluded
creek behind a curtain of mangrove bush, cautiously venturing on the open seas
at night. Every distant sail was an object of suspicion, for every man’s hand
was raised against his neighbours, and even when the Great Powers were at
peace, hostilities were continued by the filibusters on their own account, and
where they swooped down, nothing was left except smoking ruins and wasted
lands.

Yet the high prices commanded by sugar, coffee, tobacco, and other colonial
produce offering the chance of making rapid fortunes, continually attracted fresh
speculators, ready to risk their lives in a deadly climate, and surrounded by con-
stant perils from war, arson, and lawless raiding. To clear the ground and
cultivate their fields they had no longer the aid of the aborigines, exterminated
during the first years of the conquest; but they kept under the lash gangs of
blacks imported from Africa by the slavers.

INHABITANTS OF WEST INDIA. 851

But out of all this chaos of wars and slavery, of standing feuds and rivalries,
there gradually arose colonies of peaceful populations, whose heterogeneous primi-
tive elements have been merged in a small number of types with well-marked

Fig. 165.—SNaxE-CaTCHER AND CHarcoaz Girt, MARTINIQUE

transitions. The majority are half-breeds, people of colour sprung from the
alliance of European men with negresses from Africa. Between these two distinct
elements a complete fusion has taken place, to such an extent that, of the five

352 MEXICO, CENTRAL AMERICA, WEST INDIES.

million inhabitants of the Antilles, at least three millions belong to the mulatto
element. Yet this mongrel race has sprung up in spite of the severe enactments
promulgated against such miscegenation. In the French Antilles, whites convicted
of being the fathers of coloured children were mulcted in heavy fines, and their
offspring confiscated for the benefit of the hospitals without the option of ransom.
A repetition of the offence involved ear-cropping, and even hamstringing, in case
of repeated attempts at escape.

Notwithstanding the measures taken to prevent combinations and conspiracies
on the part of the slaves, those of San Domingo, who were called in 1790 to
exercise their political rights, felt themselves also strong enough to vindicate their
right to the title of men. After two years of struggle they compelled the home

Fig. 166.—PREPONDERANCE OF THE WHITE AND Buack Races in THE West INDIEs.
Scale 1 : 30,000,000.

Yaitlor S* Dormingo—

Y= DP
= { om
————— |

a as ISIE
DATIRICA — = Puerto Fico: ==

UE
SN \

WN A
NN

rai

LL
Preponderance of the whites. Preponderance of the blacks.

620 Miles.

government to issue the edict cf emancipation which Bonaparte, eight years
afterwards, in vain attempted to revoke. This was the beginning of the new era
for the Antilles, where slavery was eventually abolished in the British colonies
in 1832, in the French islands in 1848. The work of social transformation was
completed in 1886, when the last slave was liberated in Cuba.

Despite the differences of origin, the “Creoles” of the Antilles, that is, all
natives of the islands, whether white or coloured, present certain outward resem-
blances, due to their common environment. They are usually well-made, shapely,
vigorous and active, brave, lively, and quick-witted, but also at times vain-
glorious, untrustworthy, and indolent. A remarkable fact, attested by many
observers, is that the blacks and people of colour have moulded themselves in the
several islands on their former masters, reproducing their good qualities and short-

INHABITANTS OF WEST INDIES, 853

comings. Between the Dutch, English, French, and Spanish negroes the same
contrasts have been observed as between the peoples whose speech they have
adopted, and with whom they have become more and more associated in their
traditions and habits of thought.

As regards their speech, the negro English patois is less harmonious than
the French creole, but it is equally lively and terse. _ Apart from a few simple
expressions, the uninitiated Englishman would never succeed in understanding his
mother-tongue as spoken by the Jamaica or Barbadoes islanders. Of all the local
jargons, the most corrupt is the papamiento of the Venezuelan seaboard, in which
the chief elements are Dutch and Spanish, and which has preserved a few Carib
and Goajir terms.

The West Indies are about three or four times more densely peopled than Mexico
or Central America. They have also developed a much larger foreign trade, esti-
mated at present at a total yearly value of about £27,000,000. The various groups
are connected by numerous lines of steamers, while the larger islands have been
brought into telegraphic communication with the rest of the world by submarine
cables to America and Europe.

In their political distribution the islands do not follow their natural divisions.
The two independent republics of Haiti and St. Domingo occupy the large central
island far removed from the republics of the mainland, and intervening between
the Spanish possessions of Cuba on the west and Puerto Rico on the east. Tothe
share of England have fallen Jamaica and the Caymans on the side of Cuba, the
Bahamas and Bermuda in the open Atlantic, and numerous members of the Lesser
Antilles. A few islands of the same chain belong to France and Denmark, while
those of Holland are partly in this chain, partly in the group contiguous to ihe
Venezuelan coast.

The various political groups will be found tabulated in the Appendix.

CHAPTER VII.
CUBA.

UBA, largest of the Antilles, occupies a central geographical position
between the Gulf of Mexico and the Caribbean Sea. It was the
first extensive stretch of land diseovered by Columbus in the New
World, although with strange obstinacy he persisted in regarding
it as a peninsula of the Old World, like the mysterious Zimpango

of the far East. His account is too vague to determine the spot where he first

landed, more especially as the island of Guinahani, whence he reached Cuba,
remains itself still unidentified.

According to Las Casss and Herrera it was at Baracoa, near the eastern
extremity of the island, that he first beheld “ the fairest lands that the sun shines
on and that the eye has ever seen.” Navarrete thinks that Nipe was the first
Cuban port entered by the caravels of Columbus, while Washington Irving
removes the spot farther west to the port of Nuevitas. But in any case, in 1492,

‘that is, during his first voyage, the navigator coasted a great part of the north-east

side, and in 1494, during his second voyage, he traced the southern shores, with all
their bays and inlets, as far as the present Cortes Bay, not far from the western
extremity of the island. It was here, within 60 miles of the terminal headiand,
that he assembled his crews to appeal to their testimony that Cuba was no island,
but really a part of the mainland. Nevertheless he must have had his doubts, for
he had even recourse to threats, and any expression of opinion contrary to his own
might, in fact, at that time have cost the sceptic the loss of ears or tongue.

Thus Cuba continued, by decree of the admiral, to be an Asiatic peninsula
down to the year 1508, when Ocampo, coasting the north side, reached Cape San
Antonio, and passed round the island through the Yucatan channel. Three years
later, the Spaniards took possession of Cuba, where they founded their first settle-

ment, Baracoa.

The contour-line of the seaboard has been gradually traced by careful maritime
surveys, while the development of the interior, the construction of roads and rail-
ways, have supplied materials for a tolerably correct map of the island. But no
beginning has yet been made with the geodetic measurements needed for the con-
struction of a topographic chart on a level with those of West Europe.

The various names given to the island during the first years of the discovery
—Juana, Fernandina, Santiago, Ave Mar.a, Alfa y Omega—have ail been for-

PHYSICAL FEATURES OF CUBA. 399

gotten, and Cubanacan, the native name of a part of the central region near the
present district of the “ Five Towns,” has survived under the mutilated Spanish
form of Cuba, the Coube of the French buccaneers. Most of the old names of
districts and provinces have also been preserved, and still recall the long-vanished
primitive populations.

PuystcaL FEATURES.

Amongst American islands Cuba presents a unique form, which by Spanish
geographers has often been compared to a “bird’s tongue.” From Maisi Point to

Fig. 167.—La Couse (Cuba) AND THE Mer DE LENTILLE.

JA COVBE “55

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ageurny?

PARTIE-DE-LA-MER DE LENTILLE

Cape San Antonio it describes a curve of 900 miles with a mean breadth of not more
than 60 miles. But the characteristic feature of its geography is the contrast pre-
sented by the coastlands. The eastern section, running from Maisi Point westwards
to Cape Cruz and dominated by the Sierra Maestra, or main insular range, may be
regarded as the fundamental or primitive part of the land ; the western, comprising
all the rest, both north and south, presents a more changing and uncertain
character in its chains of reef, its shallows, islands, and islets.

The primitive seaboard is distinguished by its rectilinear axis, which is con-

356 MEXICO, CENTRAL AMERICA, WEST INDIES.

tinued seawards by the Caymans, the series of the Misteriosa banks, and a sub-
marine ridge between the Bartlett and Yucatan troughs south and north. Even
the Coxcomb Mountains, the backbone of British Honduras, form part of this
western continuation of the Cuban relief. The other sections of the seaboard
nowhere present this rectilinear formation, but on the contrary develop irregular
curves, and in many places they are so fringed with coral reefs and marshy tracts
that it seems almost impossible to trace the true coast line with any certainty

Fig. 168.—Western Drvision oF CuBa.
Scale 1 : 6,009,000.

———— 25°
CoN orenwe—-——
pers i SU Zk

Ju Ssbua Na) Grande e

es 7

38, Cianfuego
uegox

=== AVS TL RC
ie

Sa
SS
— ==

as =
SSS

RDA LEE

West of Greenwich

Depths.
== — un ==
0 to 500 500 to 1,000 1,000 to 2,000 2,000 Fathoms
Fathoms. Fathoms. Fathoms. and upwards.

124 Miles.

Hence Pichardo’s estimate of 2,200 miles as the total length of the periphery can
only be accepted in a general way, apart from the thousand creeks and inlets, and
the outer lines of fringing reefs. On Esteban Pichardo’s large map in twenty-
two sheets, the contour, with all indentations, actually exceeds 6,800 miles.

According to Coello the superficial area is 45,000, and, including the double isle
of Pines and the other islets on both sides, 47,000 square miles. In other words,
Cuba is nearly equal in size to all the rest of the West India islands; it is larger
than Portugal, and nearly one-fourth the size of the mother country.

PHYSICAL FEATURES OF CUBA. 857

Cuba, however, is exceeded in altitude and general relief by San Domingo.
The only well-defined mountain range is the Sierra Maestra, which rises abruptly
above the water’s edge on the south-east coast over against Jamaica. The range
begins at the sharp headland of Cape Cruz, and rises rapidly through a series of
terraces to a height of 3,300 feet in the Ojo del Toro crest. Farther on the chain
culminates in a summit usually called the Pico de Tarquino, perhaps a corruption
of Pico Turquino, or ‘‘ Blue Peak,” which is variously estimated at from 6,900 to

Fig. 169.—Eastern Division or CuBa.
Scale 1 : 6,000,000.

=
Ir VI STAI
oe ——

Fernands.— 9

3, dèWuevitas®
TZ

LA ap
PUERTO-PRINC) PE Uh
ee

West of Greenwich

Depths.
0 to 500 509 fo 1,000 1,000 to 2,000 2,000 Fathoms
Fathoms. Fathoms. Fathoms. and upwards.

— es 124 Miles.

8,400 feet. Here the mountains, falling precipitously seawards, merge inlend in a
broad plateau, whose furrowed slopes incline towards the Rio Cauto valley. But
farther on the chief range, here called the Sierra del Cobre (“Copper Mountains”),
is gradually contracted, and after developing an amphitheatre of low hills round
the city of Santiago, dies out on the marshy banks of the Rio Guantanamo. One
of the peaks in the Sierra del Cobre takes the name of La Gran Piedra (5,200 feet)
from a huge block of conglomerate poised on the summit. The main formation of
the Sierra Maestra consists of diorites and porphyries underlying tertiary rocks,

358 MEXICO, CENTRAL AMERICA, WEST INDIES.

interspersed near Santiago with trachytes and basalts, but with no trace of recent
lavas, scoriæ, pumice, or volcanic craters. Yet in this region of the island earth-
quakes are most frequent and violent.

A transverse depression separates the Sierra Maestra and the plateau on which.
it stands from the rest of the island. The mountains strewn in disorder over the
eastern extremity of Cuba constitute a system quite distinct from the main range,
and far more irregularly disposed. They begin at the very headland of Cape
Maisi, and are carved by the rivers into numerous secondary groups, which in
many places terminate in sharp crests, the so-called cuchillas, or “knives.”

Near the terminal headland rises the superb truncated cone of the Yunque de
Baracoa, some 3,300 feet high. Farther on the mountains are continued in
irregular masses running parallel with the northern seaboard. Here and there
granites crop out above the calcareous deposits by which they were formerly covered,
but they nowhere develop dominating crests. The whole upland system falls gradu-
ally from east to west, and in the middle of the island all eminences have already
disappeared. This part of Cuba, here narrowed to a width of not more than 46
miles, is partly occupied by marshy coastlands, between which stretches a low-lying
plain. Before the construction of the railway connecting both coasts, a érocha,
or track, traversing the forests was regarded as forming the parting-line between
the two halves of the island. During the insurrection which nearly resulted in
the separation of Cuba from Spain, the Government troops had erected a line of
forts along this track in order to close the routes to the western towns and planta-
tions against the rebels holding the eastern uplands.

Beyond this central depression the ground again rises to a moderate elevation,
most of the heights having an altitude of scarcely more than 800 or 1,000 feet.
But their abrupt slopes and deep rocky ravines impart a wild, rugged aspect to
these heights, which are separated by intervening rolling ground. According to
Rodriguez-Ferrer the culminating-point of this central region is the Potrerillo
(2,900 feet), north-west of Trinidad in the district of Cinco Villas, on the south side.
Were the island to subside 300 or 400 feet it would be decomposed into groups
disposed like the chain of the Bahamas, one of the largest of which would be that
dominated by the heights lying west of the central depression of the Cinco Villas.

In the western region between Matanzas and Havana the uplands nearer the
north coast culminate in the Pan de Matanzas (1,300 feet), while west of Havana
the Cordillera de los Organos rises in the Pan de Guajaibon to a height of about
2,000 feet. This extreme western range projects its last headland to the north
of Guadiana Bay, beyond which a low peninsula of sandy dumes, swamps and
brushwood terminates in Cape San Antonio on the east side of Yucatan channel.

The whole of this western part of Cuba usually takes the name of Vuelta de
Abajo, or the Leeward region. Hence the extreme eastern section cf the island,
directly exposed to the trade wind, should take the corresponding designation of
Vuelta de Arriba, or Windward region. But this term is applied not to the eastern
but to the central districts, which, relatively to the inhabitants of Havana, already
le to windward.

RIVERS OF CUBA. 359

Except on the uplands Cuba mainly consists of calcareous rocks, which appear
to have been deposited in the same way as the present fringing reefs have been
formed, presenting the same irregularities, the same fractures and deep cavities.
So numerous are the underground galleries that the whole island may be said to
form a vast vault, beneath which the waters are collected either in streams or
stagnant reservoirs. Explorers have penetrated for leagues into the labyrinthine
passages of many caves without reaching the end, and every year fresh discoveries
are made. In many places rivulets are seen to plunge into chasms, reappearing
farther on as more copious streams swollen by subterranean affluents.

In the Vuelta de Abajo a river near Pinar del Rio passes under a superb arch-
way like that of the bridgeat Arc. Elsewhere the running waters flow in narrow
gulches, where the overharging walls here and there meet overhead. The best-
known caverns are those of Monte Libano (“Mount Lebanon’’) in the eastern
peninsula north of Guantanamo, Near Cape Maisi, at the eastern extremity of
the island, there is also a famous grotto, in which animal remains have been
discovered.

Rivers.

Although mostly short and with narrow catchment basins, the Cuban streams
are generally copious. The Cauto, which is the largest, flows through the longi-
tudinal vailey along the north slope of the Sierra Maestra, where it collects
numerous affluents on both sides. From the Sierra del Cobre to Manzanillo Bay
it has a total length of about 139 miles, nearly half of which is navigable for
small craft ; vessels of 50 tons ascend as far as the village of Cauto, the ‘“ Embar-
eadero,”’ as itis called. In its lower course the mainstream ramifies into two
branches, and during the floods into several secondary channels intersecting the
low-lying, themselves the creation of the river.

The alluvia have even encroached on the sea in a long marshy peninsula,
which divides the bay into two secondary inlets. In the sixteenth century the
bar is said to have been much smaller than at present, and at that time a brisk
trade was carried on in the lower reaches of the river. But in 1616 a great flood
shifted the bar and completely closed the mouth of the Cauto. As many as thirty-
three vessels were suddenly cut off from access to the sea and had to be abandoned
by their crews. Many families, ruined by the cessation of traffic, ultimately
removed to Havana. About the middle of the present century the guns of a man-
of-war stranded by the disaster were fished up from the muddy bed of the Cauto.

The other Cuban rivers, of which the lirgest are the Sagua la Grande and
Sagua la Chica on the north side, are all far inferior in volume to the Cauto.
Several, however, are famous for their cascades, their underground course,
reappearance on the surface, and their estuaries. Some fail to reach the sea,
running out in marshy tracts where the fresh and salt waters are intermingled.
These swampy districts attain their greatest development along the south coast,
where the extensive Cienaga de Zapata (‘Marsh of Zapata’’), south of the Matanzas
uplands, skirts the shore for a distance of 60 miles between the Broa and Cochinos

360 MEXICO, CENTRAL AMERICA, WEST INDIES.

ensenadas (inlets). This vast morass stands nearly at sea-level; but although
almost a dead flat, it presents a great diversity of aspects. In some places the stag-
nant waters are dammed up by sandy strips along the coast ; in others the surface
is concealed by dense mangrove thickets; elsewhere channels without perceptible
current, the remains of former rivers, wind sluggishly amid the sedge; here and
there open sheets of water sparkle in the sun, while others disappear beneath the .
round leaves of water-lilies (nenuphar). In certain districts the ground is firm
enough to support a clump of trees; but most of the surface consists of quagmires
or boggy expanses inaccessible to man or beast. The term savana la mar,
applied to many places on the shores of the Antilles, recalls the primitive aspect of
the savannas now partly flooded by the marine waters.

REEFs AND Cays.

Beyond the coastline the islets and fringing reefs constitute, like the inland
morasses, a transitional zone between land and sea. About half of the Cuban
seaboard is thus marked by a false shore which greatly obstructs the coast naviga-
tion, but which, on the other hand, presents many sheltered expanses once the
outer line of breakers is crossed or turned. All these fringing reefs are of recent
calcareous origin, being the creation of the same coral-builders that may be seen
through the transparent waters still at work on the marine bed, decking rocks
and sands with their graceful and many-coloured tufts of foliage.

The upheaved cliffs, with their cavernous recesses washed by the swirling tide,
represent in the incessant changes of the terrestrial surface the geological epoch
which follows the formation of the inland calcareous rocks with grottoes watered
by “ babbling brooks.” But they are of slower growth than the reefs of Florida
and the Bahamas turned towards the ocean swell, where the polyps thrive better
than on less exposed shores. On the north side of Cuba the growth of the fring-
ing reefs has been slow enough for the coast streams to maintain their estuaries
in the form of lagoons while the calcareous deposits were forming on both sides.
Hence the unusual number of excellent havens developed along the Cuban seaboard.

Some of the cays are large enough to form veritable islands, inhabitable in the
few places where fresh water lodges in the depressions or wells up through the
porous rocks. Thus the Cayo del Sabinal, as well as those of Guajaba, Romano
and Cocos, sepirated by narrow channels, develop an outer coastline over 120
miles in length; the Cayo Romano, largest of these upheaved reefs, has an
estimated area of 180 square miles, and its surface is broken by three hillocks.
Natural salt-pans have been formed along the margin of this and the neighbour-
ing cays; they consist of depressions from 12 to 16 inches deep, separated from
the sea by coral banks, over which the waves are washed in stormy weather.
Then during the hot season these shallow basins are evaporated, leaving a
perfectly crystallised bed of white salt used for curing purposes. The pans
of the Cayo Romano alone might supply far more salt than is needed for the
ordinary consumption of the whole Cuban population.

REEFS AND CAYS OF CUBA. 361

The chain of cays from the Sabinal to the Cocos reefs is so regular and pierced
by such narrow channels that it might be regarded as a long peninsula running
parallel with the mainland. But farther west it is continued by a series of reefs
which are breached by wide openings, and which lie close to the shore, like a
beach in process of formation, and already partly attached to the coast by the
regular spit of Punta Icacos between Cardenas and Matanzas.

Fig. 170.—Carr San ANTONIO AND CORRIENTES Bay.
Scale 1 : 1,300,000.

C7 exe Sot

ÉCPTE SL

ae ca

sls
i

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a
Il

No
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— ; _—$—¥

——>

——————
4 SS

—

West of Greenwich

Depths.
0to5 5 to 50 59 to 500 500 to 1.000 1,000 Fathoms
Fathoms Fathoms. Fathoms. Fathoms. aud upwards.

30 Miles. k

Including the western chain of reefs and cays the outer shoreline has a total
length of over 300 miles. West of Havana other fringing reefs extend for about
140 miles from Bahia Honda to Cape San Antonio. They rest on a coral bed
in shallow water, revealing to passing seafarers a shifting panorama of alge,
madrepores, and banks of shells.

On the south side of Cuba the reefs and islets are even more numerous than

362 MEXICO, CENTRAL AMERICA, WEST INDIES.

on the north coast, but they are far less regular, nor are they disposed parallel
with the shore. Here the coralline structures are spread out to a great distance
from the land, wherever the relatively smooth water is not exposed to the scouring
action of marine currents.

Thus reefs are somewhat rare on the part of the coast washed by the deep
Windward Channel between Cape Maisi and Cape Cruz. They are also absent
along the middle section of the south coast owing to the neighbourhood of the deep
Yucatan passige and to the swirling waters of a lateral current. For the same

Fig. 171.—JARDINILLOS.
Scale 1 : 1,000,000.

oe =
a

Depths. aa
Sands exposed at 0 to 24 23 to 500 500 Fathoms
low water. Fathoms. Fathoms. and upwards.

25 Miles.

reason no coral reefs occur towards the western extremity of the island swept
by the waters of Corrientes Bay, so named from the currents which impinge on
this coast and are thence deflected to Yucatan Channel.

Manzanillo Bay, cn the contrary, is more than half covered with reefs, which
are continued westwards by the so-called Cayos de las Doce Leguas, the ‘‘ Twelve
League cays.” Farther on the Isle of Pines is connected with a labyrinth of
reefs and islets, of which the best known are those of the Jardines Bank and the
Jardinillos, forming a seaward prolongation of the marsh of Zapata. In the

REEFS AND CAYS OF CUBA. 363

Jardines, so named from the verdure-clad islets strewn like “gardens” amid
the blue waters, springs of fresh water bubble up from the deep, flowing probably
in subterranean galleries from the mainland.

The Isla de Pinos (Pinos Island, or Isle of Pines), which les off the south-
west coast of Cuba, is alone more extensive than all the other 1,500 isles and
islets strewn round the Cuban seaboard. It consists in reality of two islands

Fig. 172.—Istz or Pines.
Scale 1 : 900,000.

7 VOI)

——
——————

ine)
no

0 to 3 3 to 16 16 Feet
Feet. Feet. and upwards.
18 Miles,

separated by a tortuous passage, half channel half swamp, which winds at a nearly
uniform width for about 3 miles from west to east. This céenaga, or ‘ marsh,”?
as the Spaniards call it, is a rivière salée (“salt river”) analogous to that of
Guadeloupe. Towards its eastern extremity a few rocky ledges flush with the
water have been utilised to make a camino de piedras (‘stone causeway’) between
the two sections of the island.

364 MEXICO, CENTRAL AMERICA, WEST INDIES.

À great contrast is presented by these sections : that on the north is diversified
with ‘“sierras,” groups of hills, and isolated eminences, one of the summits in
the Sierra de la Cañada rising to a hcight of 1,540 feet; but the southern section
is everywhere low, although the swampy savannas and impassable quagmires are
here and there interrupted by sharp rocks, intersected by fissures and pierced by
seborucos, or pits. This part of the island seems to have been upheaved in
relatively recent times, for even within the historic period various islets on the
coast have been merged in continuous land by the mangrove thickets spreading
over the intervening straits and shallows.

Similar phenomena have been observed at other points of the Cuban seaboard
where certain banks of dead coral, built by the same polyps that still inhabited
the surrounding waters, stand at present at a height ef over 30 feet above sea.
level. The hills in the neighbourhood of Havana, some of which are over 1,000
feet high, are certainly of coralline origin.

CLIMATE.

The climate of Cuba, which lies entirely within the tropical zone, corresponds
to that of the neighbouring seas, Here the atmospheric phenomena present
great uniformity in their main features, and in this region, at the very source of
the Gulf Stream and of the aérial currents sweeping across the Atlantic to West
Europe, many of the disturbing elements of the north temperate zone may be
conveniently studied.

But even in Cuba itself, which stretches across eleven degrees of the meridian
from the Atlantic towards Yucatan, considerable climatic contrasts have been
observed. Everywhere northern winds prevail, especially in winter, and every-
where the rains are most copious in summer, when the sun passes the zenith.
But as a rule the rains brought by the trade winds are more frequent and heavier
towards the eastern than the western extremity, on the northern than on the
southern seaboard. Hail is rare, though thunderstorms are common enough.
The rainfall is also said to have generally diminished since the destruction of the
forests, which has taken place especially on the central and eastern lowlands,
Moreover the rains, which at Havana nominally exceed 40 inches, appear to have
been retarded, falling regularly in June and July, instead of in April and May as
formerly. Even where there is no actual precipitation the air is always charged
with moisture, usually to an extent of over 85 per cent., and this moisture, favour-
ing the development of minute destructive organisms, renders the preservation
of archives almost impossible in such a climate.

The whole of the island lies within the zone of hurricanes, and here the most
continuous and exact study has been made of these terrible disturbances. The
hurricane of 1846, which levelled nearly 2,000 houses in Havana, which damaged
more than 5,000, sank 235 vessels in the harbour and wrecked 48 others, has
often been referred to as a typical cyclone, though, fortunately, its track was
limited to a space of not more than about 20 miles.

FLORA AND FAUNA OF CUBA.

C9
(on)
Gr

Frora, Fauna.

Cuba, the ‘“ Pearl of the Antilles,” is indebted for this title especially to the
wealth and variety of its flora, in which are represented nearly all the forms
occurring elsewhere in the West Indies and along the Central American seaboard
from the peninsula of Florida to the Orenoco delta. All the large trees of the
Mexican coast, so remarkable for their majestic growth, for the beauty of
their foliage, the splendour and fragrance of their flowers, reappear on the
Cuban seaboard. Over 30 species of palms are here met in association with trees
such as the pine, which would seem so characteristic of the temperate zone, and

Fig. 173.—PLANTATION OF PINEAPPLES.

which gives its name to the “ Pinos” Island, where it is found intermingled with
palms and mahogany. The catalogue of 1876 enumerates altogether 3,350 indige-
nous flowering plants, besides those introduced by Europeans. But many of the
native forms have already disappeared, and the forests are now largely replaced
by plants of low growth, such as the dwarf fan-palm (chamerops), scrub, plantations
of pineapples, and other prickly plants.

Before the discovery the only mammals in Cuba were bats and a few species
of rodents, such as the guaquinaji, which was probably a racoon (procyon lotor).
The manatee, still seen in the Jardinillos cays, was very common on the coast,
as shown by the names of numerous gulfs, bays and beaches. The guaquinaji

366 MEXICO, CENTRAL AMERICA, WEST INDIES.

and two or three other indigenous forms have disappeared, while the domestic
pig and dog, introduced from Europe with the roebuck, have reverted to the
wild state. In Cuba the canine species rapidly develops new varieties, from the
little “ Havana ” lap-dog to the huge bloodhound, till recently employed in captur-
ing runaway slaves.

Most of the Cuban birds belong to the North American fauna, and only one
species of humming-bird is peculiar to the island. The reptiles also have immi-
grated from the neighbouring mainland, though it is remarkable that none of the
local snakesare poisonous. The natives are not a little proud of the fact, and
even assert that venomous species when introduced gradually lose their poison.
The bite of the scorpion also is said to cause only a slight irritation. Land
tortoises abound, and, as elsewhere in the Antilles, the molluscs, of which there
are several hundred species, are for the most part distinct from those of the
continent. One of the curiosities of the Cuban fauna is a ‘“ vegetating bee,”
a species of polistes, which grows a fungus of the c/avaria genus. The pheno-
menon is analogous to that presented by the New Zealand caterpillar, spheria
Roberts’. .

The fossil animals, such as the megalonyx, elephants and hippopotami, found
in the miocene rocks of the United States, have also been discovered in the
Cuban formations of the same epoch. Hence the inference that at that time the
island was connected with the neighbouring mainland, and that the Gulf Stream
must have set in a different direction from its present course.

INHABITANTS.

Cuba has certainly been inhabited from a very remote epoch. Diorite and
serpentine hatchets of the polished stone age have been found, especially in the
neighbourhood of Bayamo in the eastern province. Archæologists have also
explored several of the caneyes, or heaps of human remains, occurring in various
districts. In 1849 Rodriguez-Ferrer picked up on a cay south of Puerto
Principe a human jawbone in a fossil state; later he found in a burial-place
near Cape Muisi some native skulls with artificially-depressed foreheads. This
was a feature common to the human types represented on the Palenque monuments,
and both may possibly have belonged tg the same race.

With the exception of the savage Guanataveis (Guanahatabibes) occupying
the western peninsula near Cape San Antonio, the native populations found in
the island by Columbus certainly spoke the same language as the Yucayos of the
Bahamas and the people of Haiti and Jamaica. But the local names occurring
in Española (San Domingo) were partly of Arowak origin; hence it was con-
cluded that the inhabitants of the Great Antilles were mostly Arowak immigrants
from South America, where they still occupy the Essequibo and Surinam valleys
as well as the Sierra Nevada de Santa Marta uplands.

On the other hand, when Grijalva first coasted Yucatan he was accompanied
by Cuban interpreters who conversed freely with the natives, so that, if not of the

INHABITANTS OF CUBA. 367

same race, they must have had frequent relations with them. The Mayas them-
selves, who claim to have sprung from the sea, regarded the islanders as kinsmen,
and Orozco y Berra has suggested that the Mayas may have passed from Florida
through the Bahamas and Cuba to Yucatan.

But in any case the Mayas greatly resembled the Cibuneyes of Cuba as described
by the historians of the conquest. Both were stoutly built, with broad face and
chest, brown complexion and artificially-depressed forehead; both were also of
equally peaceful disposition and ardent lovers of freedom. Nevertheless, the
Cibuneyes were vastly inferior to the Mayas in general culture. Nowhere in
Cuba have monuments been found comparable to those of Palenque, Uxmal or
Chichen-Itza. A few cairns, graves, and rude carvings on the rocks are all the
remains that can be attributed to the primitive inhabitants. Amongst these
carvings noteworthy are the crude representations of manatees in every respect
resembling those found in the mounds of Ohio, and strongly suggesting a common
origin.

The dwellings, which varied with the different tribes and the rank of the
owners, were usually the so-called barahacs, vast structures of branches, foliage
and reeds large enough to shelter hundreds of persons. They had also broad-
beamed craft, in which they ventured far seawards. They tilied the land and
were skilful fishers, and were even said to have acquired the art of capturing
turtles by means of the pegador fish (echeneis naucrates).

In three years, 1512-15, the interior of the island had been explored, and in
many districts the aborigines had already disappeared. They offered no resis-
tance, but simply perished. The cacique Hatuei alone, who had reached the
eastern part of the island from Haiti, attempted to fight. It was he that, even
under torture, refused to be baptised in order to avoid entering the same heaven as
the “ good”’ Spaniards.

In 1524 the Cuban Indians had already been reduced by two-thirds; some
yielded to their sufferings, others hastened their end by swallowing earth and
gravel, or eating the bitter manioc before being deprived of its poisonous sap.
According to an official report scarcely 4,000 natives had survived till 1532, so
that in twenty-one years nearly the whole race had completely disappeared ; yet the
names of the various tribes and the territories occupied by them have all been care-
fully preserved. In 1554, 60 families of aborigines still wandering over the western
part of the island were confined in a sort of lazaretto at Guanabacoa, near Havana,
but a few fragments of tribes still survived in the uplands of the eastern districts.

Even so late as the year 1847 Rodriguez-Ferrer visited a family of full-blood
Indians which oceupied a valley of the Sierra Maestra near Tiguabo, and which
comprised over a hundred members with children, grandchildren, and great-grand-
children. Several other families in the same district are supposed to be of Indian
origin, though the racial characteristics have been modified by alliances with
blacks and whites. Miscegenation has been even more general than is usually
supposed. Nearly all the women were taken by the Spaniards, and tneir offspring
were regarded as belonging to the dominant race.

368 MEXICO, CENTRAL AMERICA, WEST INDIES.

The negroes imported to replace the exterminated natives increased very
slowly, so that the losses on the plantations had to be incessantly repaired by fresh
consignments, Even in the middle of the present century, despite the con-
ventions signed with Great Britain, despite the laws interdicting the purchase of
blacks under the severest penalties, from 30 to 50 shiploads of bozales, or “raw
negroes,” continued to be yearly smuggled into the island. The total number
thus introduced since the official abolition of the traffic in 1820 is estimated at
about 500,000. This was actually more than the number openly imported during
the 300 previous years (1521—1821), which was estimated by Humboldt at 413,500
and by Zaragoza at no more than 372,000.

The black population did not begin to increase spontaneously till about the
close of the last century. Its growth, however, was then so rapid that in 1817

Fig. 174.—-Porrricaz Divisions or CUBA BEFORE THE SPANISH CONQUEST.
Scale 1 : 12,000,000

West of Greenwich

1. Guanahacabibes. 6. Macorijes. 11. Magon. 16. Boyuca. 21. Bayamo. 26. Sagua.

2. Guaniguanico. 7. Cubanacan. 12. Ornofai. 17. Cueiba. 22. Malye. 27. Macaca.

3. Marien. 6. Hanamana. 13. Camaguei. 18. Maniabon. 23. Maguanes. 28. Bayaquitiri.

4. Habana. 9. Jagua. 14. Guaimaros. 19. Bani. 24. Guai-Maya. 29. Maisi.

5. Sabana 10.Guamuhaya. 15,Cayaguayo. 20. Guacanayabo. 25. Barajagua. 30. Baracoa.
245 Miles.

the coloured already outnumbered the white population. But the definite sup-
pression of the slave trade, followed by the war of secession and the abolition
of slavery in the United States, led ultimately to a similar measure in Cuba.
During the insurrection in the eastern districts the revolted planters themselves
emancipated and armed their slaves against the Spanish troops, and the gradual
extinction of slavery was officially decreed in 1880. Absolute emancipation
was proclaimed seven years later, when not more than 25,000 slaves remained to
be enfranchised.

But the change was more apparent than real; the blacks continued in a state
of virtual servitude, in which wages were merely substituted for board and lodg-
ing. In any case slavery in Cuba had always been of a milder form than in the
colonies of other nations. The slaves had been guaranteed the “four rights”

ECONOMIC CONDITION OF CUBA. 369

of free marriage, of seeking a new master at their option, of purchasing their
freedom by labour, and of acquiring property.

With emancipation came the necessity of procuring labour from other sources.
While the English and French planters had recourse mainly to Indian coolies,
those of Cuba applied to Macao and Canton for Chinese hands, “engaged”? for a
term of compulsory labour. But the Asiatics at present in the island are far inferior
to the class introduced about the middle of the century. Very few women ever
accompanied them, and nearly all were condemned to perish without posterity.
The census of 1877 returned 45,800 Chinese in Cuba; 120,000 had been intro-
duced altogether, and over 16,000, or nearly 12 per cent., had died on the passage.
Thousands of Mayas have also been procured from Yucatan.

Cuba and Puerto Rico may be referred to as tropical lands where the white
race has been permanently acclimatised. Cuba alone contains ten times more
whites of Spanish stock than all the British West Indies contain whites of English
stock. Nearly half of the labourers on the sugar plantations and in the sugar
refineries are of Spanish descent—Andalusians, Castilians, Basques, Galicians,
Catalonians and Isleños, that is, Canary Islanders—and all these settlers con-
stitute the class of peasantry called b/ancos de la tierra or goajiros. The Basques and
Catalonians, settled chiefly in the towns, are the most active, energetic and indus-
trious ; to them is largely due the material progress of the island.

Recent PoLiTicAL Events.

Despite the Monroe doctrine, “America for the Americans,” Cuba still
belongs to the descendants of the Spanish conquerors, although all the Spanish
possessions on the mainland have become independent. Yet the island was often
threatened by the English and French buccaneers. Twice Havana was occupied
by British troops, and since the beginning of the present century a rebellious spirit
has been manifested by the natives themselves against the mother-country.

As in Mexico, the Spaniards by birth held the creoles in contempt, and
allowed them no share in the administration. The creoles on their part avenged
themselves by squibs and lampoons, calling the Spaniards ‘“Godos,” or Goths,
meaning barbarians still enslaved by the superstitions of former times. Class
hatred spread even to the women, and while the Godas wore their hair long, the

Cuban dames cut theirs short, whence the name of pelonas, or ‘“croppies,” given
them by the Spaniards.

Despite the prevailing discontent no insurrection broke out at that time, and
the two classes even became suddenly reconciled in 1812 on hearing that the negroes
of the eastern district, near Holguin and Bayamo, had revolted. The planters
of Puerto Principe organised battues against the rebels, who were hounded down
and massacred in the forests, their leader, Aponte, being hanged, with eight of
his associates.

Later, after losing all her possessions on the mainland, Spain granted the

Cubans the right of representation in the Cortes, and afterwards deprived them
57

370 MEXICO, CENTRAL AMERICA, WEST INDIES.

of the privilege. The island was virtually under martial law, and the captain
general was permanently invested with the powers of a commander of a besieged
citadel. But this dictator himself was a mere tool in the hands of a secret power,
the ‘ Casino español,” that is, a combination of the great slave-owners. Thanks to
its wealth, this association easily controlled the legislature, bribed venal governors
and crushed those opposed to its policy, which aimed at the maintenance of the
slave trade and of slavery.

Hence the object of the first insurrection about the middle of the century
was not to abolish slavery, but on the contrary to annex Cuba, the “ Lone Star,”
to the other American “stars,” and add half a million of slaves and the powerful
body of the Cuban planters to the political empire of the Southern States. The
Washington Government, at that time in the hands of the slave party, winked
at or even encouraged the expeditions fitted out in its ports. Nevertheless, they
all failed, and Lopez and his filibusters were unable to hold out for two days at
Cardenas, where they had landed in 1851. A second attempt was equally
unsuccessful, and Lopez was put to the sword, with fifty of his followers.

Still the country remained in a chronic state of revolution, and after Spain’s
indignant refusal to sell the island to the States for £40,000,000, the great
insurrection of 1868 broke out at Yara, in the same eastern district where so many
risings had already taken place. The movement, which this time aimed at the
abolition of slavery, spread from the Sierra Maestra over nearly half the island,
and the #ambi, as the rebels were called, kept the field for ten years. Its sup-
pression cost Spain altogether nearly 100,000 men, and an expenditure of about
the very sum offered by President Buchanan for the purchase of Cuba.

A main object of the revolt was also effected, and in 1880, two years after the
capitulation of the last republican leaders, the Government found itself compelled
to pass a law decreeing the gradual extinction of slavery, while safeguarding the
interests of the great landowners. Cuba is henceforth an integral part of the
monarchy and at present Spain seems less threatened with the loss of her “ pearl”
than she was fifty years ago.

TopoGRAPHY.

The present capital, Habana or Havana, that is, according to Bernal Diaz, the
“‘Savanna,’’ was not the first Spanish settlement, nor does it even occupy the site
where it was originally founded. Coming from Espafiola the conquerors naturally
began by securing a footing in the eastern district, where they made choice of
Baracoa, near Cape Maisi. Then moving westwards they reached the far more
convenient port of Santiago de Cuba, which was afterwards replaced as the capital
by the inland town of Bayamo. The first Havana, lying in the western district
on Broa Bay, east of the present town of Batabano, was the fourth capital, but
it was of difficult access and stood on marshy soil.

Hence in 1519, seven years after the foundation of Baracoa, the centre of
administration was removed to the north coast, where the first buildings were
erected at the mouth of the Chorrera, or “ Ravine,” called also A/nendares, where

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GENERAL VIEW OF HAVANA, TAKEN FROM CASABLANCA.

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TOPOGRAPHY OF CUBA. 371

now stands the Torre de la Chorrera, known as the “ Buccaneers’ Fort.” Then
the rising city was removed farther east to the peninsula separating the sea from
the Carenas basin, the new capital, at first called San Cristobal, gradually taking
the name of the district——Havana.

This site offers many advantages, a vast and perfectly-sheltered harbour easily

Fig. 175.—Cuorrera Tower (‘‘ Buccaneers’ Forr’’), AT THE Moura OF THE ALMENDARES.
g

i \
ih

A
D

defended, and surrounded by highly productive plains, but especially a vitally
important geographical position about the centre of the American Mediterranean
and at the very source of the Gulf Stream, that is to say, the natural starting-point
of the highway between the Antilles and West Europe. Hence its title of Llave
del Nuevo Mundo, “ Key of the New World,” indicated by a key in the city arms.

Havana, by far the first city in the Antilles, occupies a peninsula running

372 MEXICO, CENTRAL AMERICA, WEST INDIES.

west and east and terminating in the Morro headland, which commands the
entrance to the harbour, scarcely 370 yards wide at its narrowest part. On the
opposite side of the channel rise the strongly-fortified Cabanas hills, whose guns
produce a cross fire with those of Fort Principe commanding the city on the
west side, and with other military works round the harbour.

Beyond the peninsula new quarters have sprung up westwards, while the
ever-growing suburbs are gradually covering all the encircling heights, The
population already exceeds a quarter of a million, or about one-sixth of that of
the whole island. But although the general effect of the picture is pleasing for
its brightness and animation, there is nothing very imposing either in the aspect
of the place or in the character or grouping of its public buildings. The houses,
mostly low, are painted in vivid green, sky blue, pink or yellow colours; the open
spaces are relieved with clumps of palms, while the various quarters are separated
by broad leafy avenues, Conspicuous amongst the public monuments are the
university, Government palaces and several churches, including the cathedral,
which, like Santo Domingo, claims to possess the remains of Columbus. Thus the
great navigator has two resting-places, as he has had several native towns.

Till recently Havana was badly supplied with water, hence was generally
unhealthy and frequently ravaged by epidemics, although visited in winter by
thousands of invalids from the States. The public fountains were fed by a stream
derived from the Rio Almendares, which, after tumbling over a series of pictu-
resque cascades on the west side, winds round Fort Principe through a pleasant
valley to the sea. Now the city is supplied by an aqueduct which taps the Rio
Vento, an upper affluent of the Almendares, and which yields over 5,000,000 cubic
feet daily to the reservoirs 120 feet above the highest quarters.

The harbour, although partly made a receptacle for the sewage, is still
one of the finest in the world, with several square miles of good anchorage, and
accommodation for a thousand vessels. The foreign trade, averaging £8,000,000
yearly, is chiefly carried on by American steamers, which here ship coffee, sugar
and tobacco, the three staple exports of the island. This agricultural produce
is brought down from the rural districts by three main lines of railway, which
also serve to distribute the foreign wares over the western and central parts of the
island. Havana is connected by submarine cables with the United States by Key
West and with Mexico and Central America by Vera Cruz.

