SMITHSONIAN INSTITUTION LIBRARY
INSTITUTE OF SOCIAL ANTHROPOLOGY
PUBLICATION NO. 7
CULTURAL GEOGRAPHY OF THE
MODERN TARASCAN AREA
by
ROBERT C. WEST
SMITHSONIAN INSTITUTION
INSTITUTE OF SOCIAL ANTHROPOLOGY
PUBLICATION NO.7 ~
CULTURAL GEOGRAPHY OF THE
MODERN TARASCAN AREA
by
ROBERT C. WEST
Prepared in Cooperation with the United States Department of
State as a Project of the Interdepartmental Committee
on Scientific and Cultural Cooperation
One of a series of monographs describing the results of the joint field investi-
gations of the Institute of Social Anthropology and the Escuela Nacional de
Antropologia of Mexico in the Tarascan area of Michoacan, Mexico, 1945-46
—.—————————————————————————————
UNITED STATES GOVERNMENT PRINTING OFFICE e WASHINGTON :1948
For sale by the Superintendent of Documents, U.S. Government Printing Office, Washington 25,D.C. - - - ---+-+-++-+ee28 6 Price 75 cents
LETTER OF TRANSMITTAL
SMITHSONIAN INSTITUTION,
InstiTuTE oF SoctaL ANTHROPOLOGY,
Washington 25, D. C., June 13, 1947.
Srr: [Ihave the bonor to transmit herewith a manuscript entitled “Cultural
Geography of the Modern Tarascan Area,’’? by Robert C. West, and to recom-
mend that it be published as Publication Number 7 of the Institute of Social
Anthropology.
Very respectfully yours,
Grorce M. Foster, Director
Dr. ALEXANDER WETMORE,
Secretary of the Smithsonian Institution.
Preface. __-_-
Iphoneticmotes.—2 oe =) eee
CONTENTS
Thesmodern Tarascan. areas -=._---.---2--=-===-
Tarascan population—____
The physiographic areas____-__ ~~~
Climateiand vegetation--—~—.=-- _-- --=-.—_ =
The recession of mative: evan
Modern linguistic distributions______-
Tarascan settlements _----___-- ee oe eae
IEOUSeHUYIDCS= = 22 = eee eo ea een
The land system and the pueblosos2 22 sse225-
Tarascanveconomy====-~ == 2222522252822 22 - ee
QaQOorwnre
SHO AOANOARWN
Agricultural systems and associated crop types-
Field agriculture and associated crops___-
Monbiculnlte saan = aes ee eee
PAGE
Vv
VI
Tarascan economy—Continued
Bibliography----__--
Stock raising and animal products___-__-___--
Food- patie ae ecuvitles en ee Sigs
Fishing... Be Re ee ee ee
umbering activities: =_- =. 229) 225) sae
andicraftis=--=- So - 2
@Weramics=. 2. 225 2k oe ee
chextiles= 22 a5 == ee ee AS Soe ees
Wooderafts=—-2---.53
Lacquer work _______-
Leathercraft______ 2
Metalcraft ___-
Stonecutting_____
Trade and transport __
ILLUSTRATIONS
PLATES
(All plates at end of book)
. Physical landscape.
. Water supply and settlement.
House types.
House types.
. Maize culture.
Wheat culture.
. Horticulture and domestic animals.
. Fishing and forest exploitation.
. Ceramics.
. Ceramics.
Pottery making at Cocucho.
Pottery making at Cocucho (con-
tinued).
. Textiles.
. Textiles.
. Woodwork.
. Markets and transport.
FIGURES
. Decline of Tarasean population, 1500—1940____
. Growth of population in the Sierra, 1750-1940_
aelarascan planting tO0lss=s==-—5— eer a= ase =
. The T‘apdératdirakua irrigation device__-____--_
ae Lhedishyspearseandfisqa_ =. see = 2-2 se
Srbhegwheellathesea=s a= ee eee eS SS
PAGE
22
23
37
48
52
68
. Distribution of
MAPS
. Topographic map of the modern Tarascan area_
. Geognostic map of the modern Tarascan area__
. Length of frost season in northwest Michoacdn_
Climati¢e map of Michoac4n=_.--_--------=.-
Vegetation types in the modern Tarascan area
Soil types in the modern Tarascan area_______
. Pre-Conquest and modern boundaries of Taras-
Can speecht. == ==. eee {8
. Area of Tarascan speech, ca. 1750________----
. Area of Tarascan speech, ca. 1800____--------
. Area of Tarascan speech, ca. 1850__- ~~ --- oaEe
, Area.of Tarascan’ speech, 1940._> -=2=-2222==
. Distribution of Tarascan speech by settlements,
. Distribution of monolinguals in the Tarascan
area 19408250252 so: 3 ee
. Distribution of La Cafiada settlements, 1580
and. 19462222. 3232-2 222 eee
ePlanvof Uringuitiro,, 194622 = — 3: See
. Plan of Ahuiran,
=ePlan of irindaro, 04 G2e= see =e ee
. Distribution of house types in the Tarasecan
194625. 22. S22 eeee ee e
ares sl 78oandel94Gr cee e. = ee eee
handicrafts in the modern
Tarascan area
. Distribution of markets and their local trading
territory in the modern Tarascan area------
1m
PREFACE
The present study was done under the auspices
of the Institute of Social Anthropology, Smith-
sonian Institution, Washington, D. C., and in
cooperation with the Escuela Nacional de Antro-
pologia, Mexico, D. F. The study proposes to
serve as a background for the various detailed
pueblo monographs executed in the Tarascan
area by other members of the Institute.
Being a report on the cultural geography of a
region, the present paper is chiefly descriptive,
although a developmental treatment has been
employed wherever the scanty historical materials
would permit. Physical background is only
briefly considered; emphasis is on material culture,
particularly modern Tarascan economy: agricul-
ture, handicrafts, and trade. In addition, an
attempt is made to describe the areal recession
of Tarascan speech since Spanish contact.
Field work was done in April, May, and June
of 1946. With the exception of Cherandtzicurin,
all Tarascan towns were visited. Many neigh-
boring mestizo pueblos (formerly Tarascan) were
inspected to obtain comparative data. Approxi-
mately two-thirds of the field season was spent
in the Sierra. Archival research was done in the
Archivo del Arzobispado de Michoac&n, Morelia,
the Archivo General de la Nacién, Mexico, D. F.,
and the Museo Nacional de Antropologia, Mexico,
D. F.
I am especially indebted to Sr. Pablo Valasquez
G., a native Tarascan and anthropology student,
who accompanied me in the field. His intimate
knowledge of the Tarascan Sierra, its language,
and many of its customs was an invaluable aid,
not only in the field, but also while the report
was in preparation. Velasquez read a large part
of the manuscript and corrected the use and spell-
ing of all Tarascan words employed in the text.
Rosert C. West.
Mexico, D. F.
March 1947.
PHONETIC NOTE
The phonetic symbols used conform to the Tarascan alphabet approved by the Congreso
de Filélogos y Lingitistas of México in 1939 and employed by the Tarascan Project of the
Departamento de Asuntos Indigenas. The alphabet is based on standard Spanish usage
insofar as possible, with additional symbols added for Tarascan and with some clarification
of the Spanish symbols as indicated below.
The vowels a, e, 7, 0, u have Spanish values. The vowel a is intermediate between Spanish
t and u.
The consonants b, d, f, g,j, k,l, m, n, p, 7, s, and t have regular Spanish values. In addition
the following symbols are used:
is the equivalent of English or Spanish ts.
is the equivalent of English ch.
is used for the sound of English vg in “‘sing.”’
is the equivalent of French j.
is intermediate between Spanish l and r.
is the equivalent of Spanish rr.
is the equivalent of English sh.
is the equivalent of English z.
‘ &, k‘, p‘, and ¢‘ are aspirated forms of the consonants given above.
Mm & HS BR Org OD
_
—,
e tava
eae al got
ae Wing =
vd
Willa Jiménez
rajomonsaie 3
Be
‘ H 0
' dae }
f ‘ £ Tanganofcuoro /
re 1) a % ©.DEEA ALBER
a eel \v \ a
“La Wontera L-- Ko
a : 7
S-—s8000—
>
yi -
ase,
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aad £3 a a
ae San José em
j
at) '
fa MS °
~ a Los Ganoas
IONACIO.
‘OR
Tipidio Gres
Sec ae | — y
sree soles mie, ) 2
i via
3 S
if Wieden hgaw
a
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pTifguindin }
| we f uv Ss ‘y >
bat Santo nr Fr Gu j
0,
Tocumbo
!
Hi
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~cherén
ee ant ne ‘| (one axAWpana
Zipcitos | 2 t
7 .
bZsonBenito 1 Aeiees
{Rancho Nuevo, i Peicciehs
f CELA ALBERGA ‘ & %
ra jes ‘ / \ ce 4 =
wy ‘ so me Tee Ahuiron s/f . ( sa
Sicvichoy | M4 co ‘ Boon ; Fi at
| vase Bhardan, - om , s Me Nahuatzen va M5660
Chefatog seRANJUATA oy 4 sabe «) “ 4 o> 1)
2, 4 eed ~ . J gXxuian
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a
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CDE LA VARA oo ii Pomacuordn fr j
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~ rongérfeuard
ve Sli IF ae buSrey
A Neen, ek”
pio Siago°
“VS UATRER! H
‘ ) ‘s~, NG:DESGHIVOIE aroeutin
“Pog uare!
Nocutzepoo,
ed toa ee \
Capacuaro/ AS me
1 lit, Lat (yes whta's. 900 y
( ELA ¢ RONA) Y, we EL REY VALIENTE! SS Ne
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TARASCAN PUEBLO
MESTIZO PUEBLO
TARASGAN RANCHO
MESTIZO RANCHO
sm ALL-WEATHER HIGHWAY
—— ORY SEASON AUTO ROAD
owm= TRAIL
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Contour interval 1000 feet
748988 O - 48 (Face p, 1)
Map 1.—Topographie map of the modern Tarascan area.
6
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101° 30°
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BARRA
101°30°
Cultural Geography of the Modern Tarascan Area
By Rosert C. West
THE MODERN TARASCAN AREA
The present territory of Tarascan speech con-
sists of a relatively small area (about 3,500 sq.
km.) in northwestern Michoacan. Approximately,
the modern area extends eastward from the
Zamora-Los Reyes railroad to the east shore of
Lake PAtzcuaro, and southward from the M éxico-
Guadalajara highway to a line drawn between
Patzcuaro and the peak of Tancitaro (map 1).!
A few small islands of Tarascan-speaking folk
exist south of the main area. Within the present
area nearly 55,000 individuals of indigenous speech
live in 66 Tarascan pueblos and 50 ranchos.
Four geographical regions comprise the modern
Tarascan area. (1) The Sierra (called by the
Tarascans Sierra or Siéris) is the largest of the
regions, the main portion of which extends west-
ward from Lake Patzcuaro to slightly east of the
Zamora-Los Reyes railroad.“ The northern
! Map 1 is based on an enlarged portion of sheet 643A (Uruapan) of the
AAF Preliminary Base, 1:500,000. This sheet was compiled by the U. 8S.
Aeronautical Chart Service in January 1945 from AAF trimetrogon photog-
raphy taken in December 1942. Positions and names of topographic fea-
tures which appear on the accompanying map were checked on the ground
during the spring of 1946. Some errors were encountered on the original
map: misnamed localities (e. g. Ajuno), small errors in routes of highways
and railroads, mistakes in elevations. Drainage was found to be fairly
correct. Onmap1only the more important trails are indicated. Numbered
localities refer to the following ranchos:
1. Guarachanillo. 14. San Maros Aracht- 27. Patambicho.
2. Aranza. cuta. 28. Ojo de Agua.
3. Las Trojes. 15. Huancho. 29. Ichupio.
4. Las Cafias. 16. Las Cocinas. 30. Tarerio.
5. El Venado. 17. San Nicolas. 31. Ucasandstacua.
6. Tapan. 18. La Alberca. 32. La Vinata.
7. Tierras Blancas. 19. La Atascada. 33. Las Granadas.
8. La Mesa. 20. El Rosario. 34. Yunuén.
chars 21. El Tepemal.
9. La Tinaja. 22. Tepetate 35. Tecuena.
10. Queréndaro. 23. Tejamanil. 36. Urandén Morales.
11. Zarzamora. 24. Pacdpatiro. 37. Urandén Morelos.
12. San Luis Sorena. 25. Chupicuaro. 38. Urandén Carian.
13. La Jolla. 26. Oponguio, 39. E] Padre.
The following Tarascan ranchos (listed in the official 1940 census) are not
located: Tzintzicha (municipio of Chilchota); Agua Escondida (municipio
of Tangancicuaro); Las Encinillas and Los Laureles (municipio of Tanga-
mandapio); La Providencia and El] Tropezén (municipio of Los Reyes); El
‘Tejocote (municipio of Paracho); Revolucion (municipio of Erongaricuaro);
and Itziparamucu (municipio of Tzintzuntzan).
1a On modern maps the high area west of Lake Patzcuaro is termed “‘Sierra
de los Tarascos.’’ In colonial documents the area was usually called ‘‘Sierra
de Michoacan.”’
boundary approximates the México-Guadalajara
highway, while the steep escarpment that plunges
into the Balsas-Tepalcatepec Basin marks its
southern limit. An eastward extension lies south
and southeast of the lake and joins with the Sierra
de Ozumatlan in eastern Michoacan. Containing
60 percent of the present indigenous group, the
Sierra west of the lake is the modern center of the
Tarascans. (2) The Lake Patzcuaro (Japinda.zu,
Inéimecuatu) area contains 19 percent of the
Tarascan population distributed in 13 pueblos and
13 ranchos along the lake shore and on the islands.
Formerly one of the political centers of the
Tarascan Empire, the lake region, in terms of
indigenous speech, has declined rapidly since late
colonial times. The speech of the entire south
shore and the towns of Quiroga, Tzintzuntzan, and
Erongaricuaro is predominantly Spanish. North
and northeast of the Sierra lie two small areas of
indigenous speech, which appear to be remnants
of the once large northern Tarascan zone. One of
these is (3) La Canada (EréSeman), a small narrow
valley located at the northern edge of the Sierra.
This valley was the region of the ‘‘onze pueblos” of
colonial days. Today nine towns with 9 percent
of the total Tarascan population are clustered
along a strip of alluvium within the valley. (4)
The other remnant of the northern zone lies north
and northwest of Lake Patzcuaro and contains
seven pueblos and 9.5 percent of the total number
of Tarascan-speaking folk.2 Other regions of
Tarascan speech consist of “islands” south of the
main area. Cuanajo, located southwest of Mo-
relia in the western extension of the Sierra, is the
Jast fragment of the former indigenous area south-
east of Lake Patzcuaro. San Angel Zurumucapio
and the newly formed towns (Caltzontzin and
Villa Silva) harboring refugees from the stricken
2 These pueblos include Tirindaro, Tarejero, and Naranja on the shore of
former Zacapu marsh; Azajo and Comanja on the northeastern edge of the
Sierra; Teremendo and Zipiajo at the northern foot of Cerro el Zirate.
ry
2 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
zone around Paricutin Volcano, are the remaining
predominantly Tarascan settlements in the tierra
templada, the upper part of the plateau escarp-
ment (2 percent of Tarascan population in 1940).
Formerly an important part of the Tarascan
Empire, the hot lands of the Tepalcatepec and
Balsas Basins (tierra caliente, Jusio) have lost
completely the last vestige of spoken Tarascan.
A small number of Tarascan-speaking folk live
in some of the larger mestizo towns adjacent to
the main Tarascan area: Uruapan, Patzcuaro,
Coeneo, Zacapu, Zamora. With the possible
exception of a few old households in Uruapan, the
presence of aboriginal speech in the large mestizo
settlements probably represents a recent influx
from rural areas (a desire for urban life, migration
from the voleano-devastated areas) rather than
linguistic remnants.
THE PHYSIOGRAPHIC AREAS
The Sierra.—The Tarascan “Sierra” is not a
mountain chain; it is rather a volcanic plateau,
whose average elevation is some 1,500 feet higher
than that of the surrounding areas and whose
surface has been roughened by large composite
volcanoes, scores of small cinder cones, and ex-
tensive lava flows (malpais). Lying within Mex-
ico’s transcontinental volcanic axis, the Sierra is
the locale of the country’s newest active volcano,
Paricutin.’ Within the central part of the area
elevations range from 6,900 feet to over 12,660
feet (Cerro de Tancitaro). The altitude of the
plateau increases from west to east. Elevations
of towns in the western half of the Sierra range
from 5,180 feet (Atapan) to 7,800 feet (Pamaté-
cuaro);in the eastern half, from 8,040 feet (Sevina)
to 8,460 feet (Cumachuén), the highest pueblo in
the Sierra west of Lake PAtzcuaro. Even higher
settlements (e. g. the rancho of Cruz Gorda,
8,987 feet) exist southeast of the lake, and the
highest point in Michoacan, the Cerro de San
Andrés (12,840 feet), lies in the Sierra de Ozu-
matlin, 62 km. east of Morelia.
Tertiary and Quaternary vulcanism has pro-
duced the major land forms in the Sierra (map 2).
In age the volcanic forms range from probably
Eocene to the present time. The oldest are mas-
sive composite volcanoes, the highest and most
8 The chief scientific references on the Paricutin Voleano include Ordéiiez
(1945), Robles Ramos (1943), Pérez Pefia (1946), Mexico City Universidad
Nacional Instituto de Geologia (1945).
prominent landmarks in the area: Cerro de
Tancitaro (12,660 feet), Cerro de Patamban
(12,300 feet), Cerro de Quinseo (10,800 feet),
Cerro el Zirate (10,955 feet). The flanks of these
mountains are composed mainly of andesite with
some pinkish rhyolite near the summits; small
veins of mineral-bearing quartz sometimes occur
within the andesite. Conical shape and radial
drainage characterize these voleanoes, but most
craters have been destroyed by erosion. Fre-
quently erosion of soft consolidated ash situated
between andesite flows has formed caves, which
have acquired importance in Tarascan folklore.
Cinder cones and lava flows, Pleistocene to
Recent in age, represent the younger forms in the
Sierra. The entire area is dotted with cones, 250
to 700 feet high, with no apparent alinement.
Most are composed of semiconsolidated ash,
cinder, and large blocks of explosion remnants.
Two types of cones occur: (1) the symmetrical
cone with a well-developed, flat-floored crater,
and (2) the breached cone, with one side partially
destroyed, initially by explosion or lava flow and
subsequently by erosion. Some cones are ribbed
by radial drainage; others carry scars of surface
slips; owing to porous surface materials, a few
show little effects of erosion, in spite of high
(35°-45°) angle slopes.
Basaltic lava flows, originating usually from
Pleistocene or Recent fissures in the sides of old
volcanoes or occasionally from large cinder cones,
have descended slopes in narrow corridors and
have fanned out in wide expanses on gentle
eradients. Fantastically rough surfaces charac-
terize the flows, which form the Sierra’s badlands—
agriculturally unproductive and barriers to horse
and wheeled traffic. Comparative age of the
flows can be roughly determined by the degree
of rock decomposition and character of vegetation
cover. In some flows, such as that south of
Pomacuaran, depressions and crevasses are par-
tially filled with alluvium; large areas are covered
with a thin soil mantle; sizable pines and oaks
cover most of the flow. These features evidence
a long period of exposure. In contrast, the
rough, blackened, almost treeless malpais north-
west of Zacapu at the Sierra’s northern edge,
appears to be a much younger flow.
Volcanic activity in the Sierra has possibly been
continuous from Eocene to the present day.
Jorullo (1759) and Parfcutin (1943) represent
102°30
Map 2.—Geognostic 1
(malpais). (4) Le
of stream alluviu
oe en ae
rn ar
a
102° 30°
id
oa
he Torecuato
wake
Patambon
Pomatdcuaroo | fo Cocucho ot
Urapicho, A
e
Ms ¢ <= oAhuiran
Sicuichog | =®
° Choropaneee @
eo?
ae
ee
s
oAngahua
“hee e
e
©Zirosto
e e
°
Peribon : A
o e A
De
, Oo
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eg
Q oO
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mroageifeaera see »
°
PGtzcuaro \
go GD)
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aot
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101" 30°
(2) Recent cinder cones.
Data from aerial photographs and field notes.
(3) Recent lava flows
(5) Large flattish-floored basins
7148988 O - 48 (face p. 2)
CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST 33
historical examples of vulcanism within or ad-
jacent to the area. However, vulcanism associ-
ated with human ancient settlement in the area,
is unquestionably evidenced by the occurrence of
charred maize ears embedded in a basaltic lava
flow 18 km. northwest of Morelia.*
Aside from land forms resulting directly from
vulcanism, others caused by depositional processes
occur within the Sierra. Between the old com-
posite volcanoes and young cinder cones flattish
surfaces have been formed first by ash and cinder
fall and later by aeolian and alluvial deposition
from surrounding slopes. Such surfaces, which
compose only a small percentage of total land
area, are the agriculturally important sections of
the Sierra. Some form saddles or cols between
adjacent hills; the larger plains form basins of
interior drainage. The largest basins are Llano
Grande, southeast of Charapan; the Plan de
Nurio; that of Paracho, Aranza, and Cheran; the
plain of Nahuatzen; of Sevina; of Paracho; ete.