A few ports presenting a remarkable analogy in their formation follow along
the coast west of Havana. Such are Mariel, Cabanas and Buhia Honda, all,
however, inferior in size to Guanajay and Pinar del Rio, the largest inland towns
in the Vuelta de Abajo, or western extremity of the island. Guanajay is sur-
rounded by coffee plantations, while the Pinar del Rio district yields the finest
tobacco in the whole world. The mineral waters of San Dicgo, in the Organos
Hills north-east of Pinar, are much frequented in summer.

South and south-east of Havana are several flourishing places, the largest of
which is Guanabacoa, crowning a hill which commands a fine panoramic view of
the capital, its roadstead and environs. Guines, the chief agricultural centre south

Scale, 1: 14,000.

HA AA

GENERAL VIEW OF MATANZAS.

TOPOGRAPHY OF CUBA. 373

of the capital, lies about midway between that place and the little port of Batabano
on the south coast over against the Isle of Pines. Tnis island itself remained
uninhabited till the last years of the eighteenth century ; here a military station was
founded in 1828 to guard the approaches to Havana from the south side.

Matanzas, the second city and seaport of Cuba, occupies a position analogous to
that of the capital, on a deep inlet of the north coast. Its present name, meaning
the “ Butcheries,” replaces its official title of San Carlos Alcazar, and recalls a
massacre of the aborigines during the early days of the conquest. But the town
itself dates only from the year 1693, when it was founded at the Yucayo headland
at the extremity of the bay between the Rios Yumuri and San Juan. But the
city has spread far beyond that headland, and the left bank of the Yumuri is occu-

Fig. 176.—Cupan Srarorts West or Havana.
Scale 1: 640.000.

SS Sn
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Depths
0 tod 5 to 250 250 Fathoms
Fathoms. Fathoms. and upwards.

12 Miles.

pied by the pleasant suburb of Versalles (Versailles), while the industrial quarters
of Pueblo Nuevo extend eastwards beyond the San Juan.

The region stretching south and east of Matanzas towards Cardenas is the
mast fertile in Cuba, and here are situated all the most important sugar mills and
refineries. Hence Matanzas, the natural outlet for the produce of this district,
has developed a large export trade, especially with the United States. Unfortu-
nately the harbour has become so obstructed by siltings and sediment from the
rivers that vessels of heavy draught have to ride at anchor in the roadstead.
The caverns at the foot of the neighbouring limestone cliffs have been converted
into delightful bathing-places, protected by gratings from the sharks.

Cardenas, founded in 1828 on the. coast east of Matanzas, has also become a
thriving seaport, doing a large export trade in sugar and molasses. It lies on a
spacious bay sheltered from the north-west winds by the long promontory of
Punta Icacos. Like Matanzas, Cardenas is connected with the Cuban railway

374 à MEXICO, CENTRAL AMERICA, WEST INDIES.

system, and by regular steamers with all the coast towns. In the interior the
chief centre of the sugar industry is Colon, formerly called Nueva Bermeja.

Beyond these districts life and industry are shifted from the northern to the
southern seaboard, although the region kad remained almost deserted for 300
years. Cienfuegos, so named in honour of a Cuban governor, is a modern place
situated on a magnificent harbour, which had already been visited by Columbus
and thoroughly surveyed by Ocampo in 1508. Herrera speaks of this haven as
“unrivalled in the world,” yet the town dates only from 1819, when it was
founded by the Louisiana planter, Louis Clouet, with some forty families from
Béarn, Gascony, the Basque country and refugees from San Domingo.

The harbour, 26 square miles in extent, though not the largest, is considered

Fig. 177.—Maranzas.
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the best in Cuba. The trade has increased rapidly, and it is now the chief outlet
for the produce of the district of Cinco Villas (“Five Towns”), which have
become ‘‘six” since the foundation of Cienfuegos. It is now the second sea-
port in the island, having far outstripped Trinidad, which has no less than three
harbours and an excellent roadstead farther east on the same coast. The Mani-
caragua plain between the two towns grows an exquisite tobacco scarecly inferior
to the finest brands in the Vuelta de Abajo.

Trinidad, one of the oldest of the original “ Five Cities,” dates from the first
years of the conquest, when were also founded Santo Spiritu (Sancti Spiritu) in
the interior, and San Juan de los Remedios, called also Cayos because the first

TOPOGRAPHY OF CUBA, 975

settlements had been made on a cay on the north coast. But the incursions of
the French and English buccaneers drove the inhabitants to take refuge farther
inland, where they founded Santa Clara (Villa Clara) in 1690. Lastly, a fifth
city, Sagua la Grande, on the river of like name some 12 miles from the sea,
gradually replaced a group of huts at the head of the fluvial navigation. In this
district of the Cinco Villas are found the auriferous sands worked by the first
settlers; they are now nearly exhausted.

Fig. 178.—TrINIDAD AND 178 HARBOURS.
Scale 1 : 250,000.

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The provinces of Santa Clara and Puerto Principe are separated by the Moron
depression, where the two sections of the island are, so to say, soldered together.
Camaguey, capital of Puerto Principe, and the chief place in the central region of
Cuba, claims to be the most creole (“ criolisima”’) of Cuban towns. The Cama-
gueyanos, as the natives are fond of calling themselves, are certainly the finest,
the most valiant, and independent people in the island. Puerto Principe, the
official name of Camaguey, is the largest city of the interior, for, despite its name,
it lies, not on the sea, but on an extensive plain about midway between the

376 MEXICO, CENTRAL AMERICA, WEST INDIES.

north and south coasts. Its outlet is the vast basin of Nwevitas on the north side,
which was visited by Columbus in 1492, and to which he gave the name of Puerto
Principe, afterwards transferred to the inland city.

Fig. 179.—Crntrat Istomus or Cusa.
Scale 1 : 1,500,000.

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18 Miles.

The harbour of Nuevitas is perfectly sheltered by the promontories of the
mainland and by the Sabinai Cay; it is no less than 60 square miles in extent,
but studded with reefs and of difficult access, its narrow winding seaward channel
being exposed to the full fury of the trade winds.

GENERAL VIEW OF SANTIAGO, CUBA.

TOPOGRAPHY OF CUBA. 977

In the basin of the Cauto the de place is Bayamo, which was founded on a
southern affluent of the main stream during the first years of the conquest. It
was at Yara, a little south-west of this place, that the great republican rising took
place in 1868. Next year, when the Spanish troops made their appearance, the
inhabitants themselves set fire to their houses. Holguin, Las Tunas (“the
Nopals”’), Guaimaro, and all the other towns of this region, were taken and re-
taken during the war, and it was at Guaimaro that the federal republic and the
emancipation of the slaves were proclaimed in 1869. Most of the plantations
were ruined, and the whole country was wasted and depopulated, so that the
western and eastern sections of the island became separated by an intervening
manigua, or wilderness.

But many of the towns have already been rebuilt, and much of the land
has again been cleared. The port of Manzanillo, south of the Cauto delta, is the
natural outlet of the whole region; since the restoration of peace it continues to do
an increasing trade in tobacco, sugar, wax, honey, and other agricultural produce.

Santiago de Cuba, or simply Cuba, is the capital of the eastern department, as
well as its largest city and most flourishing seaport. It stands on one of these
admirable havens on the Cuban seaboard which communicate with the sea through
narrow passages in the fringing reefs. At its narrowest part the Santiago
passage is only 180 yards wide, but it gives access to a magnificent basin, disposed
in secondary creeks and inlets large enough to accommodate all the shipping of
the island. The city, which is defended by strong fortifications, lies in a circular
cove at the north-east extremity of the basin, where its houses rise in tiers on the
slopes of the encircling hills. Its many-coloured structures, its promenades,
gardens, and superb prospects over the neighbouring uplands, make Santiago one
of the most marvellous cities in the Antilles. But the oppressive heat and
insalubrity of the stagnant atmosphere, pent up between the surrounding moun-
tains, have diverted much of its traffic, and Santiago now ranks only as the third
seaport of Cuba.

Moreover, the steep cliffs of the Sierra Maestra, separating the city from the
rest of the island, greatly impede communication with the interior. Hence,
Santiago has not yet been connected with the general railway system, and has
only a few local lines, amongst others, one running from the little port of Judian,
on the opposite side of the harbour, to the town of Cobre, a noted place of
pilgrimage and centre of the copper-mines in the Sierra Maestra.

In this monotonous region is also situated the ancient Indian village of Caney,
or the “Grave,” round which the wealthy merchants have built their country
seats. The neighbouring iron-mines of Jwragua are actively worked by their
owners, a community of miners from Pennsylvania. The most productive, which
employ 1,200 hands, lie 16 miles east of Santiago, with which they are connected
by rail.

Santiago is a telegraphic centre, whence radiate the submarine cables for the
western department and Mexico, for Jamaica, South America, Haiti, Puerto Rico,
and the Lesser Antilles.

378 MEXICO, CENTRAL AMERICA, WEST INDIES.

Midway between Santiago and Cape Maisi, the south-east coast is indented by
the still larger basin of Guantanamo, which, however, is almost useless for trading
purposes. It has been gradually obstructed by the alluvial matter of several

Fig. 180.—Santraco DE CuBa.
Scale 1 : 70,000.

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Depths.
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2 Miles.

streams, one of which is navigable for small craft as far as the towns of Saltadero
and Santa Catalina.

Baracoa, near the eastern extremity, was the first Spanish settlement in Cuba,
and here are still seen the ruins of Diego Velasquez’ house. It was the Puerto
Sante visited by Columbus, but it never prospered, owing to its remoteness from

ECONOMIC CONDITION OF CUBA, 379

the central districts, its damp unhealthy climate, and the exposed position of
the channel giving access to its harbour. At present some trade is done in
bananas, cocoanuts, and other tropical fruits with the United States. One of
the most romantic roads in Cuba connects Baracoa with Santiago across the rugged
crests of the Cuchillas range.

Economic Conpirion oF CuBA.

Despite revolutions, wars, and epidemics, the population of Cuba has increased

Fig. 181.—Port or GUANTANAMO.
Scale 1 : 320,000.

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6 Miles.

at least sixfold since the beginning of the last century. Enforced immigration
of whites, negroes, Chinese, and Mayas has ceased, and free immigration is now
encouraged by grants of land. But independently of this movement, there is a
considerable natural increase by the excess of births over deaths. In time of
peace, the annual increase may be estimated at from 15,000 to 20,000, a rate

380 MEXICO, CENTRAL AMERICA, WEST INDIES.

according to which the whole population might be doubled in fifty years. It rose
from 600,000 in 1811 and 1,000,000 in 1841 to 1,521,000 in 1887 (last census),
and may now (1891) be estimated at 1,600,000.

Under the old régime of absolute monopolies Cuba remained stationary, and
the first impulse to her subsequent prosperity was given by the British occupation
of the island in 1805. In ten months the hitherto-deserted port of Havana was
visited by over a thousand vessels, and trade and agriculture advanced by leaps
and bounds. After the restoration the old system was revived, but in 1818 free
trade was definitely established, and the island, instead of being a burden to the
mother country, contributed as much as £6,000,000 a year to her exhausted treasury.

Rather more than a fourth of the land is either under tillage or pastures, and
the total value of the agricultural produce is estimated at about £200,000,000.
The staple produce is sugar, of which Cuba yields about one-fourth of the world’s
crop, valued at £10,000,000 yearly, exclusive of rum and molasses. Some 2,600
square miles altogether are under sugar, and the plantations, mainly held by a
few great landowners, are supplied with the very finest machinery from the
European and American workshops.

In the very first year of the discovery the envoys of Columbus reported the
practice of tobacco-smoking among the natives of Cuba. Since then the practice
has spread over the whole world, while the Cuban leaf has maintained its pre-
eminence. But in its annual production Cuba is surpassed not only by the
United States and the Eastern Archipelago, but even by France and Manila.

Coffee, at one time the first, now ranks as the third colonial product in import-
ance. The island also grows cotton, cereals, manioc, and fruits, but in relatively
smaller quantities; hence rice, wheat, bacon and other provisions have to be imported.

The domestic animals introduced during the first years of the settlement have
here found a favourable environment; but while multiplying they have become
more or less modified. The horse, of Andalusian stock, has lost in size, but gained
in staying power and vitality. Before the insurrection of 1868 this animal was
so numerous, especially in the central and eastern districts, that nobody travelled
on foot ; all the insurgents were mounted, and it was owing to this fact that they
were able to hold out so long. Excellent mules are also bred and employed as
pack animals in all the hilly districts. But the camel, introduced from the Canaries,
failed, chiefly owing to the jigger (puler penetrans), which attacked its feet.

In certain parts of the island, especially in the Baracoa district, the ox is
used both as a pack and saddle animal, as in South Africa. The goat and sheep
have prospered less than the pig and horned cattle, the former losing all its
vivacity, the latter exchanging its fleece for hair.

The land being mainly held by a few large planters, Cuba has developed
scarcely any local industries, so that most manufactured wares are imported.
Hence foreign trade has flourished, and the total annual exchanges are now
estimated at about £16,000,000 or £10 per head of the population. Besides this
foreign traffic, which is carried on chiefly with the United States and Spain, thou-
sands of small craft of less than 50 tons burden are engaged in the coasting trade.

ADMINISTRATION OF CUBA. 381

Railway operations began as early as the year 1837, but were at first restricted
to a few short lines connecting Havana with the surrounding plantations. Even
still a regular system of lines is confined to the western districts, the eastern
parts of the island possessing only the first links of future projects. The “Central
Railway,” which is ultimately to traverse the whole of Cuba from Cape San
Antonio to Cape Maisi, still exists only on paper. On the other hand the telegraph
system already covers the whole island, and is connected by submarine cables with
the rest of the world.

ADMINISTRATION.

The central authority is represented ia Cuba by a governor-general, residing
at Havana, and controlling the land and sea forces. Under his orders is a civil
governor for each of the six provinces. According to the electoral law, voters who

Fig. 182.—Rarzways or CuBa.
Scale 1: 12,000,000.

Grand-Exuma ——

Zong-/sla pd = 325"

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West of Greenwich

Dep‘hs.
0 to 500 590 to 1.000 1,000 to 2,000 2,000 Fathoms
Fathoms. Fathoms. Fathoms. and upwards.

186 Miles.

have been ten years free and pay an annual tax of £5, send to the metropolitan
senate 16 members, 3 for Havana, 2 for each of the provinces of Matanzas, Pinar del
Rio, Puerto Principe, Santa Clara, and Santiago, one for the university and special
schools, and one jointly with Puerto Rico for the various “economic societies.”
The members of the Cortes are returned in the proportion of one for 40,000 inha-
bitants. ach province has also its local assembly, while the municipalities are
administered by councillors varying in number with the population of the comnrune.

Instruction is obligatory for all between six and nine years of age. The army,
including one battalion of blicks, consists of 19,000 men on a peace footing, paid by
the local revenue. About half of the public income is derived from the customs,
25 per cent. being levied on all imported goods. One fifth of the expenditure is
absorbed by the interest of the debt, which amounts (1891) to £38,000,000.

Cuba is divided for administrative purposes into six provinces, tabulated in the
Appendix.

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CHAPTER VIII.

JAMAICA.

ILTHOUGH classed with the Great Antilles, Jamaica is far exceeded
in size both by Cuba and San Domingo. But in respect of popu-
lation the difference is less, the relative density being higher in
the smaller island. Jamaica alone represents nearly one-third of
the collective area of all the British West Indies, and nearly one
half of their population. It has a superficial area of 4,200 miles, 1-10th of Cuba,
with a population (1890) of 635,000, or considerably more than a third of that
of Cuba.

The name of Jamaica might, at first sight, appear to be of European origin, as
if connected with that of Jaime, or “ James.” But there can be no doubt that it
is a native word, its true form being Xaymaca, that is “ Island of Fountains,” or

‘ of torrents,” in the language of the extinct aborigines. When Columbus dis-
covered it in 1494, during his second voyage, he called it Santiago, a term that was
soon forgotten.

The Spaniards settled in the island in the year 1509, when they founded a few
stations, round which the natives grouped their dwellings. These natives had been
reduced without bloodshed under the mild administration of the first governor,
Esquivel. But this beneficent ruler was succeeded by ruthless conquerors, whose
historic rôle was almost exclusively limited to the work of extermination. A
century and a half after the occupation, the whole population had been reduced
to 3,000, free and slaves, of whom one-half were Spaniards. Most of these took
refuge in Cuba in the year 1655, when a fleet despatched by Cromwell against
San Domingo, having been repulsed from that island, indemnified itself by seizing
Jamaica.

The land thus conquered by the English was colonised the next year by
settlers of all kinds drawn from the West Indies, and from the coasts of Scotland
and Ireland. The population rapidly increased, thanks to the privileges granted
to the colonists; and amongst the immigrants came a large number of Jewish
traders. During the next few decades Jamaica became a busy centre of bucca-
neering and of the slave trade. It was at Port Royal that the famous corsair,
Morgan, prepared his expeditions, and the same town was the great mart whence
the slaves imported from Africa were distributed throughout the West Indies and
on the mainland.

JAMAICA. 383

PuystcaL FEATURES.

Taken as a whole Jamaica is an elevated region with a mean altitude fer
greater than that of Cuba. It has scarcely any of those marshy coastlands fringed
with mangroves, or of those outer shore-lines formed by fringing reefs, such as
abound in Cuba. The shore is almost everywhere rockbound, and cliffs occupy
considerable stretches in a total coast-line of about 500 miles.

As in Cuba the highest uplands occur in the eastern part of the island, where
they take the name of the Blue Mountains. To mariners coasting along these
shores the range running about midway between the north and south coasts appears
in the distance nearly always wrapped in a blue haze, not dense enough, however,

Fig. 183.—Hirty REGION 1N West Jamatca.
Scale 1: 520.000.

LS ae E ssanta-Cruz
K = =

West of 77°40

12 Miles.

to veil the crests and valleys, with their varying tints produced by the cultivated
tracts and zones of vegetation. The Cold Ridge, loftiest summit of the rugged
chain, attains an altitude of 7,423 feet according to the careful measurements of
Maxwell Hall.*

West of Catherine Hill (4,460 feet) the main range is broken by a depression,
and the irregular uplands, which farther on rise in ridges, masses or ravined
plateaux, scarcely anywhere exceed 3,300 feet. Collectively they form an intri-
cate labyrinth due to the action of running water, which has excavated deep
channels and levelled the valleys in broad basins or narrow glens. Some of the
amphitheatres thus formed in the region beyond the hills are locally known as

* cockpits.”
* Proc. of the R. Geo. Society, September, 1887.

334 MEXICO, CENTRAL AMERICA, WEST INDIES.

The southern extremity of the island terminates in the Portland Ridge pro-
montory, a crest of slight elevation now connected by a depression with the main-
land, but at one time forming a distinct island. The western extremity of Jamaica
also terminates in a bold promontory 3,500 feet high, which has been named the
“ Dolphin’s Head,” from a fancied resemblance to that cetacean. ‘The whole mass
of which it forms the extreme point is almost completely separated from the rest of
the island by the depression through which flows the Great River.

Although, like the other large West Indian islands, Jamaica has no active
volcanoes, old eruptive matter occurs near Spanish Town on the south side, and
earthquakes are by no means rare. Towards the end of August, 1883, prolonged
rumblings, like the sound of distant thunder, were heard in the Cayman Islands.
It has been suggested that these sounds, which caused great alarm amongst the
natives, were an echo of the terrific eruption of Krakatau, propagated across the
globe from the Sunda Archipelago to the Antilles.

For a distance of about 60 miles east of the Great River the northern slopes of
the hills are formed of calcareous rocks analogous to coralline reefs and pierced by
countless caverns and cavities through which the running waters escape. In many
places the surface of the rocks remains dry at all seasons, however copious be the
rains. This part of Jamaica is like Yucatan, but the resemblance is still greater
to Carniola, owing to the rugged character of the land. There are few regions of
the globe more rich in underground reservoirs and streams which again well up
to the surface all round the verge of the limestone district. Here and there the
subterranean rivers and their branches may be traced by the springs and fountains
in the caves occurring at intervals along their course. The slope of the hidden
watershed is often different from that of the surface. Lakes also are formed
either on the surface or in underground cavities above the rocky sills.

Rivers.

The Black River, which reaches the sea on the south-west coast, comprises in
its basin a large number of underground feeders. It is also the only river in the
island that is navigable for 30 miles by flat-bottomed craft. None of the others
are navigable at all, not even the Dry (Minho), or the Cobre, which are the two
largest. Both water the southern slope of the island, which is the most extensive,
but which receives the least quantity of rain, not being exposed to the moist trade
winds. During the floods the Cobre has occasionally a discharge of 80,000 cubic
feet per second, but its normal volume is only about 360, and at low water not more
than 100 cubic feet. Like the north-western streams, the Cobre has its underground
system of drainage.

CLIMATE, FLORA, Fauna.

The climate o_ Jamaica resembles that of Cuba, presenting the same contrasts
between the northern and southern seaboard, between mountains and plains,
between the leeward and windward quarters. Although somewhat sheltered
from the moist rains by Cuba and San Domingo, it lies fully in the track both of

FLORA AND FAUNA OF JAMAICA. 385

the tropical rains and of the hurricanes. On the north-east slopes of the Blue
Mountains the rainfall has oceasionally exceeded 100 inches, while the plains of
Spanish Town have at times suffered from long droughts.*

In its indigenous flora and fauna Jamaica resembles its two neighbours, Cuba
and San Domingo. A certain number of vegetable species has been introduced
from Africa by the slavers, amongst others the horse bean (canaralia ensiformis),
which, being poisonous and used for incantations, was probably brought by the
negro medicine-men. It is still regarded as a charm against thieves, and the
blacks give it the name of overlook, in the sense of “watch” or “ guard,” and
entrust to it the safe keeping of their cabins and gardens. Another plant, the
‘“ trumpet-tree,” supplies the porous branches from which the negroes make their
koromanti flutes, a kind of hautboy with soft and shrill tones.

Amongst the local animals the writers of the sixteenth century mention the

’

alco, or “dumb dog ” of Cuba, which was probably not a dog, but the procyon
lotor, or North American raccoon. They also speak of several species of small
monkeys inhabiting the woodlands. But the animal in which the early settlers
were most interested was the land crab (cancer ruricola), which is found also in
the other Antilles, but which appears to be everywhere threatened with speedy
extinction. It has the curious habit of living in the mountains, but migrating to
the seashore to deposit its eggs. Towards the end of April or beginning of May
these little crustaceans emerge in myriads from the fissures of the rocks, and
march straight for the coast, preceded by battalions of males to explore or clear
the way. The eggs are laid at the very edge of the surf and buried in the sand ;
as soon as hatched the young crabs set out in countless multitudes for the
mountains, which they reach in interminable processions, although preyed upon
along the line of march by birds, reptiles, ants, and other enemies.

But the greatest scourge of the plantations is the rat, which has increased
in prodigious numbers, despite the constant efforts to exterminate it by poison,
traps, dogs, and even the Guiana toad imported from Martinique. A voracious
ant (formica omnivora) was also introduced from Cuba to war against these
rodents, against which was afterwards let loose the East Indian mungoos (herpestes
griseus). This species of ichneumon in its turn peopled the island in myriads,
preying not only on rats but also on birds and snakes. It even infests the farm-
yard, devouring the poultry and sucking their eggs. Thus from being an ally
the mungoos has become a foe to the peasantry.

INHABITANTS.

Jamaica presents almost as great a contrast as Haiti to the Spanish island of
Cuba, in the African origin of the vast majority of its present inhabitants. In
fact, scarcely any whites are seen except in the towns. When they took possession

* Meteorological conditions of Kingston (nineteen years’ observations) :—Mean temperature, 74°
Fahr.; highest, 92° Fahr.; lowest, 66° Fahr. Mean rainfall, 44 inches; north-east district, 88inches ; the
whole island, 66 inches.

386 MEXICO, CENTRAL AMERICA, WEST INDIES.

of the island the English expelled the old Spanish landowners, but thev kept the
slaves that had not escaped from the plantations, and took active steps to increase
their numbers.

In Jamaica the Bristol and Liverpool traders henceforth possessed a depôt
where they could consign their human freight while awaiting purchasers from
the rest of the Antilles. Bryan Edwards estimates at 2,130,000 the total number .
of blacks imported by the English slavers into the New World, and at 610,000
those landed in Jamaica alone between the years 1680 and 1786. But the traffic
had already begun in 1628, so that from the time of the English conquest down
to the abolition of the slave trade in 1807, Jamaica must have received altogether
nearly a million of blacks, about half of whom may perhaps have been destined
for the plantations of the island itself.

Yet when the abolition of slavery was proclaimed in 1833, only 309,000
remained to be emancipated. This was due to the fact that most of those
imported died out without leaving any posterity, and the stock had to be con-
stantly renewed by fresh supplies from Africa. A great bar to the formation of
family groups was the practice of polygamy, which still continued to prevail
even under the slave system. Down to the beginning of the present century the
black “‘commanders”’ had the right to take from two to four wives according to
their rank in the slave world, so that the number of bachelors was all the greater
amongst ‘the common herd.”

Other African customs were also long preserved. The magicians offered
sacrifices to Tuniu, the evil spirit who sent storms, and thanked Naskiu, the
good deity who took the blacks after death back to their African homes. When
a serious charge was brought against anyone his lips were rubbed with a little
earth from a fresh-dug pit, and this was supposed to act like the poisoned cup
amongst the Congo tribes.

The slaves were subjected to very harsh treatment by the Jamaica planters, and
the laws passed against them were more severe than in the other West Indian
islands. Many of the owners had their initials branded with redhot iron on the
bodies of their human chattel. A negro convicted of having twice beaten a white
was quartered, or burnt over a slow fire, beginning with his feet. Civil rights were
withheld from freedmen till the third generation, or till they had seven-eighths of
white blood. In criminal cases their evidence was not accepted against whites,
and their rights of property or inheritance were strictly limited.

But the neighbourhood of the wooded uplands, with their labyrinthine valleys
and “ cockpits,” offered a refuge to the runaways, who found a sufficient support
by clearing the forests, planting yams, and hunting the wild boar. From the
time of their arrival in the island the English had failed to recover all the fugi-
tives from the Spanish plantations; a few little republics had even been set up in
the forests, and these gradually expanded, especially by the escape of the Kru or
Koromanti, the most indomitable of all the blacks. Their language, mixed with
English elements, even became the current speech amongst the Maroons,* as the

* That is, “wild,” “ savage,’’ a contraction of the Spanish cimarron, from cima =a mountain-top.

INHABITANTS OF JAMAICA. 387

runaways were called. A few words, especially terms of endearment, still survive
of this idiom.

Thanks to their knowledge of the locality, and to the “drum language,” by
which news was rapidly spread from hill to hill, as amongst their Dwalla kindred
of the Cameroons on the West Coast of Africa, frequent communications were kept
up from one end of the island to the other; munitions and other supplies were also
obtained through their secret intercourse with the plantation negroes. Their
bands, confined chiefly to the upper valley of the Dry River, towards the centre
of the island, constantly harassed the planters, who had to barricade their dwell-
ings and keep continually on the watch. Exposed places had to be guarded by
soldiers, and the governor occasionally applied to the mainland for help. Thus
were formed those friendly relations between Great Britain and the Mosquitos
Indians of Nicaragua which were afterwards used as a plea for assuming a protec-
torate over the inhabitants of the seaboard between Yucatan and the Rio San
Juan.

At one time the Jamaica planters were even fain to sue for peace, andin 1759
the little Maroon republics were formally constituted, with their towns, respective
limits, and recognised rights. But in their excessive confidence they also under-
took to construct roads in order to open up the country. In the termsof the treaty
of peace the Maroons were also required, in return for the concession of territory
and political independence, to respect the laws published by the whites, and to
surrender, “alive or dead,” all runaway blacks seeking to escape from the servitude
of the planters. This was a fatal mistake, for the “ republicans” thereby forfeited all
hope of aid from the plantation negroes, when the final strugglecame. The stipu-
lation was faithfully carried out by the Maroons of the free villages, who sent back all
fugitives to their masters, while the planters, gradually enlarging their domains,
narrowed to a corresponding extent the cordon of guarded lines encircling the
African republics.

At last, in 1795, came the inevitable conflict. Two Maroons of Trelawney
Town, convicted of having stolen a pig, were sentenced to be publicly whipped by
the hangman. Great was the indignation of their comrades. ‘You might have
beheaded the thieves,” they exclaimed, “and we should not have raised a protest ;
but you have inflicted a punishment on them reserved for slaves, which is contrary
to the treaty.” They complained at the same time that some of their land had
been appropriated, and chiefs imposed on them whom they had not elected.

Martial law was at once proclaimed throughout the island, and British troops,
aided by a band of allied Maroons, invaded the reserved territory of Trelawney
Town. But the expedition, having been repulsed, was changed to a blockade. Had
the plantation negroes at that juncture revolted, the whites must have met the same
fate as those of Haiti. But the slaves, accustomed to regard the Maroons as for-
midable enemies and accomplices of their masters, never stirred, while the whites,
assisted by 200 bloodhounds they had obtained from Cuba, were still able easily to
maintain the blockade of the revolted territory, and thus reduce the Maroons to
helplessness. ‘

388 MEXICO, CENTRAL AMERICA, WEST INDIES.

After seven months of hopeless resistance they at last capitulated, to the num-
ber of 1,400 on the condition of being spared their lives and lands. But the governor
hastened to violate the convention, and the unfortunate captives were removed to
Nova Scotia, where thousands of their posterity still survive. From Nova Scotia
large numbers were also later transported to Sierra Leone, whence many of their
ancestors had originally been imported.

After the suppression of a general insurrection of the slaves, the abolition of
slavery was decreed in 1833, and this step was followed in 1838 by further
economic changes, which assumed the character of a social revolution. Trading
relations were abruptly diminished with Great Britain and the rest of the world,
and at the same time the number of whites was considerably reduced. This sudden
crisis is easily explained by the prevailing system of land tenure. The Jamaica
planters, grown powerful by their accumulated wealth, had for the most part
returned to England, leaving their estates to be managed by agents. But their
lavish expenditure in the metropolis soon exceeded their income, and their lands
were so deeply mortgaged that they could not be cleared even by the £5,855,000
of public money received in compensation for the enfranchisement of the slaves.
Ruined by their extravagances, they did not fail to attribute their misfortunes to
the abolitionist policy, thus transferring to others the consequences of their own
errors.

Meantime the plantations remained in the hands of agents, who were no longer
provided with the funds necessary to keep them in order. The houses crumbled
to ruins, and the cultivated tracts were speedily invaded by a rank vegetation of
weeds, brushwood and even forest growths. Most of the old white families who
had remained after the emancipation now also emigrated in the wake of the
ruined planters. In 1852 a memorial addressed to the Governor of Jamaica by
eleven residents certified that they were in charge of 123 plantations, partly as
owners, party as agents.

THe WHITES OF JAMAICA.

Since the abolition of slavery, the white population has diminished by one-fourth,
while the number of blacks has been nearly doubled. This result has been mainly
attributed to the climate, which is injurious to the white race and especially to
those of North Europe, and favourable to the development of the African people.
Certainly there is some truth in this assertion, and although numerous cases may
be cited of Englishmen enjoying perfect health in Jamaica during a long life passed
in hard work, the island is, on the whole, unsuitable for British settlers.

Nevertheless the decrease of the white population is chiefly due to the emigra-
tion, especially of the women. The majority of young girls are sent for education
to England, and many of these never return. The white element has altogether
been reduced far more by the economic conditions than by the climate. The most
unhealthy part is the southern peninsula in the basin of the Dry River, and
yellow fever, which confines its ravages almost exclusively to the whites prevails

Fig. 184—VrEwWw TAKEN AT THE NEWOCASTLE SANATORIUM, JAMAICA.

INHAB.iTANTS OF JAMAICA. 389

only on the low-lying coastlands, As in the Mexican state of Vera Cruz, the

scourge rarely ascends to an elevation of over 1,300 or 1,400 feet, and never reaches
altitudes of 2,500 feet.

The so-called “dry colic,” a disorder at one time greatly dreaded, has almost

entirely disappeared. Consumption also carries off fewer victims than in Eng-
land itself; it is even successfully treated in the health resorts of the uplands,
especially in the cinchona forests of Hope Gardens, and on the hills in the New-
castle district, where the garrison troops are encamped at an altitude of 3,820

390 MEXICO, CENTRAL AMERICA, WEST INDIES.

feet. The climate of Mandeville, in the centre of the island, also enjoys a good
reputation.

The decrease of the white and expansion of the black race have coincided with
a radical change in the cultivation of the land. The great sugar plantations,
which numbered 859 in 1805, were reduced to 300 in 1865, and in the same period
the annual export of sugar had fallen from 137,000 to 23,750 hogsheads, while
the coffee crop was reduced in like proportion from 10,000 to 1,350 tons.

Economic CONDITION OF JAMAICA.

But if the great planters have disappeared, their former slaves have in their
turn become landowners, occupying small holdings on the redistributed plantations
where their fathers had worked under the lash. Few of these blacks will now
consent to toil for the whites, even when offered high wages. Most of them have
abandoned the workshops, and content themselves with tilling a bit of ground
near their cabins. During the eight years that followed the emancipation they had
acquired the absolute ownership of over 100,000 acres, and had founded two hun-
dred villages. As if to efface the painful memories of the plantation days, they
have changed their very names, selecting others from the almanack, from history
and mythology. The revolution is complete under the new order of things, and
on the vast domains that still remain the planters now employ coolies imported
from India, with a few hundred Chinese and Mayas from Yucatan. But since
1886 the importation of Asiatics has ceased.

The land was formerly cultivated chiefly to enable a few families to live in
affluence ; at present the soil is tilled mainly to supply the local wants, and in this
respect the people have succeeded perfectly. The chief crops are maize, yams,
bananas, and other fruits, especially oranges. A small export trade is supported by
the cultivation of tobacco, ginger, and coffee. Bee-farming is also carried on in
some places, and cinchona was introduced in 1868 in the Blue Mountains, where
the rising forests are tended by the blacks; the tea shrub thrives in the same district.

The negroes have even begun to grow sugar on their own account, and some
of the old plantations are now parcelled out in as many as thirty little holdings
each with its own wooden mill. Other more enterprising growers have combined
to purchase more costly machinery, and thus increase the yield or improve its
quality. In general the people enjoy a fair degree of comfort, and the native
population increases on an average at the rate of 8,000 a year; in 1888 it rose to
10,000. Hence the case of Jamaica has been badly chosen by those political .
economists who regard the falling off of foreign trade as a proof of internal decay.
The island has, on the contrary, become a centre of culture, especially for the
Central American coastlands from Yucatan to the isthmus of Darien, where
the development of trade and the industries is mainly due to the immigrants
from Jamaica. In this respect the island has had far greater influence in pro-
moting the general progress of the American populations than any other member
of the Antilles.

ECONOMIC CONDITION OF JAMAICA. 391

But although emancipated from forced labour, the negroes of Jamaica have
acquired neither political independence nor social equality, as shown by the san-
guinary conflict that occurred in 1865 between the two races near Morant Bay in
the eastern district. On that occasion eighteen whites were killed and thirty-one

Fig. 185.— Disrrtct or Morant, JAMAICA.
Scale 1 : 390,000.

° NX
AN I

; iss He

\
Ve
\

W
Z

te 0 ~

= = SSSouteia

76°15 West of Greenwich

Depths.
0 to 5 5 to 100 100 Fathoms
Fathoms. Farhoms. and upwards,

9 Miles.

wounded ; but the massacre was avenged with extreme severity, and a subsequent
official inquiry reported that 438 people of colour had been killed, over 600 sen-
tenced to the lash or the bastinado, and a thousand houses delivered to the flames.
According to the commission, the revolt itself, so ruthlessly suppressed, might cer-
tainly have been avoided had the peasantry of the district received the lands to

392 MEXICO, CENTRAL AMERICA, WEST INDIES.

which they were entitled, and been treated with common justice by the local tribu-
nals. Although reduced to an insignificant minority, the white planters still claim
absolute political control over the black populations whom they formerly held in
bondage.

ToPoGRAPHY.

Kingston, capital of Jamaica, lies on the south coast where it is indented by a
large inlet separated from the sea by a long spit of sand. Its low houses, dusty
streets, and dead walls are relieved by extensive gardens which occupy a con-
siderable space at the extremity of a plain commanded on the north by Long

Fig. 186.—Kiyeston anp Port Royat.
Seale 1 : 222,000.

Depths.
AE: == ==
Reefs exposed at 0to5 5 Fathoms
low water. Fathoms. and upwards.

+ Lighthouse.
3 Miles.

Mountain and the Liganee (Liguanea) Hills, whence the city derives its supply of
water. Kingston became the chief harbour of the island in the year 1693, after an
earthquake had destroyed the city of Port Royal, which stood at the extremity of
the “ Palisades,” that is, the sandy spit which develops an irregular crescent south
of the bay.

The disaster was one of the most terrible recorded in the history of under-
ground disturbances. The shock raised the waves mountains high, and hurled
the shipping against the city, which was flooded to the roofs of the houses. Most
of those that escaped were saved by clinging to the wreckage, whence they were
taken on board a frigate that had been landed by a wave on the ruined houses.
Much damage was also done in the interior, where the Cobre river was dammed
up by great landslips, and all the lower course long remained dry. The earthquake

TOPOGRAPHY OF JAMAICA. 398

was followed by malignant fevers, by which the island was ravaged, and whole
districts depopulated.

In 1772 Port Royal was again destroyed, this time by a cyclone, and it also
suffered much from fierce conflagrations. At present it is merely the outer port
of Kingston, the military and naval quarter, while trade and the industries are
centred in the capital. The channel giving access to Kingston Harbour, at the
western extremity of the Palisades, is defended by recently-constructed fortifica-
tions; it has a depth of 26 feet, and a width at its narrowest part of not more
than 55 yards. In the harbour, anchorage is afforded to large vessels in depths of
over 30 feet.

Several lines of steamers connect Kingston with the rest of the Antilles, and
all the trade of Jamaica with Great Britain, Canada, the United States, and other
countries is carried on through this seaport. From Kingston also radiate some
submarine cables, and it is connected with Spanish Town by a railway, which,
beyond that point, ramifies to the north and west of the island.

Spanish Town, which retained the official title of capital down to the year
1869, is the ancient Santiago de la Vega, founded by Diego Colomb in 1525. Its
port, lying to the south-west on an island-studded bay, which is sheltered on the
south side by Portland Ridge, is known by the name of Old Harbour, but is at
present little frequented. The waters of the Cobre river are distributed over
the surrounding plain by irrigation canals with a total length of over 30 miles.

The plains encircling Kingston and Spanish Town are dreary and monotonous ;
in the disafforested parts ; but the neighbouring hills and mountain slopes on the
north are covered with magnificent plantations, parks, and public pleasure-grounds ;
here are also the botanic gardens and forests of acclimatisation whence, in the last
century, more than a hundred useful plants, amongst others the bread-fruit tree,
were distributed over the island and throughout the Antilles. The heights of
Newcastle, which command a view of Kingston plain and harbour, with the long
verdant crescent of the Palisades, are also covered with recent plantations.

Beyond Old Harbour the south coast presents no havens or any accommodation
for shipping except a few dangerous roadsteads, such as those of Black River
Village and Savana-la-Mar. Nor are there any inlets on the west side except the
little creeks of Negril; but on the north-west coast are the safe harbours of Lucea
and Mosquito Bay, followed by Montego, which, though less sheltered, is more
frequented by vessels engaged in the coasting trade. In the last century Montego
was the seaport of the little republic of Zrelawney Town, called also Maroon Town.
Falmouth, lying farther east at the mouth of the Martha Brea river, also does a
brisk trade, although vessels drawing over 12 or 13 feet are unable to cross the
bar.

Sevilla, about the middle of the north coast, over half a mile from the present
little seaport of Santa Ana, formerly Santa Gloria, was the first settlement made
by the Spaniards in Jamaica. Its site is still marked by the ruins of a church.
Beyond it follow Port Maria and Annotta, on the north-east coast, and, farther
east, Port Antonio, the chief mart for bananas in the island. The negroes of this

394 MEXICO, CENTRAL AMERICA, WEST INDIES.

district have for some time been engaged in a lucrative export trade in fruits
with the United States. Horant Town, on the south-east side, near the extreme
eastern headland of Morant Point, also carries on a considerable trade in oranges
and other fruits. The oranges of Jamaica are the most highly appreciated in the
American market. The term Morant, applied to the village, cape, bay, and har-
bour, is of Spanish origin ; it has reference to the long ‘ delay ” to which vessels
coming from the southern part of the island are frequently subject while endea-
vouring to double the extreme headland in the teeth of the regular east winds.

ADMINISTRATION.

For more than 150 years Jamaica enjoyed almost absolute political autonomy ;
that is to say, the planters, masters of their slaves, were also masters of the

Fig 187.—Curer Towns oF Jawatca.
Scale 1: 2,700,000.

Depths.
0 to 100 100 to 500 500 Fathoms
Fathoms. Fathoms. and upwards.

60 Miles.

other inhabitants of the island, “little whites” and emancipated people of
colour. The administration was, in fact, entirely in their hands. But after the
abolition of slavery, the blacks, legally free, but de facto still enslaved, subjected
toa thousand vexations on the part of their former owners, and deprived of all
help from the planters, vainly attempted to take a modest share in the social and
political life of the community. The pretended colonial autonomy of Jamaica was,
in reality, nothing more than the absolute control of the white aristocracy over the
coloured population, and the British Government was at last compelled, under
pressure of public opinion, to put an end to the scandal.

But instead of granting a few rights to the people of colour, it proceeded to

ADMINISTRATION OF JAMAICA. 395

deprive blacks and whites alike of all participation in the administration of their
own affairs. The governor, members of council, and other functionaries were
nominated by the Sovereign, and Jamaica became a Crown Colony.

Since 1884 this political system has been slightly modified. Five members
only of the legislative council are chosen by the central authority, nine being
elected by the people. In each of the fourteen parishes also the white and
coloured electors, who numbered about 27,000 in 1887, elect the councillors
charged with the administration of the local affairs.

Fig. 188.— Cain or tHe Cayman IsLanns.
Scale 1 : 2,200,000.

lacs SOOO — ——

Little Ly 772.

— —————
= =a

Depths.
€ to 1,000 1,000 to 2,000 2,000 to 3,000 3,000 Fathoms
Fathoms. Fathoms. Fathoms. and upwards.

60 Miles.

The church is separated from the state, and the blacks, in opposition to their
old Anglican masters, mostly Episcopalians, have all become Baptists, Methodists
or Presbyterians. Instruction has become general, and in 1890 about one-ninth
of the whole population were attending the primary schools. The army com-
prises a force of over 1,200 men, besides about 1,000 constabulary.

The banks and islets of the Jamaican waters, such as the Morant Cays on
the south-east and the Pedro Cays on the south, are natural dependencies of the
island, visited chiefly by collectors of turtles’ eggs and birds. Political and
administrative dependencies of Jamaica are also the two islets of Cayman Brac
and Little Cayman, together with Grand Cayman, which form a seaward continua-
tion of Cape Cruz and consequently belong geographically to Cuba. They have
a fishing population of about 4,000, and are remarkably salubrious.

7 PA

CHAPTER IX.
SAN DOMINGO (HAITI AND THE DOMINICAN REPUBLIC).

I.—GENERAL SURVEY.

= AN DOMINGO,* if this term be applied to the whole island, is the
second of the Antilles in size and population, but the first iu
altitude, diversity of outline, picturesque prospects and the natural
fertility of its valleys. It is also the only island in the American
Mediterranean which does not depend politically on some European
power. Whether united in a single state, or, as has more frequently been the

case, constituting two distinct republics, both sections of Domingo have hitherto
succeeded in preserving their autonomy.

Had this autonomy been vindicated by a white creole population it would
have ranked in modern history as an event of secondary importance, analogous to
that of the colonies on the mainland, which, according as they felt strong enough,
have successively asserted their independence of the mother countries. But in
this instance the rebels who compelled their former masters to recognise an
accomplished fact were blacks, slaves, and the descendants of slaves, people
formerly regarded by the whites as scarcely belonging to their common humanity.
The independence of Haiti, accomplished in the West Indian world in the midst
of the islands where slavery was still upheld with all its accompanying horrors,
appeared to the planters in the light of an unnatural event. The general feeling
inspired by it amongst the slave-owners, whether French, English, Spaniards,
Dutch, Danes, or Americans, was one of horror.

The very name of Haiti was proscribed on the plantations, as belonging to an
accursed land. Yet there can be no doubt that this example of a black community
enjoying political freedom and self-government, living as freemen after a suc-
cessful revolution, tended indirectly to hasten the day of emancipation in the
surrounding insular groups. The fear of a disaster similar to that which over-
whelmed the San Domingo planters could not fail to bear fruits elsewhere. It
may be admitted that neither of the two republics, frequently exposed to foreign
wars, torn by civil strife, or a prey to personal ambition, has yet succeeded in

* Properly Santo Domingo ; in correct Spanish usage the full form Santo is reserved exclusively for
St. Dominic, founder of the Order of Preachers.

,
Pr.

PHYSICAL FEATURES OF SAN DOMINGO. 397

acquiring a prominent position amongst civilised nations; but in the midst of so
many perils and difficulties, it is something to have survived at all.

The very term Haiti (Hayti), often extended to the whole island, is an indication
of the changes that have taken place since the plantation days. This appellation,
which is said to mean “ Highlands,” in the language of the aborigines, had fallen
into abeyance, like Quisqueya, “Great Land” or ‘ Mother of Lands,” which,
according to Charlevoix, had also served to designate this member of the Great
Antilles. Columbus, who discovered the island in 1492, called it Española, or
“Little Spain ;”’ but this name was gradually replaced by that of the capital, Santo
Domingo, which is now applied in a special sense to the eastern section of the
island. The revival of the old Arawak word, Haiti, by the blacks of the western
section was due to the natural feeling of reaction against the memory of the
hateful days of slavery.*

PuysicaL FEATURES.

Considered in its relations to the other Antilles, San Domingo evidently forms
part of a well-defined geographical region. Continuing the axis of Puerto Rico
the island gradually broadens westwards; in this direction it ramifies into two
branches, which are themselves again prolonged in the same direction, one by the
island of Cuba, the other by Jamaica. The soundings taken in the intervening
waters show that Puerto Rico is, so to say, the root, and San Domingo the stem,
throwing off two western branches or peninsulas towards Cuba and Jamaica.

Submarine beds and even reefs and islets rising above the surface serve to
indicate the physical connection of all the islands across the channels by which
they are now separated. Thus between Puerto Rico and San Domingo the Mona
Strait is nowhere 500 fathoms deep. The Windward Channel between Haiti and
Juba is no doubt deeper; nevertheless, the flooded sill presents the form of a
rampart between two trenches. In the Jamaica passage an analogous structure is
observed between Cape Tiburon and Morant Point.

As regards its general relief, San Domingo forms several distinct orographic
regions. It may be described as composed of longitudinal islands connected by
intermediate plains, so that a subsidence of the land would resolve the whole into
four islands disposed from east to west, but slightly diverging, like the ribs of a
half-open fan. The northern fragment is clearly separated by the great plain
stretching from Samana Bay to Manzanillo Bay. A second and much larger
orographic section is formed by the zone of hilly lands which runs diagonally
across the island from Cape Engaño to St. Nicholas’ Head; the third upland mass
is limited northwards by the River Artibonite, eastwards by the Neyba or Yaqui

* The disuse of Española, Latinised Hispaniola, as the exclusive general term for the whole island
is to be regretted. In the absence of such a general term both San Domingo and Haiti are now
commonly used in this sense; but as these words are also the official designations of the eastern and
western states respectively, much confusion often arises from their twofold meaning. It is as if the
term Britain, or Great Britain, were to become obsolete, and both England and Scotland were to be used
in a general sense for the whole island, while retaining their special meanings as the proper names of the
southern and northern divisions.—Eptror.

398 MEXICO, CENTRAL AMERICA, WEST INDIES.

Chico, and on the south by a chain of lakes; lastly, the fourth segment is formed
by the south-western peninsula and the mountains in which it is rooted.

The northern chain itself consists of two distinct groups very unequal in size.
The Samana peninsula at its eastern extremity, even within quite recent times,
formed a separate island, and at the beginning of the present century a branch of
the Yuna known as the Gran Estero (‘Great Inlet”) still communicated east of
the peninsula with Escocesa Bay. The bed of the sound, although now completely
silted up, might easily be restored and transformed to a navigable canal.

Nevertheless, the northern range of San Domingo begins in the Samana penin-
sula in the abrupt Pilon de Azucar (‘ Sugarloaf 7), about 2,000 feet high, and the

Fig 189.—Monrs-Cristr RANGE AND VEGA Pain.
Scale 1 : 1,250,000.

5 S x
SIN NES ER) jrs DE é A ; y ne
Fy Hey, ' oS noe KE ÉD

West of Greenwich

18 Miles.

neighbouring Monte Diablo rises somewhat higher. Farther west the uplands
develop a coast-range running west-north-west for about 136 miles entirely within
San Domingan territory. This range, which takes the name of Monte Cristi from
the bluff at its western extremity, gradually contracts westward, but increases in
altitude from 1,200 or 1,300 feet to its culminating point, the Diego Campo, 4,000
feet. Farther on the range again falls, and its last crest, the Sella de Caballo, or
“ Horse-saddle ” (3,900 feet), terminates in the table-shaped Monte Cristi, so
named by Columbus, which rises sheer above the sea to a height of 790 feet.
The whole ‘system has its steeper escarpments facing southwards, while its longer
slopes terminate on the north or Atlantic side in limestone cliffs with fringing

Fig. 190.—Virw TAKEN From THE MÔôLe Sr. Nicozas PENINSULA, Hartt.

PHYSICAL FEATURES OF SAN DOMINGO. 399

coral reefs which follow all the windings of the headlands and islets along the
seaboard.

The main range, running from Cape Engaño for 340 miles across the island
westwards to the St. Nicholas Mole, is at first merely a long ravined rid ge, nowhere

TTT
{III

AAA

more than 1,000 feet high. But towards the centre it increases in height and
breadth, after which it ramifies into two branches, one of which runs north-west
in the direction of its prolongation in the island of Cuba, This main axis of the
Haiti orographic system has a mean altitude of over 6,600 feet, while some of its

400 MEXICO, CENTRAL AMERICA, WEST INDIES.

peaks, such as Entre los Rios, Gallo and Jicoma, rise to a height of 9,000 feet, It
was this section of the San Domingan highlands to which the aborigines applied
the name of Cibao, that is. ‘“ Mountain ” in a pre-eminent sense.

But the two culminsting summits lie beyond the axis of the Cibao range.
These are the rugged Pico de Yaqui, often called Rucillo, or “Grey,” from its
cloud-capped crest, and farther south the Loma Tina, neither of which has yet been
ascended. They are both probably about 10,000 feet high, Yaqui, the more central,
being also the loftier of the two. North-westwards the range terminates in the
long promontory of St. Nicholas Mole, so named from its resemblance to an
artificial breakwater.

The group of uplands branching off south-westwards from the Cibao range,
about the centre of the island, are so completely interrupted by the broad basin of
the Rio Neyba or Yaqui that they may be regarded as forming an independent
system. After rising to heights of 6,260 and 7,540 feet in the Loma Paciencia
(Pansa) and Loma Barranca respectively, they fall in the direction of the west,
where they are divided by the running waters into irregular sections. They are
continued south of the Artibonite river in offsboots running parallel with the
Cahos mountains, which dominate the opposite slope of the valley, and which are
connected with the northern range by the Monts Noirs branch. Gonave Island,
in the bay west of Port-au-Prince, forms a chain of hills disposed in the same
general direction as the neighbouring coast-ranges.

The south-west peninsula of Haiti, from Neyba Bay to Cape Tiburon, con-
stituting the fourth mountain system of the island, has its origin within San
Domingan territory, where it develops a huge triangular mass terminating south-
wards at Cape Beata (Petit Mongon) near the islet of like name. This hilly and
densely-wooded region has not yet been visited by scientific explorers. It is
skirted on the north by the Baburuco (Bahuruco) crest, which, after penetrating
into Haiti territory, culminates in the Sierra de la Selle (8,900 feet). One of its
spurs, running north-west towards Port-au-Prince Bay, rises in Prince’s Peak
(Mont Noir) to a height of 5,000 feet.

Beyond a depression near the neck of the peninsula the system again rises to
a considerable altitude, developing the magnificent La Hotte range with Mount la
Hotte (7,400 feet) and terminating in the abrupt headland of Cape Tiburon

2,870 feet). From Neyba Bay to this point the system has a total length of
230 miles.

Rivers, Lakes, Frincinc REErS.

San Domingo is abundantly watered, having a heavier rainfall than the two
western islands, while the limestone caverns where the surface waters disappear
are far rarer than in Jamaica. Every district has its rivulet or river, and the
whole island might be transformed by irrigation into a vast plantation capable of
supporting millions of inhabitants.

The Yaqui peak in the main Cibao range is the chief centre of the hydro-
graphic system. From its slopes descend two rivers, the North or Great Yaqui,

RIVERS OF SAN DOMINGO. 401

largest stream on the north side, and the Neyba, or Yaqui Chico (“ Little
Yaqui’’), the largest on the south side. From the Cibao range also flows a
main branch of the Artibonite (Atibonico of the Indians), largest river on the
west side and in the whole island. After collecting all its affluents from the
uplands this watercourse enters the Haiti territory as a considerable stream,
navigable for small craft for some distance from its mouth.

Fig. 191.—Ozama AND BRUJUELAS Basins.
Scale 1 : 1,600,000.

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Los Llanos

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Depths.
0 to 100 100 Fathoms
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30 Miles.

On the east slope the largest basin is that of the Yuna, which flows to
Samana Bay. The plain traversed by this river belongs to the same depression
as that of the Great Yaqui, the uncertain waterparting between the two basins
being scarcely 680 feet high. This is the magnificent region to which Columbus
gave the name of Vega Real.

Amongst the secondary rivers one of the most copious is the Ozama, which

402 MEXICO, CENTRAL AMERICA, WEST INDIES

collects all its headstreams a short distance above San Domingo, capital of the.

Spanish republic. Its tributary, the Rio Brujuelas (“ Witch River”), appears to
be one of the few underground streams in the island. After flowing on the
surface to within 12 miles of the coast, it suddenly plunges into a chasm, its
course being here arrested by a long cliff skirting the limestone shore. The

tarns scattered over the plain are formed by the rainwater which collects in these .

little closed basins. The whole region stretching east of the capital to the
extremity of the island appears to have been formerly under water.

But elsewhere the only lacustrine basins still surviving are those of the
depression which extends north of the Selle and Baburuco chains, between
Port-au-Prince and Neyba Bays. So level is this plain, which was formerly a

Fig. 192 —Israwus or THE Lares, San Dominco.
Seale 1 : 550,000.

ES. LN BY

West of Greenwich

12 Miles.

marine channel, that no fluvial basin has yet been developed in it, so that the
surface waters find no outlet seawards.

The largest of the flooded depressions stands about the middle of the isthmus
at a height of some 300 feet. Its old Indian name was Xaragua; but the
Spaniards usually call it Enriquillo (“ Littie Henry ”), from a chief who long
held out against the conquerors. He had taken refuge at last in an islet of the
lake, which is now inhabited by wild goats, and hence called Cabritos. The
French negroes call the lake Etang Salé, from its saline water. This closed
basin, formerly a marine inlet, but now cut off by a bar from the ocean, is still
inhabited by sharks and porpoises, and even by caymans, although these
saurians generally avoid saline waters.

The lake is very deep and has an area of 170 square miles. After heavy
rains it occasionally forms a continuous sheet of water with another basin, the
Laguna de Fundo, or Étang Saumache, which forms its north-western extension

——

SS EE CON SNS ee

CLIMATE OF SAN DOMINGO. 403

_towards Port-au-Prince Bay. The united reservoir has then a total length of
about 60 miles, with an average breadth of 9 or 10 miles, and is consequently
larger than the Lake of Geneva. According to Tippenhauer the Étang Saumache,
that is, “Brackish Lagoon,” scarcely deserves its name, for its water is quite
potable with a very slight saline taste. It becomes really brackish, however,
during the temporary inundations of the Étang Salé.

Farther south, in the same depression, but at a soraewhat higher elevation,
stands the freshwater lake, Icotea de Limon, which is fed by torrents from the
Baburuco hills, and probably sends its overflow through underground channels to
Lake Enriquillo. There is still another link in the lacustrine chain, the Rincon,
which communicates with the Yaqui Chico delta, while the depression is con-
tinued to the sea by the so-called ‘“ raques,” that is, muddy and partly-flooded
morasses.

The San Domingo seaboard is in many places fringed with reefs, but on the
whole it is far more accessible than that of Cuba. The coralline structures are
developed chiefly in the interior of the bays, and Samana Bay is thus more than
half filled with reefs. Manzanillo Bay is similarly obstructed, while the Monte
Cristi range is continued far seawards by a vast “garden” of reefs, banks and
islets. The western gulf terminating in Port-au-Prince Bay, has also been
invaded by the coral-builders, and Gonave Island is connected on both sides with
the shore by causeways of reefs pierced by a few open passages. The coast
facing the Ile-à-Vache is also bordered by a labyrinth of corals, and at the
eastern extremity of San Domingo, Saona or Adamanay Island, as well as Cape
Engaño, are surrounded by fringing barriers

CLIMATE, FLora, Fauna.

Resembling that of the neighbouring islands in its main features, the local
climate is distinguished chiefly by the contrasts between uplands and lowlands,
seaboard and interior, windward and leeward aspects. More oceanic in its position
than Cuba and Jamaica, San Domingo is more exposed to the regular north-east
trades, but on the Azua plateau, and in other districts sheltered by the mountain
ranges, the rainfall is very slight, and vegetation is supported chiefly by the
copious morning dews. At Port-au-Prince the mean annual rainfall is 62 inches,
while the temperature ranges from 58° to 97° Fahr.

Hurricanes are rarer than in the Lesser Antilles, and although sight vibra-
tions of the ground are frequent, violent shocks occur only at long intervals.
In 1564 Conception de la Vega was destroyed; in 1751 the rising city of Port-
au-Prince was converted into a heap of ruins, and the same fate overtook Cap-
Haitien in 1842.

Thanks to its more abundant rainfall and greater diversity of aspect, San
Domingo is richer in vegetable forms even than Cuba itself. The interior has
not yet been cleared, and the forests covering the slopes of the mountains for
thousands of square miles contain in abundance such valuable timbers as rose-

404 MEXICO, CENTRAL AMERICA, WEST INDIES.

wood, ironwood, mahogany, satinwood, pines, and oaks. All the tropical fruit
trees have been introduced on the plantations, and the jambosa, imported from
Jamaica in 1791, has almost become a nuisance, growing wild in dense thickets.
Like Cuba, Haiti possesses no venomous snakes; but the cacata, a species of
spider, is much dreaded by the natives. The rivers and lakes are peopled by two
species of saurians, and clouds of aquatic birds hover over Altavela, Beata,
Gonave, and the other coast islands, all rich in guano and phosphate of lime.

INHABITANTS.

At the arrival of the Spaniards the population was probably as dense as at
present. Columbus estimated it at nearly a million; but Las Casas calculated
that as many as three millions had fallen victims to the greedy and ferocious
conquerors.

The island had long been occupied by peoples of various origin; it had its
historic and prehistoric times, its myths and legends referring to an epoch of vast
antiquity. To those remote ages belonged the greenish stone hatchets which
are picked up here and there, and which the black medicine-men use in their
magic rites. The aborigines claimed to have sprung from the soil, and celebrated
the origin of the world in certain caves, several of which are still shown, especially
in the western districts. According to the negroes of the north-west the first
man appeared quite suddenly, accompanied by the sun and moon, at the entrance
of a cave near Dondon, and here the natives formerly came to offer sacrifices to
the divinities of heaven and earth. The figures of turtles, frogs, scorpions,
crocodiles, and other animals carved by the primitive artists on the surface of
the rocks in this cave have already become encrusted with calcareous concretions.
Rudely-carved stones have also been discovered in the mountains of the Cibao
range and in other places.

Nearly all the aborigines, the western Cebuneys akin to the Cubans and the
Arawaks of the centre and east, spoke dialects of a common language, and
resembled each other in their usages. They probably belonged to the same stock,
and occasionally combined to resist their common Carib enemies, who frequently
landed on the east coast, killing and eating the men, and keeping the women as
wives or slaves. Most of the Haitians were of small stature, and their skin was
scarcely darker than that of the Spaniards themselves. They were a peaceful
race, and war seldom broke out between the five kingdoms, the names and limits
of which have been preserved by the chroniclers.

Columbus speaks of these communities in terms which have been seldom
applied to other men. “They love their neighbours as themselves; their speech,
always kindly and soft, was accompanied by smiles.” Yet the very person who
gave them this high praise began their enslavement by stratagem and violence.
His associates and successors surpassed him in cruelty, amusing themselves by
setting their bloodhounds loose against the unhappy natives, who were often torn
to pieces by these ferocious beasts. In vain they revolted, for the war led only

NWN}
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Al
/ Du

TURTLE ISLAND—VIEW TAKEN AT THE MOUTH OF THE THREE RIVERS.

INHABITANTS OF SAN DOMINGO. 405

to more wholesale massacres. In order to hasten the end of their wretched
existence the Haitians themselves are said to have sworn to allow no more births,
thus condemuing the whole race to extinction.

In half a century the people whom the Spaniards were burning to ‘convert
to the true faith ’’ had ceased to exist, or the few survivors had become merged
in other ethnical groups, white or black. About midway between San Domingo
and Samana Bay lies the village of Boya in a wooded upland valley, whither the
last Haitians retired after the almost total extermination of the whole race.
They were left in peace; their chief even obtained the title of don, and called
himself, “ Cacique of the Island Haiti.” But they did not long retain their racial
purity, and at present it is difficult to recognise the half-caste descendants of the
primitive Haitians. What distinguishes them best is their long, lank and very
black hair. But many words of their language were borrowed by the Spaniards,
and thus passed into the other European tongues. Such are potato (patata),
cassava, maize, tobacco, iguana, canoe, cacique, and perhaps hammock (amac).

During the first years of the conquest the Spaniards had been accompanied by
some negroes, and in 1505, African slaves were sold by the Spanish traders to the
San Domingo miners. The trafic was officially recognised in 1517, when a royal
edict authorised the yearly importation of 4,000 blacks from the coast of Africa to
the island of Haiti. The trade was made a monopoly in favour of a chamberlain
of Charles V., who sold it to some Genoan merchants.

But the negroes were far too few to compensate for the extirpated Indians.
Hence many Spanish settlers, having no slaves to work the mines or cultivate the
plantations, hastened in search of fresh adventures, and the marvellous reports
from Mexico and Peru caused the emigration to become general. San Domingo
would have been completely depopulated had not the governor forcibly retained
all the officials still in the island.

The occasion was favourable for the English and French buccaneers, who
raided the unoccupied parts of the island, sweeping away the cattle, horses, and
swine that had multiplied on the savannas. They became strong enough to drive
the Spaniards towards the capital, but as yet they had no fixed stations beyond the
trysting-places where they kept hides and other plunder for sale to passing
vessels.

One of these places was a haven in Tortuga (Turtle) Island, on the strait which
separated this long mountain mass from the mainland. Thinking themselves
strong enough to found a permanent settlement here, they erected some houses
and depots with the aid of the French residents in St. Christopher, and began to
clear the ground for plantations. Driven out by the Spaniards in 1638 and again
in 1654, they took refuge at Petit-Goave on the north side of the south-west penin-
sula, and this place became a chief centre of the trade in tobacco and hides.
Tortuga was retaken by the French in 1659, but the land being nearly exhausted,
most of the settlers withdrew to the mainland, where the fortress of Port-au-Prince
had already been erected.

The French colony was thus definitely established in the western part of the

406 MEXICO, CENTRAL AMERICA, WEST INDIES.

island, where the plantations began gradually to spread. The chief point now
was the introduction of a better class of negroes in the agricultural districts. in
most of the other Antilles the gangs of slaves had to be continually recruited by
fresh purchases, owing to the lack of women. But such was not the case in Haiti,
where the buccaneers, more eager for booty than agricultural work, had from the
first introduced the negresses captured in other islands or on board the slave vessels.
At the census of 1687 the coloured population, about half of the whole, comprised
more women than men, while the community increased normally by the excess of
births over deaths. Although more males were afterwards imported than women,
still the disproportion between the sexes was never so great as in the other West

Fig. 193.—Cuter SLAVE-TRADE ROUTES.
Scale 1 : 150,000,000.

Richmond, x

60° Meridian of Greenwich 0°

3.100 Miles.

Indian islands; and the flourishing state of the indigo and sugar trades during the
eighteenth century enabled the planters to procure the very best “raw material ”
in the slave market. But probably to this very circumstance was due the defeat
and massacre of the white proprietors. The blacks imported as slaves gradually
merged in a vigorous race ripe for independence. The Haitian negroes are still
noted for their size, strength, and muscular development.

At the dawn of the revolution those of the French colony numbered half a
million, owned by rather more than 30,000 whites, while the intermediate class of
mulattos, nearly all freedmen, scarcely exceeded 27,000. In the Spanish part of
the island the whole population was much less, and the two elements far more evenly
balanced. Here the plantations numbered only about 5,500, not half as many as in
the French part, which supplied Europe with more than half of its annual con-
sumption of cotton and sugar.

E“ —

INHABITANTS OF SAN DOMINGO. 407

The revolution, which, at this distance of time, seems like a sudden event,
really took place very gradually, and but for foreign intervention might have
pursued a peaceful course. After 1789, and the shout of freedom echoed beyond
the seas, fifteen years passed before the Haitians proclaimed their independence. At
first they thought only of seizing the land which they tilled, and making them-
selves the political equals of the French planters. Political and social equality
were claimed only by the “petits blancs,” that is, the despised European bour-
geoisie, and by the still more despised mulatto element. But these two classes were
themselves hostile to each other, and conflicts had even broken out between them.

On the other hand the National Assembly, afraid to offend the great planters,
hesitated to act, and in response to the philanthropists clamouring for the aboli-
tion of slavery, limited its action to the electoral law of 1790, in which the right
of the people of colour to vote was not even explicitly recognised. But the
mulattos claimed the right, though their champion, Vincent Ogé, had to take
refuge in Spanish territory, whence he was “extradited”? and broken on the
wheel. The fury of the planters rose toa white heat when, in 1791, the Constituant
Assembly conferred on the half-breeds born of free parents the right of election
to the Colonial assemblies. It was then that the dominant party proclaimed in
most of the parishes their independence of the mother-country. The planters
appealed to England, and their envoys, dressed in British uniforms, were de-
spatched to Jamaica for assistance against France.

But the negroes had already been drawn into the revolutionary movement, and
the war of races was precipitated by the action of the clergy, under whose influence
the slaves, like the peasantry of La Vendée, at first took arms as Royalists (“ Gens
du Roi”). Then the fate of the distant monarchy was soon effaced by the smell of
blood, and on both sides the war rapidly assumed a character of extreme ferocity.
Unassuilable in their upland fastnesses, the blacks slaughtered the whites of the
plains, but only to be slaughtered in their turn whenever, intoxicated by success,
they ventured to approach the fortified towns. Scarcely any prisoners were made,
‘and the captives were often tortured to death. The hostile camps were surrounded
by bodies dangling from the branches of the trees, or by human heads stuck on
every post.

But, in the language of Toussaint-Louverture, the whites were as two or three
light grains lost in a vessel full of black maize, and the massacres told in favour of
the African element. Moreover, the emigration of the whites to Jamaica, Cuba,
Puerto Rico, Spanish Florida, and the United States became a veritable exodus.

On the invitation of the whites and a section of the people of colour, the
English, accompanied by French émigrés, came to take possession of the magnifi-
cent colony offered to them. St. Nicholas, the chief arsenal,.and Port-au-Prince,
the capital, fell into their hands. On the other side the Spaniards, representing
the Bourbon monarchy, had taken into their service the “Gens du Roi,” and
had advanced into French territory. Of the old colony only two or three points
were still held on the north and south coasts, that is, precisely where the bucca-
neers had begun their work of conquest. ,

408 MEXICO, CENTRAL AMERICA, WEST INDIES.

It was then that the commissioner Sonthonax, realising the desperate state
of affairs, proclaimed the emancipation of the slaves, causing the edict to be
ratified by that section of the planters which had refused to betray the mother-
country. This step was followed by the decree of the National Assembly of
February 4th, 1794, recognising equality of rights between all races.

So great was the moral effect that in a few weeks the material position was
completely reversed. On the appeal of Sonthonax, now become “le bon Dieu,”’
a whole army sprang from the ground; the black insurgents fighting in the name
of the Spanish king changed their flag, and voluntarily espoused the cause of the

Fig. 194.—Scene or THE WAR OF INDEPENDENCE.
Seale 1 : 3,250,000.

me
GE E
= FE Z- Croix des Bouquét
£ RE 27 S01 -7——$——— OR EAUEPRIN ES
Wee —— We a

MER i —
EU SANTE eoganee “iy

74° West of Greenwich aks

60 Miles.

French republic. After driving their late allies back to the eastern part of the
island, they successively captured the western towns that had been occupied by
British garrisons. Toussaint Breda, the black general, changed his name to
L’Ouverture, to show that a new era was dawning and a new order of things had
certainly been ushered in. Work was resumed on the plantations, no longer for
the benefit of a few great landowners, but to the profit of thousands of freemen,
and the rural settlements again prospered.

In 1795 the treaty of Basle yielded to France the Spanish part of San
Domingo, and the French republic thus became official mistress of a far larger
colony than that inherited from the monarchy. But the political ties between the
twe countries were ruptured by the action of France herself. The first consul,

INHABITANTS OF SAN DOMINGO. 409

Bonaparte, after overthrowing the republic and restoring the ancien régime under a
new name, attempted to effect a similar work in Haiti.

The blacks at first hesitated, or resisted in a half-hearted way, especially after the
treacherous capture of their leader, Toussaint-Louverture. But the truth gradu-
ally leaked out, and the existence of the decree re-establishing slavery and the slave
trade in the Antilles became known to all, especially after some mulattoes imported
from Guadeloupe were publicly sold as slaves. The black troops immediately
deserted and the war was resumed. As before, it assumed an atrocious character,
and Dessalines, the black leader, ordered the massacre of all whites, the burning
of the towns and plantations.

The French on their part gave no quarter; they even brougnt to the siege of
Leogane two hundred Cuban bloodhounds, “ that were fed on negro flesh and made

Fig. 195.—Disputep TERRITORY BETWEEN Harri AND San DouinGo.
Scale 1 : 7.000.000.

Sallie. Mee
AST Mul ? .
7PM apg FTE
Ma

= Sonaives4

emi Ss
parte =
quar

ti rs

Depths.
Disputed 0 to 1,500 1,500 Fathoms
Territory. Fathoms. aud upwards.
125 Miles.

more savage vy hunger.” But the climate, on which the Haitians had calculated,
at last secured them the victory. <A frightful outburst of yellow fever almost com-
pletely destroyed the invading army, carrying off 24,000 of the 35,000 that had
been landed, and leaving only 2,200 capable of bearing arms when the time came
to evacuate the island. Separation was now an accomplished fact, and on January
Ist, 1804, independence was proclaimed at Gonaives.

After its revolutionary period of fifteen years, Haiti, like the mother-country,
constituted itself an “empire;” then followed its monarchies and constitutional
presidencies, and even a second empire (1849), just as in France, and then another
republic, which still keeps up the outward semblance of a civilised state.

In 1848 the alliance imposed by force on the Spanish section of the island was
broken, and all subsequent attempts to restore the union have ended in failure.

410 MEXICO, CENTRAL AMERICA, WEST INDIES.

The severance of the two states is sufficiently explained by the differences in speech,
traditions and race. While full-blood negroes dominate in Haiti, the people of
colour, that is, mulattoes, form the great majority in the neighbouring state, The
former speak French, or a creole patois of French origin, and their relations are
mainly with France; the latter are of Spanish speech, and their associations have
chiefly been with the Hispano- American republics.

Of the two states the eastern has always been the weaker in population, trade
and military strength. Hence not only has its independence been more frequently
threatened, but it has had to repel the attacks of its western neighbour; its terri-
tory was even occupied by Spanish troops in 1861 and re-annexed to Spain till the
year 1865. In 1869 the United States made several attempts to attract San Domingo
within the orbit of its political sphere, and even for a time occupied Samana Bay.

The limits of the conterminous French and Spanish colonies and, later, those of

the two republics have often been modified. At present the frontier follows a very |

irregular line from north to south, and each state claims the upper basin of
the Artibonite The treaty of 1876 recognised the disputed territory as belonging
to San Domingo, allowing the Haitians to hold it for an indemnity of £30,000
and the free admission of produce by land from San Domingo. This state is
nearly double the size, but has only half the population, of Haiti.

II.—Repvsuic or Hairt.

Scarcely a single town in Haiti but recalls some siege, battle, or butchery,
The very river marking the northern frontier is known by the name of Rivière du
Massacre, in memory of a sanguinary conflict between the natives and the Spaniards.
Since the war of independence the first town west of this river bears the name of
Port-Liberté, which replaces that of Port-Dauphin. There is no better harbour in
Haiti than this extensive inlet, which is perfectly sheltered from all winds and
affords excellent anchorage in depths of from 26 to 65 feet ; but sailing vessels find
it somewhat inaccessible owing to the long winding entrance scarcely a mile wide.
Hence it is visited chiefly by steamers which here ship considerable quantities of
dyewoods felled in the districts of Trou and Ouanaminthe, the Guanaminto of the
Arawak aborigines.

On the north side the chief seaport is still Cap-Français, now Cap-Haitien, or
simply Cap, which before the war was known as the “Paris of San Domingo.”
Having been several times burnt and overthrown by an earthquake in 1842, it has
no longer any fine monuments; but its harbour, which is rather a bay sheltered
by reefs, does a flourishing trade in coffee and tafia. Near Hilo, 9 miles south of
Cap-Haitien, stands the ruined château of San-Souci, built by General Christophe,
who became “ King of the North ” under the name of Henry I.

West of Cap-Haitien follow the little havens of Port-Margot and Port-de-Paix,
the Valparaiso of Columbus. This place lies due south of Tortuga Island, the
famous stronghold of the buccaneers, and starting-point of the French conquest of
Haiti. Farther west lies the estuary of the Trois-Riviéres, which flows from the

REPUBLIC OF HAITI. 411

Black Mountams through the populous communes of Murmelade, Plaisance, and
Gros- Morne,

The Môle Saint-Nicolas, at the western extremity of the northern peninsula,
was the first point of the coast touched by Columbus when he discovered Española
(San Domingo). It was so named from the long promontory protecting the port
like a mole or breakwater, and in 1693 became the chief stronghold of the French
in Haiti; but the fortifications were reduced to a heap of shapeless ruins by the
earthquake of 1842. In 1764, 400 exiled Acadians received some lands in
the district ; but the climate, having proved fatal to most of them, the survivors
were removed to Louisiana. A similar fate befell 2,400 Germans, who settled in

Fig. 196.—Sr. Nicoras PENINSULA.
Scale 1 : 400,000.

OSLO PEELS

= = =
Port-de-Paix
os

: Depths.
0 to 500 500 Fathoms
Fathoms. and upwards.

30 Miles.

the neighbourhood about the same time, and founded the station of Bombardopolis
or Bombarde, so named in honour of a financier. Some of their half-caste descen-
dants are still found in the district, and a confluence of lagoons in the Mississippi
delta still bears the name of ‘‘ Lac des Allemands,” from the remnant of the immi-
grants who accompanied the Acadians to Louisiana.

The port of Gonaives stands on the west coast at the head of Gonaives Bay,
where two rivers of the same name and the Artibonite enter the sea. Thanks to
its central position between the northern and western provinces, Gonaives has
played an important part in the chequered history of the country. Here Toussaint-
Louverture embarked for France, and here was proclaimed the independence of
Haiti.

412 MEXICO, CENTRAL AMERICA, WEST INDIES.

Saint-Marc, farther south on the same coast between the headlands of Pointe
Diable and Cap Saint-Marc, commands the outlet of the great Artibonite valley, the
richest in Haiti, comprising in its upper basin the magnificent pastures of Saint-
Raphael, Saint-Michel de? Atalaye, and Hinche ; lower down, the mahogany forests
of ‘Las Caobas ; and on the plains the coffee and other plantations of Verrettes and
Petite-Rivière. An isolated bluff near the mouth of the river is the famous Créte
à Pierrot, which had been fortified by English engineers, and which the blacks
defended so valiantly during the war of independence.

South-east of Cap Saint-Mare, Wont- Rou’, Arcahaye, and a few other coast villages
follow as far as Port-au-Prince, capital of Haiti. This city, which owes its pre-

Fig. 197.—GuLr oF Port-au-Prince.
Scale 1 : 575,000.

——— oP!

{_—————— 2? 2oucassin—
SS >
=

——

eee Le
BK A ut AN

0 to 50 50 to 100 100 Fathoms

Fathoms. Fathoms. and upwards.
12 Miles.

eminence to its favourable commercial position, dates only from the year 1749,
when it was founded under the name of ? Hôpital; the “prince” to whom its
present name has reference has not been identified. All its old monuments have
perished in the numerous fires. by which it has so often been wasted, and it con-
sists at present of low brick or wood houses, disposed in regular blocks between
avenues lined with trees. The city, which is connected with its suburbs by a few
lines of railway, was formerly defended by forts crowning the surrounding heights.
North-east lies Croix-des- Bouquets, which so often changed hands during the revo-
lutionary wars.

The south-west peninsula, from Port-au-Prince to Cape Tiburon, is lined with

| TL
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ESS

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SS
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PRINCE.

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GENERAL VIEW OF PORT-AU

TOPOGRAPHY OF HAITI, 413

numerous trading places, every creek and inlet having its little group of houses
half concealed by forest growths. (a Jra, at the point where a chain of reefs
connects the coast with Gonave Island, is the outlet of the important town of
Léogane, the Yaguana of the aborigines, which was the capital of Haiti before
Port-au-Prince. Farther on follow Grand-Godre and Petit-Godve, the latter,
despite its name, the larger and more commercial of the two.

Farther west lies the flourishing town of Miragodne, and the less important
seaports of Nippes, Anse-a- Veau, Petit-Trou, and Baradères. A cutting of about
200 yards would suffice to connect the spacious Baradéres Bay with the Cayemites
roadstead across the low intervening promontory. Beyond Bec-d-Marsouin and
the two islets of Grand and Petite Cayemite, Peste/ and Corail serve as outports of
Jérémie, the chief town in the peninsula, but destitute of good anchorage The

Fig. 198.—Sourn-west Prenrysuna or Hartt.
Scale 1 : 2,500,000.

Sa We Tax Gonave

== PORT AU PRINCE 3

———
SS

West of Greenwich
Depths.

200520 2 24a

0 to 100 100 to 500 500 to 1,000 1,000 to 2,000 2,000 Fathoms
Fathoms. Fathoms. Fathoms. Fathoms. and upwards.

30 Miles,

surrounding district exports coffee, spirits, and the best cacao in the island, One
of the residences of Jérémie was a family inheritance of Alexander Dumas, that
great and prodigal genius whom Michelet called one of the “ forces of nature.”
Several small towns occupy the inlets at the very extremity of the peninsula.
Such are Trou-Bonbon, les Abricots, Dalmarie, properly Dame-Marie, Anse-d’ Hain-
ault, les Trois, that is les Irlandais, so named from some ‘ Irishmen” who settled
here in the eighteenth century ; lastly, Tiburon, under Cape Tiburon (Cabo San
Miguel), extreme western headland of the peninsula.
On the south-west coast, between Tiburon and Abacou Point, the best haven is
_ that of Coteaux. But the whole of this seaboard is exposed to the fury of the surf,
and even Port-Salut, despite its name, offers but a precarious anchorage to shipping.

414 MEXICO, CENTRAL AMERICA, WEST INDIES.

But farther east, the Bay of Cayes, well protected by fringing reefs (‘“ cayes ”’”)
and by the island of La Vache, is indented by several excellent harbours, accessible
to vessels of light draught. The town of Les Cayes, not far from the site of
Salvatierra, founded in 1505 by Obando, is one of the chief seaports of the
republic. But it is a very unhealthy place, standing ina marshy district at the
mouth of a coast stream subject to frequent inundations. The neighbouring towns
of Torbeck, Cavaillon, and farther east Saint-Louis and Aquin, have developed a
few industries, especially the preparation of straw hats. It was at the port of
Aquin that the English expedition of 1655, sent by Cromwell to reduce San Sal-

Fig. 199.—Les Caves Bay.
Scale 1 : 600,000.

West of Greenwich

Depths.
0 to 10 10 to 100 10C Fathoms
Fathoms. Fathoms. and upwards.

12 Miles.

vador, met with the repulse which was avenged by the conquest of Jamaica. Les
Cayes was the scene of a still more memorable event in 1816, when Simon
Bolivar organised in this place the expedition which led to the overthrow of Spanish
rule in South America.

The Ile-à-Vache, by which the Bay of Cayes is half closed, served at one
time as a place of exile for over 450 American negroes. Thousands of slaves set
free by the war had taken refuge in 1863 under the walls of Fortress Monroe
in Virginia, and the Washington Government, wishing to get rid of them, sent
batches as colonists to various parts of the West Indies and Central America. As
many as 5,000 of these freedmen had been destined for the Ile a- Vache, which

ECONOMIC CONDITION OF HAITI. 415

the Haitians had placed at the disposal of the Americans for the purpose of making
experiments. But the first essay was disastrous ; over a third of the settlers were
carried off by epidemics, hunger and homesickness, and the survivors had to be
sent back. At present the island is dotted over with flourishing banana-groves,
the produce of which is exported to the United States.

Jacmel, on the south coast where it begins to curve round to form the Beata
peninsula, has the advantage of lying near the capital by the overland route, though
distant over 280 miles by sea. Were the two places connected by a railway across
the neck of the peninsula, Jacmel would become an outlet of Port-au-Prince towards
the south. Farther east follow the little seaports of Les Cayes de Jacmel and Sale-
Trou, that is, “ Dirt-hole,” but often written Sa/trou to avoid offending the suscep-

tibilities of its inhabitants.
Economic Conpirion oF Harrt.

There can be no doubt that during the revolutionary troubles and war of inde-
pendence the population was greatly reduced, though to what extent cannot now
be determined. Most of the whites had been massacred, while those who escaped
to Cuba and other places were followed by many of their slaves. Of the blacks
and mulattoes multitudes fell in battle and the summary executions. The Haitians
were probably reduced by one-half during the fifteen years of the revolution,
falling from 600,000 to 300,000, and, according to some authorities, even to 260,000.
Since that time there has been no lack of civil strife, but it has not seriously
affected the bulk of the inhabitants. In the interior peace has been the normal
condition, and the natural fecundity of the black race is such that the population
should be doubled in fifty years. Even in the unhealthy capital the birth-rate is
twice as high as the mortality, and at present the Haitians can scarcely number
less than a million. An unpublished report made to M. Salles in 1889 estimates
them at 994,000. The density per square mile would thus be about half that of
France, not much for such a fertile country.

It has often been asserted that in Haiti as in Cuba the female population is
much greater than the male. It is more certain that the people are reverting, at
least in colour, more and more to the African type; nor could it be otherwise. At
the beginning of the revolution the half-breeds were less than one-tenth of the whole,
and the wars all tended to increase the disparity in favour of the blacks, who form
the vast majority. Hence, since the white element has almost been eliminated, the
crossings necessarily result in the gradual absorption of the half-breed in the full-
blood negro,

Butif the complexion is mostly very dark, African features, such as those of the
W olofs and Serers, are seldom met. The new environment has re-modelled the fea-
tures, which have become largely assimilated to the European type. Immigration
contributes but slightly to the growth of the population. The negroes from the
States, differing from the natives in speech, religion, and usages, generally keep
aloof, while those from the French Antilles fraternise readily with the Haitians.
Emigration is very limited and chiefly directed towards Sin Domingo and Venezuela.

416 MEXICO, CENTRAL AMERICA, WEST INDIES.

Little progress has been made in agriculture and the industries. This may be
attributed to the system of land tenure, an inheritance of the old régime. After
the expulsion of the French the system was maintained in favour of the people of
colour, who had succeeded the whites as landowners. Thus the bulk of the
peasantry were still deprived of the land, despite their frequent revolts to seize it
by force. It is often asserted that these risings of the “ piquets,” or “ pikemen,”
as’ the insurgents were called from their usual weapon, were caused by racial
hatred as between the black and coloured people. But far more important than

colour was the land question.
‘« Négue riche li mulatte,
Mulatte pauve li négue! ”

says a local proverb.*

At last, in 1885, eighty years after the proclamation of independence, a law
was passed authorising the distribution of the public domain in lots of from 33
to 6 acres to all citizens undertaking to grow coffee, sugar or other colonial
produce. But hitherto small freeholds have remained the exception, at least in
the central and accessible districts. The fertile plains continue almost every-
where under large plantations, the smaller lots being held under lease.

To prevent the return of the whites, the seventh article of the constitution
prevents all foreigners from purchasing the smallest particle of land. It is
asserted that were capitalists allowed to acquire land they would soon revive the
former prosperity of the country. Possibly they might, but at the expense of
the black population, which would be again reduced to slavery under another
name.

Sugar, formerly the chief crop, has ceased to be cultivated in a large way ; it
is now grown only for the local demand and the fabrication of rum. At present
the staple product of the soil is coffee, which is cultivated far more extensively
than during the period that followed the war of independence. ‘The assertion
that the blacks merely gather the berry from shrubs planted in the days of
slavery is a gross libel. Since the last century the plants have been renewed at
least three times, and during the war of secession the cultivation of cotton was
also rapidly developed, until the revival of the industry in the States again made
all competition impossible. Cacao has quadrupled since colonial times, and
tobacco is also more extensively grown than formerly. Amongst other articles of
export, one of the most valuable is logwood, first introduced in 1730.

Trade, which rapidly declined during the revolutionary wars, represents
scarcely one-tenth of the importance it possessed under the old system. Formerly
field labour was almost exclusively engaged in the production of colonial produce
for exportation to Europe, whereas now it is directed chiefly to the cultivation of
supplies for the wants of double the population. Commercial relations are chiefly
carried on with the United States and Great Britain, France taking only the third
position in this respect.