(map 2; pl. 1). Minor forms include dissected
aprons of alluvium and semiconsolidated ash at
the base of volcanoes and steep-sided arroyos
eroded into alluvium in the upper parts of the
basin plains.
One of the most characteristic physical features
of the Sierra is the paucity of perennial streams
and lakes. Although this is an area of moderate
summer precipitation, the porous volcanic surface
quickly absorbs most of the available moisture.
A few permanent, spring-fed streams occur on
the northern and western flanks of Cerro de
Patamban and on the western and southern sides
of Cerro de Tancitaro. Small springs occur on
the flanks of the old composite volcanoes, whose
porous rocks form a reservoir of rain water. Such
springs afford the sole water supply for many
Sierra villages. Only on the edges of the Sierra
plateau, at the contact of porous and impervious
rock layers, do large springs occur.
The Lake area.—At the eastern edge of the
Sierra exists a depression filled by Lake P&tzcuaro.
Sierran geomorphology (young and old volcanic
forms) almost surrounds the lake, but predomi-
nates on its northern, western, and southern shores.
Twelve kilometers south of Pétzcuaro small Lake
Zirahuén, within the eastern prong of the Sierra,
appears to have been formed by a lava-blocked
4 An excellent specimen of charred maize so embedded is in the Museo
Regional Michoacano, Morelia,
stream.’ Both lakes present similar shore fea-
tures—moderately steep banks alternating with
wide, flattish delta fans.
In other respects the two lakes are distinct.
Patzcuaro is shallow (deepest point in the southern
arm, 20 feet; in the northern part, 50 feet, in
1941); Zirahuén is relatively deep (148 feet, maxi-
mum sounding). Moreover, while the level of
Zirahuén (6,953 feet in 1942) is relatively stable,
that of Patzcuaro (6,671 feet in 1942) has fluctu-
ated frequently in historical times. Since 1939
the lake level has descended nearly 4 feet, exposing
large areas of mud flats along the shore and re-
vealing one new island (Pastora) near the south-
west corner of the lake (pl. 1). In some places
the descending waters have uncovered old tree
stumps, indicating that formerly the lake level
was even lower than at present. On the other
hand, the western portion of the large lacustrine
plain of Chapultepec in historical times formed
an eastward extension of the lake’s southeast arm,
denoting a former level higher than the present
one.® The cause of flucuation in level is not clear.
De Buen (1944), judging from meteorological data
(1939-43), has suggested a correlation between
rainfall and evaporation variation on the one
hand and lake surface fluctuation on the other.
The excessive evaporation and low rainfall during
those years likely affected lake volume, but normal
precipitation and evaporation in following years
have not halted the gradual decrease in lake level.
Moreover, if fluctuation is caused by meteorolog-
ical elements, one would expect neighboring lakes
to be similarly affected. Periodic clearing and
clogging of sublacustrine crevices, often associated
with lakes of volcanic origin, is another popular
hypothesis applied to Lake Patzcuaro.
The lake contains 10 islets on which live some
of the most conservative of the Tarascan people—
the fishermen. The four islands off the Taafu-k*éri
Peninsula (Pacanda, Yunuén, Tecuena, and
Janitzio) are old volcanic hilltops with steep banks
and, with the exception of flat-topped Pacanda,
with little land suitable for cultivation. In the
5 De Buen (1944) assigns the origin of all present and former lakes in the
western Portion of the Mesa Central to disruption of normal drainage by
vuleanism. He also suggests that Lakes Patzcuaro, Zirahuén, Cuitzeo, and
Yuriria were formed from portions of Rio Lerma drainage, since the fish
Chirostoma, abundant in Lake Chapala and the Lerma, is found also in these
lakes, the number of species decreasing from Chapala (10) to Zirahuén (2).
6 The 16th-century map of Lake PAtzcuaro which accompanies the Relacién
de Michoacan (1903) clearly shows the former extent of the southeastern arm.
At the time of the Conquest this section included the island of Aputato, now
a hill some 300 m, from the water's edge.
4 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
shallow southern part of the lake lie JarAcuaro,
the largest of the group, and the newly formed
Pastora. (The former island of Copujo is now
attached to the mainland.) Both islands are low,
composed of semiconsolidated alluvial materials.
Along the southern shore only low marsh now
separates the Urandén islets (low voleanic hills)
from the mainland (pl. 1).
The southern escarpment.—Although geologi-
cally similar to the Sierra, the abrupt southern
escarpment, which forms part of the Mesa
Central’s southern wall, constitutes a distinct
physiographic area. Pleistocene and Recent
vulcanism continues from the Sierra to the Balsas
and Tepalcatepec Rivers, Jorullo having been the
most recent volcanic activity on the escarpment.
The canyons formed by deeply entrenched spring-
fed streams are the escarpment’s salient features.
Some barrancas exceed 500 feet in depth. The
upper tributaries of the escarpment streams are
eroding headwardly into the Sierra, capturing
enclosed basins and intermittent water courses.’
Above the barranca area shallow basins occur in
the upper portion of the escarpment. Probably
of volcanic origin, these flattish-floored valleys are
now tapped by escarpment streams. Typical
examples are the plains surrounding Uruapan,
those below Periban and Los Reyes, the valleys
of Tingambato and Tacambaro, all important
sites of former Tarascan settlement in the tierra
templada.
The northern plateau area.—The former Taras-
can area north of the Sierra forms part of the
interior plateau county of Central Mexico. For
the most part physiography is characterized by
old volcanic hills and mountains separated by
flat to rolling plains country. The part of this
region formerly inhabited by Tarascans extends
from Lake Chapala east to the Sierra de Ozumatlan
and from the Sierra north to the Lerma River.
(The low areas near the river and its tributaries
are often termed the ‘Bajio.”’) A narrow belt
of the hill and plains landscape also extends south
from Lake Chapala to include the Cotija-Tin-
giiindin area along the western side of the Sierra.
Average elevations in the interior plateau decrease
from 7,200 feet along the flanks of the Sierra de
Ozumatlin to 5,000 feet at Lake Chapala. The
7 For example, this phenomenon has occurred at the southwestern edge
of the Sierra, where a tributary of the Tepaleatepee has apparently captured
the drainage of the structural basin which runs east-west from Parangaricu-
tiro to Periban.
higher hills and mountains rise 2,600 to 4,000
feet above the surrounding plains.
The young volcanic land forms found in the
Sierra are lacking in much of the northern area,
where the principal elevations consist of eroded
composite Tertiary voleanoes. A few tongues of
Recent lava flow from the Sierra into the northern
edge of the plains, and cinder cones extend north-
ward from El Zirate. Many lakes, some cecupy-
ing structural basins, dot the northern area. The
extensive sections of old alluvium, which form a
good part of the plains, probably represent beds
of Pleistocene lakes. At the northern and north-
western base of the Sierra many spriag-fed lakes
and marshes existed in historical times, e. g.,
Ciénaga de Zacapu, de Tangancicuaro, de Chapala,
ete. The lacustrine basins and the borders of
the former lakes and marshes were the major
areas of Spanish settlement in the Tarascan North,
for both afforded year-round pasture and _ sites
for irrigated wheat farms. Some marshy sections
still exist, but natural desiccation and artifical
drainage have converted much of the wet area
to dry farmland. The once extensive chain of
lakes in the Cotija graben, west of the Sierra, has
almost completely disappeared, and the marshes
of Zacapu, around which are grouped a few rem-
nant Tarascan pueblos, have been converted into
a large farming area.
A unique physiographic subarea of the northern
zone, called “La Canada,” a narrow east-west
depression at the northern base of the Sierra, is
still one of the significant Tarascan regions. The
valley floor, 10 km. long and 2 km. wide, decreases
rapidly in altitude from 6,360 feet at its eastern
end to 5,840 feet at Chilchota, near the western
extremity (pl. 1). The western end of the valley
is marked by an ancient lava flow, which once
partially blocked normal drainage. Subsequent
deposition of alluvium (possibly lacustrine) behind
the lava dam has resulted in the present wide
flattish floor of the valley’s western half. Today
the stream draining the valley flows subsequently
through a deep gorge cut through the northern
end of the lava flow. The numerous intermittent
streams which descend from the adjacent hills
have built up small alluvial fans along the valley
sides. Like other areas at the edge of the Sierra,
La Canada is favored by numerous large springs
issuing from fissures at the southern and eastern
borders of the depression. Alluvium and water
rn
CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST oO
have attracted human settlement to the valley
since prehistoric times. Sierra Tarascans, who
‘all La Cafiada “ErdéSemen”’ (view from above),
probably visited the valley for chile and early
maize before the Spanish Conquest. Spaniards
immediately seized the well-watered plains near
Chilchota for wheat fields. Today La Cafiada is
a garden spot of orchards and wheat fields amid
recky volcanic hills.
CLIMATE AND VEGETATION
Meteorological data.—In dealing with meteor-
ology, northwestern Michoacan will be treated as
a whole; attempts will be made to point out
regional differences in temperature and rainfall.
Meteorological stations in the area are few; data
are entirely lacking for the Sierra. Consequently,
only general statements can be made concerning
the weather and climate of modern Tarasca.
102°30.
Zamora
60
/ F
©o Chilchotans
[e} °
al
eharapane
\
S\/
-u OD
S072.
o
Tarecuato
fe}
2
Zirosto
CDE TANCITARO
102°30'
Map 3.—Length of frost season in northwest Michoacsn.
Annual temperature ranges throughout the area
are small.§ Lowest winter temperatures occur in
the Sierra, the Tarascan tierra fria, where noctur-
nal freezing and frosts are common from November
to March ® (map 3). Winter temperatures in the
northern plateau and Lake P&tzcuaro areas are
somewhat milder then those of the Sierra (January
avereges: Zamora, 16.2° C.; Zinapecuaro, 15.9°;
Paétzcuaro, 13.9°), and the number of days with
frost is smaller. winters of the upper
escarpment (tierra templada) are frost-free (Jan-
uary average for Uruapan, 16.0° C.).
The
Summer
§ Data from seven stations in the area give annual temperature ranges from
3.9° C. (Hacienda Tequecsran, 10 km. south of Uruapan) to 7.7° C.
(Zacapu). The meteorological data given in text are taken from Atlas
climatolocvieo de México (Mexico, Servicio meteorlogico mexicano, 1939).
® The mining town of Tlalpujahua (elev. 8,500 feet), on the eastern border
of Michoacan, 140 km. east of PAtzeuaro, may afford temperature data
similar to that of the Sierra. December and January are the coldest months,
with average monthly temperatures of 11.8° and 11.5°, respectively. Maxi-
mum temperatures occur in April and May (15.0° and 15.9° C.). whieh are
probably somewhat lower than those occurring in the Sierra.
101°30'
Coeneo
oO
°
5150
2p o Quiroga
°
Sonto Juana
°
Tacdmboro
101°30'
Isopleths indicate the average length of annual period in
days, in which frosts oecur. . Data are mainly from reckonings by local inhabitants.
6 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
temperatures are high over the entire Tarascan
area, but less so in the higher Sierra. The
warmest months are April and May, the period
immediately before the rainy summer (May
average temperatures: Zacapu, 19.1° C.; Uruapan,
22.4°; Zamora, 23.2°; Cuitzeo, 23.2°; Pdtzcuaro,
19.9°).
Precipitation in the area, as in most parts of
Mexico, is seasonal, 80 percent of the annual
total falling mainly as convectional thunder-
showers in June, July, August, and September.
In the Sierra the summer rains often continue as
drizzles for a period of 3 to 4 days, suggesting
local cyclonic origin. Occasionally during the
months of December and January light winter
rains, called cabafiuelas, or janingerkua, occur.
These rains prevail over most of western Mexico
when cyclonic disturbances over the Pacific reach
inland, a condition which occurs every 3 or 4
years.'° Such precipitation often falls as snow
on the higher volcanoes in the Sierra, such as
Tancitaro, Patamban, and Quinseo. Freak snow
storms have been recorded in historical times; in
September 1887 several inches of snow fell in the
vicinity of Charapan and San Felipe, caving roofs
and destroying the maize crop.!! Another curious
meteorological phenomenon of the Sierra is the
prevalence of radiation fog in the low basins from
late summer to early winter. Forming in the
early morning hours (after 1 a. m.), the fog evap-
orates by noon. Its presence lowers average
daily temperatures and prevents rapid evapora-
tion of surface moisture.”
Annual precipitation in the area north and east
of the Sierra averages from 750 to 850 mm. A
greater amount is recorded around Lake Patz-
cuaro (town of Patzcuaro, 1,109 mm.), and even
more probably falls in the Sierra, where no records
exist. The greatest precipitation in Tarasca is
recorded along the southern (windward) side of
the Sierra in the upper escarpment zone. (Aver-
age annual totals for Uruapan, 1,683 mm.; Ario
de Rosales, 1,225 mm.; Tacdimbaro, 1,240 mm.)
‘0 In northwestern Mexico, particularly in Sonora and the Sierra Madre
Occidental, the winter cyclonic storms are called equipatas. Although they
are part of the same frontal system, the eqguipatas occur more frequently
than the cabaviuelas since northwestern Mexico is nearer the North Pacifie
center of frontogenesis.
'' Lumholtz (1902, vol. 2, p. 365) states that water has been known to freeze
in Cherfn and Zacapu on June 10.
The Sierra fogs are often mentioned by colonial chroniclers. One,
describing the Charapan area in 1789: ‘ . . . continwalmente se ve el terreno
cuebierto de neblas, que evaporen y eralala humedad de latierra’’ (AGN Historia,
vol. 73, f. 219).
Climatic areas and associated vegetation.—
Sufficient statistical data are not available to
construct accurately a map showing climatic
types in the Tarascan area. Using (1) the avail-
able statistics from the few existing stations, (2)
vegetation boundaries taken from field observa-
tions and aerial photographs, and (3) elevations
from topographic maps compiled from aerial
photography, an attempt has been made to locate
climatic areas based on the Koéppen system
(map 4).
The Sierra.—The Cwb and Cwe climatic types
of Képpen"™ correspond to the tierra fria of the
Tarascans—the Sierra, its eastern extension (in-
cluding the Sierra de Ozumatlan), and the south-
eastern part of the northern plateau area. A
mixed oak-pine forest forms the dominant vegeta-
tion of the Sierra and its eastern extension, and
corresponds to the higher and colder phase of the
Cwhb climatic zone. (Cf. maps 4 and 5.) Pinus
leiophylla (pino chino) and P. michoacana var.
cornuta (pino lacio) are the principal pines
(p‘ukiri) of the Sierra (Martinez, 1945). (Pl. 1.)
The former species is the main turpentine pro-
ducer, while the latter, a straight, tall tree,
affords the best lumber. Minor species of pines
found in the Sierra include P. teocote, P. pseudos-
trobus, and in the upper escarpment zone, the
subtropical pine P. oocarpa. Even at high
altitudes the pines rarely form solid stands, but
are mixed with numerous species of oak, the latter
dominent at lower altitudes, the former at higher
elevations. Some 30 species of oak (urikua,
tuktis, Sariri), both deciduous and_ persistent,
occur in the Sierra and adjacent areas. Among
the more common are Quercus fulva, Q. acuminata,
Q. circinata, Q. laxa, Q. crassipes, and Q. pandurata
(Trelease, 1924). Often mixed with pine and
oak are madrofio (pandnksa; Arbutus sp.); various
laurels (Lauraceae); many hydrophytes in bar-
ranca bottoms, such as jaboncillo (saépu), palo
blanco (udrpit-uku; Alnus sp.), palo colorado
(éaraépit-uku).
On lower slopes one often sees the Mexican
“crab apple” (actually a hawthorne) or tejocote
(kaais; Crataegus mexicana) and the “cherry” or
capulin (Séngua; Prunus capuli), both of which
13 Mathematical values of Képpen symbols: C, temperature of coldest
month between —3° and 18° C.; w, dry winter, rainy summer; b, tempera-
ture of warmest month less than 22° C.; c, temperature of coldest month
above —38° C., and mean temperature of less than 4 months out of the year
is more than 10° C.
a
Y OF THE MODERN TARASCAN AREA—WEST
CULTURAL GEOGRAPH
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8 INSTITUTE OF SOCIAL ANTHROPOLOGY
are frequently semicultivated in hedgerows and in
house lots. Agave (akimba; A. latissima, A.
americana) is also a frequent hedge plant found
particularly on the outskirts of settlements, and
the tree yucca or izote (¢ambasa; Yucca australis),
although more common at lower altitudes, is often
seen In Sierra villages. Understory vegetation in
the oak-pine zone is sparse, possibly owing to the
annual burning of herbaceous plants in the forest
to improve summer forage. Some of the more
prominent understory plauts are zarzamora
(¢ttn; Rubus sp.), a wild blackberry especially
abundant along hedgerows, and wild grape vines
(Vitis sp.). Various epiphytes, such as orchids
of many species, are found on the trunks and
branches of pine and oak throughout the Sierra.
Although meteorological data are lacking, the
climate of elevations above 10,000 feet is possibly
Cwe, i. e., cold winters and cool summers (map 4).
Such elevations occur on the upper slopes cf the
higher volcanoes, where snow occasionally falls
and where fir (Abies religvosa) forms the ,dominant
vegetation. On slopes above 8,700 feet this tree
(pinabete, t*ktimbu) starts to appear among pine
and oak. At 10,000 feet solid stands of fir begin
and continue to the mountain peaks, where high
altitude pine (P. hartwegii) has gained a foothold in
eracks and crevices in rocky cliffs. Understory
vegetation in the fir forest coasists of various
herbaceous plants, including a bunchgrass cailed
zacate or j6éin (Muhlenbergia macroura). The
green shoots of j6¢in afford the principal forage for
sheep and goat herds which are grazed on the high
slopes of Cerro de Patamban and (before the
eruption of Paricutin) on Cerro de Tancitaro.
The type of original vegetation in the basin
plains within the Sierra is problematical. Prob-
ably cleared and cultivated for more than 300
years, these plains now show little evidence of
the original vegetation cover. The dark-colored
soil of the plains suggests the former presence of
a grass cover, possibly with scattered oaks and
pines.
The Lake district.-According to temperature
figures, the shores of Lake Patzcuaro fall within
the tierra fria climate (Cwb). Owing to higher
winter temperatures than those experienced in
the Sierra, and to absence of fog, the Lake district
enjoys a warm phase of Cwh (possibly transitional
between Cwb and Cwa). Oak and associated
broadleaf trees, such as madrono, jaboncillo, ete.,
PUBLICATION NO. 7
form the dominant plant complex of a belt 3 km.
wide around the lake. Moreover, colorfn
(pforén¢a; Hrythrina americana), casahuate
(Ipomoea murucoides), and zapote blanco (uriata;
Casimiroa edulis), all characteristic of the warmer
sections of the northern plateau, are common
hedge plants in the Lake area. Along the lake
shore, water-loving plants, including a willow
(tatimu; Salix bonplandiana), shrubs of ““tepozin”’
(Buddleia sp.), and clumps of bamboolike carrizo
(pfatamu; Arundo donar) are not uncommon;
while in marshy sections canebrakes (tule or
pa¢imu; Cyperus thrysiflorus) abound. Other
aguatic plants include various waterlilies and
hyacmths (Nymphaea sp.; ichhornia speciosa).
Possibly a mixed pine-oak forest once covered the
lower slopes bordering the lake, but, if so, the pines
have long since been destroyed for firewood and
lumber. Occasionally lone specimens of Pinus
leiophylla are found on the outskirts of lake
villages.
The northern plateau.—The Cwbh climate ex-
tends northward from the Sierra into the south-
eastern part of the northern plateau area. In the
middle and lower Rio Lerma Basin (Bajio) and in
La Canada, however, the Cwa climate of the
tierra templada occurs. In both Cwa and Cwhbh
areas of the northern plateau, oak and pine forests
occupy only the summits of the higher hills, below
which exist stands of oak and madrofo. The
lower slopes and plains carry an association of
grass and shrub, the latter consisting of casahuate,
zapote blanco, tejocote, palo blanco (Lysiloma
candida), granjeno (Celtis pallida), jara amarillo
(téksten; Senecio salignus), all typical of the more
humid portions of the central plateau. Xerophy-
tes, such as huisache (Acacia sp.), mesquite
(Prosopis juliflora), and various cacti (mainly
Opuntieae), are common. In the plains, fresnos
(padimu; Fraxinus sp.) form gallery forests along
streams, and in draws within the hills hydrophy-
tes, such as wild ahuacate and other laurels, pre-
dominate. Formerly extensive meadows existed
at the edge of swamps and lakes, particularly in
the lowlands east of Lake Chapala and the well-
watered plains near the northern edge of the
Sierra. In the northern plateau pine and oak
forests were formerly more extensive than at
present. Many of the hilltops north of the
present México-Guadalajara highway, which are
now barren cf arboreal vegetation, were once
DW mw me 4
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Ree FIR FOREST \
V////\ PINE-OAK FOREST (a large port cut over & cleared for cultivation) | “
0° | OAK & SCRUB OAK FOREST = /
eae SIERRA BASIN ASSO. (probable grass & open woods, now in plowland) ‘oO |
FORMER MARSH ASSO (areas now drained & converted to plowland) {i
GRASS-SCRUB ASSO. OF NORTHERN PLATEAU mG |
TROPICAL SCRUB OF SOUTHERN ESCARPMENT ° | ob0-¢ 55° MEL, fs /| |
9 [06 bol
102°30'
101° 30°
748988 O - 48 (Face p- 8)
i hs and field notes.
a) egetation types in the modern Tarascan area. Data from aerial photograp
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CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST 9
covered with pine and oak within the memory of
living inhabitants. Increased cultivation of slopes
and constant cutting for firewood and charcoal
will soon destroy the greater part of the pine-oak
remnants in the northern plateau.