Public works are still in a rudimentary state. The roads are badly kept :

* That is, “ Negro enriches mulatto; mulatto impcverishes negro.”’

ECONOMIC CONDITION OF HAITI. 417

bridges rare and neglected. The capital is unconnected by a single railway with
the other towns, whose streets are dusty and filthy in dry, muddy quagmires in
wet, weather. Fires, often kindled by rival factions, have destroyed most of the
public buildings ; in a word, towns and villages are mere groups of straw huts and
log cabins.

According to law education is gratuitous and compulsory; but in Haiti the

Fig. 200.—Grovr or Harrrans.

laws are not always enforced, and the bulk of the people remain in a state of
profound ignorance. There are three lyceums, and in 1884 the primary schools
numbered 400, with an attendance altogether of less than 25,000. The inheri-
tance of past superstitions, both pagan and Christian, still persists. The
people share with some of the French peasantry the belief in wehr-wolves, and,
like their African ancestors, still practise ‘‘ vaudoux,”’ or snake-worship. The
obi, papa-kings and mama-kings (papalois and mamaniois), sacrifice cocks and
60

418 MEXICO, CENTRAL AMERICA, WEST INDIES.

white goats, and even the “ goat without horns,” that is, children, are also said to
have been sacrificed.* Wizards and witches have preserved the receipts for the
preparation of charms, philters or poisons. Many Catholic ceremonies are mingled
with heathen rites, and at “camp meetings ” the crowd is sometimes seized with a
religious frenzy, dancing with wild contortions, rolling on the ground, howling
and shouting like bedlamites. The so-called ‘‘ moanes-pouvoir,” persons possessed
of supernatural power, cast the horoscope of their enemies, and hold intercourse
with the invisible world by uttering certain words incomprehensible to the profane,
and agitating head, arms, and body like dancing dervishes.

Nevertheless the people are endowed with a considerable share of natural intel-
ligence. They have their historians, journalists, and especially poets, and some of
their odes and elegies are masterpieces of the French-Creole language.

ADMINISTRATION.

In Haiti paper constitutions have followed in rapid succession, but they have
been so often violated or abrogated that it would be useless to enumerate their
various provisions. According to the charter of 1867 the machinery of govern-
ment comprises an upper and lower chamber with legislative functions, a president
or chief of the executive, and six ministers. The deputies, one for each commune,
three for the capital, and two for each of the chief towns of the departments,
are returned by universal suffrage for three years. One-third of the senate retires
every two years, and its 39 members are chosen, not by the electors, but by the
lower house, from two lists presented by the electoral colleges and the executive.

There is no state religion, although the bulk of the people are nominal
Catholics, whose priests since 1861 have been exclusively of French birth.
Methodism and the Baptists have made a few thousand converts in the capital and
the northern districts.

The army comprises 7,000 or 8,000 volunteers or conscripts, but in theory all
citizens between twenty and fifty years of age are enrolled in the National Guard
for four years. The “generals” are reckoned by hundreds, and this military
system, combined with the extortions of certain presidents, and the indemnity of
£6,000,000 due to the old planters, has thrown the public finances into. disorder.
The consolidated debt amounts to £2,720,000, exclusive of the floating debt,
represented by the paper currency. The revenue, derived almost entirely from the
customs, varies from £1,000,000 to £1,120,000. Since 1886 the French indemnity
has been completely discharged.

The republic is divided into five administrative departments, tabulated in the
Appendix.

III.—$Sax Domineo.

The Spanish republic presents less dramatic unity in its historic evolution than
Haiti. Its independence was acquired later, and down to the year 1809 a French

* Relation des visites pastorales de Mgr. Hillion, 1880-82; Sir Spencer St. John, Hayti or the Black
Republic, 1884.

TOPOGRAPHY OF SAN DOMINGO. 419

garrison was maintained in the capital. Then came the English, and after them
the Spaniards, followed in 1821 by the revolt against the mother-country under
the Colombian flag. But Bolivar was too far off and too hard pressed by the
Spaniards to come to the aid of the insurgents, and the new republic had to
unite with Haiti in a single state. In 1844 it regained a precarious auto-
nomy, more than once threatened, first by France, then by Spain and the United

States.
On the south coast the chief place west of the capital is Azwa (Azua de Com-

postela), which occupies a healthy site on a terrace some six miles north of Ocoa
Bay. The town had already been founded farther south by Diego Colon in 1504;

Fig. 201.—Azua anp Ocoa Bay.
Scale 1 : 1,000,000.

West of Greenwich

18 Miles.

but after its destruction by an earthquake it was rebuilt on its present site on
the Rio Via. The district abounds in salt, bitumen, and mineral waters, while
vast grazing-grounds occupy the upper Neyba and Artibonite valleys, especially
about the towns of Banica and San Juan de Maguana. It was at San Juan that
Schomburgk discovered the most remarkable objects of pre-Columbian culture,
including a circle of granite blocks supposed to represent the serpent biting its
tail, symbol of eternity. '

Santo Domingo, the capital, which has given its name to the republic and to
the whole island, is one of the oldest European settlements in the New World.
In 1596 it succeeded to the station of Natividad which Columbus had founded on
Caracol Bay in the north-west part of Española. Built at first by Bartholomew

420 MEXICO, CENTRAL AMERICA, WEST INDIES.

Columbus on the left bank of the Ozama, it was soon removed to the opposite side
of the river. Thanks to the neighbouring gold-mines it has always been the
political centre of the country, although its harbour, separated from the sea by
the bar of the Ozama, is accessible only to light craft.

The city, which is still enclosed by the old Spanish ramparts, is dominated by
the domes and belfries of several churches, one of which, the cathedral, of imposing
aspect, claims like Havana to possess the remains of Columbus. According to the

Fig. 202.—Santo Dominco.
Scale 1 : 28,000.

Pec G
i nat
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x D FO G A
RATE
RSI LENS as °

ti qn
Meta %
25. old
QI L

“20
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———$———<——<—<————
——

. -69°53'40

0 to 10 10 to 20 20 to 30
Feet. Feet. Feet.

----- Site of the old fortifications.

1,100 Yards.

popular tradition, the body of Diego Columbus was by a “ pious fraud ” substituted
for that of Christopher at the time of the official translation in 1781.

Numerous small towns, such as San Carlos, Rosario, Pajarito, and San Lorenzo,
are dotted round about the capital, which is connected by rail with the mines and
plantations of the interior. Farther west the chief places are Bani and San Cris-
tobal. astwards stretches a region of forests and savannas, where are situated the
stations of Los Llanos, Hato Mayor, Santa Crus del Seibo, and Salvaleon de Higuey.

TOPOGRAPHY OF SAN DOMINGO. 421

On the opposite slope of the mountains the north-east corner of the island is
occupied by the district of Samana, with its magnificent bay, spacious enough to
shelter whole fleets. Icaco Point, on the south side near the inlet of La Gina, pro-
jects to within a short distance of several islets by which it is continued across the
entrance of the bay nearly to the north side. This outer barrier is pierced by two
channels, the larger of which is less than a mile wide, while the other is so narrow
that sailing vessels run great risk in attempting to enter without a pilot. Thus
the bay might easily be defended by fortifications, erected on the reefs and head-
lands. In the neighbourhood are some rich coal-mines, hitherto very little worked.

In 1869 the United States purchased for £30,000 the right of establishing a
naval station in Samana Bay. An American company also obtained the commercial
monopoly of the district. But fortunately for the independence of San Domingo

Fig. 203.—Samana Bay.
Scale 1: 700,000.

names

West of Greenwi ch

0 to 32 32 to 160 160 Feet
Feet. Feet. and upwards.
12 Miles.

the company failed, and about the same time the United States surrendered the
protectorate.

The port of Las Flechas, near the extremity of the peninsula, has been almost
abandoned in favour of Santa Barbara (Samana), where a trading community of
Americans, Englishmen, Italians, and others has been established, although the
inlet is inaccessible to vessels drawing more than 13 or 14 feet.

West of Samana peninsula the basin of the River Yasica is largely cultivated by
North American negroes settled here by the Florida planter, Kinsley, who had
framed a scheme of gradual emancipation for the slaves. But scarcely had they
landed when they emancipated themselves, and these “ Kinsley boys,” as they are
familiarly called, have prospered and multiplied in the district. The pearl-fisheries
of San Lorenzo, near Savana-la-Mar on the south side of Samana Bay, have been
abandoned.

422 MEXICO, CENTRAL AMERICA, WEST INDIES.

The basin of the Yuna, which flows eastwards to the head of the bay, and which
is now traversed by a railway, is the richest district of the whole island, and might
alone support a larger population than that of both republics. This is the famous

’ whence its capital takes the name of Concepcion de

region of Vega, or the “ Plain,’
la Vega. Other flourishing towns in this privileged district are Moca, Cotui, San
Francisco de Macoris, and Santiago de los Caballeros, the last-mentioned near the |
waterparting on the slope watered by the Yaqui, which flows west to Manzanillo
Bay. Thanks to its favourable position between the two basins and on the trans-
verse route connecting the capital with Puerto Plata, Santiago has become the first
city in the island both for population and the extent of its trading relations. It
is the centre of the tobacco plantations which supply the market of Hamburg
Puerto Plata, its seaport on the Atlantic, has replaced Zsabella, founded by
Columbus as the future capital of the New World.

The port of Monte-Cristi, north of the Yaqui estuary at the extremity of
the Monte-Cristi range, is little frequented, this borderland between the two states
being almost an uninhabited wilderness.

Economic ConpITION AND ADMINISTRATION OF SAN DomiIxGo.

In recent times San Domingo has made rapid material progress, thanks to the
natural increase of population, the maintenance of peace and the considerable stream
of immigration from Jamaica and Puerto Rico.

The resources of the state are not so exclusively agricultural as in Haiti.
Mining operations are already in progress, especially in the gold and silver dis-
tricts; there are also extensive savannas large enough to raise sufficient live-stock
for the whole of the Antilles. The chief cultivated plant is the sugar cane, intro-
duced from the Canaries in 1506. Coffee is also largely grown, and in recent years
the cultivation of tebacco has much increased.

Foreign trade, greatly inferior to that of Haiti, is carried on chiefly with the
United States and the depôts of St. Thomas in the Danish Antilles. The exchanges
have considerably increased since the opening of the railways, especially the line
70 miles long between La Vega and Samana. The telegraph system is connected
with the outer world by submarine cable, but owing to the prevailmng ignorance of
the people, it is little used except by the commercial class.

The constitution of 1844, when San Domingo was separated from Haiti, has
been frequently modified, and was even suspended for two years at the time of the
Spanish invasion. Since 1887 the legislature is invested in a national congress
elected for two years by universal suffrage, each province or district returning two
members. The president, elected in the same way, is assisted by six ministers.
Each province has its local legislature, in which the central authority is represented
by a governor nominated by the president. Catholicism is still the State religion,
though all others are tolerated. The army of a few thousand men is a heavy
charge on the revenue, which scarcely exceeds £300,000, derived chiefly from the
customs, controlled by a financial company.

Ar ï nant =

CHAPTER X.
PUERTO RICO.

UERTO RICO, the Borinquen of the Arawak Indians, ranks in
size only as the fourth of the Great Antilles, but takes the first
place for density of population and general prosperity.

Physically it forms an eastern continuation of the line of

upheaval indicated by Jamaica and the southern seaboard of San
Domingo. In outline it presents the appearance of an almost geometrically
regular parallelogram, nearly three times longer than broad, with its four sides facing
the four cardinal points, but with a slight eastern convergence of the northern and
southern coasts. Both of these are indented like the edge of a saw, and towards
the south-west the coastlands, rising little above sea-level, are strewn with swampy
tracts.

Even the islands and islets scattered along the east side seem to form a half-
upraised prolongation of the geometrical insular mass. Such are Vieques, or
“ Crab ” Island, disposed in a line with the main southern ridge, and La Culebra,
standing like a cornerstone of a future structure, continuing the north side east-
wards. Mona Island, also, off the west coast in the passage separating Puerto Rico
from San Domingo, stands on the same submarine bank as the large island of which
it is a political dependency. Thus the parting-line between the Atlantic and
the Caribbean Sea is continued west and east of Puerto Rico in such a way as to
connect this island on the one side with San Domingo, on the other with the
Virgin Islands. But northwards and southwards the submarine slopes fall
regularly to depths of from 1,000 to 2,000 fathoms, and on the side of the ocean
even to over 5 miles.

PuysicaL FEATURES.

In general elevation Puerto Rico is far inferior to the other Great Antilles. It
is even rivalled in height by some of the peaks in the Lesser Antilles. Its uplands
are disposed in masses and ridges which present no clear arrangement in their
general disposition. The culminating-point is the Yunque (‘“ Anvil”) de Luquillo,
or simply Luquillo, so named from the town at its foot. It rises to a height of
3,680 feet, in the north-east corner of the island, whence the crests ramify between
the river valleys. The chief range, consisting mainly of calcareous rocks, lies
near the south coast, where it ramifies westwards into several branches, some of
which terminate in headlands on the coast.

424 MEXICO, CENTRAL AMERICA, WEST INDIES.

Round the whole periphery of the island numerous fluvial valleys are disposed
at right angles with the coast. Some of these streams are over 60 miles long, and
several on the north slope take the name of ‘ Rio Grande,” being both considerably
larger and more copious than those flowing southwards.

INHABITANTS.

Having no inaccessible places of retreat in the mountains, the aborigines, not-
withstanding their numbers, rapidly disappeared after the conquest. According
to the early chroniclers they numbered nearly a million, all subjects of a single
cacique. They are supposed to have been of the same race as the Haitians, and
arms or ornaments are often turned up by the plough attesting the originality of

Fig. 204.—Pusrto Rico.
Scale 1 : 2,250,000.

5+ #7: we Marertos— —

0 to 50 50 to 500 500 to 1,000 1.000 Fathoms
Fathoms. Fathoms. Fathoms. and upwards.

60 Miles.

their culture. They consist of heavy collars of syenite or other massive stones, and
are found only in Puerto Rico and some of the neighbouring Lesser Antilles,
though objects of a somewhat similar character have also been picked up in the
territories of the Mexican Huaxtecs and Totonacs. Some of them, weighing as
much as 65 pounds, are of perfectly regular form, but without any embellishment,
while others terminate in a more or less decorated plaque. Their use is unknown,
though some archeologists have compared them to the cangue worn as a punish-
ment by culprits in China.

As in the other Antilles the aborigines were replaced by the black race on the
plantations. Caparra, the first settlement in the island, was founded in 1509 by

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GENERAL VIEW OF SAN JUAN BAUTISTA, PUERTO RICO.

PUERTO RICO. 425

Ponce de Leon near the village now known as Pueblo Viejo (“Old Town’’), south
of the present capital. Colonisation was at first retarded by hurricanes, a Carib
invasion, and other disasters, which led to a temporary abandonment of the island.
Tn 1700 it had only three villages, but during the last hundred years progress has
been remarkably steady and interrupted only by an outburst of cholera which
carried off 30,000 persons in 1855. The population, which numbered nearly 45,000
in 1765, now (1891) exceeds 820,000, and has doubled itself on an average every
thirty years, a rate almost as rapid as that of the French Canadians. This expan-
sion is partly due to the natural fertility of the soil and the uniform relief of the
land, partly to the large immigration from Spanish America during the wars of
independence between the years 1810 and 1825. Puerto Rico itself revolted in
1867, but an earthquake terrified the conspirators, and a fresh rising the following
year was promptly quelled. Since that time no further attempt has been made to
sever the ties with the mother-country.

Puerto Rico is one of the few countries in tropical America where the whites
outnumber the other races. But it was not always so, and in 1775 the position
was reversed—29,000 Spaniards, nearly all Andalusian peasantry, to over 50,000
pure and mixed blacks. Towards 18530 the two elements were about balanced, and
at the census of 1887 the whites exceeded the blacks by about 150,000—475,000
and 324,000 respectively. At the same time some doubt may prevail as to the
accuracy of these returns, for it is notorious that many with a strain of black
blood in their veins claim to be of pure Spanish descent. In any case it is
remarkable to find the European race on the whole increasing more rapidly than
the African in a climate certainly more favourable to the latter.

It also appears from the last census that amongst the whites the males
exceed the females, the contrary being invariably the case everywhere in Europe.
The phenomenon is partly explained by the movement of immigration, which
here, as elsewhere in the New World, comprises more men than women.

TopoGRAPHY.

San Juan Bautista de Puerto Rico, present capital of the island, stands, not
on the mainland, but on a coralline reef forming an outer shore and enclosing a
winding lagoon, which is here crossed by a bridge. The settlement dates from
the year 1511, and in 1534 were begun the fortifications which add so much to
the picturesque appearance of the city, but which also invited numerous attacks
during the colonial wars. Although these attacks were for the most part success-
fully resisted, they had probably the effect of retarding the development of San
Juan, which is surpassed in size by some other towns.

The harbour, which is deep enough to admit large vessels, communicates with
the open sea by a winding and difficult channel, which cannot be navigated
without the aid of a pilot. West of the lagoons which form an extension of the
basin the River Bayamon has deposited an alluvial peninsula which is gradually
encroaching on the lateral inlets. This river gives its name to the town of

426 MEXICO, CENTRAL AMERICA, WEST INDIES.

Bayamon, the most important place in its valley, capital of a department and
centre of a rich and highly-cultivated agricultural district.

Rio Piedras and Santurce, which are both situated in the same territorial
division, are the chief rural retreats in the neighbourhood of San Juan. Here
numerous suburban villas are scattered amid the shady groves which fringe the
banks of the running waters.

Arecibo, also a departmental capital, is one of the places that exceed San
Juan in population. Yet it stands some distance from the sea on an unnavigable

Fig. 205.—San Juan Bautista, Purrro Rico.
Scale 1 : 600,000.

= NS

—fort-de

SAN HAN:

DRE ROSES
Cataño; 7
nag eae

aot ae 7° e
Oy Gea

West of Greenwic

Depths.
— — P=
0 to 16 16 to 32 32 Feet
Feet. Feet. and upwards.

12 Miles.

stream, which reaches the coast opposite an exposed roadstead dangerous to
shipping in rough weather. The Rio Grande d’Arecibo, as the river is called,
flows mainly north through the extremely fertile hilly districts, where the chief
centres of population are the towns of Adjuntas and Utuado. In the department
of Arecibo occur numerous stalactite caves.

Aguadilla, on the west coast, is a thriving seaport, possessing the advantage of
a spacious bay sheltered from the trade winds. Here are shipped the sugar and
coffee of Lares, Pepino, Moca, and other agricultural centres in the Colubrinas

TOPOGRAPHY OF PUERTO RICO. 427

valley. As indicated by its diminutive ending, Aguadilla (‘Little Aguada’’)
was formerly a smaller place than the older town of Aguada, which lies some
distance inland, and which has now been surpassed in size and activity by the
coast town.

Farther south on the same side of the island, the Mayaguez inlet is much
frequented by vessels engaged in the coasting trade and even by steamers, which
here ship coffee, bananas, and oranges for the foreign market. The growers of
Mayaguez and of the neighbouring towns of Axaso, Cabo Rojo, and San German
boast that they raise the finest crops in Puerto Rico.

Fig. 206.—Souru-wxst Corner oF Puerto Rico.
Scale 1 : 450,000.

a
SS ae
—- Je A, a
TETE

pare Soyvada—) Cabo ro, 4
———— CR Se eh

ae Guar 2 Wa

M
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à

West of Greenwich

Depths.
0tod5 5 Fathoms
Fathoms. and upwards.

6 Miles.

Dependent on the department of Mayaguez is the island of Mona, which
gives its name to the broad. channel flowing between Puerto Rico and San
Domingo. Mona, that is, the “‘ Monkey,” Passage terminates on the west in a bold
headland topped by a huge overhanging rock known to seafarers by the suggestive
name of Caigo 6 no Caigo? (“Shall I fall or not?”) The neighbouring islet
has been christened Monito, the “ Little Monkey.”

Guanico, the westernmost haven on the south coast, is also the best in the
whole island. But it is seldom visited, being surrounded by a low marshy
district difficult to traverse. Guanico serves as the outlet for the produce of the

4258 MEXICO, CENTRAL AMERICA, WEST INDIES.

nearest towns, San German, Sabana Grande, and Yauco. Eastwards follow the
bays of Guayanilla and of Ponce (La Playa), the latter the largest city and the
true capital of the island. Ponce lies three miles north of the bay on a rich
plain surrounded by gardens and plantations. The neighbouring thermal waters
are highly appreciated by invalids. The Playa, or “ Beach,” is occupied by
extensive depôts for the produce of the interior, which is forwarded through
Ponce, the trading centre of the island. Next to this flourishing seaport the
largest places in the department are Yauco and Juana Diaz, both situated at the
south foot of the sierra.

The eastern division of Puerto Rico is less densely peopled than the west; it
is also less conveniently situated for trade, lying on the windward side and
offering little shelter to shipping. Here all the chief towns lie inland, or at least
at some distance from the coast. Such are Cayey, Caguas, and San Lorenzo or
Hato Grande, which are situated in the hilly region amid rich coffee plantations
and extensive grazing-grounds. Guayama and Humacuo, the two departmental
capitals, have been founded in the maritime district a few miles from the sea.

At the north-east corner of the island some shelter is afforded to small craft
by chains of islets and reefs, and some inlets on the coast. One of these little
havens at the island of Culebra is frequented by fishers and woodcutters. Vieques,
or Crab Island, which points like a spearhead towards the north-east, is occupied
only by the solitary village of Zsabel Segunda on its north side. La Culebra and
Vieques also take the name of Islas del Pasaje, because they lie in the “ passage ”
between Puerto Rico and the Virgin group.

Economic Conprtion oF Puerto Rico.

The prosperity of Puerto Rico is shown quite as much in its general material
progress as in its increased population. Since the middle of the last century the
social condition of the inhabitants has undergone a complete change. At that
time there were no towns, and the peasantry assembled only on feast-days in the
centre of their respective parishes. They dwelt in rude hovels without shutters
to the windows or doors to the entrance, and their only utensils were calabashes ;
an empty bottle was handed down 4s an heirloom to the favourite son.

At present more than half of the inhabitants have gravitated towards the
towns, especially those of the seaboard, and foreign trade has familiarised them
with all modern inventions tending to domestic comfort. The movement of
exchanges “is nil,” said Iiigo Abad, a local historian, writing in 1772. In fact
it was restricted to a little barter in the only haven officially opened to trade,
supplemented by some smuggling in the other inlets round the coast, the whole
representing a value of perhaps £2,000.

Since that period the yield of sugar, coffee, tobacco, and to a less extent honey
and wax, has enriched the island, which now possesses the means of purchasing
all the wares of the civilised world. Most of the exchanges are carried on with
the United States, whence corn, flour, salt meat, fish and lumber are imported in

ADMINISTRATION OF PUERTO RICO, 429

return for sugar, molasses, and coffee. Nearly all the seaborne traffic is conducted
under foreign flags, the islanders showing little taste for seafaring life.

In respect of its internal communications Puerto Rico is a model West Indian
island. All the towns are connected by highways, which develop round the
periphery of the quadrilateral a second quadrilateral all the sides of which are
united at intervals by transverse routes. A railway has now been commenced,
which is also to follow the shore-line with a circuit of 300 miles, and short branches
to all the seaports and inland markets. All the main lines of the telegraph system
are already completed ; but little use is made either of the wires or the post-office
by a population only one-seventh of which was returned as capable of reading
or writing at the last census (1887). Since then, however, public instruction has
made considerable progress.

ADMINISTRATION.

For administrative purposes Puerto Rico is regarded, not as a colony, but as a
Spanish province, assimilated to those of the metropolis. The governor-general,
representing the monarchy, is at the same time captain-general of the armed forces.
In each departmental capital resides a military commandant, and each borough
has its alealde nominated by the central power. The provincial deputies are elected
by universal suffrage on the same conditions as in Spain. The garrison consists
of about 3,000 men, and the yearly budget averages £800,000.

Including the district of the capital there are seven administrative departments,
which are tabulated in the Appendix.

CHAPTER ak
Virein ISLANDS AND SANTA Crvz.

HE Virgin Islands were so named by Columbus because they covered
the sea in a long procession like that of the “eleven thousand
virgins” of the Christian legend. ‘This chain of islands forms a
prolongation of Puerto Rico, but bends round somewhat te the north-

east before joining the Lesser Antilles. They form, so to say, the
keystone of the vast semicircle described by the whole of the Antilles. But both
as regards the submarine bed on which they rest and their general trend, they
belong far more to the group of the Great than to that of the Lesser Antilles. On
the east side the separating channel is over 1,000 fathoms deep, while the distance
to the nearest members of the smaller group exceeds 250 miles.

Santa Cruz, which is associated politically with the Virgin archipelago, is
geographically distinct, for it is separated from the northern chain by a “ tongue
of the ocean,” and on the other hand its marine bank forms an advanced prom-
ontory of the Lesser Antilles. Thus the two insular systems overlap at their
converging extremities.

Culebra and Crab, depending politically on the neighbouring Puerto Rico,
really form part, of the Virgin group. St. Thomas and St. John, the next two
going eastwards, together with the outlying Santa Cruz, are Danish possessions,
while all the rest as far as Anegada form part of the British Colonial Empire.

Sr. THomas.

Notwithstanding its small size, St. Thomas was formerly the most important
of the Antilles as the general depot of European trade with the West Indies. It
had originally been a rendezvous of the buccaneers, and then in the hands of a
financial company became the chief centre of the contraband trade with the
Spanish colonies, and one of the great markets for negroes imported from Africa.
The Elector of Brandenburg was director of the company, and he having been
succeeded by the King of Denmark, the island ultimately lapsed to that power,

Being a neutral island St. Thomas naturally attracted much trade during the
Napoleonic wars. Then it continued to thrive as a free port after the abolition of
the slave trade and the separation of Spanish America from the mother country.
In its warehouses, nearly all held by Jews, the West Indian planters found every-

ST. THOMAS. 431

thing that they required, provisions, woven goods, machinery, as well as the most
costly products of European industry. Free trade thus enabled St. Thomas to
profit by its advantageous geographical position at the extreme convexity of the
great bend described by the West Indian Islands, that is, at the very point whence
commodities are most easily distributed throughout all the surrounding insular
groups.

Moreover, St. Thomas possesses an excellent harbour, although deficient both in
size and depth. It forms a nearly circular basin on the south side of the island, of
easy access and well sheltered from the trade winds by a promontory and an islet.
Nevertheless, hurricanes have occasionally penetrated into this amphitheatre, as

Fig. 207.—Sr. Tuomas Istanp.
Scale 1 : 300,000.

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West of Greenwich

Depths.
Oto5 5 to 25 25 Fathoms
Fathoms. Fathoms. and upwards.

6 Miles.

they have also into the port of Havana; in 1819 nearly all the vessels in the
harbour were stranded, and the shore strewn with dead bodies: and wreckage. In
1837 and 1867 the place was again visited by destructive cyclones.

Steam has changed the commercial system of the West Indies. The consumer
is now directly supplied with all his wants by regular services of packets, which
visit every island and which are independent of winds and currents. Hence a
general entrepot is no longer needed, and St. Thomas has lost its former monopoly.
Nevertheless, the port, which bears the official name of Charlotte Amalia, is still
frequented, and long-established usage enables it to maintain an important com-
mercial position, Its 12,000 inhabitants speak every language—Spanish, Dutch,

432 MEXICO, CENTRAL AMERICA, WEST INDIES.

Danish, French, and especially English ; but the old creole dialect, which possesses
a copious religious literature, has mostly disappeared. Some Protestant emigrants
from the south of France reached the island from Holland, after the revocation of
the edict of Nantes, and occupied the Brandenburg quarter beyond the town.

Fig. 208.—Sr. Taowas Harsour.
Scale 1: 27,000.

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Depths.
0 to 16 16 to 32 ‘82 Feet
Feet. Feet. and upwards.

1,100 Yards.

The main thoroughfare, a mile and a half long, skirts the shore, and above it
rise tiers of houses on the slopes of the porphyritic hills encircling the harbour.
From the culminating point of the island (1,560 feet) an extensive prospect is
commanded of the surrounding island-studded waters.

—

SANTA CRUZ. 453

During the first years of its commercial decay, the Danish Government offered
St. Thomas and St. John to the United States for £1,000,000, and the inhabitants,
when consulted, gave their unanimous consent to tlie arrangement; but the offer
was declined, the price demanded being regarded as too high.

ST. JOHN.

St. John, which follows east of St. Thomas, does not, like its neighbour, lie
in the track of trading vessels, and its portof Coral Bay, on the east side, although
said to be the best harbour of refuge in the Antilles during cyclones, is visited
only by fishing-smacks and other small craft. The English call it Crawl Bay, a

Fig. 209.—Virein IscanDs.
Seale 1 ; 400,000.

== =

TS EE OP pol ge

West of Greenwich

Depths.
0 to 12 12 to 50 50 Fathoms
Fathoms. Fathoms and upwards.

9 Miles.

corruption either of the Spanish Corral (“enclosure”), or of Coral, from the
reefs encircling the harbour. The capital of the island is merely an obscure
village on the north side.

SANTA CRUZ.

Santa Cruz, the third Danish island, so named by Columbus at the time of his
second voyage, was inhabited by Caribs when the Spaniards arrived. But as it
possessed no precious metals, the strangers soon quitted it without massacring the
natives. But the Spaniards were succeeded by English buccaneers, and these by
the French, who sold the island to the Knights of Malta in 1650. Thus the
ancient Ayay of the Caribs passed from hand to hand, until at last it was sold by

434 MEXICO, CENTRAL AMERICA, WEST INDIES.

France to the Danish Government for the sum of 750,000 livres (£30,000). But
meantime the unfortunate Caribs, reduced to slavery and treated with like cruelty
by all, had completely disappeared.

Santa Cruz, whose planters grew rich during the flourishing times of slavery,
was one of the best-cultivated islands in the Antilles. It was entirely covered
by plantations up to the very summits of the hills, and from a distance the reddish
soil of the tilled land could be seen alternating with the verdant crops. Santa
Cruz is both better watered and more pleasantly diversified with hill and dale
than the Virgin group. The craggy heights have nowhere prevented its cultiva-
tion, and nearly the whole of the south side is a fertile plain, with a gentle incline
on a substratum of calcareous formation. The heights which skirt the north-
west coast attain their culminating point in Mount Eagle, about 1,300 feet high.

Fig. 210.—-Santa Cruz.
Scale 1 : 500,000.

—- sues
eS SSS
Se Se AGERE D. =

Depths.
0 to 5 5 to 50 50 Fathoms
Fathoms. Fathoms. and upwards.

9 Miles.

The capital, called the Basin, or, in official language, Christianstæd, lies at
the head of an inlet on the north side, which has been to a great extent choked
with mud. It is connected with all the surrounding villages and plantations by
good roads lined with palm-trees. Most of the Santa Cruz negroes belong to the
religious sect of the Moravian Brothers, who have for generations ministered to
them, and who were themselves at one time slave-owners. Their apostolic zeai
had strangely degenerated since the days of the first missionaries, Leonard Dober
and Tobias Leupoldt, who had sold themselves into bondage in order to evangelise
their fellow-slaves.

The emancipation of the blacks was proclaimed in 1848; but the freedmen
complain that the promised lands have not been assigned to them, More than once
partial insurrections have broken out, but have always been sternly repressed.

Fig. 211.—View TAKEN rw Santa CRUZ IsrAND.

SANTA CRUZ. 435

In 1878 the town of Frederikstæd, on the west coast, was burnt by the insurgents.
In recent years large numbers have emigrated, and in the single decade from
1871 to 1881 the island lost nearly one-fifth of its population. This emigration,

due to the decadence of St. Thomas, and the depreciation of agricultural produce,

partly explains the large excess of females over the males in the Danish islands.
The governor resides alternately at Santa Cruz and St. Thomas, six months ©

in each place.

436 MEXICO, CENTRAL AMERICA, WEST INDIES.

TorToLA.

Tortola, largest of the English possessions in the Virgin group, is disposed 1m
form of a crescent north-east of St. John. It is an elevated land, traversed in its
entire length by a ridge which culminates in a peak 1,800 feet high. A chain
of islets and reefs, beginning in the island of José Van Dyck, north of Tortola,
sweeps round to St. Thomas, while another barrier reef diverges from St. John
towards Virgin Gorda, enclosing with Tortola a vast basin of smooth water.
Sailing over this almost landlocked inland sea, far removed from the heaving
ocean, the traveller descries at intervals between the cliffs of the encircling
islands the distant prospect of the open sea with its restless line of breakers.

After being a stronghold of the buccaneers, Tortola was for a time occupied
by a number of Quakers, who emancipated their slaves and made them grants
of land. But they had no imitators, and after the abolition of slavery the plan-
tation negroes emigrated in swarms to St. Thomas and other islands. The
impoverished whites also left, and the population rapidly fell from 11,000 to 4,000.
Road Town, the capital, lies on a creek in the ‘ Road of the Virgins,” as the
inland sea is generally called ; pineapples are the chief produce of the district.

Virein Gorpi—ANEGADA.

Eastwards stretches Virgin Gorda, called by the sailors Spanish Town, a word
which the negroes have corrupted to Penniston. Its arid heights are almost
uninhabited, though one of the isthmuses guarding the approach te the inland sea
was till recently defended by a fort.

The north-east point of Virgin Gorda is continued by a line of reefs developmg
a semicircular rampart along the margin of the submarine plateau, and terminat-
ing in the long island of Anegada, or the “ Drowned.” This flat low-lying land
is so named because it is often half submerged during high tides im stormy
weather. But the central part does not appear to have ever been under water.

The dangerous reefs of Anegada have often been strewn with wreckage, and
the crews of vessels east on these rocks have seldom escaped with their lives.
According to a local legend, a Spanish galleon laden with gold and silver was
lost on this island, and the treasure deposited by some of the survivors ina cave
in the interior. But though often searched for by the buccaneers and inhabitants
of the neighbouring islands, the stores of gold and silver have never been
discovered.

The Virgin Islands are a Crown Colony.

À
iM
hy!

CEHRPTERETE
THE BAHAMAS.

WHE island-studded submarine plateau which has preserved its
Indian name of Bahama is also known by the designation of
Lucayas ; this term, which might be supposed to be derived from
the Spanish word, cayos, “ reefs,” is also of Indian origin. Abaco,
one of two large southern islands, bears the name of Yucaya,
or Lucaya, a word which has been extended to the whole archipelago.

The Bahamas stretch north-west and south-east between the Florida and San
Domingo waters a total distance of 780 miles. The English, political masters of

the archipelago, comprise under this designation the northern and central groups
alone, excluding the Caicos ard Turks Islands, which stand on the southern part
of the coral plateau. But this arbitrary division can in no way be justified, for
the Bahamas, with the Caicos and Turks’ groups, constitute a perfectly distinct
geographical region, all the members of which have the same general aspect and
the same geological origin.

The actual land surface is somewhat larger than Jamaica; but it is quite
impossible to determine the number of islands, which change with the storms, and
almost with every tide. During spring tides some of the islets become decomposed
into several fragments with intervening channels, while others disappear altogether
below the surface ; at low water the process is reversed, and whole clusters again
become united in continuous land. According to Bacot,* the Bahamas, excluding
the Caicos and Turks groups, comprise 690 islands and islets, and 2,387 rocks or
separate reefs, with a total area of 5,600 square miles. With the Caicos and Turks
the actual number can scarcely be less than 3,200, of which only 31 were inhabi-
ted in 1890, with a total population of 54,000.

Historic Survey.

The Bahamas were the first islands of the New World discovered by Columbus,
who landed at Guanahani, re-named by him San Salvador. But he did not
determine the position of this island with sufficient accuracy to identify it with
absolute certainty. The Spaniards, eager to discover treasures, made no stay
on these coralline rocks, and continued their route towards the “Indies” in search

of gold and diamonds.
* The Bahamas, a Sketch.

438 MEXICO, CENTRAL AMERICA, WEST INDIES.

But the rumour had been spread that one of the Bahamas possessed a treasure
far more precious than gold or silver, that marvellous ‘fountain of rejuvenes-
cence’ which was fabled to restore vigour and health to old age. At all times
the myth had haunted the popular imagination, and the poets and painters of
this epoch, itself an epoch of “renaissance,” had endowed the mysterious “ spring
of life ” with a sort of reality. It had now only to be discovered, and the men

Fig. 212.—Brmint ISLAND AND Banks,
Scale 1 : 950,000.

“Elbow hank

= the 74 —————
SOAP AINE Fe ya stle 226
= =— ¥ =
=== SS - —Murnings-Knolt-
79°10° West of Greenwich
Depths.
0 to 10 10 to 32 32 to 320 320 Feet
Feet. Feet, Feet. and upwards.

18 Miles.

who had found a new world naturally seemed destined to eclipse their astonishing
achievement by this last and greatest of triumphs. Pagan and Christian ideas
were intermingled in their fancy, and as Columbus thought he had re-discovered
the earthly paradise, Ponce de Leon hoped to quaff the source of immortality
spoken of in all the mythologies. In 1512 he sailed from Puerto Rico with three

THE BAHAMAS. 439

vessels to tread the maze of the Bahamas in search of the miraculous fountain. His
weary search was in vain, and when his successor, Perez de Ortubia, at last
reached the long-sought islet, one of the Bemini reefs on the east side of Florida
Passage, the thin thread of water springing from the rock was found to possess
no efficacy.

These pioneers, who fancied themselves predestined to recover the Garden of
Eden, must have formed strange notions regarding the abode of bliss, for they
began their work by enslaving and destroying the natives. They formed no
settlements on these flat Bahaman rocks, but they endeavoured to “exploit ” the
inhabitants by transporting them to the plantations and mines of the other
Antilles. In 1509 King Ferdinand authorised the sale of the Lucayans, and
forthwith the unhappy victims of Spanish greed were hunted like game, and
even tracked with bloodhounds ; in this way a few years sufficed to depopulate the
whole archipelago.

Attempts were especially made to utilise the marvellous diving powers which
the islanders shared with the inhabitants of Micronesia. The molluscs visible on
the marine bed through the depths of the clear waters supplied the Lucayans with
much of their daily food. For every meal they had but to dive amid the corals
and algæ of the marine bed, and bring up a fresh supply. Accordingly, a high
price was set on these skilful divers by the Spanish owners of the Cumana pearl-
fisheries on the South American coast. As much as 150 ducats was paid for a
single adult ; but in a few years not one remained, and at present but few traces
can be found of their former existence.*

On reaching the Caicos group the first English settlers are said to have picked
up a few Indian skulls in a cave; they also found various objects of the old
industries, especially earthenware, as well as a stone hatchet on which had been
carved a dolphin’s head. In Crooked Island other stone weapons have been met
in large numbers, all wrought from a silicious stone not occurring in the Lucayas
themselves. Hence they must have been obtained by trading with the other
Antilles or the neighbouring mainland, which necessarily supposes a certain
degree of civilisation on the part of the islanders.

After the disappearance of the natives the archipelago was deserted for over
a century, though still regarded as belonging to Spain. But when the coast of
Carolina was occupied by English settlers, the Bahamas were regarded as a
natural dependency of the new colony, and the labyrinth of reefs and islets
seemed admirably placed for surprising passing Spanish vessels laden with
merchandise and the precious metals. Adventurers of all sorts lurked in ambush
about the straits, and the trade of the ‘‘wreckers and rakers”’ had as the centre
of its operations the port of New Providence, which was “ providentially”’
situated at the converging line of two oceanic routes.

From time to time the Spaniards of Cuba sent expeditions to destroy this nest
of pirates; but after their departure the “trade” was always revived by fresh
comers. At last the islands were permanently occupied by British troops in 1718,

* MacKinnen, 4 Your through the British West Indies.

440 MEXICO, CENTRAL AMERICA, WEST INDIES.

but no serious attempt was made to cultivate the land till after the American
War of Independence, when some loyalist planters removed with their slaves to
the archipelago.

PuysicaAL FEATURES.

While the Bahamas remained in the power of the corsairs the true form of .
the various groups necessarily remained unknown. But since the establishment
of legitimate trade their outlines have been revealed and reproduced in admirable
marine charts. The contour lines of all the clusters and of the submarine banks
on which they rest are now known in full detail. Taken as a whole the Bahaman
plateau may be compared to the island of Cuba, which it greatly exceeds in
extent. Like Cuba, it is an insular mass of great length, but relatively narrow,
fringed by countless reefs and indented by deep inlets.

The geological formation is also the same, except that Cuba is already old
and increases but slowly, whereas the sister island is being built up under our
very eyes by the incessant work of the coral-builders. The land already above
water is all composed of whitish calcareous rocks fused in a homogeneous mass
differing in age alone from the ragged coralline reefs mingled with sands and
broken shells which line the beach. The rock grows continuously on its outer
or seaward face, where the structures of the animalculæ rise gradually higher
and higher, and become consolidated by their very rupture, thanks to the
calcareous cement by which the broken fragments are again soldered together.
Thus the British frigate Severn, wrecked on a reef of the Turks group in 1793,
is now completely encrusted with a rocky coating of still living coral.

In the neighbourhood of the same islands, as well as at some other points
round the periphery of the plateau, certain reefs, known by the name of coral-
heads, affect the form of huge mushrooms shooting up from the depths of the
sea. The stems, from 30 to 50 feet high, with an average width of about 16
feet, support extensive heads or platforms 300 or 400 feet in circumference, which
are exposed at low water. Ebb and flow being very slight in these waters, the
polyps are able to build up their structures without much disturbance from the
waves. At last the stony piles coalesce together, leaving below them submarine
caves and galleries, where the water, rushing in, drives the confined air forward,
and reappears farther on in broad sheets of foam. Whipple relates that a
wounded whale escaped by plunging into one cavernous recess and emerging
some distance off at the other end of the reef.

Since the polyps have been at work the relative level of land and sea has
undergone little change, for the mean elevation of the islands above the Atlantic
tides scarcely exceeds 7 or 8 feet. In some the surface is slightly undulating,
or disposed in receding terraces with rocky escarpments indicating the old shore -
line. The whole system culminates in a hill in Cat Island, which is scarcely
400 feet high.

But despite their low elevation above the surface, the islands present pro-
digious altitudes, measured from the ocean bed. In this respect the Bahamas

THE BAHAMAS. 441

are almost unique, for their rocky walls rise at angles of 50 or even 35 degrees
from abysses 2,000 to 2,500 fathoms deep. The oceanic basin is everywhere
abruptly limited by this coralline rampart, which forms an advanced coast-line
of the mainland, deflecting the Atlantic currents towards the north-west; to this

Fig. 213.—Tonaue or THE OcEaAN.
Scale 1 ; 2,500.090,

—S=S=S=SS__=_=_
SSS ei
SS 2/72 202

Depths.
_0 to 16 16 to 3,200 3,200 Feet
Feet. Feet. and upwards.

60 Miles.

general movement of the ocean stream, sweeping along the sands, living organisms
and other materials used by the corals in the construction of their buildings, the
islands and chains of reefs doubtless owe their elongated form, disposed in the
direction from south-east to north-west. Where the current gains access through
open breaches it develops graceful curves in the interior of the archipelagoes,

442 MEXICO, CENTRAL AMERICA, WEST INDIES.

forming either straits or sounds, such as Providence Channel, and farther south
those of Crooked Island, the Caicos and Turks groups, or else land-locked inlets
such as Exuma Bay and the Tongue of the Ocean east of Andros. These long
lines of solid rock, whose form and disposition depend on the action of fleeting
waters, are one of the most remarkable phenomena of physical geography.

In the direction from east to west, that is, from the Atlantic towards the
entrance to the Gulf of Mexico, the Bahaman plateau decreases in altitude; the
upraised lands grow less numerous, the shallows more extensive, until at last
the whole submarine bank becomes separated from Haiti and Cuba by a profound
trough with abysses of over 2,000 fathoms in the east. But towards the west
it again shoals a little to form the Old Bahama Channel, and farther on the
Santarem Channel, continued northwards by the New Bahama Channel, better
known as Florida Strait.

West of Santarem Channel, quite beyond the Great Bahama Bank, and
midway between Cuba and the Florida reefs, is situated the triangular plateau of
Cay Salt Bank (Salt Cay or Key),* which is everywhere encircled by marine
waters over 300 and towards the west over 600 fathoms deep. This bank affects
somewhat the form of a saucer, with depths of from 4 to 6 fathoms in the central
parts, which are enclosed by an outer rim either of submarine shoals or of
upheaved reefs, some bare, others covered with moving sandhills. The encircling
reefs, formed of corals and shells fused in a conglomerate mass by a calcareous
cement, receive the deposit of fine sands washed up by winds and waves, and
develop little dunes 15 to 20 feet high wherever the reefs offer a sufficiently
broad foundation. A curious effect is produced by these isolated sandhills rising
in the very midst of the marine waters, those of recent formation resembling
ships under sail, but the majority already bound fast, anchored so to say, by
trailing plants and lianas (batatas üittoralis), which spread their firm network of
green meshes over the shifting sands. The bank takes its name from Salt Cay,
the largest of the group, so called from a salt-water lagoon in the centre. This
lagoon takes a slight orange tinge from a little seaweed which grows in dense
masses round the margin, and which resembles putrid flesh both in appearance
and odour.

Being formed like Yucatan of fissured coralline limestones with numerous caves
or cavities, the upraised parts of the Great Bahama Bank are destitute of springs
or running waters. Andros alone, on the west side of the Tongue of Ocean, has a
few brooklets, or rather marshy rills. At high water this island becomes divided
into three separate fragments. Asin Yucatan, the rainwater is collected in under-
ground reservoirs, though in many places the neighbouring marine waters filter
through and render the lacustrine basins quite brackish. In some of the islands
the tides penetrate into the wells under the fresh water, causing a slight rise and
fall with flow and ebb. Before these wells were sunk the early settlers still found
sufficient potable water in a plant of the mistletoe family (viscum caryophylloides),

* The Spanish cayo takes the form of cay in English and fey in American geographical nomen-
clature ; hence Salt Cay and Key, Key-West, Marquesas Keys, «ce.

THE BAHAMAS. 443

which grows on the branches of several kinds of trees. During the rains it became
saturated and when squeezed like a sponge yielded a considerable supply.

FLoRA AND FAUXA.

Despite the apparent aridity of these calcareous lands, the Bahamas have a
remarkably rich flora, supported by a rainfall exceeding 40 inches in the northern
islands, a saturated atmosphere and underground reservoirs. The negroes pre-
pare the ground for tillage by breaking up the crust of the rocks with crowbars,
and reducing it toa fine powder, which forms the vegetable soil. The large
islands, and especially Andros, have extensive forests composed of the same
species as those of Haiti and Cuba. Mahogany was very common at the time of
the first settlement, and the United States pitch-pine ranges as far south as
Nassau, about the parallel of the southern extremity of Florida.

In its land fauna the Bahama group differs in no respect from Cuba, except
that its birds of passage, migrating between North America and the Lesser Antiiles,
are more numerous. The sparrow, recently introduced, has multiplied so pro-
digiously that the legislature has offered rewards for the heads and eggs of this
troublesome intruder. Turtles and fishes, several locally bearing the same names
as different European species, abound in the creeks and marine caves, and to the
countless shells (conchs) of the Bahaman waters the islanders are indebted for
the nickname of “ Conchs ” by which they are known in the West Indies.

Some of the deeper basins, better sheltered by encircling reefs, have received
the name of “ gardens of the sea”’ from the lovely growths of polyps which float
on the heaving waters, expanding and closing their beautiful blossoms at the
passage of the bright-coloured fishes. The crocodile, elsewhere confined to sweet
or brackish waters, is an inhabitant of the Bahaman seas, although not found in
the southern Antilles; its flesh is much appreciated by the islanders.

INHABITANTS.

The great bulk of the Bahaman populations are negroes, who, unlike those of
the other West Indian archipelagoes, are said to have preserved the tradition of the
African peoples whence they have sprung. Thus the coloured ‘‘ Conchs ? appear
to be still divided into Yoruba, Egba, Ebo (Ibo) and Congo groups, each tribe
annually electing its own ‘“ queen,” and recognising her authority in the admi-
nistration of local affairs.* Although slavery is abolished, racial distinctions are
maintained with the same tenacity as in other regions where Anglo-Saxon and
negro communities dwell side by side. The blacks are even virtually excluded
from the Protestant churches, although most of the whites are Methodists, and
consequently less exclusive than Anglican congregations.

By a system analogous to the Mexican peonage the traders hold the coloured
proletariate class in a kind of servitude, giving them small advances of provisions

* Powles, The Land of the Pink Pearl.

444 MEXICO, CENTRAL AMERICA, WEST INDIES.

and clothes in return for their future labour. The creditor takes care that the debt,
limited by the law of 1885 to ten shillings, is never extinguished, while the debtor
is also required to sign the “ seamen’s articles ” binding him to join a ship’s crew
whenever called upon by the magistrate. Of all the blacks the most wretched are
those engaged in the sponge-fisheries, and none draw their wages in cash except
those seeking employment on the neighbouring American coastlands.

ToPoGRAPHY.

Great Bahama, which lies nearest to the mainland, and which probably gave
its name to the whole archipelago, long remained unoccupied and even still is one
of the least densely peopled. The few planters are of Scotch descent. The contour
lines of this island harmonise with those of its eastern neighbours, Little and Great
Abaco, which were formerly called Yucaya or Lucaya, a name that has also been
extended to the entire insular group. -Great Abaco is one of the most thickly
peopled members of the archipelago. Its inhabitants (3,610 in 1881) are whites,
all descendants of the American loyalists, who, to preserve the purity of the race,
have always intermarried within the same family circles; hence, according to
passing observers, a marked physical degeneration of the race. Hopetown, the chief
village, occupies a long narrow peninsula between two seas, where its little houses
are interspersed amongst the palm-groves.

The little cluster of the Berry islets at the western entrance of Providence
channel is occupied by a few pilots on the look-out for vessels plying in the dan-
gerous passages between the Atlantic and the Gulf of Mexico. The more intri-
cate channels are provided with lights, and on Florida Strait, near the famous
Bemini islets, stand the magnificent lighthouses of Isaac Cay and Gun Cay.

New Providence contains over 15,000 inhabitants, nearly one-fourth of the
whole Bahaman population. This old nest of pirates has been selected by the
British Government as the official capital, and, thanks to its.central position, it has
become the chief commercial mart of the archipelago. The port of Nassau, called
also New Providence, has a depth of over 16 feet ; it lies on the north side of the
island, and would consequently be exposed to the full fury of the trade winds but
for the shelter afforded by a chain of reefs known by the name of Hog Island.
Nevertheless, during the hurricanes, which visit these waters about every four
years, vessels in the roadsteads have occasionally been hurled over the reefs and
stranded on the coast.

During the War of Secession Nassau almost suddenly acquired great wealth,
thanks to the blockade-runners, who made this place one of their chief headquarters.
The dangerous traffic began in 1861, when a Confederate vessel, with a cargo of 140
bales of cotton, ran the blockade and reached Nassau, a distance of about two days
by steam. The vessels, chosen from the swiftest of the British commercial fleet,
usually sailed from Nassau laden with all kinds of war materials, and when suc-
cessful brought back a cargo of cotton. During the five years of the war 397 ships,
of which two-thirds were steamers, entered Nassau after running the blockade,

— ee

— |
=!

GENERAL VIEW OF HOPETOWN, ABACO ISLAND.

TOPOGRAPHY OF THE BAHAMAS. 445

while 688 sailed from this place chiefly for the Confederate seaports of Charleston
and Wilmington. The last venture reached Charleston safely, but was captured
in the harbour, which had just been taken by the Federal troops. The risk was
tremendous, and 42 steamers altogether were taken, while 22 ran on the rocks to
escape capture. But the profits were correspondingly great, and towards the end of
the war both captain and pilot received £1,000 a trip, besides a few bales of cotton
“bought for its weight in gold.” The trade of Nassau increased thirtyfold, but
it drew all hands from the fields, which have been mostly invaded by the busk.
After the storm and stress period Nassau has resumed its modest réle as a
little centre of distribution for fruits and molluscs. In winter it is frequented

Fig. 214.—Nassav-
Scale 1 : 38.000.

+ rip
M ro ae
West of Greenwich 77°22"
Depths.
0 to 16 16 to 32 32 Feet
Feet. Feet. and upwards.

1,100 Yards,

by invalids from the States, although the climate is at times severe, while the
natives themselves suffer considerably from diseases of the respiratory organs. In
general the Bahaman climate is most efficacious for nervous affections.

The American winter visitors reside especially at Dunmore, in the little
Harbour Island, near the north-east angle of the long hook-shaped Eleuthera.
Harbour Island, the “ Montpellier of the Bahamas,” is the only member of the
archipelago which is densely peopled relatively to its extent, a circumstance due
to its healthy, bracing air. Its 2,000 inhabitants, concentrated in a space scarcely
two square miles in extent, are proud of their descent from the buccaneers, and

- still observe the old rule respecting land tenure: the cultivator alone is recog-
nised as the owner, and only of so much as he actually tills. He is not permitted

446 MEXICO, CENTRAL AMERICA, WEST INDIES.

to enclose his plot, and may be dispossessed by the first comer the moment he
ceases to work it.

Some of the planters of Eleuthera reside in Harbour Island for the con-
venience of its excellent anchorage; here they ship large quantities of the
exquisite pineapples grown on the more fertile soil of the larger island. Eleuthera
takes its name from the e/euthera croton, a drug formerly much in vogue in the
European pharmacopeia. Conservative physicians long preferred the bark of
this plant to that of the cinchona as a specific against fevers.

Cat Island, so named from the domestic animal, which since its introduction
has here run wild, resembles Eleuthera in form but presents a less graceful

curve and a more elevated surface.

Fig. 215—WATLING ISLAND. By many writers it has been identi-
ao LUE fied with the Guanahani (San Salva-

dor) discovered by Columbus in 1492 ;

a country residence even bears the

name of Columbia, as standing on

the very spot where the navigator first
landed in the New World. Since 1625,

when this identification was first em-

bodied in Joannes de Laet’s map of
the New World, Cat Island long
figured on all documents as the real
Guanahani, and both Washington
Irving and Humboldt lent the support

of their great authority to the same

view.
But at the end of the last century
the flagrant contradictions between

the accounts of Columbus’ voyage, as

74°40"

given by himself and reproduced by

= = — == Las Casas, and as described by Wash-

Oto 100 100 to 500 500 to 1,000 1,000 to 2,000 2.000 Ftms. : vin o ise t

ne Rete ot Nae ee ee ington Irving, gave rise to doubts
12 Miles. and to fresh theories. The nearly

uninhabited Watling Island, about
50 miles east of the southern extremity of Cat Island, was substituted by Muñoz
for the latter, and this view, afterwards supported by Bezher, Peschel and Major,
has long been accepted as the more probable. Navarrete, another Spanish historian
of the New World, suggested a third and totally different route, according to
which Columbus first landed at Great Turk Island, far to the south of the Great
Bahama Bank. Lastly, Varnhagen found the “true Guanahani” in Mariguana,
about midway between Watling and Turk.
Such were the various hypotheses prevalent down to the year 1880, when the
American navigator, G. V. Fox, perfectly familiar with the Bahama waters,
made the discovery of a fifth Guanahani, which really seems to be the right

TOPOGRAPHY OF THE BAHAMAS. 447
t

one.* Still it is impossible to speak with certainty, for the new theory is far from
solving all the difficulties. Samana or Atwood Cay, the island indicated by Fox,
must certainly have undergone considerable change during the last four centuries ;
its east point must have disappeared by erosion or subsidence, while the inner
lagoon spoken of by Columbus must have dried up, if this be the first land
reached by him. But from Samana to Cuba the coincidence between Columbus’
log and the itinerary assumed by Fox is all but complete.

Cat Island, notwithstanding its fertility and size—165 square miles—was
found to be entirely abandoned in 1785, when over 100 loyalists from the United
States occupied it with their slaves. At present it has a population of over
4,000. Watling and Rum Cay, its eastern and southern neighbours, as well as
the narrow limestone reefs of Great Exuma and Long Island, are also inhabited
by small communities.

South-eastwards follow the three islands of Fortune, Crooked and Acklin,
which really constitute a single island, divided by channels fordable at low water.
Fortune has become the most flourishing of all the Bahamas, and the rival of
Nassau as a port of call for steamers plying between New York, the West Indies
and the Hispano-American coastland.

Andros, the largest member of the archipelago, is usually spoken of as a
single island, although in reality forming a group of several islets separated by
shallow sounds and straits. The group, which is the most densely wooded of all
the Bahamas, represents more than a third of all the dry land of the archipelago ;
it is, moreover, conveniently situated near Nassau, the capital, and between the two
channels which converge westwards to form the entrance to the Gulf of Mexico.
But Andros is of difficult access, and much of the surface is covered by swamps and
brushwood.

Great Inagua, at the southern extremity of the Bahamas, occupies a position
somewhat analogous to that of Andros opposite Windward Channel; but it is
almost uninhabited. According to MacKinnen it owed its name, originally
perhaps Iguana, to these reptiles, which abound in all the Bahaman islands.
On the side facing Cuba the most thickly-peopled land is the so-called Great
Ragged Island, lying in the chain of reefs called by the Spaniards Cayos Jumentos.

The circular Caicos bank east of Inagua is fringed by a few inhabited islets.
The Turks islets, belonging to the same group and lying still farther east, have
also received a few settlers. Here the prevailing vegetable form is a species
of dwarf cactus (cactus coronatus), familiarly known by the name of the “ Turk’s
head,” having somewhat the appearance of a head with white hair wrapped in a
turban. Hence the name given to this south-easternmost cluster of the Bahamas.

Economic CONDITION OF THE BAHAMAS.

The population increases but slowly, being affected by all the vicissitudes of
trade, good and bad harvests, and hurricanes which ruin the crops and enrich the

* An Attempt to Solve the Problem of the First Landing-place of Columbus. United States Coast and
Geodetic Survey, Report for 1880.

448 MEXICO, CENTRAL AMERICA, WEST INDIES.
4

wreckers. There is scarcely any immigration, so that the increase is almost
entirely due to the relatively high excess of births over the mortality. The chief
produce are fruits, such as pineapples and oranges, raised for exportation either
in the natural state or in the form of preserves. The products of the fisheries
—turtles, shells, pearls, ambergris, and especially sponges—also contribute to
the commercial prosperity of the natives. The large shells intended for the
cameo artists are sent chiefly to France. According to Powles 500 smacks, with
average crews of eight men, are engaged in the turtle and sponge fisheries.
Salt is also a considerable source of wealth, especially in the Caicos and Turk
groups. The salt-pans recently conceded to various companies might suffice to
supply the whole of the United States with marine salt but for the prevailing heavy
tariffs. Thanks to the salt-works the trade of the Caicos and Turks Islands is
relatively much greater than that of the other Bahaman groups.

The attention of planters has lately been directed towards the cultivation of
henequen, or “Sisal hemp,” and analogous varieties known in the Antilles by
the general name of farata. These plants thrive in the Bahamas fully as well
asin Yucatan, and the 330,000 acres recently granted to capitalists are being
rapidly planted.

About two-thirds of the foreign trade of the Bahamas is carried on with the
United States, especially New York and Key West.

ADMINISTRATION.

The government of the Bahamas is entrusted by the Crown to a governor, assisted
by an executive and a legislative council, both composed of 9 members. The repre-
sentative assembly comprises 29 deputies, nearly all New Providence merchants
elected by owners of property. The assembly is, in fact, a sort of club where
the white aristocracy meets in the capital.

The Caicos and Turks groups depend on the Jamaica Government, and are
administered by a commissioner and a council of 5 members.

The annual budget of the Bahamas exceeds £40,000, while that of the Jamaican
dependencies averages £10,000. The latter have no debt, but the former are
burdened with a public charge of £80,000. Education, though not obligatory, is
general amongst tie blacks and people of colour as well as amongst the whites.

CHAPTER XIE

THE BERMUDAS.

HE little Bermudas group, which rises in absolute isolation above
the Atlantic abysses, still bears under a slightly modified form
the name of the Spanish navigator, Bermudez, by whom it was

discovered about the beginning of the sixteenth century. Some
hundred years later it was re-discovered by Somers, an English
explorer who had deviated from the usual track. Henceforth the archipelago
frequently took the name of Somer’s Islands, sometimes changed to Summer
Islands, as if in reference to their mild climate, described as an “everlasting
summer.” But the name of the first discoverer ultimately prevailed.

The group lies in the broad Atlantic about 600 miles east of Cape Hatteras,
the nearest point on the North American mainland. The distance is much
greater from the Bahamas, although the Bermudas belong rather to this archi-
pelago than to the continent so far as regards the aérial and marine currents,
which set either north-east and south-west or south-west and north-east. In
the same direction are disposed the submarine plateaux on which stand the
Bermudas and their prolongation, the Challenger and Argus banks. The axis
intersecting the diameter of the Bermudas would also traverse the two south-
western banks, while its extension would about bisect the chain of the Bahamas.

PuysicAL FEATURES.

Altogether the Bermudan islands and banks form a nearly regular oval stretch-
ing north-east and south-west a distance of about 23 miles; but only a very
small part of this space is occupied by dry land. The whole plateau enclosed by
the six-fathom line comprises a superficial area of 264 square miles, whereas the
Bermudas properly so-called have an extent of only 20 square miles at low water,
that is, scarcely one-thirteenth of the rocks raised from the abysmal depths by
the coral builders. The portion rising above sea-level is disposed along the
eastern margin of the Bermudan plateau, and then bends round southwards in
the form of a hook. It consists of one island, with sharp headlands projecting
westwards like the horns of a beetle, and of some fifteen narrow islets disposed
in a line with Great Bermuda. Including all the upheaved reefs, the cluster
comprises at least 150 distinct rocks, and “more than the days in the year,”

450 MEXICO, CENTRAL AMERICA, WEST INDIES.

reckoning all the points of coral exposed at low water. Extensive basins or
sounds offer here and there perfectly sheltered anchorage, but for the most part
communicate with the open sea only through dangerous winding passages.

The oval curve of the island is itself inscribed within a larger oval, which on
the south-west, west and north sides consists merely of submerged plateaux which
form a circular rampart against which the waves break; the whole system thus .
presents a dangerous circuit of coralline reefs, interrupted by a few “cuts,” or
navigable openings. The Narrows, as the chief entrance is called, have a depth
of 26 feet, and give access from the north-east to the central basin, which has a
mean depth of 50, and, in the deeper cavities, of over 80 feet.

The whole periphery of the outer banks, a distance of about 40 miles from the
Narrows to the southern convex side of the large island, presents at low water
nothing but three rocks, 8 to 10 feet high, rising like monoliths on a horizontal
ledge almost perfectly levelled by the action of the waves. Serpule grow in
countless masses on the outer edge of the reef, encircling it with a rampart which
resists the fury of the Atlantic billows.

The various coralline groups composing the great mass of the plateau affect
the form of craters, hollow in the centre, and completely encircled by an elevated
rim. Like those of the Bahamas and the Pacific ocean, they are so many little
atolls grouped together in large systems, which merge in one vast complexity
of islands and banks, the atoll of atolls. The existence of coralline reefs under
such a high latitude, north of 32° N., or some 2,300 miles from the equator, is a
unique phenomenon due entirely to the influence of the Gulf Stream, which brings
the tepid waters of the Caribbean Sea, and with it the minute organisms that have
gradually built up the structure of the Bermudas in depths of 1,500 and 2,000,
and in one place even 2,500 fathoms. The climate, however, is too cold for some
species of coral-builders, which, nevertheless, are very common in the Bahaman
waters. The reefs themselves differ greatly in size, and are separated by shallow
troughs, and even by navigable channels.

According to most naturalists, the Bermudan archipelago is one of those
whose phenomena agree best with the hypothesis of Darwin, who explains the
continuous growth of the reefs on banks several thousand feet high by the gradual
subsidence of the submarine pedestal. Certainly no change of level has taken
place since 1843, all the navigable channels having remained the same. But if
early records can be credited, the islands were much larger when first discovered
than at present. In 1870, when the great graving-dock was constructed in
Ireland Island, on the west side of the group, at nearly 50 feet below ebb tide, the
workmen came upon some peat and vegetable humus, which were exactly similar
to that on the surface of the existing islands, and which contained trunks of
“cedars,” land shells, and the remains of birds.

On the other hand, a relative upheaval may perhaps have taken place before
the subsidence, for the limestone cliffs of the islands exceed 160 feet in height.
Gibb’s Hill, at the extreme southern bend of Great Bermuda, whence a panoramic
view is commanded of a labyrinth of wooded headlands and verdant flats, stands

THE BERMUDAS. 451

with its lighthouse 400 feet above the sea. Nevertheless, the Bermudan heights
may possibly be due to the action of the winds, for these rocks, mostly granular
and friable, though hard and compact in some places, are in process of formation
under our very eyes, like the dunes of the landes in Gascony. Hence the geologist
Nelson has given them the name of “ Æolian rocks.” The moving sands of the
beach, stirred up by the winds and carried inland, become gradually consolidated

Fig. 216.—Tue BErmupas.
Scale 1 : 650,000.

Yia-slana

SOS Ran wera

a Aa

——

Horn SF LE
== = rat os “Ha

West of Greenwich

Depths.
0tod 5 to 50 50 Fathoms
Fathoms. Fathoms. and upwards.

12 Miles.

by a vesture of vegetation, while the fine calcareous dust of the slopes is partly
dissolved by the rains and transformed to a granular incrustation made fast by a
natural cement. Fresh sands, brought by the winds, are in their turn hardened
in the same way, and thus are formed regular stratified layers. There is not a
single roadside cutting in the Bermudas but presents a perfect section of these
thin scaly tufas, each recalling the geological work of wind and rain.

The red earth covering the soil in horizontal layers is also of recent formation,

452 MEXICO, CENTRAL AMERICA, WEST INDIES.

being derived from the disintegration of the surrounding rocks. It is composed
of substances found in the calcareous sands, and left as a residuum after repeated
rain washings. It thus belongs to the same class of fertile soils which are also
met in Cuba and other islands of coralline origin. The reddish clays forming
the marine bed in depths of over 2,000 fathoms, are similarly derived from the
remains of foraminiferæ, showered down in countless myriads from the surface of
the sea, and dissolved by the salt waters during their descent.

The porous nature of the ground facilitates the formation of this red earth,
which is continually dissolved by the rains percolating freely through the rocks,
Hence the surface waters nowhere develop streams, though they are here and there
collected in cavities near the shore. ‘Tidal wells,” as in the Bahamas, supply
drinking-water; but the rainfall itself is sufficiently copious to enable the inha-
bitants to depend on the cistern erected at the side of every dwelling.

CLIMATE.

Thanks to the Gulf Stream and aérial current setting in the same direction,
the climate of the Bermudas is warmer than might be expected from their latitude.
The mean temperature is about 70° Fahr., or nearly*four degrees higher than that
of Madeira, which lies under the same parallel. Between the coldest and hottest
months (February and June) the range is 27°, 60° and 87° Fahr. respectively
Thus, despite the tropical character of the climate, the alternation of the seasons
is well marked, being the result of the play of the shifting polar and equatorial
winds. It is probably to this periodical change, better regulated and extending
over a wider range than in Madeira, that the English residents in Bermuda are
indebted for their general good health; the average mortality amongst them is
23 per thousand, or about exactly the same as in England Tropical disorders
are rare, although in 1856 the white population was decimated by an outburst
of yellow fever introduced from the Virginian coastlands.

Like most oceanic islands, the Bermudas, despite their distance from the main-
land, do not constitute a distinct vegetable centre. The spontaneous flora, apart
from that introduced by man, consists exclusively of species brought either by
the Gulf Stream or by the south-west trade winds. Seen from the summits of the
eminences, the islands appear to be almost completely clad with a dark mantle

of “cedars” ( juniperus barbadensis), from the Lesser Antilles; they are always
associated with a verbena (/antana odorata), also from the Antilles, which has
driven out the native grasses. The rocks, being destitute of vegetable humus, are
clothed with the stenotaphrum americanum, a herbaceous plant from the Bahamas.
As in Cuba and Mexico, the shores are fringed with mangroves ; but the only
member of the palm family which grows freely is the palmetto sabal of Florida.
All the other palms are exotics, even the magnificent oreodoxa, which lines certain
avenues about the capital, and which the Bermudans are proud to show to visitors.
Both the date and cocoanut palms are grown, though the fruit seldom ripens.

Altogether, the vegetation, springing from a porous limestone soil, where the

sé ~, i a - =
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Fig 217.— View taken From GisBs Hitt, Bermupas.

THE BERMUDAS. 453

surface waters disappear rapidly, lacks the tropical exuberance attributed to it by
certain travellers. The more common European trees are nowhere seen in the

woodlands, whose general aspect is monotonous, recalling that of the northern

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pine-forests. But in the rainy season the masses of pink blossom covering the
acclimatised oleanders are suggestive of Sicilian scenery.

No indigenous mammals occur in the Bermudas, the rats and mice being of
European and the bats of North American or West Indian origin. From North
America come nearly all the other animals, of 188 species of birds 3 alone
belonging to the Old World. The solitary Bermudan reptile is also of American

454 MEXICO, CENTRAL AMERICA, WEST INDIES.

origin. Even of lower forms the native species are very few; not more than
about a dozen of the 170 marine molluses and less than half of the 30 land
molluses are peculiar to the archipelago, all the rest belonging to the West
Indian fauna.

INHABITANTS, TOPOGRAPHY.

At the time of the discovery the Bermudas were uninhabited. The present
population, of which three-fifths are full-blood or half-caste negroes, has been
introduced from the other British colonies, mainly since the abolition of slavery.
The increase is entirely due to the natural excess of the birth-rate over the
mortality. All are concentrated in three little towns and a few hamlets.

Hamilton, the capital, alone contains more than half of the islanders. It lies
on the south side of a long peninsula towards the centre of the large island; but
the harbour, deep enough to admit the largest vessels, is too exposed to the west
winds. The town is extremely clean, but offers nothing remarkable beyond its
gardens, its avenues and dazzling white villas relieved by the creepers entwined
round their verandahs. Even the roofs are regularly scrubbed and whitened
twice a year to prevent any impurities from being washed by the rains into the
cisterns. Reservoirs have been constructed at intervals to husband the overflow
for periods of drought.

St. George, at the northern extremity of the archipelago, is of more easy
access and safer than Hamilton. Vessels drawing 16 feet have no difficulty in
penetrating through a well-buoyed channel into the vast triangular basin, which
is entirely enclosed by islands and islets, and defended by forts and redoubts.

Formidable military works have also been erected at the other extremity
of the archipelago, where it curves round from east to south. An arsenal, a
citadel, barracks, fortified piers, pontoons, and a penal station with accommoda-
tion for 1,500 convicts, form an imposing group of somewhat uninviting
establishments on Ireland Island, at this approach to the Bermudas.

The Bermudas present too small a surface for extensive agricultural operations.
But the fruit and vegetable gardens cover a space of about 3,000 acres, where
potatoes, onions, and tomatoes are grown for the New York market. The maranta
arundinacea also yields a tapioca of excellent quality, but not in sufficiently large
quantities to remunerate the planters; hence this plant, as well as the orange
and lemon, has ceased to be cultivated. The industries are even of less import-
ance than husbandry. Formerly large vessels were built in the Bermudas, where
nothing is now produced except some small craft, furniture, and some smaller
articles, such as the wood for lead-pencils, made of the so-called “cedar,” or odori-
ferous juniper. The archipelago has a semblance of representative government
modelled on that of the United Kingdom, with governor, a legislative council of
9 members named by the Crown, and a chamber of 36 deputies elected by popular
suffrage.

EX | ou

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ATEN ail Wit

CHAPTER XIV.
THE LESSER ANTILLES.

NDER the general name of the Lesser Antilles are usually comprised
all the islands of the Caribbean Sea except Cuba, Jamaica, San
Domingo (Haiti), and Puerto Rico. But those fringing the Vene-
zuelan coast, including Trinidad and the neighbouring Tobago, are

too closely connected with the South American mainland, both in
their position, relief, and geological constitution, to be separated from that conti-
nent in a general geographical treatise.

In fact, the term Antilles should be restricted to the chain of islands which
develops a graceful curve from north to south, beginning at Sombrero and
terminating at Grenada and Barbados. It should also, strictly speaking, include
the Bird Islets (Aves), situated in the Caribbean Sea within the space enclosed by
the rampart of islands washed on the east by the Atlantic, but on a chain of
parallel banks which an upheaval of the marine bed would transform to a second
group of Lesser Antilles.

The English administration, misunderstanding the reports of navigators,
usually apply the expression ‘“ Leeward Islands” to the northern section of the
Lesser Antilles as far south as Dominica, and inclusive of the Virgin group. The
southern section from Martinique to Trinidad is in the same way grouped under
the designation of the ‘“ Windward Islands.” But these expressions are inaccurate
and misleading, for all the islands standing on the outer margin of the Caribbean
Sea are alike exposed to the action of the trade winds. Hence the terms, windward
and leeward, have no geographical meaning or any value except from the stand-
point of the British colonial administration. Even in this sense it is confusing,
for despite the official nomenclature, the French islands of Guadeloupe and
Martinique are members of the so-called ‘‘ Leeward” group.

. Altogether the Lesser Antilles, from Sombrero to Grenada with Barbados

but without the Aves, have a collective area of over 2,550 square miles, with a
population of about 800,000, which for the New World is exceptionally dense.
Since 1856 the Aves group, important for its rich guano deposits, has formed
part of the Venezuelan Republic.

Politically the Lesser Antilles are very unequally distributed. The two
largest, Guadeloupe and Martinique, with their dependencies, are French colonies,
but they do not form a distinct group, being separated by the intervening British

456 MEXICO, CENTRAL AMERICA, WEST INDIES.

island of Dominica. The British possessions, more numerous and collectively
more extensive than the French, form two main groups in the northern and
southern sections of the chain, besides the just-mentioned Dominica, whose
central position between Guadeloupe and Martinique makes it the most vital

Fig. 218.—Sr. Krrrs.
Scale 1 : 430,000.

62°50' West of Greenwich
Depths.
0 to 10 10 to 50 50 Fathoms
Fathoms, Fathoms. and upwards.

6 Miles.

strategic point of this insular world. A small group in the north-west over
against the Virgin archipelago belongs to Holland, but all the rest are British.

PuysicaL FEATURES.

The system of the Lesser Antilles does not forma single line, but two per-
fectly distinct chains. Of these the more important is that which extends from
Saba and St. Eustatius to Grenada, developing a curve of about 370 miles.

THE ,LESSER ANTILLES. 457

St. Christopher (St. Kitts) and Nevis may be taken as a typical specimen of the
general disposition of this inner or western chain.

The outer, about equal in length, sweeps round from Sombrero to Barbados.
Like the first it describes the are of a circle, but is disposed exactly north-
west and south-east in such a way as to form a tangent to the convexity of the
inner circuit. Guadeloupe is thus constituted a double island, belonging partly
to one, partly to the other system. A third line, scarcely indicated above the
surface, is revealed by Aves and the neighbouring shoals.

The main chain of the Antilles consist of elliptical lands with their long axis
disposed in the same direction as the chain itself. Each island has also its little
backbone which again follows the same general curve. The ranges culminate in
the three central islands of Guadeloupe, Dominica and Martinique; but all
members of the system are very elevated relatively to their limited areas; some of
the islets even constitute a single cone, rising many hundred feet sheer above the
surface, and in their very form betraying their igneous origin.

In general the mountains consist of porphyries and lavas, and evidently had
their origin on a submarine fault, whence they rose gradually above the sea. Some
are even still growing by the accretion of fresh eruptive matter.

But the outer range, from Sombrero to Barbados, is not volcanic, or at least
the igneous rocks thrust from the marine bed upwards have not yet reached the
surface except at a few isolated points. The plateau on which the islands stand is
almost everywhere covered with calcareous formations of oceanic origin. Nowhere
is the contrast between the two chains more striking than in the twin islands of
Guadeloupe, one elevated, bristling with craggy peaks, scored with lava streams,
abounding in running waters, the other low, or gently undulated, fissured with
crevasses and honeycombed with caves in which the waters disappear.

But if the calcareous range rests on a rocky bed, the igneous system itself is
not exclusively formed of eruptive matter, for these upheaved volcanic islands have
also their margins of oceanic origin. Round the base of the porphyry or trachyte
escarpments have been accumulated to a height of over 800 feet great masses of a
grey conglomerate, tinged with red and yellow, in which have been embedded huge
blocks that have toppled over from the upper slopes. This conglomerate had its
origin below the surface at a time when the sea-level was relatively higher than
at present. The marine formations deposited at the foot of the volcanoes now
stand above the sea in consequence either of a subsidence of the waters or of an
upheaval of the land. Should the movement continue, the banks of reefs or cays at
present encircling the submerged base of the islands will be seen to rise above the
surface, especially on the side facing the Atlantic.

The composition of the rocks is the same in the still flooded reefs as in the
already upraised cliffs; even in appearance they differ little, though the more recent
coralline growths are somewhat softer, and of a less yellowish colour. In some
places the conglomerates on the coast are interrupted by lava streams, and both of
these formations being contemporaneous, fragments of each are found embedded in
the different deposits.

458 MEXICO, CENTRAL AMERICA, WEST INDIES.

CLIMATE.

The climate of the Lesser differs little from that of the Great Antilles. The con-
trasts, in fact, are far more striking between the opposite slopes of the islands them-
selves than between the two extremities of the American Mediterranean. Those
members of the chain which are disposed in the direction of the meridian present
the most marked differences between the sides facing the Atlantic billows and
those washed by the still waters of the sheltered Caribbean Sea. In the French
colonies one slope takes the name of ‘‘ Capesterre ”’ (Cabesterre), the other that of
‘ Basseterre.”?

The climatic differences have caused great contrasts in the density of the popu-
lation, in the local industries and the trading relations. Endless diversity is also
caused by the mountainous character of the volcanic islands according to their
altitude and aspect. Withina few hundred yards of the burning coastlands the
inhabitants find a moderate temperature, the upland glens and _ breezy headlands
offering more salubrious atmospheric conditions, so that every island is provided
with its natural health resort. But in the various sections of the islands them-
selves the different temperatures present little variation throughout the year, the
glass nowhere rising or falling more than about 36 degrees.*

The-rainfall varies far more than the temperature, according to the different
aspects and disposition of the relief, in one place arresting, in another giving free
passage to, all moisture-bearing clouds. Thus the showers are more copious on the
Capesterre than on the Basseterre, and they also increase with the altitude. In
this respect a regular gradation may be observed, even in an island like Barbados
where the differences of relief are relatively slight.f Although not absolutely
unknown hail is even of far rarer occurrence than in Cuba; in Guadeloupe the
phenomenor has only been once recorded, in the year 1805.

Fiora AND FAUNA.

Forms from every division of the American mainland are intermingled in the
local flora, which is extremely diversified relatively to the small extent of the islands,
and which often presents considerable contrasts even in contiguous districts. Plants
from the Old World would also seem to have reached the West Indies even before
the arrival of the Europeans and their African slaves. Botanists, however, are far
from being of accord with regard to the origin of cultivated plants possessing para-
mount importance in the trade of the world. Certain varieties of sugar-cane are
known to have been imported; but the species found by the first French settlers

* Temperature of the Lesser Antilles :—

Rainfall,
Latitude. Mean. Min. Max. inches.
Guadeloupe (Pointe-à-Pitre) . : 16° 14’ 78° F. 67° F. 101. 43
Martinique (Fort-de-France) . : 142 365 Bile 63° 85° 84
Barbados (Bridgetown) ‘ d ISIS aye ide 64° 88° 62
+ Rainfall of Barbados :—-
Inches. Inches.
From sea-level to 200 feet . : 45 From 600 to 800 feet 60
From 200 to 400 feet . ; , 47 From 800 to 900 feet ; , 46

From 400 to 600 feet . Ë ; 48 From 1,000 to 1,140 feet. ; 47

FAUNA OF THE LESSER ANTILLES. 459

in St. Christopher, Guadeloupe, Martinique, and St. Vincent has always been
regarded by them as indigenous.

Similar doubts have arisen respecting the origin of certain animal species, such
as that of the monkey till recently surviving in the woods of Barbados. While
Schomburgk regards it as an American species, Fielden identifies it with the West
African cercopithecus callitrichus, presumably introduced from Guinea by the first
settlers, and found also in St. Kitts, Nevis, and Grenada.

Each island has its special fauna. ‘Of 128 species of birds collected by Ober
seven only are common to all the Lesser Antilles, while as many as 52 occur only
in one island. Barbados, of oceanic origin and never connected with the mainland,
appears to have received both its plants and animals by the winds, the marine cur-
rents, the action of birds and men. Some of the forms found in the Lesser Antilles
by the early colonists have already disappeared. Such was a large pigeon at that
time very common, but:now occurring only in the fossil state and in South America.
According to Darwin the modifying influence of the environment is shown
especially in the European butterflies, which become wingless in the West Indies,
where the wings would be a disadvantage, serving as sails for the winds to drive
them seawards.

Naturalists who study molluses and other lower orders discover endless examples
of strange contrasts between the local faunas. Certain forms found in remote lands
are wanting in the intermediate insular chains, as if the links belonging to different
periods of formation had been formerly connected by isthmuses to different conti-
nents. The existence of such limited biological areas is associated with the most
difficult problems of geology and natural history. A casein point is the bothrops
lanceolatus, a poisonous trigonocephalous snake confined exclusively to Martinique
and two other members of the Lesser Antilles, where it is much dreaded by the
natives. Besides man it has many enemies, such as the steel-blue covbo adder, the
ant which attacks its eyes, and the mungoos which devours body, fangs and all.
There are no less than eight varieties of this dangerous reptile, none more than
6 or 7 feet long, another nearly 10 feet long having disappeared since the last

century.
INHABITANTS.

At the discovery the inhabitants, all of Carib race, were distinguished by
their physical appearance, language and usages from the mild and peaceful natives
of San Domingo. They are described by the early writers as brave, fierce and
indomitable, rushing fearlessly on danger and boasting of their wounds, but
ferocious and pitiless towards their captives. They were even cannibals, possibly
on religious grounds, or to enhance their courage by devouring the heart of the
enemy. The first European visitors were horrified at the sight of human limbs
strewn on the ground, or hung on the doorposts, or roasting on spits.

Nevertheless, these fierce warriors were trustworthy friends, and faithful
observers of the duties of hospitality, at times risking death itself rather than
abandon their guests. They were also daring seafarers, venturing in their frail

460 MEXICO, CENTRAL AMERICA, WEST INDIES.

craft hundreds of miles from the land, and familiar with all the straits and coasts
from South America to the Great Antilles. Their habit was to land in small
bands, and surprise the village of some hostile tribe of the Guatuaios (Ineri or
Igneri) of Arawak race, and carry off the plunder, with the young men reserved
for the banquet or bondage, and the women for wives and drudges.

The Caribs appear to have reached the Lesser Antilles only one or two genera-
tions before the discovery. They have been regarded as Aztecs, Mayas, Peruvian
Quichuas or even Redskins from North America. But their traditions, as well
as their language and usages, point especially to Veneznela, Guiana and Brazil
as their primeval homes. They are, in fact, akin to the Galibi of Guiana and to
the Indians of the Xingu River recently visited by Ehrenreich.*

The national name has been diversely explained. In the Tupi language of

9) 66

Brazil, Cari-aiba is a collective name used in the sense of “ bad people,” ‘ pirates,”
or “cannibals.” But whatever its origin, it was ultimately adopted by the West
Indian Caribs themselves in a noble sense, for they even applied it to the whites
in recognition of their superior intelligence. Amerigo Vespucci states expressly
that the natives of the Paria coast called the Spanish navigators ‘“ Carabes,” in
this sense, and the French and Portuguese were also called “‘ Caraybbes, Caryba.”’

In the Antilles the Carib women spoke a peculiar language differing con-
siderably from that of the men, which was originally that of the Galibi who
overran the islands as far as Haiti. The female speech, on the contrary, was funda-
mentally that of the Arawaks whom the Galibi had vanquished, slaying the men
and capturing the women. Eventually this Arawak tongue acquired the pre-
ponderance, partly because the education of the children was in the hands of the
women, and partly also because it was a richer and more developed form of speech.

As the Caribs had “eaten” the Arawaks, so they were in their turn devoured
by the Spanish, French and English settlers. The history of every island,
especially Martinique, Dominica and St. Vincent, is a record of massacres, and
now only a few half-caste Caribs survive in the remote upland valleys of those
islands. Dominica appears to have about 30 such families, and in 1881 there
were 192 persons in St. Vincent calling themselves Caribs.

And now the white destroyers of the Indians might seem themselves slowly
succumbing, not to massacres, but to the climate and changed social relations.
During the period of colonisation the increase of the European element was
always due to voluntary or forced immigration. Most of the settlers were, in
fact, not “free inhabitants,” but ‘engaged ” or, rather, temporary slaves. Epi-
demics frequently swept away whole communities, and even since the colonies
have entered on a period of peaceful development the white mortality has often
exceeded the birth-rate, especially during the prevalence of yellow fever.f
Altogether decrease was the normal condition, so that the race seemed threatened
with extinction by the slow but pitiless hand of nature.

* Congress of Americanists, Paris, 1890.

+ Mean mortality of yellow-fever patients in Martinique from 1802 to 1869, according to Béranger
F raud, 232 per thousand.

INHABITANTS OF THE LESSER ANTILLES. 461

Nevertheless, there are indications that under favourable conditions the North
European may become perfectly acclimatised in the West Indies. As regards
the Spaniards and Canary Islanders there can be no doubt, as is evident from

Fig. 219.—A Marriniqve CREOLE Woman.

the rapid increase of the Puerto Ricans. But numerous instances can also be
adduced of French, Dutch, English and Scotch families persisting from genera-
tion to generation, and even distinguished by sound constitutions, great muscular
strength, rare physical beauty and brilliant intellectual qualities. A better know-

462 MEXICO, CENTRAL AMERICA, WEST INDIES.

ledge of hygienics, the increasing facilities of locomotion and frequent shiftings of
the population, with the establishment of health resorts at various altitudes, tend
to render the acclimatisation of all European residents more and more feasible.