The escarpment zone.—South of the Sierra lies
a series of climatic types arranged in altitudinal
sequence. The upper part of the escarpment
(5,600 to 3,600 ft.) is characterized by a narrow
belt of Cwa (tierra templada) climate, which is
followed abruptly by the subhumid tierra caliente
(below 3,600 feet), or Aw. Below 2,000 feet with-
in the Tepaleatepec and Balsas Basins, a semiarid
tropical climate (BSh) prevails.
The pine-oak association of the Sierra spills
over onto the upper escarpment, but the sub-
tropical Pinus oocarpus becomes the dominant
pine. Between 4,600 and 3,600 feet, pines disap-
pear, leaving an open oak forest mixed with sub-
tropical and tropical plants of southern Mexico.
At lower elevations the latter plants become
dominant."
SOILS
Three soil types, which tend to coincide with
climate and vegetation, predominate in the Taras-
can area: (1) a yellowish-brown leached soil of
the upper mountain slopes (Cwb to Cwe, pine-fir
cover); (2) a dark, fine sandy loam (t‘uptiri) of the
lower slopes and basins in the Sierra (Cwhb, oak-
pine, probably grass vegetation); and (3) the
reddish-brown clay soil (¢ar4nda) of the lower
altitudes (warm phase of Cwb, Cwa, broadleaf
vegetation) around Lake PAatzcuaro, in the lower
elevations of the northern plateau, and in the
escarpment zone (map 6). Transitional and special
soil types also occur; for instance, many of the
Sierra soils are termed “charandosas,”’ having a
; gees
higher clay content than the t‘uptri loams.
Yellowish-brown soil.—This soil develops in
high altitudes under seasonally humid conditions
“The tropical vegetation of the escarpment is characterized by a great
variety of genera and species. The most common plants include the
milky-sapped trees and shrubs of the family Moraceae—comuchin (Ficus
padifolia), siranda (F. petiolaris), saruma (Ceropia mexicana); the pod-bearing
Mimoaceae—timbin (Mimosa stipitata), guaje (Leucaena sp.), huisache
(Acasia sp.), tepehuaje (Lysiloma sp.), parota (Enterolobium cyclocarpum),
timuche (Pithecellobium lanceolatum), guamuchil (Pithecellobium dulce),
Calliandra sp.; the pod-bearing Caesalpiniaceae—habilla (Cassia occidentalis),
easacalote (Caesalpinia coriaria), etc.; the edible fruit-bearing plants of the
Annonaceae—chirimoya (Annona cherimolia); of the Lauraceae—ahuacate
(Persea americana); of the Sapotaceae—chicozapote (Achras sapota), mamey
(Calocarpum mammosum); of the Anacardiaceae—circuela, cupu (Spondias
mombin); of the Mirtaceae—guayaba (Psidiwm quayaba); and the copal-
bearing Burseraceae—copal ( Elaphrium jorullense).
and fir-pine vegetation. It is the soil of the higher
hillside maize plots in the Sierra; leached and
infertile, it will produce crops for no longer than
4 or 5 years, after which the field is abandoned.
The fine, sandy topsoil, however, is moisture
retentive, and is therefore known as “‘tierra de
humedad,” in which crops can be p'anted 2 months
before the rains. Podzolic soils (uncultivated)
probably occur above 10,000 feet in the fir forest.
T‘uptri.—The most productive of the highland
“humedad” soils is t‘uptri. Like the yellowish-
brown soil, the texture of the topsoil is extremely
fine. (Analyzed as fine sandy loam: 56 percent
fine sand, 23 percent silt, 21 percent clay, 1 per-
cent coarse gravel.) The surface drys to a fine
powder and acts as an insulator, preventing the
evaporation of moisture from the soil beneath.
Consequently, in April and May near the end of
the dry season the t'uptri soil is well moist 3
inches below the surface. T’uptiri usually occurs
between 6,500 and 8,600 feet on both the lower
slopes and in the basin plains. Being porous, the
soil soaks up moisture rapidly, preventing serious
sheet or guily erosion even on the steeper slopes.
Generally, the basin t‘uptiri is more fertile than
the yellowish-brown, the topsoil of the former
having a high humus content (6 percent), a fair
content of critical elements (e. g. 0.09 percent N),
but a deficiency of lime (0.31 percent). Various
subtypes of t‘uptiri occur, differences being based
mainly on soil texture. At the base of slopes or
on alluvial fans the topsoil is often partially com-
posed of coarse voleanic cinder. Such soil is
locally called ‘‘cascajo,” or gravel. Other sub-
types are characterized by an increase in clay con-
tent. These eecur on the lower slopes, and are
sometimes referred to as “tierra charandosa.”’
Caranda.—This is a reddish-brown clay soil,
which prevails below 6,500 feet and develops trom
the spheroidal weathering of volcanic rock under
warm summer and mild winter temperatures and
a cover of broadleaf plants. (Textural content:
39 perceat sand, 26 percent silt, 35 percent clay.)
15 Surface soil samples (to a depth of 25 em. below surface) were taken by
the writer in the Sierra and Lake areas and were analyzed by the Comisién
Nacional de Irrigaci6n, Direccién General de Agroeconémica, México, D. F.
‘Texturally the highland yellow-brown soils are sandy loams, (60 percent fine
sand, 20 percent clay, 20 percent silt, are highly water-retentive (30 percent),
and are low in hummus (4to 10 percent). All soils analyzed (including t‘uptri
and ¢aranda types) were low in lime content (0.24 to 0.34 percent), and
slightly alkaline to alkaline (pH values: yellow-brown mountain soils, 7.22
to 7.24; t‘upuri, 7.44 to 7.71; ¢aranda, 7.21 to 7.42; uirds, 8.05 to 8.13). Since
profiles were not determined, classification according to world soil groups is
not possible at this time.
ca
‘
PUBLICATION NO.
INSTITUTE OF SOCIAL ANTHROPOLOGY:
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CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST Tel!
Large cracks occur in the soil surface during the
months of March and April, and moisture is evap-
orated from a depth of many inches. Conse-
quently éardnda is a ‘‘temporal”’ soil, i. e., it can be
planted only after the rains begin. Because of its
clayey texture, it erodes easily once the plant cover
is stripped and the soil structure is destroyed.
The cultivated slopes around Lake Pitzcuaro, for
example, are one of the worst-eroded agricultural
areas of Mexico. Wherever éar4nda soils occur,
the surface is scarred by gullies, which are becom-
ing a characteristic landscape feature in the low
areas surrounding the Sierra.
Minor soil types——Among the most fertile in
the Tarascan area are a few minor soil types.
These include the alluvium in La Cafada and
the lacustrine deposits around the shores of Lake
Patzcuaro and within the recently desiccated
Zacapu Basin. Containing abundant organic
material and essential chemical elements, most
of these soils are cropped annually without fallow.
A peculiar soil type, called wirds, occurs near the
edge of a lava flow on the southwestern shore
of Lake P&atzcuaro, on Jaracuaro Island, and near
Thuatzio. The subsoil is a fibery-textured white
clay (35.4 percent fine clay), from which the
whitish-gray adobe bricks of Jaricuaro and
Thuatzio are made; the topsoil, when mixed
with lacustrine deposits (as on JarAacuaro Island),
forms a fertile loam extremely high in organic
matter (nearly 5 percent) and calcium carbonate
(7.7 percent). On the other hand, when the parent
material lies close to the surface (as around
Arécutin), the wirds is one of the poorest soils in
the vicinity.'®
16 A similar soil type occurs at the edge of a lava flow along the highway
on the outskirts of Zacapu. The relation between vulcanism and the forma-
tion of wirds is not clear.
TARASCAN POPULATION
THE RECESSION OF NATIVE SPEECH
One of the outstanding developments in Ta-
rascan history has been the drastic areal recession
of indigenous speech. Today the territory in
which Tarascan (P‘orépeéa) is spoken represents
only one-fifteenth of its pre-Conquest extent.
The pre-Spanish linguistic area (discussed by
Brand, 1944) included most of the present State of
Michoacan, except the Pacific slope of the Sierra
Madre del Sur between Colima and the lower
Balsas (map 7). The political limits of the
Tarascan state, however, extended beyond the
language boundary: in the west into Jalisco, in the
south to the Pacific, and in the north to the Bajfo
of Guanajuato (Brand, 1944; cf. Stanislawski,
1947 a). The Tarascan cultural core centered in
the north-central part of the Empire, comprising
the Lake P&tzcuaro-Cuitzeo area and the pine
forests of the Sierra and the upper escarpment
zone (Stanislawski, 1947 a). Tarascans extended
their speech southward into the tierra caliente
(basins of the Tepalcatepec and Balsas) by colo-
nization from the highlands during the 14th and
early 15th centuries. Likewise, the P‘orépeta
settlements around the eastern end of Lake
Chapala and south thereof (Mazamitla) appear to
have been 15th-century colonies. Within the
pre-Conquest area various islands of foreign
tongues existed; these represented colonies settled
with permission of Tarascan chiefs. There were
three inclusions of Matlaltzinca or Pirinda (Otomf
stock): (1) the largest, near present Morelia, from
Undameo northeast to Charo, (2) at Taimeo,
southeast of Lake Cuitzeo, and (3) at Huetamo
near the Balsas.” Moreover, a group of Apaneca
colonists lived at Guayameo, near Sirandaro on
the Balsas, and an islet of Teco occurred between
Tancitaro and Uruapan."®
Various factors contributed to the areal retro-
gression of Tarascans during the Spanish colonial
and postcolonial periods. One factor was actual
decrease of Indian population caused mainly by
European diseases. The population of some
areas was further weakened or depleted by
migration of Tarascans as laborers to distant
mining and agricultural centers. Moreover,
Spanish and mulatto settlement within the indig-
enous area was a powerful force of hispaniciza-
tion; wherever stock-raising estancias or sugar
haciendas were established, native speech slowly
disappeared. Conversely, in those areas shunned
by Spanish settlers, Tarascan has been preserved
to this day.
The most serious shock which the indigenous
cultures suffered from Spanish contact was the
frightful toll taken by the contagious European
diseases that became epidemic throughout centro’
1 Data obtained from the following Relaciones Geograficas in Mus
leg. 102: Rel. de Necotlin and Rel. de Cuseo; Mus. Nac., leg. 99
Charo Matlalzingo.
18 Mus. Nac., leg. 102, Rel. de Sirandaro y Guayameo; P’
1872, vol. 1, p. 131; Mus. Nac., Col.de Gomez Orozco, vol. 1, ”
102°
INSTITUTE OF SOCIAL ANTHROPOLOGY-—PUBLICATION
—— mm = Limits of Torascan Speech, ca.1550 (Brand)
Guadalajara
ch Inclusions of Foreign Speech, ca 1550
T7 > Area of Tarascan Speech, 1946
——--— Boundory of Michoacén
As aio te
X aa =
IN cree ge the ay
» LAGO DE CHAPALA “ . ‘ ? ‘ 0
iD pene Soe ce a Sa
es ‘ f oe ena Puruandiro
y a } o Sahuayo =— Os Pe
2o---— ip oC i] ozamora “So Sy Se
( Zp aarti = = —_— es
~~ oe fe} t |
Mazamitia? 5) Sy MaravatieN
0 TSN oe Re )
mention scores of villages in the Taras-
‘hich are now nonexistent, the inhabi-
» this calculation from figures given in the Suma de
Troneoso, 1905, vol. 1).
boundaries of Tarasea speech.
tants having been wiped out entirely, or the few
survivors having migrated later to larger towns.
Spanish exploitation and settlement in Mich-
oacdn slowly effected the reduction of Tarascan
speech. Guzman’s entrada (1530) left a trail of
destruction and displacement of population
throughout northern Michoacén. Moreover, dur-
ing the exploitation of placer gold along the
tributaries of the Balsas and Tepaleatepee (1524—
35) Spanish miners destroyed and dislocated many
Tarascans through enslavement and overwork.”
On the other hand, Franciscan and Augustinian
missionaries, who by the end of the 16th century
had established themselves in most of the large
Tarascan pueblos, were strong agents of accul-
turation, replacing many indigenous material and
2 The Indice de Protocolos, vol. 1 (ed. Millares Carlo and Mantecon),
gives abundant evidence of the feverish gold panning operations in the Balsas
and Tepaleatepee drainage from 1524 to 1528 and cites the wholesale use of
Indian slave labor. Such activity probably continued until the enforce-
ment (in the 1540’s) of the New Laws, which forbade slave labor and conse-
quently deereased the profitableness of gold washing. Furthermore, many
Spanish adventurers turned from gold panning to silver mining after the
discoveries in the Tasco district during the 1530's.
LAGO DE CHAPALA
-— |
ee The mill
settlements (trapiches, ingenios), like the cattle
ranches, were centers of acculturation and misce-
genation. Large groups of Negro and mulatto
slaves, male and female, were imported to operate
the trapiches (according to colonial law, Indians
were exempt from mill labor), while Tarascan
forced and free workers planted and harvested
cane in fields nearby. Race mixing and gradual
loss of native speech was inevitable. Again, ex-
ploitation of the copper mines of the trerra caliente
and the establishment of smelting centers in
Tzatzio and Santa Clara was another activity
which helped acculturation and hastened the loss
of the aboriginal language. In 1750 the limits of
Tarascan speech still coincided with the 16th
century pre-Spanish boundaries, but in some
areas, such as the Tepalcatepec Basin, the per-
centage of inhabitants speaking Tarascan was
only 25 percent of the total. In the tierra tem-
plada sugar-growing districts south of Zit&écuaro,
in the Peribién Valley, and the upper escarpment
zone around Ario and Tacdmbaro, the ratio of
25 In 1540 a sugar mill had been established in Taximaroa, on the plateau
above Tuxpan (Paso y Troncoso, 1905, vol. 1, p. 253).
LAGO DE CHAPALA
Pajacuar(
e
lo
\ Mozomitla
i
\ Tomatién
eTepaicatepec \
ees Probable limit of Tarascan speech,
1800
Areas with 100 % Tarascan speech,
Ups 1800
Percentage of indigenous speech in towns
100%
S99 75%
74-50%
49-25%
24-0%
Map 9.—Area of Tarascan
Sty
ee
O Yurécucro™s °
t. uO: XN
XN to.
R10 g z 5 ) 59
N
i (
° = eee
LAGO DE CHAPALA
“=
¢
Cojumotidn °
‘everécuaro
=
~
ca a ©
Sbenjomillo 25% © Purvéndiro ~ ie e
e
Sohvoyo @ 7 ~ 1 ey J
/ { : ee = OKcémbaro
/ e¢4 ~ Huango s © —)o-20
\o 7, x ~ se Cuitzed XN
F ores ) ‘
‘\
Huoniqueo co)
Sea») Nie e
en CRapendare ZgsedeuarsN . . * 2a 50%
Torecuato to)
LSE: = 75% 2 N
5 Potamban » Vo \ Me
by e © Teremendo “le \
©. =
Tinguindin oldiimoroa
‘OGocupao
Tzintzuntzan
a
@Eticuara
S Tancitoro
Tacambaro
= °
e e Tomatién
\ fo}
@ Tepolcotepec \
Lo Huacono
°
eee Probable limit of Tarascon speech,
1800
Cutziog /
/
Va Areos with 100 % Torascan speech, Huetama O
pf 1800 sa eo
‘ ~
Percentage of indigenous speech in towns
100%
99-75%
74-50%
49-25%
24-00%
oooe @
en locality
748988 O - 48 (Face p. 14)
: < F iv!
‘ to total number of inhabitants at any 8!
Mar 9.—Area of Tarascan speech, ca. 1800. Isopleths indicate percentage of Tarascan-speaking i Me
i ae eee :
ie ' .< ep i
THUICATION Hos & f *
hee Siieieli ¥
hos Ts fascune,
F = 2
Pure oh Che western @
ii M catern Lorca R
te .
ays A
; ap ornrepale iia Sire
x
as ud its Europesnbcubess *
pheay hear! whe ete --
mS [acu ny iene Apatauird
the Tepulegtoneg so gma
x th, ete aun aged ebriubs! 3 eve less
ai it thd north ore niatean,
; ape bs bY abundink 2
ngs .. Sr the norili sie native
\ Pere rd ar at nt With the mika
ew
Y > +" SSS
\Viee
a a cs aoe \ ‘
= = aie i \ a eel “WW the daythtte.” Moreovery difriie:
ot an | pion aw 7 ile i uh contury Syaniantiatie
gtinambang \ ‘ i : "4 Lar 33 as bee ans and emit
sith ' dea a * oe
> — oe fy seh hk 8 ti Libs? va caliente * Th
= Ve ot SF : ; trapichal tngeniis), tise tie
F ihe; ee ous Aegis of aceulturation
privonst, +ef_ ee & 5 ey otwert rnupe ot Negre ASC
; q ie ; Prstighnd foranin, were Mipirtedte
oe } i Sy. ao jencording to oolonial law
. i ki a ? Aan a8 a fruit maiebor), while,
4 d {eee an do oiree workers phusited ‘and h ‘ube esto
¥ Ps — '
r. + Pinal i sals nearby. ee maine and ae watt
H ae: Shce a
gresae eecoves ae thm aide
} 1 20 COPPET POLS
hl et ily cap fray .
fea Soois Uinee oN anor
Peare" a! a Sah oe eats ids tte
wired lanai, o 17 28
eearh ete es i ecidod with
sre DAashs Daviniariea, Dui ai
fH ns tue ilar CR TERE « ew, a
ita: as Taraet ah
r ocmaw
ara
ee
: . ; 7 Hats v aley, aud they ‘ ut)
ao Hiet ponies temsaha'E te nseqoeag wl il eiicioal 0081 29 viasoga peoganaT i048 >,
Tht ~ OF (Puce p. 06)
arti) 2]
)
iI NO O1DN 0104 Se oe Suonp vos
osoqwo20)? Gs
a= —_----
oadodg
7 P
,
3 F ;
4 al J peta
a -
}
manch) wratahine 1]
J iis) r) \°
i
]
'
RRA’ WOE
ae ab | 1, 7B
savin leg BS gute rs a ee
' 1 Mis 4
i | ee
_ =e Prt ie & = fony
%. —-aueae| ° ® weauetinzod
t bauenit ane j
oy 2 oopn0f % (apre f d ning y
1 oe aw * a) i
F o is t
A. iat i
Ae ” °" wa rin RO rs ong gy r @ au . &)
we ones: a ie ad i } 26; |
~ ovum gy 7 & ~@- yoo rs
— re bit Pia —\
an cy s 3" in ae e > “\n macy
« Pace” ot Wl ele ak OC ota : Y 4 | : |
' 7 ee
; @ onivez noIEVsPOoA ? WF anal ane - YY = |
3 oe o ¢ f ype x the A eo
4 ven _ 4 | =
puroyoren AG | becca — =< & pag. ; ; a
a) v ef
cate oreuotgad om Ka sere g &
Lom ‘ om 4 :
Ff ~\ % “<4 Gilt ce, (Ge)
f Ganetos hoc » ‘
i ore * a) ginedtin9 oh
I
Mf eTdatieanm coos 0208 005,0f ‘& ooce
i
cf Vacdmbore
t
i ar Ze Aue
152
bafolustos eslova to jipoAl
He
qabeos O = $2 Foon we ts),
‘; 7 OLGI xivRo dotbecaib« | \ Mem atcoaritleyar Wassge: neMHET to notinditad—t aa
Nox ca) a sswoli noitplugeg to vigor ‘prnvpé mor
sizyfo. to: adivica Aguld yo dsloribai yitosel dope al etnntidodnt pra
fe insane : = it nn
cmd
aaisliconl oxi minal
CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST
TABLE 1.—Distribution of Tarascan-speaking folk by
localities, 1940—Continued
THE SIERRA—Continued
19
TABLE 1.—Distribution of Tarascan-speaking folk by
localities, 1940—Continued
THE SIERRA—Continued
Total Tarascan-speaking Total ‘Tarascan-speaking
popula- folk popula- folk
Locality tion Locality tion
(num- (num-
ber) Number | Percent ber) Number | Percent
Municipio of Paracho: Municipio of Tangancicuaro—Continued
Paracho lv) wet eee es 3, 304 1,005 30.4 Ubas anes (t)e- 5 Ss eas ne ee 51 | 20 39. 2
IMHIran(p) eeeeseee eae oe ee ee 593 593 100.0 Gusrachanillo: (1) =.= = -=---- 2-2. 52-cencc- | 22 9 40.9
Aranza (p) 792 126 17.1 Rancho Nuevo (r) 38 3 | 8.0
Arato (p) 233 0 0 [as Trojes\(r) --- 2125222 sete ces | 14 0 0
Cocucho (p) ------___- - 584 584 100.0 HOT Men uecCho(t) 2-222 2.c- esa nee 1, 735 1, 682 97.0 Ibarra (Patzcuaro Sta.)_.....__--------- 809 12 1.5
Huiramangaro (p) 540 17 3.1 emecorio: (p) Lao eee soos seen =enoee 499 0 0
San Juan Tumbio (p).- 887 0 0 Tzentzenguaro (p) 258 0 0
Ajuno (p) 540 0 0 Lazaro Cardenas (p) 412 0 0
Ajuno Sta. (rr) 719 0 0 Primo Tapia (p) 369 0 0
Municipio of Tancitaro: San Pedro Pareo (p)_-..-...------------- 384 0 0
Tancitaro (v) 1, 858 6 3 Carifin (r)__------- 37 37 100.0
"AON (D) Has=4==-5 876 0 0 Tecuena (r)___.___- 7. 73 100.0
Municipio of Tangamandapio: Urandén Morales (r) _ 2 39 39 100.0
Tangamandapio (p)-_--_.---..---------- 2, 573 12 25 Urandén Morelos (r) -_----------------- 164 164 100. 0
‘Tarecuato (p) 2, 146 2, 146 100.0 San) Pedrito (r)2-= sees enansconsee 14 14 100.0
La Cantera (r) 962 962 100.0 RV rni6mn (r) =: oe ee ee eee ses 116 116 100.0
Las Encinillas (r) 78 78 100.0 Watretzio (1h) = sos see ces ee eee 170 14 8.2
Los Laureles (r) ____ 8 8 100.0 Municipio of Quiroga:
Ucuarés (r) 308 0 0 Quiroga: (y) sees eee wee see sane 3, 009 4 1
Municipio of Tangancicuaro: San Andrés (p)_- 1,179 1, 165 98.8
Ocumicho (p) 1,040 1,018 97.8 San Jeronimo (p)_- 1, 527 1, 513 99. 1
Patamban (p) 2, 333 809 34.6 Santa Fé de la Laguna (p) 2, 036 2, 036 100.0
San José de Gracia (p)-- 170 147 86.4 A tzimbor(r) see on en ee neeeeeaceas 179 0 0
Agua Escondida (r)___ By 32 100.0 Chuptouseour)c-3 see = on. 22s ---e 31 0 0
Aranza (r) 54 21 39. 0 Touscato(h)es- 22222 - ose — oases 249 0 0
Gam écmaro;(f)eeeee P= _ = Sees 8 a2at-3 37 2 5.4 La Tirfmicua (r)___----_------- 88 0 0
Tzirandagatzio (r)--- 24 0 0
2 Locality not listed in 1940 census. Names obtained from local inhabi-
tants.