The actual decrease of the white element, all the more striking when taken
in connection with the rapid increase of the blacks, is due rather to economic
and moral than to material conditions. During the plantation days the position
of the great landowners was that of masters, of superior beings belonging, so to
say, to a distinct humanity. But after the emancipation, when many of the
negroes acquired comfort and even wealth, when education tended to diminish
racial differences, and when the African claimed his place in the council chamber,
the heirs of the white aristocracy turned with repugnance from a land where the
slaves of yesterday arrogated to themselves equal privileges and political rights.
They preferred to withdraw without any intention of returning.

On the other hand the ‘little whites,” clerks, secretaries, government officials,
agents, are now thrust aside, unable to compete with their negro and mulatto
rivals. Officials swarm just as much in the English as in the other islands, and
in virtue of their very numbers the men of colour get elected to most of the
subordinate posts. In certain districts the whites, refusing the administration
of the sons of slaves, have completely disappeared. In this struggle for existence
probably more than one-fourth of the European element has been eliminated since
the middle of the century.

Their successful rivals are no longer full-blood negroes, but mulattoes or
“people of colour.” Miscegenation has become universal despite the unfavourable
initial conditions and the severe laws formerly interdicting such alliances. At
present the insular populations present every conceivable transition from sallow
white to glossy black, though the prevalent hue is a brown yellow, a fine bronze
tint, er even that of pale gold. Certainly this mixed race has not declined, and
the half-caste creoles especially of Martinique and Dominica are amongst the finest
in the Antilles.*

Since the emancipation, slave labour has been largely replaced by coolies
from India, who, being mostly British subjects, are protected by laws and stipula-
tions, which are much better observed than the regulations formerly controlling

> is charged to represent

the power of the slave-owners. A special “ protector’
the interests of the coolies, to visit them at least every three years, and to see that
the terms of the contract be strictly observed.

But few Hindus are now engaged, and years pass without fresh importations
of hired hands. The local population is already sufficiently dense, while the
natural classification of the people according to their pursuits enables the planters
to procure all the labour they require without introducing strangers. The coolies
who have chosen to settle in the islands, about 40,000 altogether, have mostly
taken to petty trading, and merge very slowly with the rest of the population.

As under the slave system, the Lesser Antilles continue chiefly to grow those
plants which yield the so-called “colonial produce;” but this produce varies

* L. Hearn, Two Years in the French West Indies.

SOMBRERO, ANGUILLA, ST. MARTIN. 463

in importance with social and political revolutions, the oscillations of trade and
changes of tariff. Nevertheless, as in the last century, sugar is still the staple
crop, and the capital invested in this industry is estimated at £50,000,000.
Guadeloupe, Martinique, and Barbados even yield a greater average quantity
than in the most flourishing days of the old régime.

Coffee, for which Martinique was at one time famous, has ceased to be the
staple in any of the islands, while cacao has taken the first rank in Grenada.
Montserrat and Dominica prepare lemon-juice ; St. Vincent is largely occupied
with the production of arrowroot, and in most of the English islands growers are
paying increased attention to bananas, oranges, cocoa and kola nuts, and other
fruits. Collectively, the produce of the Lesser Antilles represents an annual
value of about £8,000,000, and supports a sea-borne traffic estimated at 2,000,000
tons.

IT.—Tue Insunar GRrRovprs.

SOMBRERO, THE Docs, ANGUILLA.

Sombrero, northernmost of the Lesser Antilles, looks at a distance like a
greyish ‘hat ’’ floating on the sea. It is a mere rock, regarded as of no value till
some American, traders came to work the guano deposits resting on still more
valuable beds of calcareous phosphates. After long diplomatic discussions the
island was restored to Great Britain, the deposits having already been largely
exhausted.

The British flag also flies over the neighbouring clusters of the Dogs, so named
from their resemblance to a pack of hounds in full chase over the waves, and
Anguilla, which probably owes its name to its serpentine form, though Aguila is
the designation given to it by Herrera. It is sometimes called Snake Island,
and is continued north-east by the islet of Anguilletta. Being constantly swept
by the trade winds, these low islands are very healthy, and the inhabitants, almost
exclusively blacks, are chiefly engaged in breeding little ponies that graze the
saline pastures along the beach. They also export salt, phosphate of lime, tobacco,
maize, and cattle, chiefly to the marine depôts of St. Thomas.

ST. MARTIN.

Immediately south of Anguilla follows St. Martin, which rests on the same
submarine bank, the intervening channel nowhere exceeding 100 feet. It is a
lofty island, culminating on the north side in Paradise Peak, 1,920 feet high.
Other peaks follow southwards, while westwards stretches the low-lying peninsula
of Terres- Basses, connected with the mainland by two curved sandy beaches, which
present their concave sides towards the sea; between them is enclosed the deep
basin of Simpson’s Lagoon. Other smaller inlets indent the north-west, east, and
southern shores, and penetrate far into the upland glens.

St. Martin is the only member of the Lesser Antilles which owns two masters,
the northern section, about two-thirds of the whole, belonging to France, the rest

464 MEXICO, CENTRAL AMERICA, WEST INDIES.

to Holland. The spot is still shown where the partition was amicably arranged
by treaty in 1648. Since then the arrangement has been faithfully observed,
although the island has also been occupied by some British settlers, who now out-
number both the Dutch and French colonists.

Sugar was formerly cultivated, but the inhabitants are now chiefly engaged in
the production of provisions and working the salt-pans, which yield on an average
about 10,000,000 bushels of salt.

Marigot, capital of the French part, stands on the bay of like name, north of
the now obstructed Simpson’s Lagoon. It is a free port, and being well sheltered

Fig. 220.—Sr. Martin.
Scale 1 : 250,000.

Ae TIVE Le.
== —p— ==

€. 2] = SaaS
«SÆzre Or/entale—
HE ,

Paie f/zrmarde
SS

OT aA Orl2a2?

Depths.
0 to 5 5 to 12 12 Fathoms
Fathoms. Fathoms and upwards.

3 Miles.

attracts some shipping. Philipsburg (Philisburg), the Dutch town, lies on a narrow
beach between the semicircular southern bay and a vast salt-pan worked by a

Franco-Dutch company,

ST. BARTHOLOMEW.

This islet, familiarly called St. Bart, occupies the southern extremity of the
bank on which stand Anguilla and St. Martin. It develops a crescent scarcely
6 miles long from east to west, and not more than 8 square miles in extent,
culminating in the centre in a limestone hill 1,000 feet high.

The capital bears the Swedish name of Fort Gustave (Gustavia), for the island,
after being French from 1648 to 1784, was acquired by Sweden, and again ceded
to France in 1877 for the sum of £11,000. Gustaviu stands’on the west side,

BARBUDA, ANTIGUA. 465

where its sheltered harbour gives access to vessels drawing from 8 to 10 feet.
The inhabitants, mainly of French descent, speak English, and are exempt from
most of the burdens imposed on the people of Guadeloupe, of which St. Bartholo-
mew is an administrative dependency.

BARBUDA.

This low island lies somewhat beyond the normal course of the Antilles chain,
and in deeper water, the surrounding straits having over 500 fathoms everywhere
except on the south side towards Antigua. Both islands stand on the same
plateau, which has a depth of not more than 15 or 20 fathoms. Although of
average relative size, Barbuda is of less economic value than mere islets such as
Nevis or Deseada. Yet its salubrity and fertile soil might have attracted settlers,
despite its isolation, and the absence of good harbours.

There is room in Barbuda for 100,000 peasantry; but it was never colonised,
because for two centuries it has belonged entirely to one English family, so that
nobody could acquire land, The owner so effectually made or kept it a solitude
that it is often omitted from the very list of British possessions. To the old
vassal of the Crown have now succeeded two capitalists, officially bound, as he had
been, to send a fat sheep once a year to the Governor of Antigua. They have
now substituted a deer, an animal which they introduced from Europe, and which
inhabits the forests that cover the island.

Barbuda is the only member of the Lesser Antilles in which the whites out-
number the blacks; but the whole population is less than a thousand.

ANTIGUA.

Antigua has relatively thirty times the population of its “Silent Sister,”
Barbuda. It was so named by Columbus in honour of Santa Maria la Antigua,
a church in Valladolid. Like the other members of the outer chain, it is a low
calcareous island, its highest crest not exceeding 900 feet. Nevertheless, the
south-western hills with their steep cliffs form a sort of natural stronghold where
the inhabitants might take refuge in case of invasion. Here are evidences of
former igneous action, English Harbour being a group of craters invaded by the
marine waters.

But elsewhere Antigua forms a plateau of calcareous strata, with alternating
layers of marine and freshwater deposits, and with the greatest variety of fossil
corals, and of animal and vegetable organisms transformed to agates. Like the
other limestone islands Antigua is destitute of running waters, and in 1779 and
again in 1789 the cisterns remained empty for months together, while the cattle
perished in thousands. At present the capital is furnished with a reservoir
containing 600,000 gallons of water. Antigua is supposed to be indebted for its
healthy climate to the perfectly natural system of drainage, leaving no stagnant
waters anywhere.

Antigua was first occupied in 1632 by English settlers; these were succeeded

466 MEXICO, CENTRAL AMERICA, WEST INDIES.

by the French, but the island was restored to Great Britain by the treaty of
Breda in 1666, and since then it has formed part of the British possessions. It
was the first of the English islands to abolish slavery in 1834, without awaiting
the results of the preliminary apprenticeship ; but no lands were granted to the
blacks, most of whom abandoned the large plantations, declining to seek employ-
ment under their old masters.

Cwing to these economic changes, and partly also perhaps to the exhaustion

Fig. 221.—$r. Jonn’s HARBOUR, ANTIGUA.
Scale 1 : 40,000.

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Depths.
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1,100 Yards.

of the soil, the production of sugar, the staple industry of Antigua, has consider-
ably fallen off; it is now proposed to replace it, as in the Bahamas, by hene-
quen. The Antiguan pineapples are famous in the markets of Great Britain
and the United States.

Nearly all the foreign trade is carried on through the port of St. John,
which stands on the north side at the head of a bay (St. John’s Harbour) afford-
ing good anchorage in depths of 10 to 14 feet, but of difficult access. English
Harbour, on the south coast, is a better and more sheltered haven; but it was

ANTIGUA, SABA. 467

formerly a naval station with barracks, forts and arsenals, which repelled trade,
and the basin has since remained deserted.

St. John, a town of 16,000 inhabitants, is the centre of administration for a
presidency comprising Barbuda and Redonda, and for all the English ‘“ Leeward
Islands ” from the Virgin archipelago to Dominica. Here reside the governor and
the president, who are assisted by an executive council appointed by the Crown, and

Fig. 222.—Sr. Eustatius.
Scale 1 : 86,000.

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West of Greenwich

Depths. '
Oto 5 5 to 50 50 Fathoms
Fathoms. Fathoms. and upwards.
2,200 Yards.

a legislature, half of whose members are elected by a limited body of voters. In
1885 there were only 208 electors, who were outnumbered by the officials

SABA AND ST. Eustatius.

Both of these islets, northernmost of the inner volcanic range, belong to
Holland, though English is the current language, as it is in all the West Indian

468 MEXICO, CENTRAL AMERICA, WEST INDIES.

islands between Puerto Rico and Guadeloupe. Saba is an igneous cone 2,800
feet high, with a village nestling in an old breached crater 500 feet above the sea.
A sandy cove on the south side gives access to small craft, and the rock is con-
tinued south-westwards by a submarine bank 1,200 square miles in extent, and
from 5 to 20 fathoms deep.

St. Eustatius is larger but less elevated than Saba, its culminating peak,
formerly a separate island, being somewhat less than 2,000 feet high. The
Punchbowl, as the central crater is called, is now overgrown by a dense vege-
tation. Orangetown, the capital, lies on an open roadstead on the west side.

St. Eustatius and Saba are administrative dependencies of the Dutch island of
Curacao, on the Venezuelan coast.

Sr. CHRISTOPHER AND Nevis.

St. Christopher, familiarly known as St. Kitts, was discovered in 1493 by
Christopher Columbus, who, even after visiting Deseada, Dominica, Guadeloupe
and Antigua, was so taken with its beauty that he gave it his own Christian
name. It is the only member of the Antilles that directly recalls the memory of the
great navigator. The Caribs called it Liamniga, the “ Fertile;” but this fertility
proved their ruin. Warner and his English associates, who landed in 1623, and
the French adventurers under d’Esnambuc, who arrived two years later, combined
against the natives, whom they first drove to the interior, and then completely
exterminated. Nothing now recalls their presence except a “rock inscription ”
which has not been deciphered.

Both for the English and French St. Kitts is the “mother colony,” or
“mère des Antilles; here were founded their first settlements, and from this
point the southern islands were gradually peopled. At first the two nations
divided the island between them in a somewhat eccentric fashion, the English
occupying the central hilly district, the French the two extremities, the
‘“ Capesterre”” and the ‘“ Basseterre,” while the salt-pans, though in French
territory, were to be common to both; as a set-off against this the French were
allowed to draw their supply of sulphur from the volcano in the English district.
The respective domains were limited by cactus Ledges, more effective barriers
than palisades or ramparts.

After repelling a Spanish attack in 1629 the settlers lived peaceably together
till their Governments began to contend for the dominion of all the Lesser
Antilles. St. Kitts was taken and retaken, and finally ceded to Great Britain by
the treaty of Versailles in 1783. In the French district the local names recall the
language of its former inhabitants.

St. Kitts differs in form from most of the other Antilles. The northern and
much larger section assumes the usual elongated oval shape; but it is continued
southwards by a long tongue of sand in the direction of Nevis, and terminates in
a round peninsula enclosing a saline lagoon. On the map the contour lines thus
present the form of a guitar. But the northern section, where are concentrated

ST. KITTS. 469

the towns and plantations, may be regarded as the real island, whose regular
verdant slopes culminate in the arid grey peak of Mount Misery (4,330 feet), so
named from the torrents which during the rains rush down the gorges and deluge
the plantations. Since the emancipation it has also borne the name of Mount
Liberty. The seafarers formerly fancied they detected in its outlines a vague

Fig. 223.—Sr. Kivrs—View TAKEN FROM NEVIS.

resemblance to St. Christopher bearing the infant Jesus, as in the Christian
legend.

The crater, about 1,000 feet deep, has been quiescent since the close of the last
century, and in the rainy season is transformed to a lake fringed with palms and
other trees ; but hundreds of fissures on the flanks of the mountain still continue
to emit sulphurous gases. Brimstone Hill, one of the parasitic cones, 780 feet

470 MEXICO, CENTRAL AMERICA, WEST INDIES,

high, is crowned by a citadel formerly called the “ Gibraltar of the West Indies,’’
but now abandoned as useless.

The capital of St. Kitts, which still bears the French name of Basseterre, but
which the English settlers pronounce Barr- Starr, lies at the foot of Monkey Hill,
on a bay of the western or sheltered side. The town is surrounded by gardens
and palm-groves, and here has recently been successfully introduced the famous
lodoicea Seychellarum, or sea-cocoanut of the Seychelles, which was till lately
threatened with extinction. Scarcely anything is raised in the island except
sugar, said to be the best in the Antilles, and still produced in sufficient quantities
to remunerate the planters despite the low prices. But they have often had to
suffer from long droughts, and occasionally from floods, as in 1880, when an
avalanche of water and slush from Mount Misery reached the capital, levelling
hundreds of houses, and laying all the lower quarters under mud; whole planta-
tions, houses and all, were swept down the flanks of the mountain. The estates
still remain undivided, and in the hands of the white planters; the blacks have
received no land, and cannot even build a hut without the permission of the
ground landlords. There are no Indian coolies in the island, but most of the
retail trade is monopolised by Portuguese and natives of the Azores.

The Spanish name of MVieves, given to the neighbouring islet by Columbus, in
honour of “ Our Lady of the Snow,” has been changed by the English to Nevis, as
if it had been named from Ben Nevis. It is a superb cone rising sheer above
the sea to a height of 3,460 feet, and flanked right and left by two secondary
crests. Nevis should be regarded as forming part of the same insular mass as
St. Kitts, from which it is separated only by a reef-studded channel 26 feet
deep and scarcely 2 miles wide at its narrowest part.

The precipitous nature of the surface prevents the use of the plough, so that
the whole island, even the land under sugar, has to be tilled with the spade.
In the seventeenth century Nevis had a population of several thousand whites,
who were compelled to emigrate when the land was bought up by a few great
capitalists. The blacks also readily seek employment elsewhere, so that the
women greatly outnumber the men. Charlestown, the capital, lies on the leeward
side; in the neighbourhood are some noted thermal springs.

St. Kitts and Nevis form with Anguilla a ‘ presidency,” administered like
the other divisions of the Leeward Islands. The yearly budget exceeds £40,000.

MonTSERRAT.

The igneous chain is continued southwards by the inhabited islet of Redonda
(600 feet), beyond which follows the rugged island of Montserrat, so named by
Columbus in honour of the famous Catalonian sanctuary. The jagged sierra
culminates in a peak 3,000 feet high, and from another cone, named La Soufriére,
hot vapours still escape.

Like the other islands Montserrat was long a bone of contention between
the French and English. At present it is relatively one of the most densely
peopled and flourishing of all the British Antilles. Its enterprising planters,

ee D Éd

MONTSERRAT. 471

besides the sugar and rum industries, have since 1852 covered large tracts with
lemon-groves, yielding nearly all the citric acid and lemon-juice consumed in
England.

Plymouth, the capital, lies on the west side, but che roadstead, being too
exposed for large vessels, is frequented only by small craft engaged in the coast-

Fig. 224.—MontTsERRAT.
Scale 1 : 180 000.

West of Greenwich

Depths.
0 to 10 10 to 100 100 ne
Fathoms Fathoms. . and upwards.

3 Miles.

ing trade. Its mild climate and picturesque environment have earned for this
place the title of the “ Western Montpellier.”

Tur ARCHIPELAGO OF GUADELOUPE.

Guadeloupe (Guadalupe), largest of the Lesser Antilles, has preserved under
a slightly modified form the name given by Columbus to Curucueira, as it was

472 MEXICO, CENTRAL AMERICA, WEST INDIES.

called by its Carib inhabitants. It consists really of two islands, Guadeloupe
proper, called also Basse- Terre from its leeward position, and the eastern section
which, though the smaller of the two, takes the name of Grande-Terre because it
presents a greater extent of arable land. The Riviére Salée, as the intervening
channel is called, varies in width from about 100 to 400 feet, and is navigable
for vessels drawing 7 or 8 feet of water. It might be converted into a deep
canal accessible to sea-going ships by removing the bar at the southern
extremity, and improving the channel at the northern entrance. The passage,
however, would have long ago been closed by the coral-builders but for the
scouring action of the tides.

Despite its name Basse-Terre (“ Low Land”) is really high ground, with four
lofty igneous cones :—Grosse-Montagne (2,370 feet), in the north-west, whence
radiate various ridges nearly at the same elevation; the Deux Mamelles (2,540), with
La Soufriére (4,900) farther south, and towards the southern extremity the Caraibe
(2,300), with Houelmont (1,800). These various masses merge in an irregular
sinuous range, whose watershed has been incessantly modified by the erosive action
of the tropical rains.

Igneous energy is still active at one or two points, such as Bouillante at the
foot of the Mamelles on the Caribbean Sea, where little craters in the sands emit
hot vapours; even in the sea gas bubbles rising from the marine bed are often
seen bursting on the surface. The supreme crest of La Soufriére stands in the
centre of a plain which was probably a crater and which still discharges sulphur-
etted hydrogen. A circle of crests encloses the Petite Plaine, a depression which
also represents an old crater. Gas continues to escape from a deep fissure in the
centre, which contains the sulphur deposits whence the mountain takes its name.
Numerous thermal springs flow from the outer slopes.

The whole surface of Grande-Terre is strewn with mamelons, or rounded knolls,
averaging from 100 to 150 feet in height, and consisting, like the fringing reefs,
of calcareous conglomerates full of shells and fossil corals like those still living
in the surrounding waters. Grande-Terre culminates in a hill on the south side
about 450 feet high.

Round about Grande-Terre and here and there on the coast of Basse-Terre
the land is encroaching seawards, thanks to the incessant action of the coral-
builders. Besides the living reefs, calcareous rocks continue to grow, deriving
from conglomerate sands and minute particles of shells, in which objects of all
kinds become embedded and petrified. These are the so-called ‘ maçonne-bon-
dieu” rocks, from which the inhabitants draw the stone for their buildings
without ever exhausting the supply.

It was in a rock of this kind on the east coast of Grande-Terre that were dis-
covered the Carib skeletons which became famous in the history of contemporary
geology under the name of anthropolites. The first of these skeletons, found in
1805, was captured by the En olish privateers, and deposited in the British
Museum, and since transferred to the Natural History Museum, South Kensington.
Another, now in the Paris Museum, wears a neck ornament similiar to that still

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WEST INDIAN SCENERY—VIEW TAKEN IN THE SAINTES ISLANDS.

GUADELOUPE. 473

worn by the Caribs in the seventeenth century. The same rock has yielded other
objects, such as recent potsherds, the dried grains of coccoloba uvifera, and the
skeleton of a dog. Hence the bodies embedded in the Guadeloupe conglomerate
are not true fossils, nor of any great antiquity. They may have been living since
the discovery of America, or even since the occupation of Guadeloupe.

Guadeloupe is continued eastwards by the islet of Desirade (Deseada), that is,
“ Desired,” so named by Columbus because on the voyage from Europe to Guade-
loupe it was the first land sighted by the weary mariners. It is of the same
geological formation as Grande-Terre, but more rugged, and culminating in a
peak 900 feet high.

Marie-Galante, named from one of Columbus’ vessels, is much larger but some-
what less elevated than Desirade. It looks as if built up of successive step
terraces, like an old Babylonian tower, dominated on the east by a plateau 675
feet high. Round the island a cay in process of formation forms a still submerged
terrace, probably destined one day to be upheaved like all the others. The circular
beach is about 50 miles round. |

The archipelago is completed by the Saintes, properly Los Santos, so named
because discovered soon after the feast of All Hallows (‘All Saints”). They are
the fragmentary remains of two volcanoes which were disposed in the same direc-
tion as those of Guadeloupe and Dominica. Of the seven separate rocks some are
fractured craters, others lava heapsresting on a submarine volcano, the highest
point being Le Chameau (1,040 feet), in Terre-de-Haut on the east side of the group.

The Saintes are at once the health resort and the bulwarks of Guadeloupe,
their summits being crowned with forts.

Discovered and named by the Spaniards, Guadeloupe was regarded as a
Spanish possession, but remained unoccupied till 1635, when the French adventurers
L’Olive and Duplessis landed at Allègre Point with some white labourers under
contract for three years. After a sanguinary struggle with the Carib natives
these pioneers gave way for others, and four chartered companies were successively
ruined in their attempts to plant the island, although all the Caribs, numbering
several thousand, had been removed to Dominica and St. Vincent.

Guadeloupe also suffered from the attacks of the English, and several times
changed hands. The English were in possession in 1794 when Victor Hugues,
arriving with 1,150 men, proclaimed the emancipation of the slaves on the con-
dition of their expelling the enemy. Thus freed both politically and socially,
Guadeloupe became an impregnable stronghold, bristling with forts, building
flotillas to capture the English shipping, to liberate the blacks on the surrounding
islands, and even recover some of these from the English.

But slavery was restored in 1802, and the refractory black troops massacred.
Rather than relapse into the former state of servitude, hundreds committed
suicide; Delgrés and nearly 400 followers blew themselves up in a redoubt;
altogether about 10,000 were killed or transported, besides thousands sent to the
wars in Italy. Hence the blacks assumed a passive attitude when the English
returned and captured the island in 1810, and again during the Hundred Days.

474 MEXICO, CENTRAL AMERICA, WEST INDIES.

Even the emancipation of 1848 was far from complete, for the labour market
was so controlled as to enforce periods of long contract-service on the freedmen.
But this system has fallen into abeyance since tens of thousands of Indian coolies
have been introduced, and since blacks from the English islands seek temporary
employment at harvest time. A large proportion of the people of colour have
acquired holdings, which they cultivate on their own account, raising provisions,
coffee and even sugar.

Basse-Terre, the political capital, is not the largest town, though well situated
near the south-west extremity of the island. In the neighbourhocd is the health
resort of Camp-Jacob, so named from its founder, who established it at Saint- Claude,
2,350 feet above sea-level.

Pointe-à- Pitre, the largest town in Guadeloupe, lies in Grande-Terre near the
head of the bay where the Rivière Salée reaches the coast. Here a sufficiently deep
basin, enclosed by reefs and islets and communicating with the open sea by a
winding channel, forms a well-sheltered harbour, which has become the commercial
centre of the island. Founded during the English occupation of 1759-63, Pointe-
à-Pitre developed rapidly despite many disasters, such as the terrible earthquake of
1843, by which the picturesque cliffs of Saragot, in Marie-Galante, were ruptured
for a distance of nearly a mile.

Le Moule, on the east side of Grande-Terre, ranks in size and importance next
to Pointe-à-Pitre and the capital. Despite its exposed roadstead it does a consider-
able export trade in sugar. At the Porte d’Enfer cliffs, 9 miles south-east of this
place, were found the Carib skeletons that have given rise to so much scientific
discussion. The badly-sheltered harbour of Grand-Bourg, capital of Marie-Galante,
is frequented by a few small craft; but the vast basin of the Saintes, being a naval
station, does no trade.

Sugar has long been the staple product of Guadeloupe. Coffee, which had
nearly been abandoned, has again acquired some expansion, but only in hilly dis-
tricts and altitudes of from 600 to 2,000 feet, unsuitable for sugar. The biva
orellana was formerly extensively grown, but the industry has been ruined by the
discovery of the aniline dyes. Cotton at no time possessed any economic impor-
tance, and even tobacco is grown in insufficient quantities for the local demand.
The capital invested in agricultural industries is estimated altogether at about
£6,000,000, while the shipping exceeds 500,000 tons. France is still the best cus-
tomer of the colony, which, however, does a considerable import trade also with
the United States, England, and British India.

The archipelago is divided for administrative purposes into the three arrondisse-
ments of Basse-Terre, Pointe-à-Pitre, and Marie-Galante, the whole formine on
department, with a general council of 36 members. The municipal councils are
framed on the model of the French communal councils, and the department is
represented in the French Chambers by one senator and two deputies.

The revenue, derived chiefly from the customs and excise on spirits, exceeds
£200,000, of which one-fifth is set apart for public works and another fifth for
education.

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7
,

DOMINICA. 475

DomixicA.

Dominica was so named by Columbus because he sighted it on a “Sunday ” of
the year 1493, when its sharp verdure-clad peaks rose above the horizon. In the
chain of the Lesser Antilles properly so called it is the largest of the English
islands, and it fully equals if not surpasses Martinique in the picturesque beauty
of its landscapes, its rugged forest-clothed mountains, and foaming torrents.
Diablotin, its culminating point, rivals the Grande Soufriére of Guadeloupe in
altitude, and according to Bulkeley, who gives it a height of 5,340 feet, it is the
most elevated summit in the whole range of the Lesser Antilles.

Diablotin stands at the northern extremity of the island, overtopping by about
2,500 feet an old crater in the interior, which till recently was still flooded by a
“boiling” lake, that is, heated by thermal springs bubbling up from the bottom, and
every five minutes upheaving the waters in a foaming column. Within a short
distance of the margin the tarn was no less than 300 feet deep. But in 1880 great
landslips took place, new craters were opened in the hills, the columns of water
disappeared, and the lacustrine basin lost much of its beauty. The fissures emitting
gases are continually shifting their position, and the rivulet flowing from the
lake is swollen along its course by springs of sulphurous water descending from
crevasses in the upland valley.

In 1627 the English attempted to take possession of Dominica in the name of
Great Britain, but at that time it was still occupied by some independent Caribs,
who prevented the intending settlers from landing. Over a hundred years later
it was agreed by the treaty of Aix-la-Chapelle of 1748 to regard the island as
neutral territory between the French and English, and leave it in the free pos-
session of the natives. Nevertheless it was occupied by some French planters, and
it gradually became a French island, despite the wars and the treaties twice award-
ing it to England. Even now, after a century of British rule, the English are
almost considered as aliens by the resident population.

Roseau, a dull, dilapidated town of 5,000 inhabitants, stands on the leeward
or west side, but its harbour, a mere open roadstead, is inferior to that of Ports-
mouth, at the foot of Mount Diablotin, near the north-west extremity of the island.
Great hopes are entertained regarding the future commercial expansion of Ports-
mouth ; but meantime the trade of Dominica is limited to a few exports, such as
sugar, cocoa, fruits, lemon-juice, and sulphur, of a total annual value scarcely
exceeding £100,000.

In retaining this island, which lies between the two French possessions of
Guadeloupe and Martinique, the British Government has followed the advice of
Rodney, who in 1782 had gained a decisive victory over the French in these
waters. The English admiral held that its possession would give Great Britain a
dominant strategical position in the West Indies. But the contrast which it
presents to its French neighbours from the economic standpoint is not flattering
to the nation’s pride. The Government, as Froude truly remarks, has stricken the
island with paralysis.*

* The English in the West Indies.

476 MEXICO, CENTRAL AMERICA, WEST INDIES.

Dominica is one of the poorest and most sparsely-peopled islands of all the
Antilles. Despairing of its prosperity if left to itself, certain political economists
have proposed to hand it over to a syndicate of capitalists, who under another
system might revive the flourishing plantations of the old régime.

Dominica is administered by a nominated executive council and a legislative
council of seven nominated and seven elected members,

MARTINIQUE.

This is the only large French island which has preserved its old Carib name
of Matinina or Madiana under the modified form of Martinique. It is the second
of the Lesser Antilles in size, and is also the most irregular in its contour-lines,
which deviate most from the normal elongated oval.

Although entirely mountainous, Martinique is clothed with verdure even to the
summit of its culminating point, the volcanic Mount Pelée, in the north-west
extremity (4,450 feet). Though generally quiescent, Pelée was the scene of an
eruption in 1851. It is followed along the main axis by other cones, with inter-
vening lavas and scoriæ, terminating southwards in a peak 3,950 feet high.
The three-crested Carbet, midway between the northern extremity and the capital,
nearly rivals Pelée itself in altitude.

South of Carbet and the neighbouring crests the island is nearly divided into
two sections by inlets penetrating far into the interior, and forming the Fort-de-
France Bay on the west, and the harbours of Le Robert and Le Francois on the
east side. The intervening isthmus is scarcely 6 miles wide. The southern is
far less elevated, but more irregular than the northern section. It is traversed by
two ridges, one continuing the main axis south-eastwards and culminating in
Mount Vauclin (1,665 feet), the other ramifying westward south of Fort-de-France
Bay, and indicated far seawards by the Caraibe, Constant, and other summits.

South of the Caravelle, on the east side, the outer chain of fringing reefs
extends for some miles from the coast, but is interrupted at intervals by channels
giving access to vessels of light draught.

The Carib natives remained in undisturbed possession of the island till 1665,
when it was occupied by Esnambuc in the name of France, though not formally
annexed till 1675. The Caribs, rapidly exterminated or transported, were replaced
by blacks on the petun (tobacco) and sugar plantations. Coffee also found here
a favourable home, and the planters acquired great wealth despite the wars with
England.

Seized by the English in 1794, Martinique was not restored to France till
1816. Excited by the events occurring in Haiti, the blacks had more than once
conspired against their masters, and broke into open revolt in 1831. To avoid
pending ruin 3,000 were manumitted, and soon after political rights were
accorded to the whole free population irrespective of colour. In 1853, five years
after the emancipation, Indian coolies began to replace the blacks, who had them-
selves become small landowners. Since then contract labour has been abolished on
the principle that “labour should be free in a free land.”

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MP Ss, A

GENERAL VIEW OF FORT-DE-FRANCE, MARTINIQUE.

MARTINIQUE, 477

The capital, Fort-de-France, formerly Fort-Royal, is admirably situated on the
north side of the great bay on the west or sheltered coast. It is the military
centre and arsenal of the French Antilles, the rendezvous of the navy, and the
terminus of the transatlantic steam-service, as well as of the submarine cables to

Fig. 225.—MarrTInIQuE.
Scale 1 : 430,000.

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Depths.
0 to 10 10 Fathoms
Fathoms. and upwards.

6 Miles.

North and South America and Europe. Fort-de-France was half ruined by an
earthquake in 1839, and by a disastrous fire in 1890, since when the new houses
have been made fire-proof. Here is a fine marble statue of Josephine, Napoleon’s
first wife.

Fort-de-France has been outstripped in population and trade by Saint-Pierre,
one of the most picturesque cities in the West Indies, which was founded in

478 MEXICO, CENTRAL AMERICA, WEST INDIES.

1635 by Esnambuc at the foot of Mount Pelée, on the north-west coast. Other
flourishing towns are Lamentin, near the capital, on Fort-de-France Bay ; Saint-
Esprit, farther south on the same inlet; Diamant and Marin on the south coast,
Trinité, Le Robert and Le François, on the east side ; and Macouba, at the northern
extremity of the island.

Although the interior is entirely mountainous and still mainly covered with
primeval forests, Martinique is one of the most densely-peopled spots on the
globe. On the arable lands the people are packed together as closely as in such
industrial centres as Lancashire, Flanders, or Saxony. The whites and Asiatics
number about 10,000 and 15,000 respectively; all the rest, over 150,000, are

Fig. 226.—Lines or NAVIGATION AND SUBMARINE CABLES IN THE WEST INDIES.
Scale 1 : 32,000,000.

S
Bye
&

Matanteros

Spe?
f ge:

Kingstown '
CALE £4 .
WA ‘

ANZ Z § ES

Corinté CA à BG ‘ ‘ SpGeokge
S.Juan WZ S:Juandel ||: LLC SA Hemstad - \\ # À
Pt Arend A0 en ZZ: eG L LE Ë Ay ean

Submarine Cables. Regular Lines of Steamers.

620 Miles,

blacks or people of coiour, perfectly acclimatised, and steadily increasing by the
natural excess of births over the mortality. But large numbers of young men
emigrate to France, Haiti, and the United States, so that the female exceeds the
male population by about 10,000. The proportion of illegitimate children is
about two to one, and scarcely one-fifth of the people have received any instruc-
tion.

Asin Guadeloupe, the staple product is sugar, the cane plantations covering
about 100,000 acres, or one-fifth of the whole area. Hence the exports consist
almost exclusively of sugar, rum, and tafia, estimated at a total yearly value of
from £720,000 to £800,000. A little cacao is also cultivated, but coffee has been
almost completely abandoned. The so-called “ Martinique coffee” of commerce

ST. LUCIA. 479

is really grown in Guadeloupe. More than half of the foreign trade is carried on
with France and her colonies.

Like Guadeloupe, the island is represented in the French Chambers by a
senator and two deputies, and in the general council by 56 members, nearly all
elected by a very small number of voters. There are two administrative
arrondissements, Fort-de-France and Saint-Pierre, and income and expenditure
average about £160,000.

ST. LucrA.

Like Dominica and Grenada, St. Lucia, the ‘‘Sainte-Alousie ” of the planters
of the last century, is one of those West Indian islands which have become English
possessions while remaining French in their traditions, language, and usages. It
is one of the loveliest, if not the loveliest, in the long chain of these volcanic
islands. When the traveller approaches it from the north and contemplates the
two prominent peaks, 2,690 and 2,720 feet high, and then passes between the
huge rocky walls of these majestic portals into the marvellous amphitheatre of
wooded hills encircling Port Castries, he is tempted to exclaim that surely St.
Lucia is unrivalled for natural beauty. La Soufrière, one of its volcanoes, 4,000
feet high, is still active, and in the chasms of its crater, lined with deposits of
sulphur, the eruptive matter is constantly in a state of fusion. Copious thermal
waters bubble up in various parts of the island, and one of the sulphurous streams
still flows through a half-ruined establishment erected by the French before the
Revolution.

After a long resistance to the early settlers, the Carib natives were at last
exterminated, and the island fell successively into the hands of the French and
English. But since the rupture of the treaty of Amiens it has remained in the
possession of Great Britain. On the advice of Rodney it was not restored to
France in exchange for Martinique. In that admiral’s opinion the excellent
strategic position of Port Castries, with its rocky bulwarks, was of paramount
importance for the consolidation of British supremacy in the West Indian waters.

Nevertheless, this haven, “ the best in the Antilles,” long continued to be of
slight commercial or military value. Recently, however, it has been lined with
wharves, and made a central coaling-station for steamers plying in the West
Indian waters. Since then the foreign trade has rapidly increased, the exchanges
being estimated at a total value of about £310,000. The exports alone advanced
from £117,000 in 1887 to £162,000 in 1889. But the local traffic is slight, four-
fifths of the surface being still covered with primeval forests.

Nevertheless, agriculture is being steadily developed, and the sugar, raised on
small allotments, is said by the growers to be equal in quality to that of St. Kitts.
The population has increased by immigration, and still more by the return of a
large number of blacks till recently employed on the Panama Canal works. The
whites, scarcely 1,000 altogether, are in the proportion of about one to forty of the
people of colour. Despite the bad reputation caused by the frequent outbursts of
epidemics in former years St. Lucia is really one of the healthiest of the Lesser
Antilles. Mount Fortuné (770 feet), where the troops are stationed, and the

Fig. 227.— GENERAL View or Casrries, Sr. LucrA ISLAND.

480 MEXICO, CENTRAL AMERICA, WEST INDIES,

Chabot and Chazeau heights, form convenient health resorts for the residents in
Port Castries.

NU UNS
I

The governing body comprises an administrator and colonial secretary, with
a nominated executive and legislative council.

ST. VINCENT.

This island is a typical member of the Antilles chain in its regular oval form
and the disposition of its main axis. It is also one of the most picturesque and
salubrious of the archipelago, while the slopes fall almost everywhere gently down

ST. VINCENT. 481

to the sea, and here and there present convenient terraces for plantations and
settlements.

The central ridge, which throws off spurs east and west, develops a line of
sharp peaks, clothed with vegetation to their summits, and culminating with the
Morne and Garou, 5,200 feet high. Half-carbonised tree-stems, embedded in the
layers of travertine or in the lava streams, reveal the history of old ervptions by
which the forests were successively destroyed, springing again into new life after
each convulsion. The arable soil is everywhere an extremely rich black earth,
formed of ashes mixed with vegetable remains.

According to Bulkeley, the spear-headed trigonocephalus also infests the
forests of St. Vincent, though this formidable reptile is usually supposed to be
confined to Martinique and St. Lucia. St. Vincent and the neighbouring islet
of Bequia probably served as so many stages on its migrations from South
America to the Antilles. To the presence of the trigonocephalus Bequia is said
by Labat to owe its title of “Little Martinique,” a name since transferred to
another member of the Grenadines.

La Soufrière, at the northern extremity of St. Vincent, is a mere fragment of
an ancient cone, which probably at one time rose to double the present height
of the loftiest summits of the crater. Reports, contradictory in their details, all
agree in the general statement that in the year 1718 a terrific eruption of La
Soufriére buried the whole island and surrounding waters in ashes; it was,
doubtless, on that occasion that the upper part of the cone was blown away.
The ruptured mountain was still in a restless state in 1785, but in 1812 a deep
lake flooded its terminal crater. The waters were agitated by frequent shocks,
which corresponded with similar disturbances occurring simultaneously in both
Americas and the Antilles.

On April 27, 1812, a month after the destruction of Caracas, in Venezuela, by
an earthquake, another eruptive mouth appeared on La Soufriére not far from its
first crater. A few volleys of stones and ashes were followed by more violent
discharges, which became constantly more frequent, at last merging in a con-
tinuous roar. The whole firmament was gradually overcast with dense clouds
of dust torn at intervals by the fiery tracks of blazing masses, and daylight
disappeared behind the black canopy belched forth from the bowels of the earth.
The underground rumblings were heard on the Janos of Venezuela, 600 miles
away, and for three days the shroud of night was suspended over the sea as far
as Barbados, 120 miles farther east. The troops quartered in this island, hearing
the distant rattle, fancied that two fleets must be engaged in the neighbouring
waters, and began to prepare for the possible attack of some unknown enemy.
But nothing could be descried across the “visible darkness” until the raging
storm abated, when a shower of ashes was seen pouring down from space. When
it ceased the island was found covered with the black and fertilising ashes for a
thickness of some inches. At first it was supposed that the scoriæ had been cast
up by some volcano that had risen above the ocean to the windward of Barbados,
as it seemed incredible that they could have been wafted across the sea by the

64 ,

482 MEXICO, CENTRAL AMERICA, WEST INDIES.

counter-currents to the trade winds. Great, therefore, was the amazement of
the inhabitants when they heard that the black rain had come from St. Vincent,
ejected through the trade zone to the counter-zone of aérial currents setting
north-eastwards at an altitude of 16,000 or 17,000 feet.

Several species of birds, supposed to have been exterminated or regarded as
fabulous, still survive in the caverns of La Soufrière ; amongst them is the whistler .
(sibilans myadestes).

Throughout the sixteenth century St. Vincent was left to its native Carib
inhabitants. During the following century the English and the French con-
tended for its possession, without, however, making any permanent settlements.
Even so late as 1660, after the wars which had been waged against the Indians
in most of the Antilles, it was decided to leave both St. Vincent and Dominica
to their original owners, all English and French settlers as well as other whites
being excluded, except the French priests, who were allowed to maintain the
missions at their own expense.

But the terms of the treaty were not observed, and in 1765, when St. Vincent
was definitely ceded to England and the coast districts occupied by British
planters, the intruders were again attacked by the Caribs. The war lasted ten
years, and broke out again in 1778, and during the French Revolution. The
natives had all the more reason to fear the settlers that they were no longer all
“red,” that is, full-blood Caribs, exempt by custom from servitude. Most of
them had, in fact, become “black” Caribs, that is, descendants of maroon negroes
and native women. As many as 500 of their ancestors were even said to have
been negroes from Guinea, who had escaped from a vessel wrecked on the coast of
St. Vincent. Hence they were liable to loss of freedom as well as of their lands.
They accordingly fought with the energy of despair against the British forces,
but had to surrender at discretion in 1796, and next year nearly all the survivors,
numbering 5,080, were transported to the island of Roatan, on the Honduras
coast. There still remain nearly 200, highly valued by the settlers as boatmen
and tide-waiters. Nor do they betray any of the ferocity attributed rightly or
wrongly to their forefathers. Some of the rocks in their district are covered
with rude carvings.

The St. Vincent planters soon grew wealthy by the sugar industry. But
after the emancipation they found themselves suddenly abandoned by their
former slaves, who went off to cultivate on their own account the unoccupied
lands of the interior. Most of the old plantations were abandoned, and nearly
all the English planters left the island.

At present the chief agricultural industry is the production of arrowroot
(maranta indica), which is elsewhere unrivalled for its strengthening properties
and exquisite flavour. Some attention has also been given to the cultivation of
tea, but without much success, though the shrub thrives well in the shade of the
damp forests. Alimentary plants of all kinds are raised in sufficient quantities
for the people of colour, who occupy numerous villages in every part of the
productive districts, and who appear to be gradually acquiring the ownership of

I | | 4
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KINGSTON, ST. VINCENT ISLAND.

GRENADA. 483

the arable lands. About 2,000 Indian coolies, introduced by the sugar-growers,
reside in the capital and some of the larger villages. Some Portuguese, also, and
Azore islanders have mingled their blood with that of the natives, in whom are
thus represented the three elements, red, black, and white.