3 Estimated population.
4 Entirely mestizo according to census, but 100 percent Tarascan accord-
ing to officials in San Juan Nuevo (Los Conejos) in 1946.
5 Uninhabited in 1940, but estimated population in 1946 around 35, all
Tarascan.
6 Inhabited 1944. Official census figures not available.
7In 1946, according to local inhabitants, Napizaro was only 50 percent
‘Tarascan.
8 Owing to loss of original census data, the number of Tarascans in PAtz-
cuaro could not be calculated. The percentage would probably be extremely
low.
20
TABLE 1.—Distribution of Tarascan-speaking folk by
localities, 1940—Continued
THE LAKE AREA—Continued
INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
TaBLE 1.—Distribution of Tarascan-speaking folk by
localities, 1940—Continued
LA CANADA—Continned
Total ‘Tarascan-speaking Total ‘Tarascan-speaking
: popula- folk A popula- folk
Locality tonic __ Locality tion
(num- (num-
ber) Number | Percent ber) Number | Percent
a - ~ |
Municipio of Tzintzuntzan: Municipio of Chilchota—Continued
zintzuntzeni(¢C)= 22s... 22.2----2--22-2- 1,077 | 35 (9 156) |3. 2(9 12. 7) IheiCofradia(r)i i. .s2 69 0 0
Cucuchucho (p)____--_-_-----_-________- 295 279 94.5 ADzintzichs ((t)t = esnon eas See eee oe 117 48 41.0
Thuatzio (p) 1, 206 1, 206 100.0 Municipio of Tangancfcuaro:
La Pacanda (p).---......2-..----.-.---- 247 240 97.1 Tangancicuaro (v)_- 10 2
Woenembo! (rings ao2 2s t= tc 451 0 1) IPH CuarOn (pies. sass a cee ee seed 9 1.0
Whos @orralesi(r)c 82.2 oe = 177 0 0
as Cuevas (r)<. 2 = -222- 2.5 =a... e- 69 0 0 > =
Las Granadas (r)_______.__-_-___ 92 92 100.0
CHUIDION(G) see Seen se eee 162 162 100.0 = aces: a ae aa
eerie (W) - ----------- 2222 2----- ee ue ee) Municipio of Ziricuaritiro:
i made a Restwirr Log > ocak yi hs o a San Angel Zurumueapio (p) - 970 822 84.7
- 30 ES) Aes n08 100.0 Municipio of Tingambato:
eee n0/(a} a 0 o Tingambato (p)...----.-------------- 2, 768 204 7.3
as Pilas (r)-.-------------------------- 87 0 9 Municipio of Uruapan:
Santa: @ruz:.(r) 2-2 2225-22 ences 178 0 0 Upiapanl(c) ae eee ee 20, 583 1 AE
Tarerio (r) 201 194 96,5 mcutacatol(pe. lee 509 5 1.0
El Teeolote (t)..----------------------- 12 0 0 La Rosa de Castilla (r)_.-_-_.....-...-- 60 2 3:3
Hl Tigre (1) ----. -----~-=---2-2--0----= we W) M Toreo Alto (r)_.._...------------------- 240 3 1.2
Wensansstacue:(r)..°-.22--2-22 2 222.- 110 110 100. 0 Galtzontein (p)i tee cho ’ (2) ro) (2)
La ae (1) ----------2---2--------- tk | 0 W Municipio of Ario de Rosales:
La Vinata (r)-.-------..------..-------- a a 1020 Villa Silva (p)1_.... 2.22... 2. see l@) Orde XO
i THE NORTHERN PLATEAU REGION = 10 Inhabited 1943. Official census figures not available.
Munieipio of Coeneo: ° . ° b
See ee the rt an F A Distribution of monolingual Tarascans.—In
AcaiOi(p)sameene es ae Ae 1,097 | 1,088 9.2 spite of continued areal recession of native speech
Comanja (p) 806 91 11.3 : sey =e = Bare econ 2
WMG a hens og ond infiltration of mestizos, monolingualism still
Bellas Fuentes (h) 876 1 1 exists in many parts of Tarasca. According to
HUATOC Ot) een ates Soe keane tee eee 345 | 1 3 paris 2 = (OY. a , Fe
Nee te er ; ‘ calculations from 1940 census data, approxi
auLeuibirol(t) os eeee fe seeds aaah ee 749 2 2 mately 38 percent of the Tarascan population is
Municipio of Zacapu: : é 3 o are
ie Se ois a 4 monolingual. Personal field experience, however,
Cantabria (p)_---_-----.-----.--------- 1, 132 0 0 would indicate that a smaller proportion (prob-
INBYanjai(D) coe oon soo hese ee ses ee 1, 082 763 70.5 2 9 ae by
Mareiets (ah se aa a ably 20 percent) speak only Tarascan. The mono
Guirindero}(p)smere eee ee 1, 252 686 48 linguals are composed principally of conservative
Buenavista (h) ...--.-...------- 224 7 3.1 F ae 5 . ivine in
Caches G isi : 13 women and girls and the older men living in the
San Antonio (rn)... 909 0 0 more isolated pueblos and ranchos. Pronounced
Se nee ce taie ‘ o7 monolingual centers are scattered through the
Teremendo (p)...---------------------- 1,331 379 28.4 Tarasean area and correspond to the islets of
TIRES VES) ieee caer 178 : oe purely indigenous speech mentioned above (map
= 13). One center includes the ranchos around the
LA CANADA eae
=e = we Cerro de Patamban and also the majority of
Municipio of Chilchota: women in the pueblos of Pamatdcuaro, Sicuicho,
CE TOE NG) Zale y ‘4 and Sirfo, nearby. (According to data from the
Acachuén (p) 717 712 99.3 9 5 ee
Garapanl(p)= =e ee ee ee 1,259} 1,240 98. 5 1940 census, approximately 67 percent of the
Pee aa COS eine te Tarascan population of this area is monolingual.
eban:(p)cesss-5--2s. 22222 776 776 i ‘ 5 a
Santo Tomés (p) 295 292 99.0 Following percentages in this paragraph are
MACUCO (Dp) se 22. = ce oe 445 445 100.0 ealeulated from the 1940 census.) Another center
Tanaquillo (p)_ 410 184 44.9 ri : ah f
ORE E Coe ee ee ea Saree 350 135 36 Includes Tarecuato and the adjacent rancho o
Zocopo (Pp) ---------2--2----- eee 539 539 100.0 Still
®’ Number and percentage of Tarascans in Tzintzuntzan, 1945, according
to ethnographical census.
1,231 inhabitants in Tzintzuntzan.
The percentage was calculated on the basis of
La Cantera (66 percent monolingual).
another area is situated southwest of Nahuatzen,
and consists of the pueblos of Quinceo, Turicuaro,
21
WEST
EOGRAPHY OF THE MODERN TARASCAN AREA
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22
Inhabitants
200,000 9 299 o90
\ (Mendizabal)
\
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INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
100,000 \ | |
|
| \ 22,000 (Mendizabal) | |
~~ | i;
80,000 ar F SS SS
i |
~
in | Offical census
~ dota
ec,ece LE if T AN,
| 55,000" 4,795
(Villasefior & church records)
40,000
20,000
(e)
Year 1500 1550 1600 1650 1700 1750 1800 1850 1900 1950
Ficure 1.—Decline of Tarascan population, 1500-1940. The figures for 1500 and 1550 include all aboriginal inhabitants
in the diocese of Michoacan.
Besides the Tarascans, several thousand Otom{ and some Huastec inhabited the eastern
and northeastern sections of the diocese (Guanajuato and San Luis Potosi), and many people of Nahuatl speech
lived in the western portion (Colima, southwest Michoacan).
and Cumachuén (62 percent monolingual). More-
over, the pueblos of La Cafiada, adjacent to mod-
ern transportation facilities, are surprisingly mono-
lingual (59 percent). Other scattered, ultracon-
servative towns, such as Angahuan, Cocucho, and
Cherandtzicurin in the Sierra, contain a large
number of monolinguals.
Effects of Paricutin Voleano.—The eruption of
Paricutin Volcano early in 1943 caused the redis-
tribution of some of the Tarascan population.
The inhabitants of the completely destroyed towns
of Paricutin and Parangaricutiro were transferred
to new lands near Uruapan. Those of Paricutin
were moved to the new settlement of Caltzontzin,
5 km. east of Uruapan, in February 1943. This
pueblo now forms a new island of Tarascan speech
in the tierra templada. With Government aid the
people of Parangaricutiro established a new
pueblo near the rancho of Los Conejos, 6 km. west
of Uruapan, in March 1944. Another new town,
CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST De
Inhabitants
50,000
40,000
30,000
20,000
10,000
Year 1750 1800
1g50 1900 1950
Figure 2.—Growth of population in the Sierra, 1750-1940. The population of the following towns and ranchos was
used to calculate totals for the years indicated: Ahuiran, Angahuan, Arantepacua, Aranza, Atapan, La Cantera,
Cherdn, Cherandsticurin, Cherato, Cocucho, Corupo, Cumachuén, Charapan, Capacuaro, Huiramangaro, Nahuatzen,
Nurfo, Ocumicho, Pamatdcuaro, Paracho, Parangaricutiro, Paricutin, Patamban, Pichdtaro, Pomacuardn, Quinseo,
San Felipe, San José, San Lorenzo, Sevina, Sicuicho, Sirfo, Tanaco, Tarecuato, Tenguecho, Turfcuaro, Urapicho,
Zacan, Zirosto, San Benito, San Luis, La Tinaja, El Tropezén, Uringuitiro, Zarzamora.
Data for 1750 were taken
from Villasenor and church records (AAM); for 1800, from church records (AAM); for 1845, from AAM, leg. 707,
Memorias estadisticas; for 1900, 1921, 1930, 1940, from official census.
called Colonia Dr. Miguel Silva (Villa Silva), was
founded by volcano refugees in August 1943, 5
km. southwest of Ario de Rosales, on the upper
margins of the tierra caliente. The settlement
sheltered families mainly from Zirosto and some
from Paricutin, Parangaricutiro, and Zacan.*
The highland Tarascans have encountered several
difficulties in the subtropical habitat: increased
susceptibility to disease, unfamiliarity with sub-
tropical clay soils, slow adaptation to new crop
types. Consequently, within the last year (1945-
46) the population of Villa Silva has decreased
from approximately 600 to 300, owing to high
death rate and movement of families back to the
highlands; the new settlement may be abandoned
within a short time. Besides resettlement in
newly formed pueblos, many of the families from
the stricken area have moved permanently to less
damaged towns, such as Pamatdécuaro, Charapan,
Paracho, Uruapan, and Zamora.
80 The continued activity of the voleano may force the complete abandon-
ment of the partially ruined towns of Zacan and Zirosto. In the spring of
1946 the authorities of Zirosto were seriously considering the removal of the
remnants of their townspeople to the rancho of Barranca Seca, 4 km. to the
northwest. =
Possible future trends in Tarascan popula-
tion.— Judging from the long-range trend in both
areal recession and actual numerical decrease in
Tarascan-speaking folk, it would appear that the
Tarascan language is headed toward extinction.
Figure 1 indicates the terrific human toll taken by
the European epidemics during the first 50 years
of Spanish occupation, and the leveling off of the
downward curve * until after 1920, when increases
are reported by the 1930 and 1940 censuses. In
the period 1930-40 the rate of increase in Tarascan
population equaled that of the mestizo element.
This period of increase is too short to conclude
31 At the end of the 18th century, decrease in Tarascan population was
still outstanding enough to be reported officially to the central government
in Mexico City. Commenting on the population increase in the diocese of
Michoac&n from 1700 to 1783, an official reports: ‘‘Hay el considerable aumento
de 38,449 vecinos . . . pero debe advertirse que este segun las noticias comunicadas
por los subdelegados, é informes recevidos en el asunto, es de espanoles, mulatos,
y demas castas, pues en la de los Indios se experimenta mucha decadencia o
diminucién originada en unos pueblos de la mescla de estos con distintas cali-
dades; en otros de las graves y continuas enfermedades, que han padecido; en otras
de las pensiones, que cargan insorportables a su felicidad, quando es corto el
numero de los obligados a ellos; y en otros finalmente a la exrcasez de tierras para
su precisa subsistencia, sobre lo qual para no confundir el estado antecedente se
acomparia uno, que manifiesta los Pueblos, a quienes faltan aun de 600 varas,
que por cada viento les asigna la ley .. .”. (AGN Historia, vol. 72, exped. 1
(1793)).
24 INSTITUTE OF SOCIAL ANTHROPOLOGY—-PUBLICATION NO. 7
that a new upward trend has been established.
On the other hand, there has been a considerable
increase in the population of the Sierra and Lake
towns since 1750, which probably accounts for
the level curve during the 19th century, in spite
of drastic areal recession in speech during that
period (fig. 2). Today areal recession is still in
progress, but actual numbers of Tarascans appear
to be increasing. The question is: Can the growth
in number of Tarascan-speaking children continue
to exceed or equal that of the children (of Tarascan
speaking parents) who fail to learn the language or
cease to use it in later life? Assuming equal rates
of infant mortality and similar health facilities for
both groups, it would appear that, owing to cul-
tural changes now in progress within the Tarascan
area, the indigenous speech will eventually dis-
appear. Such cultural changes—improved trans-
portation, more frequent contact with modern
life, increased educational facilities both within
the pueblos and in the large towns outside, the
Government alphabetization program—all aid
to increase the use of Spanish and to decrease
the use of Tarascan. Such factors influence espe-
cially the younger generation. Today the young
people (5 to 20 years old) of many pueblos have
not learned Tarascan, and often those who know
the language speak Spanish by preference. More-
over, as indicated above, mestizo merchants are
still moving into the Tarascan market towns and in
such centers intermarriage of Indian and mestizo
continues; the offspring of such unions rarely
learn the indigenous tongue.
TARASCAN SETTLEMENTS
The early Spanish adventurers and friars found
Tarascans living (like many sedentary Indians of
the New World) in agglomerated settlements, the
larger of which the Spaniards called pueblos, the
smaller, rancherias or estancias. The pueblo and
the rancheria (rancho) have remained the basic
units of settlement in the Tarascan area, as im
most parts of Mexico. In size present Tarascan
pueblos range from 200 to 3,400 inhabitants; the
ranchos, from 9 to 900. Invariably the modern
indigenous ranchos are offspring settlements from
a pueblo nearby. For instance, the 11 ranchos
on the southern and eastern slopes of Cerro de
Patamban were formed by families, which for
political or economic (land) reasons, left the
mother pueblo, Pamatdcuaro. Sirfo, a former
rancho of Pamatdécuaro, was made a pueblo and
tenencia ca. 1926, its name being changed to
Jestis Diaz. By such a process agglomerated
settlements begin and develop. Moreover, the
ranchos on the Tarf-uk‘éri Peninsula, Lake P&tz-
cuaro, were founded 50 or 60 years ago by fisher-
32 Although in general these two types of settlement are differentiated by
size, the terms ‘‘pueblo” and ‘‘rancho”’ have acquired political connotations,
From the point of view of State and Federal Governments the basic political
unit in Mexico is the municipio, which may contain many pueblos and
ranchos. Usually the largest pueblo within this political unit is named the
cabecera, or chief administrative town. The affairs of the cabecera and those
of the municipio as a whole are administered by a presidente or mayor. The
remaining pueblos in the municipio are regarded as tenencias, each headed
by a jefe. The ranchos are dependencies of certain pueblos, local authority
being vested in the diputado de orden. Upon obtaining sufficient size, prestige,
or political influence, a pueblo may be elevated to the rank of villa or even
ciudad Because of historical prestige small (1,077 mestizo inhabitants)
Tzintzuntzan holds the title of ciudad. Such rank, however, in no way
changes the political function of the town.
men from adjacent islands of Janitzio and Lo
Pacanda. On the other hand, the mestizo
ranchos now found in the Sierra are the product
of migration of farmers and political refugees from
the outside. One of these, Arato, was established
soon after the struggle for independence in 1810,
and in the 1930’s was given the title of pueblo
with tenencia status.
Other types of settlement in modern Tarasca
include the lumber camp (aserradero), an ephem-
eral agglomeration of workmen’s huts around the
sawmill. Such settlements disappear after sur-
rounding exploitable timber has been depleted.
In 1946 there were but three lumber camps in the
entire Sierra. In addition, a minor form of
dispersed settlement is sometimes found in the
Sierra; occasionally a woodcutter and his family
live permanently in an isolated house on a forested
mountain slope and visit the nearest pueblo only
to market products, buy supplies, and attend
fiestas.
Settlement sites——The few available early
descriptions of the Tarascan area indicate the
existence of many more Indian settlements during
the 16th century than at present.*? This was
particularly true in the Sierra, where small
agelomerations (estancias or rancherias) were
numerous. Such settlements were scattered on
33 The early sources which mention former settlements in the Tarascan
area include the available Relaciones Geograficas, 1579-81 (Mus. Nac., leg.
102); various late 16th-century documents concerning labor and associated
problems in Zavala and Castello (1939-46); many documents concerning the
congregations of 1595-1605 found in AGN Congregaciones and Tierras.
CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST
wooded mountain slopes (where maize could be
easily cultivated with the digging stick) and on
elevations difficult of access (chiefly for protection
from Chichimec raids). Many of these estancias
were likely wiped out by the early epidemics;
others the Spaniards probably congregated with
larger towns during the last half of the 16th and
first years of the 17th centuries (Simpson, 1934;
Spain—Law, Statutes, etc., 1681, ley VI, tit. 3),
in order to better instruct natives in Christianity
and to facilitate the collection of tribute and
forced labor. Probably few present Tarascan
pueblos possess their pre-Spanish sites.
Modern Tarascan settlements occupy a variety
of sites, most of which have level, or nearly level,
surfaces. Those along Lake P&tzcuaro are on
eminences or shelves above the water’s edge;
all avoid frequently flooded delta plains. In the
Sierra many towns are located on slopes or benches
immediately bordering the large basin plains;
others occupy level spots in local swales.
NS> Tirosto
Brarangaricutiro, 2
s
Tancitoro
:
ef °
fon Apotzingdn
102°30'
Map 18.—Distribution of house types in the Tarascan area, 1789 and 1946.
748988—48——3
Se
pchiTehets eon =eane
o
o?
Te
iJ
7 v,
. J wt we
. J a a
ve
Cheran
Ss
Tr Copocuaro
Uruapon?
}
:
/
f
? } ae
\
i
jo
ys
‘
@ Wooden plank walls predominant
© Adobe & stone walls predominant
© Wooden plank & adobe or stone walls
equally predominant
# Wattle-daub walls predominant
— Shake roof, 4-, 3-, or 2-shed
| Tile roof, usually 2-shed
--Approximate limit of wooden plank house
Tarejero Coeneo
roy
io
Comonjo TT
Zipiojo
VALLADOLID
LO; Kec
& cps ncunse
‘Or zintzuntzon
(eis
poe ;
7
ROOM ara yu
BF Cuonojo
Lo}
Zirohuen
oy
Opopeo
Sonto CloroO O
Tocombaro
@ Wooden plank walls
© Adobe and stone walls
© Wooden plank & adobe walls equally pre-
dominant
1] Walls of vertical planks or sticks
4 Stone walls predominant
— Shake roof
Tile roof
thatch roof
The 1789 data are from AGN Historia,
vol. 73, Calderén report.
32 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
within or near pine forests. By 1789 most of the
buildings in Tarascan towns in the Lake and
Sierra regions were roofed with shakes (map 18).
Today in the towns bordering the Sierra the red
Castilian tile has completely replaced tejamanil
and is slowly penetrating into the Sierra towns.*
THE LAND SYSTEM AND THE PUEBLO
Tarascan settlements are fundamentally agri-
cultural villages. They include not only dwellings
arranged along streets and in house lots, but also
the surrounding farm land. The land is the body
of the pueblo, whose political and economic life
revolves around land ownership and boundaries,
crop planting and harvesting.
Few records exist on the ancient Tarascan land
system; most lands, however, were probably held
in common. Each community owned surround-
ing lands, the limits of which were determined by
metes and bounds; the record and adjudication of
pueblo boundaries were in the hands of the
village chief, who apportioned agricultural plots
to his subjects.44. As in many modern Indian
areas of Mexico, the aboriginal concept of village
lands and their established boundaries is indurated
in the present political and economic structure of
the Tarascan pueblos.® Such holdings in the
Sierra include various types of land: monte, or
woodland pasture on steep mountain slopes and on
lava flows; cropland in basin floors (planes, t'pakua),
on lower mountain slopes (/aderas, uandten), and
in craters of cinder cones (joyas, t pakua-supiéu).
In La Canada often the following lands are
held by a given pueblo: irrigable alluvium on
the valley floor, temporal lands and monte on the
adjacent slopes, and hwmedad lands in the Sierra.
In the Lake area types of land vary from pueblo to
pueblo. Often small strips of irrigable vegetable
plots are held along the lake shore; most towns
hold temporal land on the lower slopes; those on
43 Although used in most Spanish towns (except mining centers) in New
Spain since the late 16th century, tiles began to appear in the Lake Patzcuaro
district only in the late 18th century. In 1789 Patzcuaro was the only town in
the vicinity with tile roofs (approximately 50 percent of the houses were
roofed with tile, the remainder, with shakes). In the same year one house in
Naranja boasted of a tile roof. (AGN Historia, vol. 73, ff. 285, 318.)
44 A copy of an aboriginal land title (1519) of CheranStzicurin is extant in
AQN Tierras, vol. 867, exped. 8.
45 In many respects the native land system in central Mexico paralleled that
of 16th century Spain. Farticularly was this true in regard to the concept of
village holdings,
the community.
the western and southern shore often have fields
in the Sierra.
Two systems of land ownership—communal
and private—prevail in most of modern Tarasca.
Since the land reforms of 1915, the ejido, a third
type of holding, has displaced most of the hacien-
das around the margins of the Sierra.
Since Spanish contact most of the Tarascan
agricultural land has become private property of
family heads. Even in the few remaining pueblos
which claim complete communal ownership of
their lands, a strong individualization of property
has developed. The historical process of the
shift from communal to private ownership is not
clear. Late 18th-century documents on land
disputes among the Tarascan pueblos indicate
that at that time the communal system prevailed
at least in the Sierra. The issuance of individual
land titles may not have occurred until after the
reforms of 1857. In the Sierra private land-
holders (propietarios) often possess one or more
plots in the plan, and still others on the less
fertile laderas. Size of individual holdings varies
greatly, since land is purchasable. Normal hold-
ings average 2 to 3 hectares per family. Traces
of the communal concept exist in the minds of the
modern proprietors. Although legally possible,
there is little desire to sell land to nonmembers of
If such a transaction should
arise, it usually must be approved by the town
council. Consequently, pueblo lands are kept
intact. Moreover, individual holdings, especially
those in the plan, are rarely enclosed, for after
harvest the fields are used as communal pasture.”
Accordingly, the final date for removal of crops
and the first date for planting in unenclosed lands
of each pueblo is communally regulated.
Vestiges of the ancient land system are retained
in the special communal holdings found in most
modern Tarascan villages. Five pueblos in La
Cafiada—Tanaquillo, Acachuén, Ichdén, Tacuro,
and Carapan—retain communal ownership of all
lands, at least in name. Family heads are allotted
one plot of temporal near the pueblo and another
of humedad in the Sierra to the south and east.
The individual allotments vary from 2 to 4
46 The Tarascan town council is normally composed of the representante del
pueblo and his committee of six. The representante deals with most internal
affairs of the pueblo.
47 Fences and ditches are used most frequently to divide cultivated lands
from pasture and to separate individual holdings on the /aderas, or slope land.
CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST 33
hectares in size,*8 and may be used indefinitely by
the recipient, provided they are not left untilled
for more than two successive years. They may
be inherited by sons, daughters, or in-laws, and
may be divided among them.
Tocuaro
©) Qa
Sa Va
Nocutzepo San Pedrow) \_
Pareo © Tzentzénguaro
San Bartolo Pareo
Santa Ana
\ PATZCUARO
oO
(Coordinates are approximate) ya
fo}
101° 40" 101235!
Map 19.—Distribution of fishers around Lake Pdtzcuaro, 1940. Data from official census, 1940,
54 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
Fishing techniques and associated tools.—
Fishing with native Tarascan nets predominates in
Lakes Patzcuaro and Zirahuén. Both the net and
the hook were employed in pre-Conquest times,!!
but at present the latter is of secondary impor-
tance. The large chinchorros (uatika) and the
smaller éerémekuas are the only nets used today.
The former is a seine, employed for catching
pescado blanco and trucha in midlake, while the
latter, a gill net with a fine mesh, is placed along
shore to trap the small é‘ara4ri and k‘uerépu 1”
(pl. 8). Prior to the introduction of the trucha
the picturesque mariposa or butterfly nets (k‘oru-
e¢a) were commonly employed for catching t*iru.
Owing to the near extinction of this fish, these nets
are no longer seen, except in Janitzio, where they
are displayed to tourists. The hand net (cuchara,
uiripu, ¢itiru) has likewise practically disappeared.
All nets used by the P&tzcuaro fisherman are
home-woven.
Other fishing tools include the spear (arpén,
atdérakua), now used to kill trucha in shallow
water, and the hook (anzuelo, jupikata-térakua) .!¥
Shore traps are occasionally used by a few fishers
of Uricho and Pudcuaro. Fish poisons are not
employed. To improve habitat conditions of
open-water fish, such as pescado blanco, portions
of the lake bottom are often cleared of aquatic
grasses (zacate, pu¢irini) with the uarématdrakua,
a pole 3 m. long with a sickle attached to the end.
An indispensible fishing tool and means of water
transport is the Tarascan canoe, a flat-bottom
dugout hewn from a pine or fir log. Owing to the
121 According to the Relacién de Michoac4n, Tarascan officials oversaw the
net fishermen and those who fished with hooks (p. 16). Moreover, “. . . de
noche pescan con red y de dia con ansuelo” (p. 149).
122 The chinchorro often measures 100 to 150 m. long and 8 m. wide. In the
center is a pocket (bolsa) of fine mesh. Four people are necessary to handle
the net in midlake, and it is usually operated from one boat. The net is
manipulated by ropes (an¢itatarakueéa), 50 to 60 m. long attached to its
twoends. Once the net is cast, it is formed in a semicircle and slowly pulled
forward and upward, while the catch setiles into the bolsa. The éerémekua
is usually 6 to 8 m. long and 40 cm, wide. This net is used somewhat like a
trap. It is fastened to poles in shallow water near the shore and left for 2 or
3 hours. When lifted, the net usually contains several small littoral fish,
their heads caught in the fine mesh. This type of éerémekua can be operated
by one person. A longer Gerémekua (often 100 m. in length) with a coarser
mesh is sometimes used to catch pescado blanco in deep water offshore. Like
the smaller variety, it is operated by one person, who attaches the top of the
net to log floats and one end to his canoe. The net and boat are permitted
to drift in midlake usually through the night, while the attendant gathers in
the trapped fish from time to time.
13 The atarakua is composed of a stalk of carrizo 4 m. long, to the end
of which is attached a long barbed-iron point (60 cm. long). The spear is
hurled either above or beneath the water. Regarding the use of the anzuelo,
the cord supporting the hook is usually attached to a piece of carrizo or otate,
1 m. long, a series of which is permitted to float on the water. A strike is
indicated by the tilting of the stick, which is hurriedly picked up by the
boatman,
drying up of lakes in the northern and western
sections of Tarasca, the distribution of the dugout
has decreased in area during the last 100 years.
At the present time the Tarascan boat is used on
Lakes Patzcuaro, Zirahuén, Cuitzeo, and Chapala;
two old dugouts on the small pond at Tarejero
represent the remnants of the once extensive canoe
traffic in the Zacapu lagoon.'* Most of the Lake
Patzcuaro boats are made in the Sierra settlements
of Cumachuén, Capacuaro, and in the highlands
to the south, mainly around the rancho of Santa
Juana. The boats are dragged to the lake shore,
where they sell for 100 to more than 600 pesos
each. They are said to last for 3 to 5 years before
becoming waterlogged. Two sizes of boats are
seen on Lake Pétzcuaro—the small ié4zuta for two
to four persons, used for shore fishing, and the
larger tep4ri, which carries from four to eight
individuals and is employed in midlake fishing
and for transport. "The smaller boat is paddled
with the pala or 8étakua, which has a round blade
of pine (25 & 28 cm.) attached to a handle of oak
or tejocote varying in length from 30 cm. (for
children) to over 2m. The larger canoes are both
paddled and rowed. Sierra folk from Cumachuén
and Capacuaro manufacture oars and paddles,
which they market in Erongaricuaro and Paétz-
cuaro.
Fishing methods.—In most parts of the lake,
fishing is done in the early morning hours between
5 and 10 o’clock. Fishing is seasonal, most
activity occurring during the dry season (Novem-
ber to May). Chinchorreros usually operate in
groups of four; often blood relations, the group
divides the catch equally. An owner of a net and
boat often hires peones to help with the chinchorro,
paying wages or dividing the catch. The wife
and children occasionally help set the éerémekua
along the shore, and often women aid with the
chinchorro. Midlake fishing is open to all inhabi-
tants of the Lake area, who pay a federal license
of 1.50 pesos annually. By custom, however, the
people of a particular settlement have exclusive
fishing rights along the shore of their lands; those
from other pueblos may not fish the shores of
14 As late as 1872 heavy canoe traffic is described between TareJero and
Zacapu (Pérez Herndéndez, 1872, p. 119). Late in the 16th century small
reed balsas were used on Lake Chapala (Ponce Relacion, vol. 2, pp. 18-20).
125 Measurements of the dugouts: The itézuta has a length of 2.5 m. to
6.5 m., width of 60 cm., and depth of 40cm.; the tepari ranges from 6.5 to 11m
long, 1 m. wide, and 50 em. deep.
CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST 5D
another without permission from the authorities
of the latter.
Fish preparation.—Pescado blanco, trucha, and
aktimaiza are usually taken to market fresh, al-
though the latter is sometimes fried on the comal
before being sold. The tiny k‘uerépu and @‘arari,
however, are invariably sun-dried, the catch being
spread on a petate, which is placed near the door
of the dwelling where it can be easily watched
(pl. 11). Since pre-Conquest days dried é‘arari
has been one of the main exports of the Tarascan
lakes. It was distributed into the tierra caliente,
the Sierra, and as far east as Toluca.
LUMBERING ACTIVITIES
The Tarascans, possibly more than any other
aboriginal group of Mexico, have been exploiters
of forest products since pre-Columbian times.
During the Empire period one of the important
officials of the caltzontzin at Tzintzuntzan was in
charge of ‘‘the keepers of the forests,’ who cut
beams and made planks for public, and probably
private, use.”® Not only were large beams and
logs used in the construction of temples, but also
in the building of forts against Aztec raids.
During the colonial period the pine forests on the
northern flanks of the Sierra de Ozumatlin were
heavily exploited by Tarascan woodmen for beams,
planks, and shakes for the Guanajauto and Zaca-
tecas mining districts.”
Much of the timber resource of northern
Michoacén was depleted by the end of the 18th
century. Relatively untouched by colonial exploi-
tation, the pine and fir forests of the Sierra de los
Tarascos, although constantly diminishing, have
remained the principal source of timber for the
indigenous population. There are few contem-
porary Sierra Tarascan men who cannot handle
an ax or lumber saw. When the maize fields do
not demand their attention, the family head and
his sons are usually in the forest cutting timber
or gathering resin. The Sierra Indian is conse-
quently both a farmer and a lumberjack. Some
are professional woodsmen, who live in the village
but seldom engage in agriculture. Little lumber-
jim Relacion de Michoacan: p.17: “. . . diputado sobre los que guardaban los
montes que tenian cargo de cortar vigas y hacer tablas y otra madera de los mon-
ee This exploitation began immediately after the Guanajuato mines were
opened ca. 1554, and extended into the post-colonial period. After the ex-
haustion of the local wood supply, Zacatecas began to draw on the northern
Michoacan lumber reserves during the first part of the 17th century (Basa-
lenque, 1886, vol. 1, p. 315).
ing is carried on outside the Sierra. Some beams
and planks are cut by the people of Zipiajo and
Teremendo, who have large tracts of forest on
the slopes of El Zirate, and some farmers of the
Lake area and La Cafiada cut small amounts of
lumber for home use.
Beals’ discussion (1946, pp. 15-19) of legal
cutting rights, lumber products, and lumber
tools for Cherin can be applied to most of the
present Sierra pueblos; therefore, only a summary
will be given here. As mentioned above, all
Sierra pueblos possess varying amounts of forest
land held as common property. Since the late
1930’s the Federal Government has attempted
to control exploitation by placing all large forest
areas under national domain, by encouraging the
organization of local lumbering cooperatives, and
by periodically inspecting lumbering activities.
In most pueblos the Federal tax on lumber prod-
ucts is passed on to the individual woodsmen,
who pay the town council a given amount for
cutting rights. In other towns lumber coopera-
tives have been formed to pay the tax, each
member contributing dues and having sole cutting
rights in the village forest lands.
Although much lumber is for local use (house
construction, fences, acqueducts, watering troughs,
shakes, etc.), most is cut for the outside market.
Raw logs, beams (vigas), planks (vigetas, tablas),
and railroad ties of pine and fir are cut and pre-
pared for lumber contractors, whose heavy trucks
visit the larger villages during the dry season to
haul the products to the nearest railhead. Wood-
cutters of the remote pueblos drag beams and
planks to market with the aid of burros and mules.
Los Reyes, Tingiindin, Tangamandapio, and
Zamora handle the forest products from the
western part of the Sierra, while Uruapan, Zacapu,
Ajuno Station, and Pitzcuaro serve as lumber
points for the eastern section. Formerly a signifi-
cant forest industry, shake making (performed
by skilled specialists) is slowly declining because
of the increasing use of tile roofing.’* Turpentine
is no longer distilled locally. (See Beals, 1946,
p. 18, for illustration of Tarascan still.) Rather,
the resin (resina) is gathered in 5-gallon tins and
taken to the village, where they are periodically
138 Although in some pueblos (Pamat&cuaro and ranchos, Angahuan,
Capacuaro) shakes are still made for export to Uruapan, most are used locally.
During colonial times and even in the last century large quantities of shakes
were shipped from the Sierra to the northern mines, where they were the
principal roofing material.
56 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
picked up by trucks from turpentine distilleries
in Uruapan and Morelia. Charcoal is a minor
commercial forest product made by Tarascans
living near mestizo towns. The latter comprise
the principal markets for charcoal, which has
never entered Tarascan culture.’ Other minor
forest products consist of ocote splinters, used
for primitive interior illumination; *° softwoods
(madroiio, jaboncillo, aile, etc.) for lathe work;
pine and fir for cabinet work; etc.
Within the last 50 years the commercial saw-
mill has penetrated into the Sierra. Lumber
companies purchase cutting rights of standing
timber from the pueblos and set up a steam- or
(when near a power line) electric-powered saw in
the midst of the forest.“! When the suitable
timber has been depleted (under Federal inspec-
tion), the mill closes down, and the remnant of the
forest reverts to the pueblo. Although most
companies bring in mestizo labor, many Tarascans
from villages nearby obtain seasonal work in the
sawmills, thereby supplementing their usually low
income. Because of their ephemeral character,
the number of mills in the area varies. In 1940
there were five mills in the Sierra proper; in 1946
the number had decreased to three.
During the last 100 years cutting has exceeded
natural timber growth in the Sierra. Clearing of
new plowland to sustain increased population and
commercial lumbering have been the major
factors of forest depletion. Moreover, disease has
recently destroyed acres of pine in the vicinity of
Tarecuato, and volcanic ash has laid waste the
forest within a 3-mile radius of Paricutin. Lum-
bering even by the Tarascan woodsmen is often
wasteful. Large trees are sometimes cut and left
unattended for years until rot renders the wood
useless.“ Improper tapping for resin and
testing for shakes often kill many trees. The
sawmills, operating on a much larger scale than
the native lumbermen, are even more destructive,
and in former years they depleted large sections
of Sierra forest. Approximately 50 years ago the
timberland in the eastern part of the Sierra east
129 The main charcoal-producing towns in the area are San Lorenzo
(Uruapan market), Opopeo and Cuanajo (PAtzcuaro market).
130 The rancheros around Pamatdcuaro gather much ocote, which the
women market in the large mestizo towns bordering the Sierra.
131 In 1944 the pueblo of San Felipe sold its forest to an Uruapan company
for two million pesos. The proceeds were deposited in an Uruapan bank,
where they remain communal property.
132 Such wasteful exploitation was much in evidence in the forest lands of
Pamatdécuaro on the southern slope of Cerro de Patamban,
of Nahuatzen, Sevina, and Cumachuén was
almost completely stripped by the mills. Today
in this area, barren, windswept sheep pastures,
supporting occasional remnant clumps of pine,
indicate the extent of forest destruction (pl. 8).
Throughout the Sierra there is probably not a
piece of virgin timber, so long and thorough has
been lumber exploitation.
HANDICRAFTS
Among most people lacking modern transporta-
tion facilities and mass production techniques,
cottage industries, often termed ‘native crafts,”
are characteristic of the local economy. Owing
to the presence of particular raw materials nearby
and/or to traditional skills, people of one village
often tend to specialize in one or more crafts.
Cottage industry and village specialization are
prevalent in most of indigenous and even mestizo
Mexico. It is and has been particularly so among
the Tarascans, whom the early Spanish chroniclers
described as a skilled and clever people (Beau-
mont, 1874, vol. 2, p. 165). Moreover, pro-
gressive exhaustion of originally poor soils and
population increase have forced many farmers of
the Sierra to turn to crafts for additional income.
Today five general handicrafts (ceramics, textiles,
woodwork, leathercraft, and metalwork) are
practiced and over 30 types of articles made
among 54 Tarascan towns and ranchos (map 20).
Only 10 Tarascan-speaking pueblos lack a cottage
industry. In 26 pueblos at least 25 percent of the
“working” population! practice various crafts.
Some villages specialize in only one industry.
For example, over 80 percent of the working
population of Santa Fé de la Laguna make pot-
tery; nine-tenths of that of Jardcuaro are hat
makers. Moreover, many towns which carry on
various handicrafts may concentrate on one.
Thus, Tarecuaro is famed for agave fiber products,
Pamatdcuaro and neighboring ranchos for wooden
spoons and bowls. In most pueblos more than
one craft is practiced, and in a few as many as
eight distinct products are made.
Like so many of his material culture elements,
the Tarascan’s crafts represent a mixture of
133 The ‘‘working’’ population in Tarascan towns is estimated by dividing
the total population by 3.5. The Tarascan family averages about 5 persons,
but often the wife devotes her spare time to cottage industry and is sometimes
helped by the older children. Boys over 12 years old usually work in the
fields as farmers or in the house at the father’s trade.
CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST 57
aboriginal and European products and techniques.
lost of his modern handicrafts are based on
pre-Conquest industries (ceramics; wood prod-
ucts; leathercrafts; metal work in copper;
weaving of cotton, agave fiber, stalks of tule).
Except in a few pueblos, European techniques are
now used in making pottery. In modern wood-
work the adz and the lathe are probably European
and cabinet work is practiced entirely with Old
World techniques. Cattle hide and horse hide
have replaced deerskin in leathercrafts, but the
tanning techniques used are possibly aboriginal.