Kingstown, the capital, is a long straggling town of about 6,000 inhabitants,
whose houses and gardens are disposed in three lines parallel with the sea and
the foot of the mountains. The roadstead opens southwards over against Bequia,
which, with some other members of the Grenadine group, belongs to the admi-
nistrative division of St. Vincent.

The colony is governed by an administrator and colonial secretary, with a
legislative council of four official and four nominated unofficial members. Its
exports rose’ from £85,000 in 1887 to £125,000 in 1889, and the population
increased from 40,000 in 1881 to about 50,000 in 1890.

GRENADA AND THE GRENADINES.

The chain of islets and reefs over 60 miles long connecting St. Vincent with
Grenada comprises about 600 separate rocks all disposed according to the general
axis of the Lesser Antilles, but offering an endless variety in their relief and
contour lines. Some are a few square miles in extent, with headlands, inlets,
hills, and dells; others are mere rocky cones or patches of verdure fringing a
circular beach, or else reefs washed by every tide. The whole group is surrounded
by deep waters, and even the narrow channels between some of the islands are
navigable by vessels of heavy draught.

Some of the Grenadines, such as the two largest, Bequia and Cariobacu, have
names of Carib origin; one is known as “Little Martinique,” but nearly all are
designated from their aspect, their form, or some natural phenomenon—Round,
Castle, Sail, Bird, Mosquito, and so on. In the larger members of the archipelago
the blacks raise sugar and coffee; but most of the inhabitants are occupied
exclusively with the production of provisions and cattle-breeding. Some of the
rocks are held by a single family, “masters of all they survey.” The native-
built craft, plying between the islands and laden with fruits or fish, pursue the
large cetaceans that penetrate amid the reefs.

Cariobacu, largest of the Grenadines, lies towards the south end of the chain,
and depends administratively on Grenada. It has an area of 7,000 acres, and
the slopes, rising to a height of 1,000 feet, are well cultivated.

Grenada, southernmost of the Lesser Antilles proper, for Tobago and Trinidad
belong geologically to South America, presents a somewhat less irregular oval
than St. Vincent, which it about equals in size. The volcanic uplands, culminat-
ing in a peak 2,750 feet high, are clothed with forest growths, which here and
there reveal the lava streams and basaltic colonnades terminating in superb cliffs
on the coast. Still open craters occur in several places, and two romantic lakelets,
fringed with bamboos and tree terns, are also probably flooded volcanic cones.
Pleasant villas and country seats are scattered over the valleys and on the slopes

484 MEXICO, CENTRAL AMERICA, WEST INDIES.

of the hills in the midst of verdant thickets and flower gardens. None of the
Antilles surpass Grenada in sylvan charms, wealth of colour and fragrant blossom.

Columbus, its discoverer in 1498, gave it the name of Ascension; but it
remained in the possession of the aborigines till the middle of the seventeenth
century, when some French settlers arrived with a large number of negroes.
They at once began to massacre the natives, and on the north coast is still
shown the “ Morne des Sauteurs,” or “Caribs’ Leap,” where the natives threw
themselves into the sea to escape their enemies.

A hundred years later the English seized the island, which they have since
retained. But the white planters, enriched by the sugar industry, were unable
to recover from the blow caused by the emancipation of the slaves. Most of
them had first to mortgage and then sell their estates, which have in great
measure been bought by the descendants of the old slaves. In 1889 there were
about 5,000 small farmers, nearly all blacks or people of colour, with holdings
from about 3 to 6 acres in extent. Hence Grenada is one of the West India
Islands referred to by political economists, according to their different theories,
as examples of disaster and ruin, or as models of prosperity. Doubtless the
old planters, having lost their vast domains and gangs of slaves, have left the
island where they had been impoverished by their lavish expenditure ; but on
the other hand the emancipated blacks have acquired sufficient land to maintain
their freedom. They swarm in the narrow island, which is relatively twice as
thickly peopled as France, and according to the testimony of all travellers the
negroes are nowhere more cheerful, light-hearted and really happy.

The export of cacao, the staple product, increases from year to year; but
sugar, tea, coffee, cotton, tobacco—in a word, almost all colonial produce—thrives
well in this favoured island, which, like Malaysia, also yields spices, nutmeg,
cloves, and ginger, besides the kola nut of Senegambia. The mean temperature
on the sheltered coastlands, which varies from about 78° to 80° Fahr., enables
the growers to cultivate all the plants of the torrid zone; but the plantations
suffer much from the depredations of the monkeys. The export of fruits to the
United States is steadily increasing, and would even acquire still greater expan-
sion were the island traversed by good roads.

Grenada, however, has an excellent narbour, the so-called Carénage, one of the
best in the Antilles, affording anchorage in 30 to 50 feet of water close inshore.
On the lava headland separating the port from the sea stands the fortress of
_ St. George, whence the town often takes the name of Georgetown.

BARBADOS.

This outlying island, which since 1885 constitutes a separate government,
does not form a link in the chain of the Lesser Antilles, from which it is
separated by a trough over 1,350 fathoms deep. From its northern extremity to
the south point of St. Lucia, the nearest land, the distance is about 95 miles.
Abysmal waters also separate it from Tobago, and its main axis is disposed

BARBADOS. 435

north-west and south-east, in the reverse direction to that island. Barbados also
differs from the other Antilles in its geological formation, being a coralline mass
resting on a trachytic core, which crops out only at one point. It seems to have
been upheaved by successive thrusts; for it consists of a series of receding
terraces, each with its circuit of scarps and cliffs, except where the old contour
lines have been modified by the erosion of tropical floods. Mount Hallaby, the
culminating point, is only 1,150 feet high. In many places the quarries have
revealed coral banks still as clearly outlined as if they had but recently been
formed in the sea.’ All round the island the reefs continue to grow, so that
here and there the outer fringe is some miles wide. It is the yearly scene of
shipwrecks, often even in calm weather, and cyclones are nowhere more frequent
than in the Barbados waters. The soil, composed of a coralline limestone mixed
with volcanic ashes, is extremely fertile.

The origin of the term Barbados (Barbadoes), the Barbiche of the early
French navigators, has not yet been elucidated. It is generally attributed to
the appearance of the large trees covered with a beard-like (‘‘barbue’’) moss
seen by the discoverers, while Froude refers it to the “bearded” natives whom
the Spaniards early in the sixteenth century came to kidnap for the plantations
of Espanola. No contemporary document throws any light on the subject, nor is
it even known whether the island was first sighted by the Portuguese or the
Spaniards. In 1605 the English vessel, Olive Blossom, making for Surinam,
anchored off the coast, and the captain took official possession of the island.
Planters arrived in 1625, and since that time Barbados has formed part of the
British possessions. It was held as a fief of the Crown down to the year 1838,
when the privileges of the feudatories were finally abolished.

During the Commonwealth many cavaliers took refuge in the island, which
within twenty years of its foundation had already 50,000 inhabitants, including
many Irish contract labourers, and thousands of Indians carried off from the
mainland. The all-powerful planters could muster thousands of armed men,
and their island was called “Little England.” In other members of the
Windward group French is, or was, the dominant speech; but in Barbados
nothing has ever been current except standard English, spoken by whites and
blacks alike, and having little in common with the jargon heard in the other
islands. Uninterrupted local traditions have fostered an ardent patriotic feeling
towards the mother country amongst the inhabitants, the majcrity of whom are
members of the English Church. In jJocular language they call themselves
‘‘ Bims,” and the island ‘‘ Bimshire.”

As in the slave days, sugar continues to be the staple product. The economic
crisis, followed by such serious results in the other islands, passed over Barbados
without causing any disasters and without profoundly changing the relations of
the blacks with the planters. At that time the whole island was already under
cultivation ; all the arable land was divided either into great domains or holdings
of 12 acres, and not a rood remained for the emancipated negroes, who conse-
quently continued in the service of their patrons no longer as slaves but as

486 MEXICO, CENTRAL AMERICA, WEST INDIES.

hired labourers. Hence the planters have had no occasion to introduce Indian
coolies, as was done in the other Antilles.

Since the period of the emancipation the difficulty of finding small holdings
' for the blacks has greatly increased, for the population has been doubled and
already exceeds 180,000. The plantations are, in fact, as crowded as the manu-
facturing districts of West Europe. Every year hundreds, and even thousands,
emigrate to the other British colonies, yet the island continues to swarm like
Malta, and its surplus population has been the prosperity of Surinam and Deme-
rara. Compared with the other English islands, the proportion of whites to
coloured is high, about a tenth ; but it is yearly diminishing.

The staple industry, which keeps five hundred sugar-mills going, leaves no
room for the cultivation of alimentary plants. Hence rice, maize, fruits, vege-
tables have to be imported into an island which might be transformed to a vast
garden. Besides sugar, a few barrels of petroleum and a little colonial produce
of minor importance are the only exports. One of the cultivated varieties of the
cotton-plant has received its name of gossypium barbadense from this island, which
has already its railway, mainly for the service of the plantations. , Barbados has
also the advantage over the other English islands of being a terminus for the
transatlantic packets, and the centre whence the secondary lines radiate throughout
the West Indies. Trade, which relatively to the size of the island is very large,
is concentrated at Bridgetown, on Carlisle Bay, near the south-west extremity.

The town, which takes its name from a bridge carried across a creek, stretches.

along the beach at the foot of a hill During the seventeenth century it was one
of the chief slave-markets of the Antilles, and it has remained one of the busiest
places in the West Indies. About a third of the whole population resides in
Bridgetown and its suburbs, which, however, lack the picturesque charm of
Roseau, Saint-Pierre, Plymouth, and so many other West Indian towns. It is
simply an ordinary quarter of London or Liverpool where even the palm-tree seems
out of place. Fontabelle, however, where the European traders reside, is a charming
district, in which the houses are embowered in verdure and flowering creepers.
The watering-place of Hastings is also a pleasant little station, and round the coast
follow some other little settlements, such as Speightstown, Hoistingtown, and Hole-
town. Codrington College, an educational establishment noted throughout the
Antilles, occupies a charming position on the north-west coast.

Barbados enjoys a larger measure of self-government than any of the other
English islands. According to its constitution, over two hundred years old, the
house of assembly consists of 24 members elected by a limited body of voters.
The central authority is represented by a governor and a legislative council of
9 members nominated by the Crown. The budget is prepared and the laws
proposed by an executive committee, comprising the chicf functionaries, one member
of the upper and 4 of the lower house. The governor is also commander of the
naval forces in the West Indian waters, and Barbados is the headquarters for the
European troops. For administrative purposes it is divided into eleven parishes,
and has a yearly revenue of about £16,000.

MERE VE

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STATISTICS.

MEXICO.

AREAS AND POPULATIONS, 1890 (est.).

States. Area in sq. miles. Population. States. Area in sq miles. Population.
Federal District . & 463 226 State of Guerrero ge 2450 332,887
State of Mexico . KRSLO , 778,969 >» Yucatan . 29,569 282,502

», Morelos . TG : 151,540 a) LLabasco: . 11,849 3 114,028
» Liaxcala eel, G22 5 155,151 », Nuevo Leon . 23,637 . 244,052
» Guanajuato . 11,413 . 1,007,116 » Sinaloa. . 36,200 . 223,684
“AG Pucbla, ..- à 12,019 .-.. 830,468 », Tamaulipas . 27,916 . 189,139
» Queretaro 5205 : 213,525 ;, Durango a ail P 265,931
», Hidalgo 6 teil 5 494,212 », Campeachy . 25,834 ; 91,180
» Aguascalientes 2,897 5 121,926 55 Chihuahua . 83,715 é 298,073
», Michoacan . 23,714 2 830,926 », Coahuila . 60,904 ; 183,327
= alascon © . 39,174 1161709 Sonora . 395020 3 150,391
Oaxaca. . 1 38,082 5 806,845 line California (Ter-

5 Vera CTUZ =. 265232 : 644,157 ritory) . : . 61,563 : 34,668
», San Luis Potosi 27,503 A 546,447 Tepic (Territory) 5 115270 F 130,019
», Zacatecas 5 DAO ‘ 526,966 —————
Se Colima. > 3; 146 : 69.547 Total . . 740,970 - 11,632,924
>, Chiapas. . 16,048 5 266,496

CHIEF TOWNS.

Population. Population.
Lower Cazrrorn:a La Paz . . . . 3,800 tilde ee eon I4 S00
Spree aa Sf Hermosillo . . . 15,000 TAMAULIPAS. | Matamoros . . . 13,800
Use UT RE 700 Hémpicos 0 0011700
Culiacan . . . . 20,000 Zacatecas. . . . 31,000
SINALOA . Mazatlan. . . 17,400 | Fresnillo . . . . 28,600
Sinaloa . . . . 15,300 Ciudad Garcia . . 26,000

ZACATE A 4
CxravuAHuA AND Chihuahua . . . 12,000 RTE Pinos . 0. 25,500
Duran Go . - |p Durango. - . . 29,000 Sonibrerota oe eo .000
Mezquital . . . 9,000 Guadalupe . . . 15,400
Gouna 7 ies altos —. "- 19,000 San Luis Potosi. . 70,000
Parras de la F dente 12,600 Rio Verde . . 26,000

5 9

sn MEN: 35,500 Since [PS eee enn Ris ee
Nuzvo Leon octor Aroyo . . 13,550 iudad del Maiz . 23,900
Binaress = = = 15000 Matehuala . . . 21,400
‘ Montemorelos . . 10,600 Catorce Cr 900

488

APPENDIX.

Curer Towns—continued.

Population.

Aguascalientes . 66,000
LeondelosAldamas 80,000

Guanajuato. . 58,300

Dolores- Hidalyo 45,000

Allende - 89,300

AGUASCALIENTES Silao 33,000
AND Celaya. 28,000
GUANAJUATO Trapuato . 27,700
Salamanca 24,000

Salvatierra . 24,000

Valle Santiago . . 23,000

Abasolo . - 21,800

La Luz - 14,700

Guadalajara . . 105,000

Lagos. . 42,400

Sayula. . 26,400

JALISCO . Tepatitlan . 23,700
La Barca. .- 22,900
SanJuandelosLigos 18,700

Zapotlan (Guzman) 15,510

: { Tepic . ae - (21900

Pepe Ann Counts | Colima. . - 938,500
, Morelia 00-10 938:600

| Puruandiro . 27,700

La Piedad 19,000

2 Zamora 14,700
TERRORS o> We Tacambaro 12,700
Ario 12,400

Extlani. ocr is 12200

Uruapan ee LS 00

( Queretaro. . . . 34,400

QUERETAEO . iSanduan . “seen .) 21,300
Cadereyta. . . 14,800

Toluca. . 1 -140/000

Tejupilco . . . . 20,600

Mieco : Tenancingo . 16,000
. Texcoco 15,700

TRADE RETURNS :—

Year. Imports.

GBS DE à di GET TAS 000 |

ieee, Me 9,000,000.

D, on ems 9,200,000.
Silver produced between 1821 and

CoInaGE OF THE MExIcANn

Silver.

£4,800,000

Mints (1890) : —

Gold.
£47,000 -

Cuter Exports OTHER THAN THE Precious Merars (1890) :—

Henequen = x À :
Coffee :

Hides and skins

Lumber . : : :

Revenue (1890), £8,350,000 ; Expenditure, £,7,700,000 ; Debt, £22,720,000.

. £1,370,000
778,000
400,000

. 280,000

Population.
Mexico . 425,000
pee d vi Xochimilco 12,800
| San Angel 10,000
Huejutla . 19,700
anne ee . Fes - 15,300
Pachuca . . 14,300
: Atotonilco 14,200
Pueblar eee 68,700
Tetela del Oro 15,500
PUEBLA . c ATISCO =. 235600
Matamoros 13,500
Zacatlan . 13,400
Vera Cruz . 18,200
| Papantla . . 14,300
Warne Cane Jalapa Goa ce 14,200
Orizaba 14,100
|s Andres . 11,500
Cordoba 11,300
M Cuernavaca . . 16,500
DEEE x { Morelos 14,300
Acapulco . 12,400
GUERRERO AND Oaxaca SRE 58,400
Oaxaca * 4 Miahuatlan . . . 35,200
Ixtlan. . . 25,900
Tehuantepec . 24,500
Tuxtla Gutierrez 22,000
San Cristobal 12,600
SES à eg 12,500
Comitan 2 105200
TABASCO . 5 San Juan Bautista. 18,600
Campeachy 15,200
| Carmen : 7,400
Merida #70 43,300
os * ) Tzamal. 25,600
[xsi see S000
Tixkotob!.. TT AUD
A]
Exports. Exports of Precious Metals.
: £8,730,000 £6,000,000
i 12,000,000 7,750,000
. 12,500,000. 7,720,000
1880: £180,000,000; gold: £968,000.
Copper. Total:
‘4 £27,000 = £4,874,000
Vanilla : - = 5 - £185,000
Live-stock 2 & = = 100,000
Gums A ~ = : ; 144,000
Tobacco . : : = À Z 190,000

Army, 34,800 of all

arms. Primary schools, 10,726; attendance: 544,000. Railways open (1890), 4,640 miles. Telegraphs

open (1890), 27,000 miles.

Area, 7,562 sq. miles; Population (1890), 28,000.

APPENDIX.

BRITISH HONDURAS.

Belize, population, 5,800; Imports, £206,000; Exports, £213,000.
Shipping, 253,132 tons, of which 185,464 with Great Britain.

Land under culture, 44,600 acres; Unreclaimed, 4,952,000 acres.
Revenue (1889), £50,523 ; Expenditure, £45,487 ; Debt, £16,000.
Schools, 27; attendance, 2,612.

Guatemala .
Honduras 2
San Salvador .
Nicaragua .
Costa Rica ~
Panama . 6

Total

Departments.
Totonicapam .
Guatemala .
Huehuetenango
Alta Vera Paz
Quezaltenango
San Marcos
Quiché . ë
Solola . :
Chiquimula .
Chimaltenango
Baja Vera Paz
Jutiapa . o
Zacapa . 5
Sacatepequez .
Santa Rosa .

Suchitepequez
Amatitlan .
Jalapa . .
Escuintla 5
Retalhuleu .
Peten . :
Izabal . 4

Livingston .

Total .

CENTRAL AMERICA.

Area in sq. miles. Population.
46,800 1,460,000
: 5 46,400 432,000
° ° 7,610 664,000
° ° 49,500 375,000
SE 0 000 220,000
° . 33,000 300,000
° eo 202,925 8,451,000
GUATEMALA.
AREAS AND POPULATIONS (1889).
Area in sq. miles. Population. Chief Towns.
2 580 158.419 Totonicapam
5 960 141,701 Guatemala À
- 9,600 133,173 Huehuetenango
S000 510408 Coban
= 2;000 . 104,800 Quezaltenango .
2.000) 190,323 San Marcos
41,800: - 87,929 Santa Cruz
‘ 700 83,804 Solola
- 1,400 64,733 Chiquimula
. 860 59,335 Chimaltenango
102100 49,822 Salama
1,600 48,461 Jutiapa
. 1,400 43,045 Zacapa .
G 300 42,852 La Antigua
100 37,499 Santa Rosa
- , 25000 36,182 Mazatenango
: 500 35,626 Amatitlan
- 1,200 35,020 Jalapa .
en 252008 ae . 380,973 Escuintla . :
A 700 24,431 Retalhuleu A
8 4000 : 8,480 . La Libertad .
-« 2;600 = Izabal
1,600 } se 0 E Livingston
. 46,800 1,429,116

Population
per sq. mile.
31
9
90
7
11

° 9

Population.
20,000
66,000

5,000
18,000
24,000

3,000

6,000
13,000

4,000

3,900

7,000

1,500

3,900
15,000

1,600

4,000

7,500

4,500

5,500

3,500

600
= 650
- 900

Full-blood Indians, 60 per cent ; Half-castes, 38 per cent.; Whites, 2 per cent.

Immigration (1889), 6,711; Emigration, 6,480.

Revenue (1890), £1,012,000; Expenditure, £920,000; Debt, £2,227,000.
Imports (1889), £1,416,000 ; Exports, £2,650,000.
Shipping (1889), 375 vessels of 463,438 tons entered.

490

Population.
. 0115720
30,428
8,600
13,715
28,000
5,980
13,820
5,210
8,750
9,450
6,846
23,800
2,200
2,880

Chief Towns.
Santa Rosa
Gracias
Santa Barbara
Yoro
Progreso
Jutigalpa
Truxillo
Comayagua
La Paz
La Esperanza
Tegucigalpa
Luxaran

APPENDIX.
Railways open (1890), 100 miles.
Telegraphs, 2,000 miles ; messages (1888), 457,000.
Post offices (1888), 157; letters, &c., forwarded, 4,522,000.
Army: 3,500 regulars ; reserve, 67,300.
Primary schools (1889), 1,327 ; attendance, 47,900.
SAN SALVADOR.
AREAS AND POPULATIONS (1890).
Departments. Area in sq. miles. Population. Chief Towns.
Ahuachapam . 2) 2000 = (tsi) : Ahuachapam
Santa Ana : DOUDOUS - 0,104 : Santa Ana
Sonsonate à SUAS Oe ee: ©: ky : Sonsonate .
La Libertad . - 460 . A9 056 : Santa Tecla
San Salvador . 2 44005 2 es24or 5 San Salvador
Chalaltenango . RATE IDES HO ETOUE : Chalaltenango
Cuscatlan 5 6600. 0060 ‘ Suchitoto .
Tua Paz . ; {SON 5 Beye LÉ Sacatecoluca
San Vicente . RASOIR 0/60 : San Vicente 5
Cabafias . : à ADS à ÉD à 5 Sensuntepeque .
Usulutan : = (sil) * . 39,300 . : Usulutan .
San Miguel . TRUE. 309207, 0% : San Miguel
Morazan . 3 > 480) % 5 als) < Gotera c
La Union é 5 40 -- # 39,620 . : La Union .
Total 6,840 684,218
Whites, 10,000 ; all the rest full-blood and half-caste Indians.
Imports (1889), £577,000 ; Exports, £1,134,000.
Shipping (1889), 343 vessels entered and cleared.
Revenue (1889), £810,000 ; Expenditure, £800,000 ; Debt, £1,130,000.
Post offices, 48 ; letters forwarded (1890), 8,880,000.
Telegraphs, 1,500 miles of wire ; telephones, 240.
Primary schools (1890), 740; attendance, 28,000.
Army, 2,500; militia and reserves, 12,000.
HONDURAS.
AREAS AND POPULATIONS (1889).
Area in
Departments. sq. miles. Population. Ladinos.
Copan . . . 7) to DOUN . 936,744 . » 32,946 .
Gracias . : 5 5 pos LOOnee 97816 . 15,906 .
Santa Barbara A « 4,400 . HO2, 084. . 29.001.
Yoro A . . A 16,000 DS 06 Re RES E) ES
Islas de la Bahia . : 150 o WIAA UT. : hails
Olancho . 5 5, LO OO0mm. a 0101028 . 24,673 .
Colon AL TT ao DONS 1 BP Reape de EE oct:
Conayagun +. 27 02 0160000, UNE V6: 780 en 010660
La Paz - . : 800 . 16 SDDSS : 19/8008
Intibucat . . 640 . 5 10420 . 10,554
Tegucigalpa . 5 5 syn ¢ CONTOUR . 46,570
El Paraiso . = 102000 5 AOD . 17,863
Choluteca > 3 5) 22500075. . 43,588 . . 389,028

Totale 1 49500, GNOME

Choluteca

APPENDIX. 491

Exports (1888), £670.000, of which £245,000 agricultural produce.
Shipping (1889), 142 vessels o' 61,000 tons entered and cleared.
Revenue (1889), £286,000 ; Expenditure, £320,000 ; Debt, £8,620,000.
Railways open (1890), 37 miles.

Post offices, 33; letters, &c., carried, 299,600.

Telegraphs: 1,800 miles; offices, 63.

Schools, 600; attendance, 13,000.

Army: 500 regulars; militia and reserves, 3,000.

NICARAGUA.

AREAS AND POPULATIONS, 1890 (est.).

Territories. Area in. sq. miles. Population. Chief Towns. Population.
Chinandega . : 2,100 : : 40,000 2 : Chinandega ; . 8,000
Leon . : 5 3,200 ‘ 65,000 : : Leon ‘ ; . 381,000

Managua and | ( Managua. . . 18,000

COGAN Fie SNR OD DD by... Granada re RE 15000
ee Masaya . : . 14,000
Rivas . ‘ : 1,100 5 5 45,000 - : Rivas : | . 12,000
Segovia ey 162600 : : 35,000 ‘ : Ocotal à 4 eo 000
Matagalpa . ë 8,400 B 5 40,000 : : Matagalpa £ . 9,000
Chontales . : 7,800 é A 40,000 : A Acoyapa . 5 02,000
Reserva Mosquita . 8,200 : 0 20,000 : ; Blewfields . : . 1,000
50,000 375,000

Imports (1888), £430,000 ; Exports, £304,000.

Imports from Great Britain, £80,000 ; Exports to Great Britain, £133,000.
Shipping (1889), 385 vessels of 398,000 tons entered and cleared.

Railways opened (1890), 105 miles.

Telegraph lines: 1,700 miles ; offices, 53.

Post office returns (1889) : letters. &c., forwarded, 3,700,000.

Revenue (1890), £800,000; Expenditure, £820,000; Debt, £505,000.

Schools, 251; attendance, 11,900.

Army: 2,000 regulars; reserve, 10,000; militia, 5,000.

Nicaragua Interoceanic Canal (begun 1889), 169 miles ; estimated cost, £15,000,000.

COSTA RICA.
ADMINISTRATIVE DIVISIONS.

Provinces and Comarcas. Cantons. Population (1888). Chief Towns. Population.

San José 3 6 64,846 . .. San José . A 14,500
Alajuela ; : 7 : : 51,087 . . Alajuela . : 3,842
Cartago c - 3 2 33,887 . CAT ago c 4,575
Heredia 5 29,409 . . Heredia . à 4,332
Guanacaste . 5 5 : 5 16,29. . Liberia A j 1,782
Puntarenas . 3 8 : : 8,409 . . Puntarenas 5 2,116
Limon . ‘ A 1 5 5 111000: . Limon : A 637
30 205,731

Area, 20,000 square miles.

Immigrants (1889), 6,330; Emigrants, 3,706.

Imports (1889), £1,260,000; Exports, £1,393,000.

Coffee exported (1890): 13,000 tons; value, £1,240,000.

Exports to Great Britain, £730,000; Imports from Great Britain, £372,000.
Revenue (1890), £1,015,000 ; Expenditure, £1,185,000; Debt, £3,542,000.

492 APPENDIX.

Shipping (1890), 309 vessels of 367,000 tons (136 British of 149,000 tons).
Railways (1891), 230 miles open or nearly completed.

Telegraphs: 600 miles; offices, 31 ; messages, 112,500.

Army: 600 regulars; 32,000 ue and reserves.

Primary schools (1890) : 300; attendance, 15,000.

PANAMA:

Area, 31,570 square miles; population (1881), 285,000; 1890 (est.), 310,000.
Chief towns: Panama, population, 15,000; Colon (Aspinwall), 5,000 ; David, 4,620.
Interoceanic Railway (opened 1855): 90 miles; passengers (1888), 1,300,000; goods, 320,970 tons.

THE PANAMA CANAL.

Length, 46 miles; begun, 1881; works susperded, March, 1889. Original estimate, £26,320,000 ;
actual outlay, £60,000,000. Work done, about 12 miles; estimate of time required to complete the
cutting, 20 years from 1891; probable cost, £120,000,000, apart from the outlay already incurred.
Total cost, including arrears of interest, deterioration of plant, &c., over £200,000,000.

WEST INDIAN ISLANDS.*

POLITICAL DISTRIBUTION. Forei
oreign Trade

1590.
Hai < : : : ; 2 : Republic
Independent a San Domingo . : ; Republic . : | eNOS
Spanish Islands Cuba, Isle of Pines, pact Hing : Assimilated colonies 12,000.000
Bermudas, Bahamas, Jamuica, urke | (PRE institu-
Kitts, Nevis, Antigua, Dominica, St. vis | tions without respon-
British Islands .{ cent, Grenada and Grenadines, Barbados sible government. 6,200,000
| Virgin Islands, Montserrat, St. Lucia. { Wit Bout : és
\ tive institutions. )
French Islands . St. Bartholomew, Guadeloupe, Martinique Assimilated colonies 3,200,000
Dutch Islands . St. Eustatius, Saba . i ’ : à jee ENED
government.
French & Dutch St. Martin Mixed system. » 1,200,000
Danish Islands . St. Thomas, St. John, Santa Cruz . pias te responnible
government.

Total Trade . ° ° £26,400,000

CUBA.
AREAS AND POPULATIONS.

Provinces. Divisions. Area in sq. miles. Population.
Pinar del Rio 2 5 ; 5,950 5 5 5 182,204
West Habana 4 < F 5 3,420 : . ‘ 435,896
i ‘)Matanzas . ; ; à 3,380 5 : : 283,121
Santa Clara . ‘ : 4 9,210 5 2 co 321,397
Central Puerto Principe . : > 12,000 . : : 69,245

East . Santiago . : 4 . 14,000 : : 229,821

otal’... 0 acee ce BSED: (SUPE Mig cok ll OL BE

* Exclusive of Trinidad, Tobago, and the islands on the Venezuelan coast.

APPENDIX. 492

Chief Towns. Population, Chief Towns. Population.

/ Havana ; A 198,720 Puerto Principe - : 46,640
Guanabacoa. : 29,790 Cienfuegos : : : 65,070

\ Replat. | RCE 11,280 Central ) Sancti Spiritu . . . 32,600

West Matanzas . : 87,760 . Trinidad . : : A 27,640
Pinar del Rio : 21,770 Santiago . . : : 71,300

[és : ‘ : 20,400 East . | Holguin . 7 : : 34,760
Cardenas. 5 17,550 Manzanillo. : ‘ 23,200

GROWTH OF POPULATION :—

DATE te Oo re 179 000 (SR CM" 12250 000
ES PAU 1891 (est.) . . 1,620,000
Negroes imported between 1521 and 1821, 413,500 (Humboldt).

FREE AND SLAVE POPULATION BEFORE THE EMANCIPATION : —

Year. Whites. Free Negroes. Slaves. Total. Year. Whites. Free Negroes. Slaves. Total.
1774 96,440 30,849 44,333 171,622 1846 895,767 149,226 323,759 1,368,752
1817 289,830 114,058 199,145 553,035 1875 915,000 220,000 235,000 1,360,000

TRADE OF HAVANA.

Shipping (1889) : 1,058 vessels of 1,266,000 tons entered.
LL, 1,333,000 ,, cleared.

Total ve) 5 2.000 eee 2,596,000 ,,

Exports, £5,856,000 ; Imports, £2,523,000. Yield of sugar (1888), 656,719 tons; yield of molasses
(1888) 157,791 tons; yield of tobacco (1888), 300,000 bales. Cigars exported from Havana (1890),
222,000,000. Revenue (1890), £5,160,000; Expenditure, £5,090,000; Debt, £37,200,000. Railways
opened (1890), nearly 1,000 miles. Telegraphs, 2,810 miles of wire. Army, 19,000 regulars of all arms.

JAMAICA.

AREAS AND POPULATIONS.

Counties. Parishes. Area in sq. miles. Population (1881).
Kingston : : : ‘ Site: F : . 388,566
: St. Andrew . ; ‘ Son ac : 5 . 84,982
SR ES RS NE CT cal a8 aa6
ee ; ë : : - 300) . 4 . 28,901
St. Catherine . : : . 465 . : A > OL STLO
fs Mary - - : O0 5 : . 39,696
Middlesex . . . ( St; Ann . > : ; = LA80%. : 5 . 46,584
(eae Bee Mane Pa RS ER
Manchester. à à 5 alse 3 : . 48,458
St. Elizabeth . : : - 486." % : c . 64,375
| Westmoreland : À 018. f ‘ . 49,035
West, or Cornwall 4 Hanover . 2 L ; TRUE : 2 . 29,567
St. James 3 é : Bye hers : é . 08,625
| Trelawney . A : VOTRE ë ; . 82,115
Total AL CRE ADO ht. te. : 680,804

Population (est.), 1890 . : 2 È : : . 635,000

A Turks and Caicos Islands i à : ; 5,000
Ap Cayman Islands . : : 5 à 4,000

Total Jamaica and Dependencies . . + 644,000

494 APPENDIX.

CHIEF TOWNS.

Population. Population.
Kingston, with Port Royal : . 40,000 | Montego . - A : . . 5,000
Spanish Town . : À : . 6,000 Falmouth . : ° . . . 3,000
Port Maria , 2 A : ee 000 |
PROPORTION OF WHITES AND PEOPLE OF COLOUR : —
Whites. Coloured. Total. Proportion.
1830 . 20/0001. > o24,0008 = . 344,000 . Lo I6
1890 . Jo 000 > 620,000 . 635,000 . toit

Indian coolies (1889), 13,000, of whom 460 under indentures.
Emigration (1889), 3,184; Immigration, 11,670.
Crops:—sugar-cane, 32,500 acres; coffee, 20,000 acres; ground provisions, 80,000 acres; Guinea.
grass, 124,000 acres ; common pasture, 310,000 acres; common pasture and pimento, 46,000 acres.

Shipping (1888): 451 vessels of 411,379 tons entered
474 Dp 412,375 ,, cleared

—

Total : 925 5 825,754, of which 93 per cent. were British.

Railways open (1890), 64 miles; passengers car- Letters passed through the Post Office, 1.452,000.
ried, 265,000. . Elementary schools, 826; attendance, 76,000.
Telegraphs: 608 miles; messages, 87,000. Garrison troops, 1,120 men; volunteer militia, 620.

ISLAND OF SAN DOMINGO:

States. Area in Square Miles. Population.
Etre : 3 ‘ 10,204 J - : 1,000,000.
San Domingo : : 18,045 - : 5 610,000.

TOR ects. is MOST Ihre ee Sale Re 610 00D.

HATTE.
ADMINISTRATIVE DIVISIONS.
Pop. of ’ Pop. of
Departments. Department. Departments. Department.
Nord . E 2 ° ° > . 250,000 Ouest . c 5 = : 5 . 390,000
Nord-Ouest . = é 4 3 . 70,000 Suda. . : ; 5 5 . 200,000

Artibonite . : 5 : 3 . 125,000
Imports (1889), £1,500,000; Exports, £2,650,000.
Revenue, £1,300,000 ; Expenditure, £1,280,000 ; Debt, £2,700,000.
Army, 7,000 men; Navy, 1 gun-vessel of 900 tons, 1 corvette, 2 sloops.
Shipping: 726 vessels of 692,000 tons entered ; 724 of 680,000 tons cleared.
National schools, 400 ; attendance, 24,000. Post offices, 31; letters forwarded, 480,000.

SAN DOMINGO.
ADMINISTRATIVE DIVISIONS.

Provinces and Popu- Chief Popu- Provinces and Popu- Chief Popu-
Districts. lation. Towns. lation. Districts. lation. Towns. lation.
Azua de Com- } Barahona . 5,000
50,000 Aza. . . 14,000 Barah - 20,000 {€
postela : sx ; MES | Neiba. . . 12,000
Santo Domingo 134,000 $. Domingo. 25,000 San Pedro . 40,000 San Pedro . 7,000
Sebo. = = 30) .06,000) Selbo <5 =. 1250u0 Samana . . 18,000 Santa Barbara 5,000
Vega . 11,000 Puerto Plata . 40,000 Puerto Plata 15,000
Vv AAU 1997000 { ae , es
SEA AU MO 18,000 Monte-Cristi . 40,000 Monte-Cristi 1,500

Santiago . . 40,000 Santiago. . 32,000
Imports (1888), £400,000; Exports, £500,000 ; total, £900,000.
Sugar crop, 18,700 tons; molasses, 22,000 tons.
Tobacco exported (1889), 8,500 tons.
Shipping, 276 vessels of 200,000 tons entered and cleared.
Revenue (1889), £306,000 ; Expenditure, £280,000; Debt, £2,000,000.
Municipal schools, 300 ; attendance, 10,000.

APPENDIX. 495

PUERTO RICO.

ADMINISTRATIVE DIVISIONS.

Departments. Pop. (1887). Chief Towns. Pop. Departments. Pop. (1887). Chief Towns. Pop.
San Juan . 27,000 Cabo Rojo. 17,000

pos Par } 131,116 | Bayamon. 15,000 | Ponce . . 48,000
: VUS Rio Piedras 11,000 Ponce. . . . 160,140 / Yauco . . 25,000
: _€ Arecibo . 30,000 Juana Diaz 21,000

9
RUES Tee Uienads . 31,000 Adjuntas . 16,000

Aguadilla . 16,000 f Guayama . 14,000
ares... 17,000 ( Caguas . . 15,000
Mayaguez. 28,000 Humacao. . . 88,270 Humacao , 15,000

SanGerman 20,000 NA
806,708

Area: 3,550 square miles. Imports (1888), £2,890,000 ; Exports, £2,410,000. Sugar crop, 62,000
tons; coffee, 23,000 tons; tobacco, 1,518 tons. Shipping, 2,812 vessels of 2,452,000 tons entered and
cleared. Railways open (1890. 52 miles. Telegraphs, 500 miles of wire. Revenue (1890), £736,000 ;
Expenditure, £726,000.

Aguadilla . . 86,551 | Guayama . . 98,814

Mayaguez . . 116,982 |

DANISH ANTILLES.

Islands. Area in sq. miles. Population,
St. Thomas 2 ‘ ; 23 : ‘ : 14,389
St. John a : 21 ; 5 = 944
Santa Cruz à : É 74 : : ; 18,430

Total : 20 Ai 5 : : 33,763

Average export of sugar, 14,000,000 lbs. ; rum, 1,000,000 gallons.
Revenue (1890), £27,000; Expenditure, £38,000.

BRITISH WEST INDIES.*

Areain Population

Groups. sq. miles. (1890). Revenue. Expenditure. Debt. Imports. Exports.
Bermudas 20 16,000 £30,000 £30,000 £7,000 £65,000 £273,000
Bahamas 5,450 48,000 46,000 46,000 83,000 176,000 131,000
Barbados 166 180,000 175,000 146,000 1,588,000 1,211,000 1,030,000
, (Antigua 108 35,000
£ Barbuda 62 800
3 | Virgin Isles 58 5,000
4 } Dominica 290 30,000
a | St. Kitts 2e 45,000 113,000 110,000 64,000 429,000 690,000
= | Nevis 50 12,000
5 | Anguilla 35 12,000
H \Montserrat 32 10,000
a St. Lucia 245 45,000
4 ä | St. Vincent 122 48,000
BS Grenada | 124,000 130,000 195,000 477,000 522,000
A and 120 50,000
= \ Grenadines ù

Bermupas :—Chief town, Hamilton; population, 8,000. Land under cultivation, 4,000 acres. Schools,
47 ; attendance, 1,409. Shipping (1889), 222,000 tons entered and cleared, of which 180,000 were
British. White population, 6,200; coloured, 9,750.

Banamas :—Chief town, Nassau; population, 5,000. Pineapples exported (1890), 285,000 dozen, value
£28,000. Sponges exported (1889), £51,000. Schools, 72; attendance, 6,000.

* Exclusive of Jamaica, Trinidad, and Tobago.

496 APPENDIX,

Barsanos :—Capital, Bridgetown; population, 25,000. Land under cultivation, 100,000 acres, of which
30,000 under sugar. Yield of sugar (1889), 65,270 hogsheads. Yield of fisheries, £17,000; hands
employed, 1,500. Primary schools, 201 ; attendance, 13,000. Railways, 24 miles.

Lerewarp Istanps:—Capital, St. Johns (Antigua) ; population, 10,000. Chief town, St. Kitts, Basse-
terre ; population, 7,000. Yield of sugar, Antigua (1889), 10,500 hogsheads, value £223,000.

WixpwarD Isnanps:—Capital of St. Vincent, Kingston ; population, 6,000; capital of Grenada, St.
George’s. Total imports and exports, £306,000. Land under cocoa (Grenada), 12,500 acres ; yield,
36,000 tons. Government and other schools, 110; attendance, 13,000. Shipping (1889), 3,114
vessels of 1,904,000 tons entered and cleared.

DUTCH ANTILLES.*

Tslands. Area in sq. miles. Population (1890). Capital.
St. Eustatius . . - c 8 - : : 2,350 : = c Orangetown.
Saba : 5 A : : 5 : 5 : 2,500 : 3 5 —

St. Martin (part of). : me fs A : ‘ 4,500 : : Phillipsburg.
Total 3 5 eH) 9,350

Average annual yield of salt, 10,500,000 bushels,

FRENCH ANTILLES.

Islands. Area in sq. miles. Pop. (1890). Islands. Area in sq. miles Pop. (1890).

St. Bartholomew . : Oo 3 2,650 Desirade . 3 ; Oe 5 1,400

Saintes . : j : OM s 1,900 Marie-Galante . à 65 . . 13/830

St. Martin (part of) AAECTPXE : 3,500 Martinique : - 400 . . 177,000
Guadeloupe . : 5 CODE . 135,650 ts =

Total . men Oars . 835,950

GUADELOUPE :—Chief towns: Basseterre (capital), population, 12,000; Pointe-à-Pitre, population, 17,250;
Le Moule, population, 10,000. Revenue and expenditure (1890) balanced at £260,000; Debt,
£40,000. Imports (1889), £975,000 ; Exports, £1,050,000. Sugar crop (1888), 49,000 tons; land
under sugar-cane, 57,000 acres. Yield of Coffee, 580 tons; coffee plantations, 125,000 acres.

- Shipping, 946 vessels of 637,000 tons entered and cleared. Primary schools, 50 ; attendance, 9,700.

Marrriavr :—Chief towns: Fort-de-France (capital), population, 15,000; Saint-Pierre, population,
26,900 ; Lamantin, population 14,000 ; Le Francois, population, 11,000. Revenue (1890), £140,000 ;
Expenditure, £84,000; Debt, £18,000. Imports (1889), £916,000 ; exports, 940,000. Land under
sugar-cane (1838), 53,000 acres; bananas, 42,000 acres. Shipping (1890), 1,920 vessels of 630,000
tons entered and cleared. Primary schools, 29; attendance, 8,320.

* Exclrsive of the Dutch islands on the Venezuelaz coast.