Although the ancient belt loom is used for most
cotton and agave weaving, for weaving wool the
European hand loom is employed. Sleeping mats
(petates) are woven of tule as they were 500 years
ago; hat making, on the other nand, is completely
European. In regard to metals, European tech-
niques have replaced native methods, and iron
has of course been introduced. Spanish friars
and master craftsmen of the 16th century did in-
deed teach Tarascans many new techniques, but
in most instances such were applied to long-
established native industries.
An interesting aspect of cottage industriesjis
their ephemeral character. Owing to movement
of artisan families from one pueblo to another and
changes in markets and fashions, certain crafts
disappear in some towns and reappear in others.
In the last 160 years 37 Tarascan villages and
ranchos have lost old crafts or gained new ones;
27 have retained their characteristic trades
(table 2).% The pottery industry in Santa Fé
de la Laguna dates only from the last quarter
of the 19th century, and in 1910 hat making was
brought into Jardcuaro by a few political refugees
from Pichétaro. A large number of Tarascan
towns were famed for leathercrafts (saddles and
shoes) during the 18th and 19th centuries, but
now, owing to changes in transportation and the
rise of factory production, local leather products
have almost disappeared. Again, the iron craft
of San Felipe de los Herreros has practically
vanished, for factory-made articles can be obtained
more cheaply from surrounding mestizo towns.
134 Insufficient data were at hand to determine possible changes in home
industries for 20 towns and ranches.
TaBLE 2.—WNative crafts in} Tarascan villages !
Pueblo 1946 1841 1822 1789
None. (?) (?) (?)
Weaving (cotton): Weaving (cotton): Knitting: Knitting:
Rebozos. Mantas. Men's stockings of cotton Men’s cotton stockings.
Belts. Belts. thread.
Tablecloths.
Woodwork: Knitting:
Violins. Men's stockings.
Turned work.
An vahuan=-= -2o-c== neue Weaving (cotton): Woodwork: Woodwork: Woodwork:
Rebozos. Shakes, Shakes. Boxes.
Belts.
Aprons.
Tablecloths.
Arantepacua- -=-.-=--<.-=-=-= Capotes. (?) (?) Woodwork:
Brooms. Saddle frames.
Aranza.- === 2222-2282" ---= Weaving (cotton): (?) (?) (Depopulated.)
Belts.
Tablecloths,
Arocutin==.—- sca. sesssese eats None. (2) (2) Petate weaving.
Atapansa2.22--- ees Weaving (cotton): (2) (?) Leatherwork:
Belts. Tanning.
Weaving (wool): Shoes.
Blankets.
See footnote at end of table.
58
INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
TABLE 2.—WNative crafts in Tarascan villages '|—Continued
Pueblo
1946
1841
Caltzontzin (Paricutin) -_____-
Capacuaros2- =: =2--2--/---2-
Charapanz<2-2-22 2-225.
Oherines e252 25.4 A
Cheranftzcicutin ___._.____.
Ohilchota.22 =~ .2:-222222-.225
Coenchoses2-22 2.22
Gomanjs 2 = et a eee 22
Conejos, Los (Parangari-
cutiro).
Weaving (cotton):
Tablecloths.
Weaving (wool):
Blankets.
Woodwork:
Broom handles.
Weaving (cotton):
Belts.
None.
Weaving (cotton):
Rebozos.
Belts.
Aprons.
Tablecloths.
Weaving (wool):
Blankets,
| Hat making:
Palm leaf.
Weaving (cotton):
Belts.
Napkins.
Tablecloths,
Weaving (wool):
Blankets.
Hat making:
Palm leaf.
Embroidery work.
None.
Weaving (wool):
Blankets.
Basketry.
Pottery.
Leatherwork:
Shoes.
Belts.
Saddle leather.
Pottery.
Pottery.
Weaving (wool):
Blankets.
Woodwork:
Cabinetmaking.
Weaving (wool):
Blankets.
Woodwork:
Cabinet work:
Boxes.
See footnote at end of table.
Weaving (cotton).
Woodwork:
Boxes.
(?)
Weaving (cotton).
Woodwork:
Rosaries.
Chocolate beaters.
(?)
(?)
Pottery.
Woodwork:
Rosaries.
(2)
(?)
Weaving (wool):
Blankets.
Weaving (cotton).
Woodwork:
Boxes.
Weaving (cotton).
Woodwork:
Cabinet work.
1822 1789
(2) Weaving (cotton).
(?) Woodwork:
Boxes.
(?) (2)
Woodwork: Weaving (cotton,
Rosaries. Woodwork:
Malacates. Rosaries.
Leatherwork: Leatherwork (1742).
Tanning.
Shoes,
None. Leatherwork:
‘Tanning.
Shoes,
(?) (?)
Woodwork: Pottery.
Rosaries, Woodwork:
Rosaries.
Other turned work.
Woodwork (1742):
Saddle frames.
Pottery (1742).
Leatherwork: Leatherwork:
Tanning. Tanning.
Shoes, Shoes.
(2) Leatherwork:
Tanning.
Shoes,
Weaving (wool):
Blankets,
Woodwork:
Piloncillo molds,
Boxes.
(2)
Weaving (cotton).
Woodwork:
Boxes,
Woodwork:
Cabinet work.
Boxes,
CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST
TABLE 2.—Native crafts in Tarascan villages \—Continued
Pueblo 1946 1841 1822 1789
Cuanajo—Continued-----_--- Weaving (cotton):
Belts. 2
Aprons.
Tablecloths.
Weaving (wool):
Blankets.
Cumachuén:--2---------=-.- Woodwork: Woodwork. Woodwork: Woodwork:
Bateas. Digging sticks. Digging sticks.
Weaving (wool): Oars. Oars,
Blankets. Woodwork (1742):
Saddle frames.
Erongarfcuaro_-_--___--------- Petate weaving (?) Petate weaving. (?)
Eu Snsito: -sseese Seth 2S Pottery. (?) (?) (2)
Nehante 2220 soe ane sea one Pottery. (?) (?) (?)
Mn wAtziove sees se er sso Petate weaving. (?) (2) (2)
Basketry.
Wanitzio’=2e--- = ess. = 2 Netting. (?) (?) Netting.
‘ Weaving (cotton):
Men's belts.
WAYACUAYO = ae" Sas ocsastec Hat making. Petate weaving. (?) Petate weaving.
Palm leaf.
Weaving.
Belts.
Adobe making.
Majbacandass2<2-2-2.-=c=-. 3 None. (2) (2) (2)
INahuatzen’=-2-- == + S.2-2--22 Weaving (wool): Leatherwork: Leatherwork: Leatherwork:
Blankets. Tanning. Tanning. Shoes.
Cloth. Shoes. Shoes, Saddles.
Saddles.
Weaving (cotton):
Belts.
Embroidery work.
Leatherwork:
Saddles.
Belts.
INaranjarss2-c2=2=2eemee ete None. (?) (2) Leatherwork:
Tanning.
Shoes.
Napizaro:=- s52=2=-~-===55--5" Petate weaving. (2) (2) (?)
IN OCULZeDO == = ose nee None. (?) (2?) None,
iINurlote et es eo sees. = Weaving (wool): Hat making: Hat making. Hat making:
Blankets. Felt. Felt.
‘Ocumicho:=- 22222 --- seen nes Clay toys. (?) Leatherwork: Leatherwork:
Tanning. Tanning.
Shoes. Shoes.
Weaving (cotton),
iPamatacnaro.. 2 2-22 snene ss Woodwork: Woodwork: Woodwork: Woodwork:
Spoons. Spoons. Spoons. Spoons,
Bateas. Digging sticks. Digging sticks. Digging sticks,
Hat making: Weaving (cotton). Weaving (cotton).
Wheat straw. *
Weaving (wool):
Blankets.
See footnote at end of table.
748988-—4 8——_5
59
60
INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
TABLE 2.—WNative crafts in Tarascan villages \—Continued
Pueblo 1946 1841 1822 1789
ParachOsseascces seca ee Woodwork: Woodwork: Woodwork: Woodwork:
Musical instrument. Musical instrument. Musicil instrument. Musical instrument.
Turned work. Cabinet work. Cabinet work. Cabinet work.
Cabinet work. Saddle frames.
Toys.
Weaving (cotton):
Rebozos.
Weaving (wool):
Blankets.
Patamban____- ELE Ste geae le Pottery. (2) Pottery. Pottery.
Weaving (wool):
Blankets.
bichstaro==ar-. see ce nee ee Weaving (wool): Weaving (agave). (?) Woodwork:
Blankets. Woodwork: Cabinet work.
Weaving (cotton): Cabinet work.
Belts.
Rebozos.
Woodwork:
Cabinet work.
| Broom handles.
Bateas.
Hat making:
Palm leaf.
Petate weaving.
Pomacuarfn- ---.--...-.____- None. Weaving (cotton). Knitting: (?)
Knitting: Men’s stockings. Woodwork (1742):
Men’s stockings. Saddle frames,
Pottery (?).
Pufcuaro.........___ ____....| Petate weaving. (?) (?) (?)
Weaving (wool):
Blankets.
Quinceo= <== == --2-_ 2-22 <5; | Weaving (wool): Woodwork: Woodwork: Woodwork:
Blankets. Saddle frames, Saddle frames, Saddle frames.
Weaving (cotton):
Belts.
Capotes.
Quriopas..2<2-22<-soste-ceece Woodwork: (?) Woodwork: Woodwork:
Bateas. Bateas, Bateas.
Turned work. Boxes. Woodwork (1742):
Chairs. Bateas.
Boxes.
San Andrés_._...._____________] Petate weaving. Petate weaving. Petate weaving. Petate weaving.
San Angoel......__......._____] None. (?) (?) None.
Bantaulé6! 2-2 2--2)-2--._- "| Pottery. (?) Woodwork. Woodwork:
Bateas (painted),
Boxes (painted).
Petate weaving.
San Felipe-_--..___. wiemee: Se Ironwork. Ironwork. Ironwork. Ironwork (also in 1644).
Weaving (cotton):
Belts.
Weaving (wool):
Blankets.
San Jerénimo....__......-.-- Petate weaving. (?) Petate weaving. Petate weaving.
Weaving (wool):
Belts.
Blankets.
See footnote at end of table.
Woodwork:
Boxes.
Pueblo
San Jos6_____
San Lorenzo----_- Sz secseesees
wRanaquillo: 92) -=2 22.20 2252-2
MarecwAatos 2282 S202. ve se Ss
eharejerOve oa. bese oe ee |
FRETEMONGO neti s eee eno oe
Mrinidaroys2s22-.os 2.
mMocuaro-=S4s<_ 5. ee Sk
CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST
TaBLE 2.—Native crafts in Tarascan villages \—Continued
61
1946 1841 1822 1789
Pottery. (?) Leather work: (?)
Tanning.
Woodwork:
Saddle frames,
Weaving (cotton): (?) (?) (?)
Belts.
Tablecloths.
Pottery. (?) (?) (?)
Woodwork: Woodwork: Woodwork: Woodwork:
Bateas. Shakes. Shakes. Saddle frames.
Weaving (cotton):
Belts.
Weaving (wool):
Blankets.
None. None. None. Weaving (cotton).
Woodwork: (Nonexistent.) (Nonexistent.) (Nonexistent.)
Spoons.
Bateas.
Pottery. (?) (2) (?)
Petate weaving.
Capote making.
Weaving (wool):
Blankets.
Weaving (agave):
Morrales.
Ayates.
Pottery.
Weaving (agave):
Morrales,
Ayates.
Costales.
Weaving (cotton):
Belts.
Embroidery work.
Rope making.
None.
Hat making:
Wheat straw.
Palm leaf.
Weaving (wool):
Blankets.
Pottery:
(Hat making ceased in 1936.)
Woodwork:
Bateas.
Spoons.
Masks.
Pottery.
See footnote at end of table
748988—48——6
Petate weaving.
None.
(?)
(?)
(?)
(?)
(?)
(2)
(7)
Petate weaving.
(?)
(?)
(?)
(?)
Leatherwork:
Shoes.
@)
()
@)
Petate weaving.
(?)
Pottery (1742).
Woodworking (1742).
Saddle frames.
(?)
Weaving (agave).
Leatherwork:
Tanning.
Shoes.
(?)
Leatherwork:
Tanning.
Shoes.
None.
62 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
TaBLe 2.—Native crafts in Tarascan villages \—Continued
Pueblo | 1946, 1841 1822 1789
TPUPCUBTO: 2 o- ane soon a one = | Stonework: Stonework: Stonework: (?)
Metates. Metates. Metates.
| Woodwork:
Bateas.
Broom handles.
| Weaving (cotton):
Belts.
Weaving (wool):
Blankets.
Capote making,
Tzintzuntzan ---_- Pottery. Pottery. Pottery. Pottery.
Urapicho..._.._..._._._.__..-| Hat making: None. None (?). (?)
Palm leaf.
Woodwork (1742):
Saddle frames.
Uricho-=-=--<- __| Petate weaving. (2) Petate weaving.
ASCO oneness ates | (2) Weaving (cotton). Weaving (cotton): (?)
Mantas, Woodwork (1644):
Bateas.
Rope making (1664).
MALOSLO= sone h cca see _...----| Woodwork: Woodwork: Woodwork: Woodwork:
Bateas (disappeared since Bateas. Bateas (painted). Bateas.
voleano). Spoons.
Piloncillo
molds,
Weaving (wool): Weaving (cotton)’ Woodwork (1644):
Blankets. Bateas.
Rope making (1664).
! Sources: 1644, Basalenque (1886); 1742, Villasenor y SAnchez (1746-48): 1789, AGN, Historia, vol. 73; 1822, Martinez de Lejarza (1824); 1841, AAM, siglo
XIX, leg. 704, Memorias Estadisticas, 1841; 1946, Field observation.
Some industries, important in pre-Conquest
times, have completely disappeared. The fine
Tarascan featherwork was nearly extinct by the
beginning of the 18th century (Escobar, 1924,
pp. 149-151). Furthermore, the use of the ground
pith of maize stalks, from which various objects
(mainly religious) were molded, apparently flared
in the 17th and 18th centuries, and then dis-
appeared (Escobar, 1924, p. 144).
On the other hand, crafts which have persisted
in some pueblos for the last 160 years may predate
the Conquest. Witness the leatherwork of
Nahuatzen, a leather-making center in 1640, where
both deer and cow hides were tanned (Zavala and
Castello, 1939-46, vol. 7, pp. 361-362); the many
towns which still specialize in cotton weaving with
the belt loom; the petate-making towns around
the shores of Lake Pitzcuaro.
CERAMICS
Clayware is indispensable in most Mexican
kitchens,’ and tile roofing is used extensively in
most parts of the country. As in pre-Conquest
days, the manufacture of clayware in Mexico
is still a cottage industry in which various towns
specialize.
Including Tzintzuntzan (largely mestizo), there
are nine pottery towns in the present Tarascan
area: Santa Fé, Comanja, Zipiajo, Hudnsito,
Santo Tomas, San José, Patamban, and Cocucho.
With the exception of Cocucho, all are located in
the Garénda, or clay-soils district north of the
Sierra, usually near deposits of suitable firing
clay (map 20). The Cocucho potters have always
hauled clay from the vicinity of Tangancicuaro
and San José, for suitable deposits rarely occur in
the Sierra. Other pottery towns, now mestizo,
are also located in the northern clay area (Tangan-
cicuaro, Capula, Villa Morelos, Penicuaro). More-
over, other Tarascan villages in La Canada
(Sopoco, Ichaén, Tacuro, Tanaquillo), in the Zacapu
136 The common clay kitchen utensils include various types of pots (ollas) for
boiling; the comal, or round, flat piece placed on the hearth for frying, broil-
ing, and toasting; small saucers (caswelas) for frying and from which food is
sometimes eaten; water jugs (cAntaros); drinking cups (vasos).
CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST 63
Basin (Tirindaro), and in the Lake area (San
Jerénimo and Erongaricuaro) make pottery on a
small scale, mainly for local use.
Modern Tarascans use both the hand and the
mold techniques. The latter is usually accom-
panied by application of lead oxide glaze. The
former is still used in only three pueblos—Co-
manja, Zipiajo, and Cocucho, where it is per-
formed solely by women.'* In Comanja_ the
lower part of the vessel is shaped from a single
daub of clay. A depression is made in the center
and the walls are built up with the hands by press-
ing in small daubs of clay. The outer and inner
surfaces are smoothed with a corneob. The result
is a well-balanced vessel with walls of even thick-
ness. The vessels are rough-finished, rarely pol-
ished, and litharge glaze is never employed.
Firing is accomplished by placing pottery on a pile
of dried manure. The pots are covered with dried
grass (zacatén), which, when lighted, ignites the
manure. The grass ash is permitted to cover the
pots, a hole being left in the center of the pile to
permit smoke from the smoldering manure to
escape. After 3 hours the pottery is fired to
sufficient hardness. The chief ceramic products of
Comanja are the large water ollas, called “‘coman-
jas,’”’ which are marketed in the Sierra, the Lake
area, and in some of the mestizo towns to the
north. Similar ollas are made by an identical
process in Zipiajo, but on a smaller scale.
In Cocucho the ceramic process is similar to
that of Comanja, except that the base of the
vessel is formed on the bottom of a broken olla
and part of the wall is built up of rolled pieces
of clay (pls. 9 and 10). Firing is also similar, but
pine bark and rotten wood, rather than manure, is
employed for fuel; this process probably represents
the truly aboriginal technique. The Cocucho
women make large ollas with thick walls, especially
famed as tamale cooking pots throughout the
Sierra. This olla, rarely used outside of the Sierra,
is called kukiéu, from which the village derives its
name. The tunu¢i, a small flat olla used as a
tlascal (receptacle for tortillas), is also made.
136 The native hand technique was practiced in other Tarascan towns
during the 18th century. In 1729, according to Matias de Escobar, ‘‘ Es cosa
que admirar como que los he visto en Tiripitio [southwest of Morelia] como
labran cuanto [losa] quieran, sin las ruedas y moldes de los Espanoles. Un
pequeno cuero y una mala navaja son todos los instrumentos con que obran”’
(Escobar, 1924, p. 148). Both the hand and mold methods appear to be
native in Mexico, although the latter was known to Europeans. See Foster,
1948, for a discussion of native and introduced elements in the modern mold
technique.
The manufacture of these two Tarascan pots is
slowly dying. In 1946 only 10 women were
making pottery in Cocucho, whereas in 1841 it
was made in practically every household of the
village (AAM, siglo XIX, leg. 707).
Today by far the greater amount of Tarascan
pottery is made with molds by both men and
women.” None is manufactured with the
potter’s wheel. All who use molds have taken
over the European glaze technique and the firing
oven. Tarascan mold-made pottery can be
differentiated according to finish. The ‘“Patam-
ban” type, for instance, carries a beautiful green
glaze, known and admired over most of western
Mexico." Green glaze is also used in Santo
Tomas and Santa Fé de la Laguna, having been
recently introduced into the latter pueblo. Pot-
tery hand-painted with brilliant floral designs on
a background of black glaze is a specialty of Santa
Fé de la Laguna. This unusual technique was
introduced around 1900, and was readily adopted
by the inhabitants, whose former industry was
batea painting. As mentioned previously, the
inhabitants of Santa Fé de la Laguna began to
make pots during the last quarter of the 19th
century. Since then their ware has become
known throughout Mexico, and some is imported
by United States curio shops. In 1936 the
technique spread to Tirindaro, when daughters
of a Santa Fé potter married into Tuirindaro
families. The most common modern household
pottery is the Red ware, either glazed or polished,
made in Tzintzuntzan, Hudnsito, San José, and
Patamban. Before being fired the large pieces,
such as ollas and cdntaros, are usually slipped
with a red clay solution and then burnished
with iron pyrites. A handsomely polished surface,
similar to that of the pre-Conquest wares, results
after firing. (Such ware is fired only once.)
Smaller pieces are often glazed with litharge.
Glazed pieces are fired twice, the litharge being
applied after the first firing and the glazed surface
appearing after the second. Designs are often
painted in white (tierra blanca) and black (terra
de hormigén). Red ware is carried as far as Guadal-
137 See Foster (1948) for a detailed description of the mold technique used
by the potters of Tzintzuntzan.
138 To produce the green color, pulverized copper oxide (cobre quemado) and
yellow flinty quartz (pedernal) are added to the lead oxide (litharge) solution,
which is applied to the pottery before firing. A black glaze is also made by
adding a mineral called tierra de hormiga and pedernal to the litharge.
64 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
ajara, Morelia, the tierra caliente of Guerrero, and
Mexico City.
Another type of ceramic industry is represented
by the clay toy figurines made by the women of
Ocumicho in their spare time. The hollow figures
are formed with molds in shapes of diminutive
horses, sheep, oxen, and men, each with an open-
ing which serves as a whistle. After firmg, they
are painted and varnished. Owing to complete
lack of water near the town in the dry season, this
activity is carried on only during the rains.
Ocumicho figurines are seen in markets in many
parts of western Mexico and the tierra caliente of
Guerrero and Michoacan.
Red clay tiles, which are slowly replacing
shakes in the Tarascan area, are made in some
pueblos within the clay belt on the margins of the
Sierra. Tanaco is the sole town within the Sierra
proper to make this product. In Nahuatzen the
technique of making flat concrete tiles was intro-
duced in 1944. Such tiles are replacing the less
durable clay ones in some mestizo towns.
TEXTILES
In 35 modern Tarascan villages spinning and
weaving of cotton, wool, or agave fiber are
carried on as cottage industries. Both indigenous
and European techniques are employed, neither
having changed since the 16th century. Since the
beginning of the present century, however, factory-
made textiles from large Mexican towns have
begun to displace some home-woven articles, but
indigenous conservatism still supports the native
handicraft.
Spinning.—Formerly Tarascan weavers spun
raw cotton from the tierra caliente, but at present
commercial cotton thread, purchased in mestizo
markets, is prepared for weaving by twisting five
to six strands on the spinning wheel. Today only
raw wool and agave fiber are homespun, the latter
with the native malacate (uipinu), or hand
spindle with round clay wheel, the former with the
16th century spinning wheel (lorno). (See Beals,
1946, p. 36, for illustration of spinning wheel.)
Both cotton thread and spun wool are usually
colored locally with aniline dyes purchased in
mestizo markets. .
Weaving.—Tarascans weave all agave and
cotton fabrics on the native belt loom (patakua
(Paracho); jopdsatakua (Charapan, Tarecuato)),
a horizontal loom which has a backstrap and is
found in most parts of indigenous America south
of the United States (pl. 11). Customarily, only
women operate this loom; however, in Tarecuato
agave fiber is woven with it by both men and
women, and in Tanaco, exclusively by men.
Until the 1880’s the most important fabric made
with the belt loom was the cotton manta, a simple
white cloth used for native clothing since pre-
Conquest days. The cheap factory-made cottons
of Puebla and Veracruz have completely displaced
the indigenous manta, so that today Tarascans
weave women’s and men’s belts (fajas), shawls
(rebozos), aprons (delanteras), tablecloths and
napkins (servilletas). Widths of cloth ranging
from 1% inches (women’s belts) to more than a
yard (rebozos) can be woven on these looms.
Designs are usually woven into the above-named
articles, the warp threads being first arranged for
large widths on a long stick (Sekudérakua) and for
the narrow fajas on the Sekudni, an arrangement
of four to five small sticks placed in the ground.
Some of the finest examples of cotton weaving are
found in the Sierra pueblos: Paracho (whose
women make the Tarascan ‘‘rebozo corriente’’),
Ahufran (women’s belts), Angahuan (women’s
belts, aprons, rebozos), Charapan (belts, aprons,
tablecloths), San Lorenzo (tablecloths, belts).
In the early colonial period the weaving of agave
fiber was apparently widespread in the Sierra
(AGN Congregaciones, f. 14), but today it is limited
to Tarecuato and Tanaco. In these villages the
main agave fiber products are morrales (square
bag with shoulder straps), ayates (coarse piece for
wrapping articles to be carried on back), and
costales (coarsely woven sacks for carrying goods
on mules and burros). The fiber of maguey bruto
(akaémba t'aaimiti) is used for the finely woven
morrales, while that of maguey del toro (torakaémba)
is employed for the coarser ayates and costales.
Leaves of the agave plant are cut and the fiber
extracted and carded. After drying, it is spun by
(1) rolling fibers on the thigh with the band, or
(2) with the malacate. The fibers are woven on
the belt loom in the same fashion as cotton’
(pl. 11). A piece of the agave fabric is doubled
over and sewn on the sides to make the morral,
and a shoulder cord is added. Other agave fiber
products made in Tarecuato include rope and
139 Agave fiber products were manufactured in Pichdtaro during the last
century (AAM, siglo XIX, leg. 707).
40 The loom for weaving agave fiber is called u4natakua in Tarecuato.
CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST 65
cord; these and the woven articles are marketed
in Guanajuato, Jalisco, the tierra caliente, and in
all parts of the present Tarascan area.
Woolen products are woven mainly on the
European loom, which was introduced early in
the 16th century." During most of the colonial
period this loom was used principally in the
obrajes, or cloth mills established by Spaniards in
various parts of Mexico near an abundant supply
of wool. Indians first learned European weaving
techniques in these mills, the labor for which
came from surrounding native pueblos. By 1540
an obraje, operated by 26 forced native workers,
had been set up in Acdmbaro (Paso y Troncoso,
1905, vol. 1, p. 33), and before the close of the
century woolen mills existed in Taximaroa and
Valladolid (Zavala and Castello, 1939-46, vol. 6,
p. 225). Moreover, Indians quickly learned to
spin wool, for tributes of spun wool were exacted
from some pueblos, possibly to supply obrajes
nearby.” It is not clear when the Tarascans
began to use the hand loom in their own villages;
possibly some looms were set up in the northern
towns in the 16th century.'® A report of 1789
(AGN Historia, vol. 73) on the Tarascan pueblos
of Lake Patzcuaro and the Sierra, however, men-
tions the use only of the native loom. The first
indication of a native wool industry in the Taras-
can area comes from the Martinez de Lejarza
report of 1822, which cites the obrajeros of San
Juan Parangaricutiro (later the most renowned
of the Tarascan blanket-weaving towns) and of
several northern mestizo towns.'* Tarascan wool
weaving on a commercial scale may be post-
colonial, having little economic basis until the
break-down of the large woolen mills at the close
of the colonial period. Today woolen blankets
(cobijas, serapes) are made on the European hand
loom in 24 Tarascan towns, Nahuatzen and pre-
volcano Parangaricutiro being the largest pro-
141 Strands of wool are sometimes mixed with cotton in making women’s
belts. Often the warp is of woolen strands, the woof of cotton thread.
142 For example, ea. 1540 the people of Purudndiro (Michoacin) contributed
each week two arrobas of spun wool (Paso y Troncoso, 1905, vol. 1, p. 117).
43 The Relacion de Chilchota (Mus. Nac.) states that some natives in
the town made clothes of wool, but the type of loom used is not given. More-
over, according to the Relacion de Cuitzeo (Mus. Nac.), the Indians living
around the lake “‘. . . benden lana a los conmarcanos para hacer ropa para
vestirse, y sus mugeres la benefician...’’ Again, the type of loom used to
weave wool is not given.
“4The northern towns mentioned: Morelia, Zinapécuaro, Zitécuaro,
Taximaroa, Jiquilpan, Huarachita, La Piedad, Huaniqueo, and Tanga-
mandapio. At that time the latter pueblo was wholly Tarascan; according
to Martinez de Lejarza (1824, p. 227), “‘. . . sus habitantes trabajan telares de
algodén y lana.’”
ducers. In many towns only three of four
obrajeros operate full time and produce mainly
for local consumption. Raw wool is purchased
locally, is washed, carded, dried, and spun by the
obrajero. In addition to manufacturing blankets,
some weavers in Nahuatzen, Charapan, and
Tanaco make woolen cloth for the traditional
black skirt, which is still worn by most Tarascan
women. Such skirts, however, are being made
increasingly from factory-woven woolens pur-
chased in mestizo towns.
Embroidery and sewing.—In the Sierra villages
of San Lorenzo, Tarecuato, Angahuan, Ahuiran,
Cuanajo, Nahuatzen, and Charapan some women
specialize in cross-stitching and embroidering
designs on blouses (huzpiles), napkins, and table-
cloths. Many of these articles are for tourist
trade in Uruapan, Zamora, and Patzcuaro.
During the colonial period and the first half of the
19th century, the men and women of Ahuiran
and Pomacuarda knitted men’s stockings of cotton
thread, using otate needles (AGN Historia, vol. 73,
f. 344; Martinez de Lejarza, 1824, pp. 179-180).
Ahuiran stockings were sold to mestizos and
Spaniards over a wide area, but this trade declined
after the change in styles of men’s clothing in
the early 1800’s.
Hat making.—Among the Tarascans this indus-
try was introduced probably in early colonial
days.“ However, the first mention of the in-
dustry comes from the report of 1789, which cites
it in Nurio (AGN Historia, vol. 73, f. 348).
There, hats were made of wool, likely by a felting
process, but the industry had disappeared by the
end of the last century. None of the colonial
sources mentions the manufacture of straw hats
in Tarascan towns. Old men from Pichataro
remember hat making during their childhood,
which fact at least dates the industry in the last
half of the 19th century. (Palm-leaf hats were
made in Morelia at the end of the colonial period,
according to Martinez de Lejarza, 1824, p. 29.)
Today hats (principally of palm leaf, some of
wheat straw) are made in seven Tarascan towns,
Jaracuaro Island being the main center.’ Palm
leaf brought up from the tierra caliente is cut in
thin sections, which are braided into strips, called
48 According to tradition, hat making was one of the many industries
which Don Vasco de Quiroga taught the natives. (Leon, 1904, p. 63.)
448 At least one member (and often three or four) ofevery family on Jaracuaro
Island makes hats. Having little tillable land, this pueblo is one of the most
specialized home-industry towns in the Tarascan area.
66 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
trensas. In practically every Tarascan pueblo
women, children, and sometimes men weave
trensas in their spare time, while walking to and
from market, and while herding sheep. Braids
are sold in the main markets, where they are
purchased by hat makers. Little wheat straw is
now braided, palm leaf being more durable and
more easily handled.” After they are pressed
and straightened with wooden rollers (fashioned
like a clothes wringer), the braids are sewed
together in spiral form, beginning at the crown.
The brim and crown are made separately and
sewed together. In JarAécuaro wooden forms are
used to block crowns. Most hatters employ a
Singer sewing machine, but those of Urapicho,
Pamatécuaro, and Zacén sew by hand. In some
towns hat making is disappearing, owing largely
to factory competition. Pich&taro, formerly an
important hat town, now has but four hatters.
In 1936 the industry disappeared completely in
Tirindaro.
Tule weaving.—The indigenous sleeping mat or
petate (k‘uirakua) is found in most of highland
Mexico. Also, the fire fan or soplador (p‘unita-
tardkua), an indispensable kitchen utensil, is
woven of tule. Mats and fire fans are made
wherever tule is available—along the shores of
shallow lakes, marshy areas, and river banks.
Consequently, the villagers living around Lake
Patzcuaro are the chief tule weavers in the
present Tarascan area (map 20; pl. 12). In San
Andrés 90 percent of the werking population
make petates. Even a few families in the Sierra
towns of Pichaétaro and Cherdn fabricate mats
from tule reeds imported from Erongaricuaro.
Formerly the towns near the northern march
districts were important petate producers, but
there the industry has greatly declined with the
desiccation of wet areas and disappearance of the
tule brakes.“8 Tule is likewise being depleted
along the shores of Lake Pitzcuaro. The peta-
teros of Pudcuaro, Napizaro, and Uricho import
reeds from Jardcuaro Island, the local supply
having been exhausted years ago.
Tule reeds are cut with the sickle, semidried,
and bundled for transport or storage (pl. 8). In
447 Hats of wheat straw are now made only in Pamataécuaro, Teremedo, and
Apo (mestizo).
148 A few petates are still made in Tarascan Tarejero, on the border of the
former Zacapu marshes; in mestizo Ettcuaro (Tangancicuaro Basin); and in
TacAtzcuaro (near the Cotija graben lakes). Moreover, the industry is still
carried on in some of the Lerma Delta towns east of Lake Chapala, and in
a few villages around Lake Cuitzeo.
the Lake area a twilled technique is used in mat
making, which is performed on the ground, the
only tools being a knife or sharp stone to cut tule
stalks and a wooden mallet to flatten the reeds as
they are twilled. Several sizes of mats are made;
the largest, called simply k‘ufrakua-k‘éri, meas-
ures 1.5 by 1 m.“° Both mats and fire fans are
taken to the Lake markets (Patzcuaro, Erongari-
cuaro, Quiroga), where they are purchased by the
Sierra people and buyers from the tierra caliente.
Basketry.—Ihuatzio and San Jerénimo in the
Lake area are the only modern Tarascan towns in
which baskets are made. The former Tarascan
towns of Tangamandapio (west of Zamora) and
Panindicuaro (north of Zacapu) are the main
basket centers in the general area, supplying the
Sierra people with the Sindiéa, or harvest baskets
for maize. The Ihuatzio baskets are made of
split carrizo stalks, which grow in abundance in
local house lots. Both wicker and twilling tech-
niques are used (pl. 12).
Netting.—In all fishing villages around Lake
P&tzcuaro nets are made by men, women, and
children in their spare time. On Janitzio and the
Urandén Islands a few professional rederos fabri-
cate nets to sell to fishers in other pueblos. Cotton
thread purchased in P&tzcuaro is wound on the
hilador (Soréranskua) and five to six strands are
twisted with the native malacate or with the
European spinning wheel. The twisted strands
are water-soaked and sun-dried. Nets are made
with the éurikua, a large wooden needle (20 cm.
long, 2 em. wide).
Capote making.—In many parts of indigenous
Mexico the palm-leaf raincape (capote), similar to
those worn in the Orient, is a common outdoor
apparel during the wet season. Capotes are made
by women in three Tarascan towns—Quinceo,
Arantepacua, and Turicuaro—using leaves of the
palma pimu (Acoelorraphe pimo), which are im-
ported from the tierra caliente below Ario de
Rosales..° The capes are fabricated by tying
soaked strips of palm leaf onto braided cords, two
of which are stretched parallel and one foot apart
on pegs driven into the ground. The strips of
140 Other types: The k‘amériéa (1.3 m.X80 em.) and the ¢im4nitepémueta
(1 m.X50 em.), both used for sleeping; the jatapetakua, a small knee mat;
idstitan, a long, narrow mat sold to mestizos as a sort of rug. Many more
sizes and varieties occur, the names and types varying from place to place.
The terms and types given above were observed in Ihuatzio and some of the
ranchos along the shore of the Taasfu-k‘éri Peninsula.
180 Most of the palm leaves used in Arantepacua are said to come from the
localities of Rosario, La Playa, Charapendo, and San Marcos, south of Ario,
102°30'
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Map 20.—Distribution of handicrafts in the Modern Tarascan area.
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CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST 67
palm are tied on one cord, half-hitched to the
second one, and then tied back to the first; the
loose end of the strip is permitted to hang over
the second cord, thus forming a drainage surface
similar to thatch (pl. 12). The process is re-
peated, adding a new row of tied strips to the prev-
ious one until the garment (4 ft. long and 3 ft.
wide) is completed. Arantepacua capotes are
marketed as far north as Guanajuato. No men-
tion is made of these raincapes in the colonial
sources, nor is there a Tarascan word for the gar-
ment. It is not improbable that the capote is an
introduced trait.
Broommaking.—This is another minor industry
now practiced by a few men in Arantepacua.
Pimu palm leaves are symmetrically arranged
around the end of a finished pine stick and then
tied with agave fiber or a braided strip of palm.
The result is a common broom found in all parts
of central Mexico.
WOODCRAFT
According to the early Spanish chroniclers, the
Tarascans were clever craftsmen in wood, and
under the instruction of Spanish masters the
natives became among the best carpenters in
New Spain (La Rea, 1945, p. 20; Escobar, 1924,
p. 147). By 1580 Indian carpenters in at least
four towns—Pitzcuaro, Necotlin (Undameo),
Tiripitio, and Tingiiindin—were turning out
European-styled tables, chairs, and writing desks,
which found ready sale among Spanish colonists in
all parts of Michoacén.%= At that time lathework
was established in Paitzcuaro, and probably before
1540 Tarascans had begun to carve saddle frames
for Spanish horsemen (Molotinia, 1903, p. 183).
Like other Tarascan industries, woodwork was
probably a rudimentary pre-Conquest craft greatly
modified and improved by European techniques.
However, the present commercial types of Taras-
can woodwork—cabinet work, lathe work, and adz
work—all appear to have been developed in the
16th century.
Specialized woodwork (apart from lumbering
and shake making) was formerly more widespread
among Tarascans than at present. At the end of
the 18th century wood objects were manufactured
in 21 pueblos (AGN Historia, vol. 73), today in
only 13 towns. In but eight of the latter is the
“tia Rel. de PAtzcuaro, 1581 (Martinez, 1889, p. 47); Mus. Nac., leg. 102:
Rel. de Chocandiran, Rel. de Necotlin; Rel. de Tiripitio, ms. (in Garcia
Library, Univ. of Texas).
industry more than 150 years old; in only five of
the present towns do more than 25 percent of the
working population engage in woodwork.
Adz work.—This is the simplest of the wood
techniques now practiced by Tarascans (and by
other Indian groups, as well as by mestizos in
many parts of Mexico). Before the Conquest
the Indians shaped boats from a single log and
carved delicate figures on throwing sticks and
tom-toms, possibly using obsidian and copper
cutting tools. With the introduction of the
European steel adz and gouge early in the 16th
century, native wood carving was greatly facili-
tated. One of the earliest European objects
which the Tarascans carved with the adz was the
saddle frame (fuste), an industry which disap-
peared 100 years ago. Today wooden spoons
and bowls (bateas) of softwoods are the principal
adz and gouge products, Pamatdcuaro and its
offspring settlements Sirio and San Benito being
the chief producers.! These objects are also
made in the Tarascan villages of Turicuaro,
Cumachuén, Pichataro, Zirosto (formerly impor-
tant) and Sevina (where the industry was intro-
duced a few years ago), and in the mestizo towns
of Patzcuaro, Técuaro, Zirahuén, Uruapan, Qui-
roga. Spoons and bowls are made from softwoods:
jaboneillo (Sa4pu), palo blano (urapit-tku), and
aile (pamu). Occasionally bateas are made of
pine. Tools include the common adz and vari-
ously shaped gouges, which are driven with a
wooden mallet (pl. 13). The products of Pama-
tacuaro and surrounding settlements are marketed
in all parts of Michoacan and sometimes are
taken as far as Guadalajara and Mexico City.
Lathe work.—This represents one of the most
characteristic forms of modern Tarascan wood-
craft, Paracho being the center of the torneros.
Formerly the simple bow lathe was employed to
make bowls, vases, candlesticks, chocolate beaters
(molinillos), chessmen, toys (tops, yoyos), darning
eggs, etc. (See Beals, 1946, p. 43, for illustration
of bow lathe.) Since 1942, however, when a
power line was constructed near the town, most
of the bows have been replaced by electrically
powered lathes. About six torneros in Paracho
and five in neighboring Ahuiran still use the bow.
Formerly turned objects, chiefly rosaries, choco-
151 It is doubtful that wooden bateas were carved before the Spanish Con-
quest. Gourds of Crescentia alata probably functioned for the modern batea.
The “‘bateas’’? employed in early Spanish gold placering in the téerra caliente
were likely fashioned from Crescentia gourds.
68 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
late beaters, and malacates, were made in Charapan
and Cocucho, but this activity has now disap-
peared. Most of the turned objects are shaped
from madrofo wood (pandyksa). Carving is
done by pressing variously shaped steel chisels
and gouges against the whirling block of wood.
In Paracho, designs are painted and burned into
objects, and the surface lacquered or varnished.
The wheel lathe, an early Spanish introduction, is
used by most cabinetmakers in the area for
turning wood.
Cabinet work.—As mentioned earlier, cabinet
work was rapidly adopted by Tarascan craftsmen
in the early colonial period. In the 17th and 18th
centuries inventories of miners’ and merchants’
household goods in west-central and northern
Mexico rarely fail to mention chairs, tables, boxes
“de Mechoacan.”’ The majority of present Taras-
can towns has at least one cabinetmaker who
partially satisfies local demand for furniture. In
Paracho, Corupo, and Cuanajo—the Tarascan
furniture centers—carpenters make chairs, tables,
bed frames. Cuanajo is famed for its wooden
chests, which are marketed in all parts of Michoa-
cin. Most furniture is made from pine wood with
simple tools (saw, mallet, plane, chisel, gouge).
As mentioned above, chair and table legs are
turned on the wheel lathe (fig. 6). The more
common jointing techniques used include mor-
fp.
ES
Figure 6.—The wheel lathe, used by most Tarascan cabinetmakers for turning wood.
ticing and tenoning, housing, and dovetailing.
Some pieces are joined with wooden pegs; metallic
nails and screws are never employed.
Musical instruments.—The most sophisticated
of Tarascan woodwork is the manufacture of
stringed instruments in Paracho. This pueblo
has been the guitar towr of Mexico since colonial
times. In 1940 Paracho claimed 49 guitar makers
and three individuals who made violins (including
base viols). The art has spread to neighboring
Ahufran, where three men made violins in 1946.
Local woods—¢irimu, qaile, and palo blanco—are
used for the top and base of the guitars; for sides
and handles and inlaid designs walnut and cedar
are imported from Mexico. Some guitarreros
utilize local pine and fir for the tops of violins and
base viols. The wood is cut with a small saw
and planed to desired thinness. The top and
base are cut from a pattern; the side bands are
soaked and bent into place, being glued to the top
and bottom pieces and held in place with braces.
Strings and metal parts are assembled, and the
instrument is varnished and waxed, ready for the
ultimate consumer. Most guitarreros work on a
contract basis for Mexico City or Guadalajara
buyers, and many Tarascans have moved their
trade to the larger towns, mainly Mexico City,
where their products bring higher prices.
The age of the Paracho guitar work is not known.
The wheel ranges from 2% to 4
feet in diameter and is usually turned by a small boy.
CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST 69
1s first mentioned as an established industry in
the report of 1789 (AGN Historia, vol. 73, f. 344),
indicating that it had been introduced for some
time.