Abaco Islands, 444
Abbotsville, 236
Acajulta, 252
Acanti, 334
Acapulco, 41, 77, 137
Acatenango, 210
Acaxees, 84
Acklin Island, 447
Acolhuacan, 64
Acoyapa, 287
Actopan, 32
Adamanay Islands, 403
Adjuntas, 426
Agiabampo, 97
Agua Volcano, 209
Aguacatlan, 222
Aguada Town, 427
Agua de Sangre, 265
Aguadilla, 426
Aguan River, 258
Aguanaval River, 45
Aguascalientes State, 54, 107
Town, 107
Aguayo, 104
Aguila Peak, 245
Ahoga Yeguas, 313
Ahuacatlan Peak, 24
Ahuachapam, 244, 251
Ahualco Pass, 52
Ahuilitzapan, 130
Ajusco Mountain, 27, 1
Akal’mans, 88
Ake, 167
Alacran Cay, 146
Alajuela, 297, 307
Alamos Mountains, 23
Town, 97
Alanje, 223
Alberca Crater, 27
Algarrobo River, 323
Almendares River, 370
Almirante Bay, 295, 303, 312, 316
Alotepeque, 234
Altata, 97
Altavela Island, 404
Alta Vera Paz, 213, 236
Altos Region, 207
Altos Cuchumatanes Mountains, 212
Alvarado, 40, 135
Amapala, 260, 266
Amatique Bay and Town, 192, 193,
213
Amatitlan Department, 232
Lake, 214, 232
Town, 232
Amayo Volcano, 212
Ambergris Island, 195
Ameca River, 113
Town, 113

NY ee

Amecameca, 126
Amecas River, 41
America, City of, 289
Central, 201
Name of, 272
Amerrique Mountains, 272
Anahuac Plateau, 4, 20, 28, 34, 45
Andros Island, 442
Anegada, 348, 436
Angel River, 296
de la Guardia Island, 22
Angostura, 307
Anguila Island, 463
Anguilletta Island, 463
Annotta, 393
Anse-d’ Hainault, 413
Antigua Department, 231
Island, 464
Town, 231
Antilles—
Great, 354, 460
Lesser, 455
Anton Lizardo, 40, 134
Apache Mountains, 31
Apaches ‘Tribe, 84
Apacingan, 114
Apam Lake, 126
Town, 126
Apaneca Volcano, 245
Apoyac River, 41
Apoyo Lake, 284
Aquin, 414
Arawaks, 404, 460
Arecibo Department, 426
Town, 426
Ario, 115
Avispe, 95
Armenia, 252
Arrowsmith Bank, 146
Artibonite River, 397, 401
Asencion Bay, 195
Asososca Lake, 284
Aspinwall, 327
Asuncion River, 95, 146
Atenas, 307
Atiquisaya, 251
Atitlan Lake, 208, 214
Volcano, 208
Atlixco, 55, 129
Atotonileo, 116
Atoyac River, 137
Atrato River, 201, 314, 334
Atravesado Mountain, 143
Atwood Cay, 447
Aves Island, 455, 457
Ayarza Lake, 214
Ayutla, 225
Aztecs, 59, 219, 261
Aztlan, 111

Azua Province, 419
Town, 419
Azuero Peninsula, 299, 313

Baburuco, 402
Bacalar Lagoon, 170, 195
Town, 170, 200
Bagdad, 104
Bahama Bank, 442
Channel, 442
Islands, 437
Sea, 339
Bahia Honda, 361, 372
Bajo Nuevo Bank, 341
Balancan, 164
Balsas River, 41
Banderas Bay, 42
Bani, 420
Danica, 419
Baracoa, 354, 377
Baradères Bay, 413
Barbados Island, 485
Barbareta Island, 260
Barbasco, 234
Barbuda Island, 465
Barca, La (Mexico), 41, 111
Barra de Tabasco, 148
Barranca River, 306
Bartlett Point, 340
Basseterre (St. Kitts), 45, 470
(Guadeloupe), 472, 474
Bastimentos Island, 323
Batabano, 370, 373
Batopilas, 100
Baudo Mountains, 314
Bay Islands, 7, 259, 262
Bayamo, 369, 377
Bayamon River, 425
Town, 426
Bayano River, 313, 316
Belize Bay, 195
River, 195
Territory, 191
Town, 191, 196
Bellamy Peak, 194
Bemini Islands, 444
Bequia Island, 481
Bermudas, 449
Bernal Mountain, 104
Berry Islands, 444
Bird Island, 454
Bris, 296
Black River, 384, 393
Blanco River, 148
Peak, 299
Blewfields Lagoon, 277
River, 277
Town, 287
Blue Mountains, 383

498

Boca del Cerro, 148
Conil, 152
Drago, 295, 312, 316
Monte, 184
Tigre, 316
Toro, 316, 323
Boca Nueva, 236
Bohio Soldado, 327
Bolaños, 112, 286
Bolonchen, 152
Bolson de Mapimi, 32, 102
Bonaca Island, 260
Boqueron M unt in, 258
Boquilla de Piedras, 29
Borucas or Bruncas, 305
Bramador Mountain, 110
Bravo River, 14, 36
Breña, La, 23
Brewer Lagoon, 259
Bribri, 305
Bridgetown, 486
Brimstone Hill, 469
British Honduras, 191
Brito, 286
Broa Bay, 359
Brujuelas River, 402
Brus Lagoon, 259
Buenayre, 286
Bugaba, 323
Burica Point, 299

Cabafias, 372
Cabecar, 299, 305
Cabo Rojo, 427
Roxo. 39
Cabritos Island, 402
Cacahuamilpa, 136
Cachapa, 263
Cadereyta, 116
Cadereyta-Jimenez, 103
Caguas, 428
Cahabon Mountains, 213
River, 215
Cahitas, 81
Cahos Mountains, 400
Cahuinal, 229
Cahuita Point, 300
Caicos Islands, 442, 448
Cakchiquel, 219, 222
Calabozo Lagoon, 24
Calamahue Mountain, 22
Caldera Voleano, 211
Calderon, 111
Caledonia Bay, 318
California, Lower, 21, 22, 93
Gulf, 16, 22, 95
Camaguey, 375
Camargo, 03
Cameron Cape, 257
Campana Mountain, 96
Campeachy State, 142, 164
Town, 164
Cana, 334
Cafiadas Mountains, 364
Canchia Mountains, 257
Candela Mountains, 45
Candelaria River, 150
Caney, 377
Caninzio, 115
Cankun, 168
Caparra, 424
Cape River, 276
Capesterre, 458
Cap-Français, 410
Cap- Haitien, 403
Capira Mountain, 313

INDEX.

Caratasca Lagoon, 259
Carbet, 476
Carca, 283
Cardenas, 361, 373
Cardon Island, 284
Caribbean Sea, 1, 8, 13, 338
Caribs, 8, 220, 262, 283, 459, 460
Carmen City, 164
Carolina Island, 17
Aguada, 195
Carreto, Port, 333
Cartago Province and Town, 307
Casa Blanca, 122
Casas Grandes River, 44
Station, 101
Castillo, 279, 288
de Austria, 323
Castries Port, 479

' Cat Island, 440, 446

Catacamas, 265
Catherine Hill, 383
Catoche Cape, :5, 145
Catorce, 32, 10&
Cauto River, 356, 359
Cavaillon, 414
Caxinas Cape, 258
Cayemites Islands, 413
Cayes Bay and Town, 414
Cayey, 428
Cayman Islands, 2
Ccbaco Island, 3:8
Ceboruco Mountain, 24
Cebuneyes, 404
Ceiba Island, 283
Celaya, 111
Cerro de los Edificios, 107
Cerro Gordo, 130
Chacahua Mountain, 35
Chagres River, 514
Town, 327
Chalatenango Town, 252
Chalchihuites, 106
Chalchuapa, 261
Chalco Lake, 45, 124
River, 45
Chama Mountains, 193, 213
Chame Mountain, 313
Chamela, 113
Chamelicon River, 257, 258
Chametla Town, 98
Chamlico River, 258
Champerico, 227
Champoton, 15
Chañabals, 155
Changuinola River, 300
Chapala Lake, 41
Town, 111
Chapultepec Mountain, 55
Town, 123
Charco Muerto, 285
Charlestown, 445, 470
Charlotte-Amalia, 431
Chepigana, 355
Chepo Mountains, 314
Chetumal Bay, 15, 170, 194
Lagoon, 144
Chiantla, 228
Chiapa de los Indios, 161
Chiapanecs, 155
Chiapas State, 142, 161
Chichankanab Lake, 150
Chichen-Itza, 168
Chichimecs, 62, 63
Chicomoztoc, 64, 107
Chihuahua State, 22, 100
Town, 100

Chile Mountains, 257, 271
Chillador Peak, 26
Chilpancingo, 137
Chiltepec, 148
Chiltepec Volcano, 274
Chimalapa, 141
Chimaltenango. 230
Chinameca Volcano, 248
Town, 253
Chinandega, 284
Chinantecs, 88
Chinchorro Bank, 146
Chingo Volcano, 212, 244
Chiquimula Mountains, 234
Department and Town, 234
Chiri-Chiri Bay, 336
Chiriqui Bay, 201, 302, 316
Mountains, 312
Chiron- Quiaco, 130
Chirripo Mountain, 299
Tribe, 305
Chixoy River, 148, 228
Chocos, 321
Chols, 155, 218
Cholula, 68, 127
Choluteca River, 260
Town and Department, 266
Chonco Volcano, 274
Chontals Tribe, 88, 155, 250
Choroteganos, 281, 282
Chorti, 26!
Chumpan River, 100
Churubusco, 123
Cibao, 400
Cibola, 17
Cibuneyes, 367
Cienaga de Zapata, 359
Cienfuegos, 374
Cimaltepec Mountain, 35, 138
Cinco Villas, 357, 374
Citlaltepetl Mountain, 3, 29, 30
Ciudad del Maiz, 109 :
Guzman, 113
Victoria, 104
Vieja, 210, 230
Coahuila State and Town, 102
Coatepec, 130
Coatzacoa!cos River, 40, 139
Coban Mountains, 215
‘Town, 236
Cobre, 377
Mountains, 356
River, 384
Cochimi, 81
Cockscomb Mountains, 193
Coco River, 276
Cocopas, 81
Cocos Cay, 360
Cocula, 113
Codrington College, 486
Cofre de Perote, 29
Coiba Island, 299, 318
Cojutepec Volcano, 248
Cold Ridge, 383
Colhuas, 63
Colhuacan, 162
Colima River, 41
State and Town, 113
Volcano, 53
Colon (Cuba), 374
Bay, 317
Department, 265
Town, 327
Colorado River, 14, 44, 309
(Costa Rica), 279
Colubrinas, 426

Columa Volcano, 24, 212
Columbus Gulf, 294
Comayagua Department, 265
Mountains, 257
Town, 264, 265
Combey Bank, 341
Comondu, 94
Comotan, 234
Compostela, 113
Concepcion, Vega, 403, 422
Aguada, 195
(Tegucigalpa), 266
Conchagua Volcano, 249
Conchos River, 31, 36, 100
Conchs, 443
Concordia (Salvador), 252
(Nicaragua), 286
Congrehoy Cape, 257
Mountains, 257
Constant Peak, 476
Copan Department, 263
River, 234
Town, 235, 263
Coral Bay, 433
Corales Islands, 274
Coras, 84
Cordoba, 3
Corintu, 284
Corn Islands, 277, 287
Corosal, 200
Corrientes Bay, 362
Cape, 43
Cortes Bay, 354
Coseguina Volcano, 260, 272
Cosihuiriachi, 100
Costa Rica, 293
Coteaux, 413
Cotos, 303
Cotui, 422
Cozumel Island, 145, 169
Crab Island, 423, 428
Crawl Bay, 433
Creoles, 352
Crespon, 139
Crête-à-Pierrot, 412
Cristianos, Llano de los, 31
Croix-des- Bouquets, 412
Crooked Island, 447
Cruces, Las, 185
Town, 315
Cruz Cape, 340
Mountains, 32
Cuachichils, 86
Cuajiniquilapa, 220, 234
Cuautitlan, 123
River, 48
Cuba, 354
Cubilete Mountains, 110
Cucras, 283
Cucurpe River, 95
Cuencame, 102
Cuernavaca, 135
Cuevas, 321
Cuisaltepe Volcano, 272
Cuitzeo Lake, 27, 41, 45
River, 41
Culebra Island, 428
Passage, 313
Culiacan, 97
Volcano, 27
Cuma Volcano, 212
Cuna-Cuna, 322
Cupica Bay, 336
Pass, 314
Cutzarandiro Voleano, 25
Cuyutlan Lagoon, 114

INDEX.

Dalmarie, 413
Dirien Gulf, 1, 317
Harbour, 316, 335
Darienes, 321
David Bay, 201
Province, 312
Town, 323
Delon, 265
Derrumbaderos Mountains, 30
Desaguadero, 280
Desirade Island, 465, 473
Diablotin Peak, 475
Diamant, 478
Diego Campo, 398
Dipilto Mountains, 256, 257
Dirians, 281
Doce Leguas Cay, 362
Doctor Arroyo, 103
Dogs Islands, 463
Doguado River, 326
Dolores, 110
Dolphin’s Head, 384
Dominica Island, 475
Dota Marina Mountain, 29
Dorasques, 321
D >ta Mountains, 298
Dry River, 384
Dulce River, 215
Dunmore, 445
Durango Departmentand Town, 101

Elena Island, 260
Eleuthera Island, 445
Encinillas Lake, 57
English Harbour, 465, 466
Entre-los-Rios, 400
Erandique Mines, 265
Ermita, La, 231
Esclavos, 234
River, 234
Escocesa Bay, 398
Escondido River, 277
Escudo de Veragua Island, 295
Escuintla Department, 233
Town, 210, 233
Española, 397
Hsparta, 307
Esparza, 304, 306
Esperanza, 128, 265
Espiritu Santo Bay, 146, 195
Mountains, 256
Esquipulas Mountains, 215
River, 215, 249
Town, 234
Estero Real, 260, 275
Estrella Mines, 308
Peak, 125
River, 300
Exuma Bay, 442

Falmouth, 393

Flor River, 295

Flores, 237

Florida Strait, 342, 443
Fonseca Bay, 244, 253, 260
Fontabelle, 486
Fort-de-France, 477
Fortune Island, 447
Fortuné Peak, 479
Frailecitos Peak, 23
Francia, 115
Frederiksteed, 435
Fresnillo, 36, 106

Frio River, 279

Frontera de Tabasco, 162
Fuego Volcano, 24, 209

499

Fuerte Fort, 97
River, 43

Gallo, 400
Gandi Mountain, 314
Garbut*Falls, 194
Gibb’s Hill, 450
Giganta Mountains, 22
Gigante Mountain, 32, 94
Gigantes, Llanos, 31
Gila River, 14, 22
Gineta Mountain, 144
G over Reef, 197
Goascoran River, 244, 260
Gobrante, 323
Golfete, 215
Golfo Dulce (Guatemala), 215
(Costa Rica), 300
Gonaives Port, 409, 411
River, 411
Gonave Island, 400
Gracias Department, 263
River, 276
Town, 263
Gracias-a-Dios Cape,
Rapids. 191
Granada Territory and Town, 285
Grand Bourg, 474
Grande, Rio, del Norte, 14, 36
Soufriere, 475
Terre, 472
Grand-Goave, 413
Gran Estero. 398
Piedra, 306
Great Antilles, 354, 460
Exuma, 447
Inagua, 447
Ragged Island, 447
River, 384
Grenada Island, 483
Grenadines, 483
Greytown, 7, 288
Grijalva River, 146, 147
Grita Mountains, 256
Gros-Morne, 411
Grosse- Montagne, 472
Guacalate River, 220
Guadalajara, 111
Guadalcazar, 109
Guadalupe City, 124
Tslaud (Mexico), 58
Mountain, 127
y Calvo Mine, 100
Guadeloupe Island, 471
Guadiana Bay, 358
Guaicuri, 81
Guajoca Pass, 201, 257
Gualan River and Town, 234
Guanabacoa, 367, 372
Guanacaste, 294, 306
Guanahani Island, 354, 437, 446
Guanajay, 372
Guanajuato City, 110
State, 109
Volcano, 110
Guanica, 427
Guautanamo, 356
Guarisamay, 102
Guarumal, 252
Guatemala State, 206
Town, 230
Guatusos, 304
Mountains, 296
Guayama, 428
Guayanilla Bay, 428
Guaymaca Mountain, 258

500

Guaymaro, 377
Guaymas Port, 97
Guaymi, 303, 321
Guerrero State, 135
Guija Lake, 244
Guines, 372 .
Guisisil Volcano, 272
Gulf Stream, 344
Gun Cay, 444
Gustavia, 464
Guzman Lagoon, 44

Haïti, 396
Republic, 410
Hamilton, 454
Harbour Island, 445
Hastings, 486
Hato Mayor, 420
Havana, 370
Herbias River, 277
Heredia Departmentand Town, 307
Hermosillo, 95
Herradura Mountain, 298
Hicacos, 261
Hidalgo State, 116
Hidalgo del Parral, 100
Hinche, 412
Hog Island, 444
Hoistingtown, 486
Holbox Island, 152
Holetown, 486
Holguin, 369, 377
Hondo River, 15, 191, 194
Honduras Bay, 206, 270
British, 191
Cape, 258
State, 254
Hope Gardens, 389
Horqueta Mountain, 312
Hrseshoe Reef, 348
Hotte, La, Mountains, 400
Huabi, 140
Huamantla, 128
Huatuleo, 139
Huaxiacac, 137
Huaxtecs, 62, 87, 220
Hue Colhuacan, 97
Huehuetenango Department, 228
Town, 228
Huehue-Tlapellan, 62
Huehuetoca, 37, 48, 123
Hueitepec Mountain, 144
Huejutla, 88, 116
Huexotzingo, 126
Humaredas Mountains, 26
Humaco, 428
Humuya River, 257

Icacos Point, 361, 373

Icotea de Limon, 403

Iguala River, 136
Town, 79, 136

Tlobasco, 252

Ilopango Lake, 246
Volcano, 247

Inde, 102

Indio River, 277

Intibucat, 259

Ipala Volcano, 212

Irapuato, 111

Irazu Volcano, 297

Ireland Island, 450, 454

Trolo, 12€

Irritlas, 8€

Isaac Cay, 444

Isabella, 422

INDEX.

Isabel Segunda, 428
Iturbide, 168
Itza Tribe, 216, 220
Lake, 194, 216
Itzacapa River, 214
Txbul Peak, 15
Iximche, 230
Ixmul, 169
Ixtaccihuatl Mountain, 28
Ixtapalapa, 47, 125
Ixtlahuaca, 117
Ixtlan (Michoacan), 139
(Oaxaca), 111
Izabal Department, 235
Lake, 215
Town, 235
Tzalco Volcano, 245
Izamal, 166

Jacala, 116

Jacmel, 415

Jaen Volcano, 272

Jalapa (Vera Cruz), 129
(Guatemala), 234

Jalisco State, 109, 111
Town, 113

Jalpan, 38, 116

Jalteba, 285

Jaltipan, 142

Jamaica, 382

Jamapa River, 133

Jardines Islands, 362

Jardinillos Islands, 362

Jérémie, 413

Jerez River, 112

Jesus Maria Mountain, 23

Jiboa, 252

Jicoma, 400

Jimenez River, 279

Jinotega, 287

Jinotepe, 286

Jocotan, 234

Jorullo Voleano, 24, 245

Juanacatlan, 42, 111

Juana-Diaz, 428

Juigalpa, 287
Mountain, 272

Julian, 377

Jupiter Inlet, 344

Juquila, 35

Juragua, 377

Jutiapa Department and Town,

234
Jutigalpa, 265

Kabah, 168
Kachiquels, 156
Kamue Mountain, 299
Kingston, 392
Kingstown, 483
Koom, 287

La Barca, 41

Labna, 168
Lacandons, 155, 218
Ladinos, 9

Lagartos River, 153
Lagos, 112

Laguna, 153

Lajas River, 279
Lamans, 283
Lamentin, 478
Lares, 426

Leeward Islands, 455
Lempa River, 244, 249
Lencas, 261

Leon (Mexico), 110
(Nicaragua), 284
Lepaterique Mountains, 257
Lerdo, 97
Lerma River, 24, 41
Town, 117
Libano Mountain, 359
Liberia, 306
Libertad (Nicaragua), 287
(Salvador), 252
Liganee, 392
Lighthouse Reef, 197
Limon Town and District, 307
Linares, 103
Livingston, 235
Llanitos Peak, 32
Llanos, 51 ;
Loma Barranca, Pansa, Tina, 400
Loreto Mountain, 127
Town, 94
Lorillard, 164
Lucayas, 444
Luguillo Mountain, 423
Luz, La, 110

Machuca River, 279
Macouba, 478
Macuiltepec Volcano, 29, 129
Madre del Volcan, 245
Magdalena, 228
Maisi Cape, 355
Malinche Volcano, 29
Maltrata, 184
Mamanchota Mountain, 32
Mamantel River, 150
Mamé Tribe, 155, 218
Managua Lake, 272, 278

Territory, and Town, 284
Mandeville, 390
Mani, 167
Manzanillo, 377

Bay, 359, 397

Island, 327

Port, 51, 114
Mapimi, 102
Maria-Enriquez Mountains, 313
Marie-Galante Island, 473
Mariel, 372
Marigot, 464
Mariguana Island, 446
Marina, 104
Mariscal Lagoon, 195
Marnata, 114
Marques Mine, 94
Marrabios Mountains, 274
Martinique, 476

‘ Little,” 481, 483
Masaya Town, 286 .
Volcano, 274
Mascota, 113
Massacre River, 410
Matachin, 315, 327
Matagalpa Mountains, 272
River, 277
Territory and Town, 287
Matamoros, 103

de Izucar, 129
Matanzas Province and Town, 273
Mataquezcuintla Mountain, 214
Matlaltzincas, 86
Mayaguez, 427
Mayapan, 167
Mayas, 155, 220
Mayos, 81
Mazahuas, 86
Mazatenango, 222, 230

Mazatlan, 51, 97
Meco, El, 168
Medellin, 135
Mediterranean, American, 1, 338
Melchoras, 283
Memory-rock, 344
Mems, 222
Menche, 164
Mendocino Cape, 16
Mercado Mountain, 101
Merendon Mountains, 256
Merida, 165 —
Meseta Volcano, 210
Mestizoes, 74, 91
Metapan Town and District, 251
Metlac, 183
Mexcal Island, 111
Mexcala River, 25, 41, 114
Mexico City, 117
Gulf of, 1, 338
Republic, 14
State, 41, 117
Mexicans, 59, 60, 64
Mextitlan, 116
Mexquital, 102
Miahuatlan, 138
Michatoya River, 210, 214
Michoacan, 109, 114
Mico Mountains, 213, 215
Mijes, 141
Minatitlan, 40, 141
Mineral del Monte, 34, 1
Miragoûne, 413
Miravelles Peak, 296
Misery Mountain, 469
Misoco Mountains, 257
Misteriosa Bank, 340
Mitla, 137
Mixco, 221
Mixes, 88
Mixtecs, 62, 89
Mixtlan, 34
Moea, 422, 425
Moctezuma, 96
Mojada Mountains, 102
Mole St. Nicolas, 399
Mombacho Volcano. 274
Momotombito Island, 274, 282
Momotombo Volcano, 274
Mona Island, 427
Passage, 343
Monclova, 102
Montecillos, 257
Monte Cristi, 398, 422
Monte Diablo, 398
Montego Bay, 393
Montemorelos, 103
Monterey, 103
Montezuma River, 37, 46
Mont-Roui, 412
Montserrat Island, 470
Monts Noirs, 400
Mopan River, 196, 216
Mopans, 15, 220
Morant Bay, Cay, Point, Town, 394
Morelia, 34, 115
River. 45
Morelos, 136
State, 135
Moscos, 283
Mosquito Bank, 259, 277
Bay, 393
Coast, 2, 281, 287
Motagua River, 214
Moule, Le, 474
Mount Eagle, 434

INDEX.

Moyuia Volcano, 212
Muerto Lagoon, 45
Mujeres Island, 146, 169
Mulege, 95

Mu.etas Islands, 316
Muoi, 321

Nacaome Town and River, 266

Naco, 264
Nagrandans, 281
Nahuas, 61, 281
Nandaimé, 161, 286
Napipi River, 326
Naranjo Peak, 245
Narrows, 450
Nassau, 444
Nata, 323
Natividad, 419
Nautla, 13i
Navajas Mountains, 117
Navaza Island, 1
Nayarit Mountains, 23
Tribe, 107
Nazas, 102
River, 45
Negril Creek, 393
Negro River, 148, 256, 276
Nejapa Lake, 284
Nemu Mountain, 299
Nevado de Toluca, 27, 41
Nevis Island, 457, 468
Newcastle, 389, 393
New Providence, 444
Neyba Bay, 397
River, 400
Nicaragua, 270
Canal, 290
Lake, 272, 274, 279
Nicoya, 306
District, 294
Gulf, 294, 299, 300
Peninsula, 299
Nieve Volcano, 24
Nim Pokom, 228
Nindiri Town, 286
Volcano, 274
Nipe, 354
Nippes, 413
Niquirans, 281
Nito, 236
Nohpat, 167
Nombre de Dios, 102, 332
Nueva Galicia, 72
Nuevitas, 354, 376
Nuevo Laredo, 103
Leon, 102, 103
Sevilla, 236
Viscaya, 101

Oaxaca State, 135
Town 137
Obispo River, 315
Obrage, 286
Ochomogo Mountain, 201
Pass, 298
Ococingo, 163
Ocos River, 225
Ocote Mountain, 249
Ocotal River, 256, 287
Ojo Caliente, 107
del Liebre, 93
del Toro, 357
Olancho, 265
Old Harbour, 393
Olmecs, 62
Ometepe Islands, 274

Omoa Mountains, 194
Town, 257, 264
Opalaca Mountains, 257

Opatas, 81, 95
Oposura, 96
Organds Mountains, 32, 116
Cuba, 358
Orizaba, 130
Volcano, 29, 130
Oro River, 276
Orosi Voleano, 296
Orotiñans, 281
Ostua River, 249
Otomi, 62, 86
Otumba, 125
Ozama River, 401
Ozumba Volcano, 27

Paalmul, 168
Pacaya Mountains, 256
Volcano, 210
Pachuca, 45, 116, 172
Pacora Hills, 313
Pajarito, 420
Pakalah, 229
Palenque, 162
Palisades, 392
Palizada, 162
River, 150
Palma Volcano, 272
Palmas Peninsula, 313
River, 37, 104
Pamal, 168
Pamés, 86
Panajachel, 229
Panaloya, 278
Panama Bay, 323
Canal, 328
Gulf, 1, 300, 316
Isthmus, 312
Province, 312
Town, 323

Pan de Azucar Volcano, 272

Gujaibon, 358

Matanzas, 358
Panuco District, 73

River, 37

‘Lown, 105
Panzos, 236
Papagos, 81
Papaloapan, 40, 135

River, 139
Papasquiaro, 102
Paracuchichi, 336
Parismina River, 300
Parita Bay, 323
Parras Lagoon, 45
Pasion River, 148
Paso del Norte, 100
Patamban Mountain, 24
Patos Island, 97

Lagoon, 45
Patuca River, 258
Patzcuaro, 115

Lake, 45
Paya Mouutain, 257
Payas, 261
Paz, La, Bay, 22

Town, 48, 93, 265
Paza, 251

River, 206, 244
Pearl Cay, 277

Islands, 277, 299

Lagoon, 287
Pedregal, 25
Pedro Bank and Cay, 340

501

502

Pelée Mountain, 476
Peñon de los Bajos, 60
Pens:cola Island, 283
Pepino, 426
Periban Mountain, 24
Perico River, 337
Pericu Tribe, 81
Perote, 130
Pestel, 413
Peten, 199
Lake, 194, 216
Petit-Goûve, 405, 413
Peto, 169
Philipsburg, 464
Picara Volcano, 272
Pichilingue, 93
Piedad de Cabadas, 111
Piedras, 265
Negras, 102, 185
Pija Mountain, 257
Pilon de Azucar, 398
Pimal Mountain, 23
Pimas, 81
Pimeria, 81
Pinacate Volcano, 23
Pinar del Rio, 359, 372
Province, 372
Pines, Island of, 362
Pinogana, 335
Pinos, 260
Pinula, 232
Pipils, 220, 250
Pitic, 95
Plaisance, 411
Platotepe Volcano, 272
Plymouth, 471
Poas Volcano, 298
Pochutla, 35
Pointe-à-Pitre, 474
Pokomans, 220
Pokonchi, 221
Polochic River, 213, 215
Ponce, 428
Popocatepetl, 24, 27
Popolocas, 283
Port Antonio, 393
Port-au-Prince, 412
Bay, 400
Port-de-Paix, 410
Porte-d’Enfer, 474
Portillo de Tarifa, 35
Portland Ridge, 384
Port-Margot, 410
Port Maria, 393
Port Royal, 392
Port-Salut, 413
Portsmouth, 475
Potosi, 286
Potrerillo, 358
Poyas, 261
Presidio del Norte, 101
Principe, Fort, 372
Principolca, 287
Progreso (Honduras), 265
(Yucatan), 166
Providence Channel, 442
Puca Mountain, 257
Puebla Town and State, 126
Pueblo Viejo, 130, 228, 265
Pueblos, 60
Puente de Dios River, 37, 38
Puente Nacional, 130
Puerto Angel, 138
Barrios, 234
Belo, 324, 326
Caballos, 258, 264

INDEX.

Puerto Cortes, 264
Escoces, 317, 333
Escondido, 150
Gorda, 200
Icacos, 361
Limon, 307
Mico, 272
Plata, 422
Principe, 375
Rico, 423
Sal, 265
Viejo, 307

Puntarenas, 306

Purapura, 306

Puruandiro, 115

Putricanti, 333

Quekchi, 221, 236
Quelens, 155
Quemada, 108
Queretaro, 116
River, 116
State, 115
Quevas, 321
Quezaltenango, 206, 226
Volcano, 208
Quiahuitzlan, 151
Quichés, 146, 222
Quirigua, 221, 234
Quisqueya, 397

Rabinal Town and River,

Rama River, 289
Ramas, 283

Rancho Chiquito, 201
Raspadura River, 346
Real del Monte, 116
Realejo, 284

Redonda Island, 467, 470

Redondo Voleano, 212

Regla, 116

Reinosa, 103

Retalhuleu, 226, 230
Department, 226

Reventazon River, 300

Revilla Gigedo Islands, 15, 31, 58

Rio Grande (Lerma), 41

(Panama), 300

del Norte, 36

de Pirris, 300

de Tarcoles, 300

de Terraba, 300
Rio Pedras, 426
Rivas, 286

Isthmus, 279
Rivière Salée, 472
Roatan Island, 260, 262
Romano Cay, 360
Rosalind Bank, 340
Rosario, 420
Roseau, 475

Rovalo Mountain, 296, 299

Rucillo Peak, 400
Rum Cay, 447

Saba Island, 456, 467, 468

Sabaibos, 84
Sabana Grande, 428
Sabinal Cay, 360
Sacapulas, 228
Sacatecoluca, 252

Sacate Grande Island, 257

Sacbé, 168
Sacluc, 236

Sagua-la-Chica River, 359

Sagua-la-Grande River, 359
Town, 375

Sahcaja, 227

Sahuaripa, 96

St. Bartholomew Island, 464

St. Christopher Island, 457, 468

St. Esprit, 478

St. Eustatius Island, 468

St. George Island, 454
Fort, 484

St. John Island, 433
(Antigua), 466

St. Kitts, 457, 468

St. Louis, 184

St. Lucas Cape, 16

St. Lucia Island, 479

St. Marc Cape, 412

St. Martin Island, 463 ~

St. Pierre, 477

St. Raphael, 412

St. Thomas Island, 430
Bay, 240

St. Vincent Island, 489

Saintes Islands, 473

Salado River, 36

Salama, 228
River, 228

Salamanca, 111, 170

Salazar, 185

Sale-Trou, 415

Salina de Cruz, 40, 140

Salinas Bay, 286, 296
(San Luis), 109

Saltadero, 378

Salt Cay, 442, 348

Salteba, 285

Saltillo, 31, 102

Salvador State, 244
City, 252
Volcanoes, 246

Salvaleon, 420

Salvatierra, 111, 414

Samala River, 208

Samana Bay, 397, 421
Island, 447

Sambos, 262

Sanacté, 168

San Andres Voleano, 26
(Chalchicomula), 128
(Guatemala), 237
Island, 277, 323
Town, 262

San Angel, 123

San Antonio Cape, 354
Mine, 94
River, 24

San Bartolomé, 95

San Benito, 161

San Bernardo, 307

San Blas Mountains, 314
Bay, 43, 313, 316
Islands, 316
Isthmus, 316
Town, 113

San Carlos (San Domingo), 420
(Costa Rica) River, 279, 300
(Nicaragua), 288
(Sinaloa) Bay, 97

San Cristobal, 163
Lake, 45
las Casas, 162
(San Domingo), 420

San Diego, 14, 372

San Domingo Island, 396
Republic, 418

San Esteban del Puerto, 105

San Eugenio, 95
San Felipe del Agua Mountain, 34
San Felipe Port, 236, 324
San Fernando River, 37
San German, 427
San Geronimo, 228
San Gil, 236
Mountain, 2°13
San Gregorio Mountain, 111
San Jorge, 256
San José, 230, 237
Department, 233
(Costa Rica). 307
San Juan Mount. (Honduras), 257
San Juan Mountain (Jalisco), 113
San Juan River (Mexico), 37
(Nicaragua), 277
San Juan Bautista (Villa Hermosa),
162
(Puerto Rico), 425
San Juan de Dios, 244
del Norte, 259
de los Lagos, 112
San Juan del Rio (Durango), 102
(Queretaro), 116
San Juan del Sur, 286
de Maguana, 419
d’Ulua Island, 40, 131
San Juanito Mountain, 23
San Lorenzo (Honduras), 266
(San Domingo), 420
San Lucas (California), 98
(Costa Rica), 300
San Luis Potosi, 24, 108
State, 108
San Marcos, 225
Department, 222
San Miguel River, 249
Volcano, 248
Bay, 316
Gulf, 335
(-alvador), 253
Allende, 111
San Pablo Meoqui, 100
San Pedro Lagoon, 195
Village, 108
de Sula, 263
Martir, 214
River, 25, 148, 216
Sacatepeques, 225
Volcano, 208
San Ramon, 307
San Salvador Island, 446
City, 252
Department, 252
Volcano, 246
San Sebastian (Chontales), 287
Santa Ana Volcano, 245
Department and Town, 251
Santa Barbara, 258
River and Town, 104
Department, 263
Port, 263
Santa Buenaventura, 102
Sant: Catalina Mountain, 22
River, 103
Town, 378
Santa Catarina Volcano, 212
Santa Clara Town and Prov., 375
Sauta Cruz Cape, 340
Island, 430, 433
(Yucatan), 170
(Rosales), 100
Mountains, 213
(Costa Rica), 306
(Seibo), 420

INDEX.

Santa Cruz (Quiché), 227
Santa Elena Bay, 286
Santa Eulalia, 100
Santa Lucia, 233
Santa Magdalena, 95
Santa Maria Lagoon, 45
Volcano, 208
. la Antigua, 334
del Rio, 109
del Tule, 137
Santander River, 104
Santarem Channel, 442
Santa Rosa (Guatemala), 234
(Honduras), 263
Santa Tecla, 252
Santiago (Cuba), 377
(Mexico), 113
(Venta) River, 41, 258
Mountain, 313
Santo Domingo, 419
Santo Spiritu (Sancti Spiritu), 374
Santurce, 426
San Ubaldo, 287
San Vicente, 252
Volcano, 248
Saona, 403
Sapoa River, 279
Sarapiqui River, 279, 300
Sarstun River, 191, 194
Savana-la-Mar (San Domingo), 421
(Jamaica), 393
Sayula, 113
Sebastian Vizcaino Bay, 22, 93
Seco River, 148
Segovia River, 256
Territory, 287
Seguas, 321
Segura de la Frontera, 128
Selaque Mountains, 256
Sella de Caballo Mountain, 398
Sensenti, 263
Sensuntepeque, 252
Seri, 82
Serranilla Bank, 341
Sibun River, 192, 194
Sierra Madre (Guatemala . 212
(Mexico), 4, 20
(Yucatan), 143
Sierra Maestra, 355
Siguantaneo, 77, 137
Silao, 110
Silla Mountains, 103
Simpson's Lagoon, 463
Sinaloa, 97
State, 95
Sineas, 234
Siquias, 283
Sisal, 166
Soconusco Volcano, 143
Region, 142
Seaport, 161
Solentiname Islands, 279
Solola Mountain, 229
Province, 226
Town, 229
Sombrerete Mine, 36
Town, 106
Sombrero Island, 463
Somotillo, 239
Sonoala Mountains, 23
Sonora State, 23, 95
River, 95
Sonsonate, 251
Department, 251
Soufrière Mount. (Guadeloupe), 472
(St. Lucia), 479

508

Soufriére (St. Vincent), 481
(Montserrat), 470

Spanish Town (Jamaica), 393

Speightstown, 486

Stann Creek, 200

Subtiaba, 284

Suchiate River, 214

Suchil, 40

Suchitepec Volcano, 212

Suchitoto, 252

Sucio River, 309

Sula, 261

Sulaco Mountain, 257

Sumpul River, 244

Tabasco State, 142
Taboga Island, 326
Tacana Volcano, 15, 143, 208
Tactic, 236
Tacuba, 123
Tacubaya, 122, 123
Tajimaroa Volcano, 26
Tajomulco Voleano, 208
Talamanca, 303; Indians, 205
Tamahu, 236
Tamaulipas State, 103
Tamaulipecs, 86
Tamazula, 102
Tamesi River, 37, 104
Tamiahua |.agoon, 38, 104
Tampico River, 37 ; Town, 15, 104
Tamquian, 105
Tancitaro Volcano, 24
Tarahumaras, 82
Tarascos, 86
T'arcoles, 298
Tarquino Peak, 356
Tasco Volcano, 25
Taxco, 136
Teapasemi Muuntain, 258
Tecapa Volcano, 248
Tecojate, 230
Tegucigalpa, 260, 266
Tehuacan (Mexico), 28, 129
(Salvador), 252
Tehuantepec Isthmus, 14, 29, 36
City, 140
Gulf and River, 40
Tejupilco, 117
Tekax, 167, 169
Teleman, 215, 236
Telica Volcano, 274
Temascaltepec, 117
Tempisque, 284
Tenampua, 265
Tenancingo, 117
Tenango, 117
Tenochtitlan, 64, 118
Tenorio Mountain, 296
Tenosique, 15, 164
Teotihuacan, 68, 126, 129
Tepatitlan, 30, 111
Tepeaca, 128
Tepehuans, 53
Tepeyacac, 123
Tepic Mountains, 33
Town. 112; Territory, 109
Tequila, 112
Tequisquiac Mountain, 48
Terminos Lagoon, 144, 150
Terrabas, 305
Terre de Haut, 473
Tetela del Oro, 126
Teul, 108
Texcoco Lake, 45
Town, 64, 69, 125

504

Tiburon Cape, 397
Island, 82, 97
Town, 413; Peninsula, 2

Ticul, 167

Tiger Island, 257; River, 37

Tiguabo, 367

Tihosuco, 169

Tihule Pass, 314

Tikal, 237

Tilema Lagoon. 40

Tilorio River, 300

Tinto River, 246, 256

Tipitapa, 284; River, 278

Tiribi River, 300

Tiribiés, 305

Tiscapa Lake, 284

Tisingal, 308

Tizimin, 156

Tlacoltapam, 135

Tlahualila Lagoon, 45

Tlalpam, 123

Tlaluepantla Mountain, 34

Tlamecas, 34

Tlatelolco, 61, 64, 118

Tlaxcala, 27, 61, 126
State, 126

Tlaxcaltecs, 61, 64

Toacas, 261

Todos Santos, 93, 95

Tola, 281

Toledo, 200

Tolica Mountain, 27

Toliman, 116

Tollan, 62

Toltecs, 62, 220

Toluca, 21, 41, 117
Mountain, 34

Tonala, 161
River, 146, 249

Tongue of Ocean, 442

Tonila (Ococingo), 103

Torbeck, 414

Tortola Island, 436

Tortuga Island, 6, 405

Totolotlan, 111

Totonacs, 62, 88

Totonicapam, 214, 227

Trelawney, 393

Tres Marias Islands, 23, 43, 58

Tres Virgenes Mount .ins, 22

Trinidad, 347, 374
Island, 455

Triunfo, 265

Trois-Riviéres, 410

Trou-Bonbon, 413

Truxillo, 261, 265

Tucuru, 236

Tula River, 37, 46
Town, 104, 117, 281
(Tamaulipas), 104

Tulancingo, 117

Tule, 322

Tulum, 168

Tunas, Las, 377

INDEX.

Tupisa River, 334
Turganti Mountain, 314
Turialba Volcano, 296
Turks Islands, 442, 448
Turnefte Island, 196
Tuxpam River, 41
Tuxpan, 130, 180
Tuxtla, 162; Volcano, 30, 40
Tuyra River, 314, 316
Tzendals, 155, 218
Tzintzontzan, 115
Tzotzil, 155, 223
Tzutujils, 222

Ujum Mountain, 299
Ulua River, 258
Uluas, 283
Union, 253
River and Department, 253
Union-Juarez, 161
Uraba Gulf, 314, 317
Ures, 95
Uruapan, 115
Usulutan Volcano, 248
Usumacinta River, 146, 147
Utatlan, 227
Utila Island, 259
Utuado, 426
Uxmal, 158, 167

Vacas, Las, 231

Valenciana, 110

Valladolid (Morelia), 115
(Yucatan), 168

Valle Santiago, 111

Valles, 174

Vauclin Mountain, 476

Venado Island, 98

Ventanillas Voleano, 272

Vento River, 258

Ventosa, La, 40

Venturon Mountain, 274

Vera Cruz, 40, 130; State, 129

Veragua, 13, 205, 312

Vera Paz, 218

Verrettes, 412

Veta Grande Mine, 32

Via River, 419

Viceita, 305

Victoria Peak, 193

Vieja Providencia Island, 277

Viejo Voleano, 274

Vieques Island, 423, 428

Viga Canal, 121, 124

Villa Hermosa, 162
Juarez, 140; Nueva, 107

Virgin Islands, 430, 436
Gorda, 436

Virtud, 265

Vuelta de Abajo and Arriba, 358

Wanks River, 277
Watling Island, 446

END OF VOL. II

Windward Islands, 455
Channel, 338, 447

Xaltocan Lake, 45
Xaragua, 402
Xeres, 266
Xicacs, 261
Xicalanes, 62
Xinantecatl Volcano, 27
Xiximes, 84
Xochicalco, 135
Xochimilco, 45

River and Lake, 4
Xolotlan Lake, 278
Xubabal, 228

Yanks River, 277

Yaqui Tribe, 81, 94
River, 43, 96
Great, 400
Chico, 397, 401
Peaks, 400

Yasica River, 421

Yauco, 428

Yautepec, 135, 136

Yavisa, 335

Yeluca Mountains, 272

Yocoa Lake, 258

Yolaina Mountains, 272

Yoro River, 276

Yucatan, 142
Channel, 354

Yucayza Islands, 444

Yucayos, 373

Yuma, 14

Yumas, 81

Yumuri River, 373

Yuna River, 398, 401

Yunque (Cuba), 358
(Puerto Rico), 423

Yuscaran, 266

Zacapa, 234
Zacatecas, 106
Zacatlan, 126
Zacatula, 77, 137
Zacotecs, 86
Zakuleu, 228
Zampaol-tepetl, 35
Zapata, 359
Zapatera Island, 283, 286
Volcano, 274
Zapotecs, 62, 88, 89
Zapotlanejo, 111
Zayi, 160, 168
Zempoala, 40, 131
Zimapan, 116
Zitacuaro, 115
Zoqués, 88, 141
Zulia River, 343
Zumas, 283
Zumpango, 45
Lake, 45
Zuni, 17
Zunil Volcano, 208

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