LACQUER WORK
Modern lacquerwork in Michoacén is closely
associated with wood carved with the adz and
lathe. Before the Spanish Conquest various
gourds (Lagenaria, Cucurbita, and Crescentia)
were lacquered with a varnish made from the
insect axin (Coccus axin) and chia (Salvia sp.)
This industry probably centered in the Balsas and
Tepalcatepec Basins (Brand, 1944, p. 60) and was
extended into the towns near the southern edge of
the Sierra, e. g., Peribin and Uruapan. After the
introduction of Spanish adz work during the co-
lonial period, lacquer was applied to wooden bateas
im Peribin, Zirosto, Zacin, Uruapan, and Patz-
cuaro. Bateas were painted, but not lacquered,
in Cucupao (Quiroga) and Santa Fé de la Laguna.
Today few Tarascans practice the art, the famous
bateas of Uruapan being lacquered by mestizos.
Some of the turned vases and bowls of Paracho
are finished with tung oil and synthetic lacquer
purchased in mestizo markets.
LEATHERCRAFT
Probably one of the first native Tarascan crafts
stimulated and expanded by the early Spaniards
was leatherwork. With the introduction of cattle,
Tarascan tanners were able to multiply leather
production, which formerly had been based on
deerskin, to meet the heavy Spanish demand for
saddles, halters, shoes (the famous ‘‘zapatos de
baqueta de mechoacdn’’).** Tanning was done with
local oak bark, as it is today (AGN Tierras, vol.
83, exped. 13). During the colonial period leather-
crafts were centered in the northern Tarascan
towns near the pastures and hide supply, and in
a few pueblos of the Sierra. The latter included
Cheran, Cherandtzicurin, Ocumicho, and Nahuat-
zen, which was one of the largest tanning centers
182 Fray Toribio de Molotin{a’s statement of 1540 on the Tarascan leather
industry is revealing: ‘‘Han deprendido a cutir corambres . . . son buenos
zapateros, que hacen zapatos y servillas [slippers], borceguias [high shoes],
pantaflos, chapines [wooden shoes with leather straps] de mugeres; . . . este
oficio comenzdé en Michoacan, porque alli se curten los buenos cueros de venados.
Hacen todo lo que es menester para una silla ginete bastos y fuste, coraza y sobre-
corazas. . .” (Motolinfa, 1903, p. 183). According to the Relacién de Micho-
acdn (p. 16) “‘cotares de cuero,”’ or leather sandals, were made for the caltzontzin
in pre-Conquest times.
in the Tarascan area.’ By the latter part of the
19th century leathererafts began to decline, and
today within the Tarascan area only Nahuatzen
(largely mestizo) continues to tan hides and make
saddles and other riding equipment. Some
Tarascan towns now boast of one or two zapateros
who make huaraches of imported leather for local
consumption. The principal huarache-making
centers are now the surrounding mestizo towns:
Coeneo, Zacapu, Tinguindin, Los Reyes, Uruapan,
Ario de Rosales.
METALCRAFT
Copper work.—The Tarascans were probably
the foremost metallurgists in pre-Columbian
Mexico. They worked gold, silver, and copper.
The precious metals were formed into ornaments
and disks, which the caitzontzin stored on the
islands in Lake Patzcuaro; useful objects, such
as axes, coas, and spearheads, were made of
copper (Relacién de Michoacdén, pp. 104-109,
122-123). Although definite archeological evi-
dence is not yet at hand, it is probable that the
Tarascans purified native copper and extracted
metal from simple oxide ores by smelting (Hend-
richs, 1940, p. 327). From cursory inspection
of copper artifacts extant in the Museo Regional
Michoacano, Morelia, it appears that Tarascans
cast copper objects (axheads) in stone molds.
After casting, the axes seem to have been further
shaped and possibly hardened by hammering.'*®
Accidental, rather than deliberate, alloying with
tin and zine probably occurred.
The Tepalcatepec and Balsas Basins contained
the ancient copper mines and metallurgical sites.
Hendrichs (1940, 1945-46) has described several
probable ancient copper mines sites in both the
18 AGN Tierras, vol. 83, exped. 13; Zavala and Castello, 1939-46, vol. 7,
pp. 361-362; AGN Historia, vol. 73, ff. 178-179. The present northern Taras-
can towns of Zipiajo, Azajo, Companja, Tatejero, Tirindaro, Naranja, and
Teremendo were all producers of shoes and saddles in the latter part of the
18th and in the 19th century.
184 Beals (1946, p. 44) states that in 1940 one person from Aranza was tanning
hides in Cherin. The old men of Ocumicho remember the manufacture of
the black “‘zapatos de raquetas’”’ in their town during the last century. These
were sold throughout the Sierra as well as in surrounding mestizo towns.
185 The Lienzo de Jucutacato, a 16th-century representation of the migra-
tion of a people from the Gulf of Mexico into the Tarascan country (where
they learned metallurgy) clearly depicts smelting of ore or metal (probably
copper) apparently with the aid of charcoal and forced air draft (blowpipes)
at the ancient copper center of Jicalén (Jicalin Viejo), 20 km. south of Urua-
pan.
18 Microanalysis of Tarascan copperware has not yet been undertaken.
Until the results of such analyses are known, it is impossible to make definite
statements as to ancient metallurgical methods. Interestingly, the flange
shape of the modern Tarascan steel axhead is identical with that of the copper
axes found in archeological sites in the Balsas Basin.
70 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7
southern and northern drainages of the lower
Balsas (Guerrero). However, the mines of
Inguardn in the northern drainage of the lower
Balsas in Michoacdin were the main source of the
metal. Smaller deposits, such as those of Sinagua,
were gophered over a wide area. The villages
of La Huacana, Jicalin, Sinagua, and possibly
Tzatzio appear to have been the chief pre-Colum-
bian copper refining centers.'”
Needing copper for the manufacture of brass
cannon, the Spaniards quickly levied tribute in
copper bars on various pueblos in the Balsas and
Tepalcatepec Basins. Later, adventurers (in the
name of the Crown) took over the native mines
at Inguard4n, probably introducing European
smelting techniques. The main 16th-century
Spanish smelting and refining center was Tzatzio,
10 miles each of Ario. This center was located
within pine and oak forests, which afforded raw
materials for charcoal, and was near the chief
highway from P&tzcuaro to the tierra caliente.
Copper ore and probably native copper was car-
ried by Indians to Tzatzio from the Inguardn
mines, which lay 15 miles to the south (AGN
General de Parte, vol. 5, ff. 311-313, 1601).
Tzatzio was probably an ancient copper center,
and the experienced Tarascan metallurgists were
retained by the Spaniards to continue with Euro-
pean methods. Before the end of the 16th century
the Spanish Crown had established an asiento
in the Michoacéin copper industry, in order to
insure a steady supply of metal for the foun-
daries in Mexico City.! Between 1607 and 1614
187 The Suma de Visitas, ca. 1540, state that the Spaniards exacted tribute
of copper bars from La Huacana and Jicalén (Paso y Troncoso, 1905, vol. 1,
pp. 123, 294). Moreover, every 20 days 20 Indians of Coyuca carried copper
bars to Mexico (ibid., p. 80). Coyuca, located near the confluence of the
Balsas and Cutzamala Rivers, may have been a collecting point for small lots
of copper refined in various pueblos of the middle Balsas drainage. At the
end of the 16th century copper was still being mined, refined, and made into
tools at Sinagua (Mus. Nac., leg. 102, Rel. de Cinguacingo). Tzatzio was one
of the first Spanish copper smelting centers in the area, and was probably
an old Tarascan center as well (AGI Aud. de México, leg. 258). In passing, it
should be noted that the old La Huacana was located near the Inguar4n
mines. In 1759 the town was destroyed by the eruption of Jorullo, and a new
settlement, the La Huacana seen on modern maps, was established near
Tamacuaro 15 miles west of the old site (AGN Historia, vol. 73, ff. 392-394)
188 Under the asiento, or contract, system, control of various industries was
farmed out to private individuals. In the ease of the copper industry of
Michoacin, administrative control was purchased from the Crown for 6-year
periods. The administrator was obliged to furnish the Government a stipu-
lated amount of copper annually at a fixed price. In 1599 an official survey
was made of the copper industry in Michoacin. The surveyor recommended
that owing to forest depletion around Tzatzio and the consequent difficulty
in charcoal supply, refining operations should be moved to Ario, near abun-
dant pine forests (AGI Aud. de Mexico, leg. 258). It is doubtful that this
move was made, since in 1607 copper was still being refined at Tzatzio (Zavala
and Castello, 1939-46, vol. 6, p. 166).
official copper refining operations had shifted 20
miles northward to Santa Clara (Villa Escalante),
which has remained the copper center of Michoa-
cin to this day (AGN Mineria, vol. 22, exped. 3).
In addition to copper bars for the royal artillery,
the colonial administrators established the manu-
facture of caldrons and other copper vessels,
which they sold to all parts of New Spain (AGN
Historia, vol. 73, ff. 389).1 Colonial copper
production, however, was not limited to the royal
refineries at Santa Clara, for as late as 1789
braziers were still being made by native copper-
smiths at Jicalén (AGN Historia, vol. 73, f. 366).
Moreover, some copperwork was done in Pa&tz-
cuaro throughout the colonial period.!
Today the sole survivors of the former Tarascan
copper industry are some 30 mestizo copper-
smiths in Santa Clara, where the renowned casos
(caldrons), vases, and bowls are still manufac-
tured. Ore or native copper is no longer refined;
instead, scrap copper is purchased, melted down,
and cast in earthen molds. Sixteenth-century
hand bellows are still used to force an air draft;
charcoal is employed for fuel. The cast vessel is
finished and hardened by alternate annealing and
hammering.
Ironworking.—With its concomitant tools (bel-
lows, hammers, anvils, tongs, etc.), ironworking
was introduced into Tarascan economy early in
the 16th century. Curiously, one Sierra village,
San Felipe de los Herreros, became the foremost
ironworking center of Michoacén during the
colonial period and the early 19th century. In
1644 bridle bits, spurs, locks and keys were
fashioned and marketed in surrounding Spanish
and mestizo towns (Basalenque, 1886, vol. 1,
p. 467). As late as 1851, 68 families (practically
the entire town) were professional smiths, supply-
ing the countryside with plow tips, hoe blades,
axheads, woodworking tools, etc. In 1946 three
169 During the 17th century Tarascans from all parts of Michoacin were
forced to work in the Inguara4n mines and the fwndiciones at Santa Clara.
Most of the fundidores came from the tierra caliente and from the tierra fria
towns of Zirosto and Patzcuaro (Zavala and Castello, 1939-46, vol. 6, p. 166;
vol. 7, p. 240). In 1789 there were 8 copper refineries at Santa Clara, each
operated by 30 to 40 men (AGN Historia, vol. 73, f. 389).
160 The Relacién de Patzcuaro of 1581 (p. 47) mentions “‘herreros y calderos.””
Basalenque (1886, vol. 1, p. 451), writing in 1644, states that copper bells were
made in Patzcuaro. As late as 1862 (Romero (1862, p. 7) writes of PAtzcuaro
coppersmiths, who were refining ore from Inguarén and Churumuco. Several
new copper deposits in Michoacan were exploited during the last quarter of
the 18th century, e. g., the mines of Apupato, near the old site of Urecho
(AGN Historia, vol. 73, f. 888) and those of Chirangangueo, near Tusantla,
south of Zitacuaro (AGN Mineria, vol. 62, exped. 1; Martinez de Lejarza,
1824, p. 92).
CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST al
old smiths, who work at their trade only part
time, represented the remnant of a once thriving
home industry.
The former source of metal for the San Felipe
smiths is problematical. According to a local
informant, during the 1880’s ‘“‘planchas de hierro”’
were brought in from Cotija, a muleteer and trade
center having close connections with the tierra
caliente and the Sierra of Guerrero. This infor-
mation points to Coalcomén in the Sierra Madre
del Sur of Guerrero as the principal source of
iron. Other ironworking towns of Michoacan
include Irimbo and Nahuatzen. Mestizos in the
latter pueblo fashion knives and machetes.
STONECUTTING
Stonework among modern Tarascans is limited
to approximately 12 metate makers in Turfcuaro.
Formerly this village was noted throughout
Michoacdn for the high-quality metates (iaudn),
manos (poaékua), and molcajetes (Stiimatakua)
carved from a fine-grained andesite (¢akaépu
amiakiti, or “good stone”), found near the summit
of the composite voleano Kandkuarani (Cerro de
la Corona) nearby. Since the introduction (ca.
1925) of the engine-powered nixtamal mills in
mestizo and larger indigenous towns, demand tor
new metates has sharply declined.!®
Metates and molcajetes are roughly shaped at
the quarry on Kandkuardni and are carried down
to the pueblo on burro for finishing in the stone-
cutter’s house. Stone is worked with steel tools,
e. g. the pick (pikua) and sledge hammer (pikua-
k‘éri), and is finished with a polishing stone (jand-
mu). Several sizes of metates are made and sold to
traveling merchants who pass through the town.
TRADE AND TRANSPORT
The structure of trade among the Tarascans is
not dissimilar to that of most Indian groups of
central Mexico. Although every settlement has
at least one store where general merchandise can
be purchased, most trading is done at the tianguis,
or market, held regularly in the larger towns.
Throughout the area professional traders—huaca-
leros (who carry merchandise on their backs),
arrieros (who haul products on the backs of
burros), and lately, wholesale buyers from the
16t According to local informants, in 1912 practically every family in the
village made metates. Since that time most of the villagers have turned to
woodwork (mainly bateas).
large mestizo towns (who ride in trucks and
busses) —all serve as distributing agents.
The market (uasajpikuagu, or ‘‘the place where
people sit’’).—Sunday is the most important
market day for the Tarascans.'” Large groups of
Indians from neighboring pueblos flock to the
regular markets held in the large mestizo towns
within or on the edge of the Tarascan area. Since
colonial times Paracho has been the largest
Indian commercial center of the Sierra. To the
south Los Reyes and Uruapan are the exchange
centers for tierra caliente and tierra fria mer-
chandise."* A lesser number of Indians attend
the northern market towns: Zamora, Tingiiindin,
Purépero, Zacapu, and Chilchota (the commercial
center for the La Cafada pueblos). Generally
speaking, each large Sunday market draws upon
a certain Indian area defined by a walking or
riding distance of one day or less (map 21). On
occasion, however, the Pétzcuaro or Uruapan
tianguis is visited by Indians who live more than
1 day’s travel away. In the Sierra often the
entire family attends the regular market, leaving
Saturday with handicrafts or farm products
(usually fruit, chickens, or eggs) packed on
burros, and arriving at the plaza at night.!*
Sunday morning is a time of brisk trading. By
afternoon most of the traders have sold their
wares, purchased supplies, and have departed for
their respective pueblos. The Lake Patzcuaro
fishers got to market in boats, carrying fish and
vegetables to Patzcuaro, Erongaricuaro, and
Quiroga to trade for maize, wheat, and firewood.
Lesser markets are regularly held in a few
smaller Indian towns. For example, there is
a Sunday market at Charapan, attended by
people from Cocucho, Urapicho, Corupo, San
Felipe, and Nurio. On Saturdays and Mondays
there is some commercial activity in Cheran, as
professional traders pass tbrough the town going
to and coming from the Sunday Uruapan market
(Beals, 1946, p. 80). Again, on Thursdays
182 An important exception is the Pétzcuaro market held on Fridays and
Sundays. A minor fish market occurs also on Tuesdays.
163 Formerly Peribin was one of the largest tierra caliente—tierra fria markets
in Michoacan, but since the close of the colonial era it has ceded most of its
trade to Los Reyesnearby. Important fiesta markets are still held in Periban
however.
164 Within the last 8 years the pueblos along the Uruapan highway have
ridden busses or taxis to market. Since 1943 similar transport has been
extended to Charapan, Zirosto, and intermediate pueblos. Moreover, during
the dry season lumber trucks haul loads of men and women from some Sierra
towns to mestizo markets.
7
INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO
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CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST 13
professional traders gather at Patamban to buy
pottery for the various Sunday markets.
Besides the regular weekly markets, in practi-
eally every village lively trading accompanies the
annual religious or semi-religious celebrations. In
some instances such markets are large enough to
be termed fairs. Commercially, the most im-
portant of the annual fiestas is the pueblo’s saint’s
day, attended by traders and villagers from miles
around. Other fiesta markets occur during the
Corpus Christi, Easter, and Christmas celebra-
tions. Often a particular village, such as San
Juan Parangaricutiro, holds special religious (and
commercial) festivals to honor a special saint or
miraculous event.!®
Trading in the market is done mainly on a
monetary basis. Little outright bartering takes
place. An interesting exception occurs at Erong-
aricuaro, where wives of fishermen exchange
baskets of fresh or dried fish for piles of firewood
carried in from the Sierra. Another instance of
barter takes place at the Patamban market; there,
women from the Pamatdcuaro ranchos trade
tamales for pottery and fruit.
The market takes place in the town plaza, and
when the number of traders is exceptionally large,
some sellers are crowded off into adjoining streets.
Each vendor pays the municipal authorities the
piso de plaza, or tax for the use of a small selling
space on the sidewalk. By custom, stalls are
segregated according to the type of article sold,
pottery being dispensed in one section of the plaza,
foods in another, etc. (pl. 14). (See illustration
of Chilchota market in Beals, 1946, p. 84.) Ex-
cept in special markets, such as Patamban, the
number of merchants of fruit and vegetables ex-
ceeds all others. (See Beals, 1946, p.82.) More-
over, in the large towns professional mestizo
vendors of factory-made clothing, hardware, ete.
are numerous, while the Indians selling handicrafts
are relatively few. The P&tzcuaro, Erongarf-
cuaro, and Paracho markets, on the other hand,
are composed of a much larger percentage of
native traders.
The village stores.—Almost without exception
every Tarascan village boasts of at least one store
165 Of interest are the Palm Sunday (Ramos) fairs held in Periban, Zamora,
Uruapan, and Patzcuaro. Exchange of tierra caliente and tierra fria products
is particularly significant at these markets.
166 At the Ramos fair at Periban (April 14, 1946) at least three-quarters of
the selling space was occupied by tropical fruit vendors and sellers of factory-
which handles mainly staple food imports (salted
dried beef, dried fish, salt, piloncillo, lard, beans,
and wheat flour) and beverages (soft drinks, beer,
and hard liquors). A small assortment of canned
goods can be purchased in the stores of the larger
towns. Often other items, such as cigarettes,
kerosene, and metal household ware, are carried.
In the small villages stores are customarily oper-
ated by well-to-do Tarascan families, often by the
wife and children, while the man farms.'*” In the
large pueblos the storekeepers are usually mestizos
who have moved in from neighboring towns.!®
Significantly, the infiltration of Spanish-speaking
storekeepers into indigenous towns often repre-
sents one of the initial steps toward hispaniciza-
tion of the native population.!”
The professional traders.—The huacalero (in-
spikuuiri, or ‘‘one who trades”) represents the last
vestige of the ancient Indian carriers (tamemes),
formerly important agents of distribution throvgh-
out Mexico. Few such traveling merchants, each
of whom carries his wares in a wooden crate
(huacal, képartakua) tied to his back, remain;
the majority have been displaced by burro and
motor transportation. As late as 1900 large
numbers of Tarascan huacaleros from many
Sierra villages carried handicrafts into the Balsas
Basin, the coast of Guerrero, and Colima and
returned with tropical fruit, salt, and cheese.
Today about 15 huacaleros operate out of Pama-
tacuaro, carrying locally made wooden spoons
and bateas, Patamban pottery, morrales from
made goods from Zamora, Guadalajara, Morelia, and México. Regional
handicrafts were represented as follows:
Article: Origin Vendors (number)
Blankets 222-2 2222 --5-- Gharapan=<_ 27 - ssssae- 10 walking vendors.
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Rebosos: ss. sass 4235 Paracho 1 stall
Women’s belts__--_---- Nahuatzen_--- 1 stall
Strew. hats: 2-:__=-.-<:- IADOs -222c8-s5-
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PLATE 1.—Physical landscape. a, Portion of a Sierra basin near Arantepacua. 6, Southwestern part of Lake Patzcuaro; Jaracuaro Island and newly formed
Pastora Island, upper center. c, Cultivated floor of cinder cone crater near Charapan. d, Lake Patzcuaro, looking northward; note voleanic islands in
middle of lake and the Urandén Islets immediately off shore. e, Mixed pine-oak forest at edge of maize field, Char apan. f, La Canada, looking westward,
or down valley.
PLATE 2.—Water supply and settlement. a, Wooden aqueduct at Pamatacuaro, which brings water from the local spring (center) to the outskirts of town.
», Hoisting water from one ofthe public wellsin Charapan. c, Street in Ihuatzio, Lake Patzcuaro. d, Panorama of San Jeronimo on Lake Patzcuaro, show-
ing compact assemblage of adobe structures. e, Partial view of Zacdn near Paricutin Voleano (background), showing grid street pattern, scattered dwellings,
and large lots. f, Los Conejos (San Juan Nuevo), founded in 1944 to house refugees from destroyed San Juan Parangaricutiro. Nearly all trojes were trans-
ported from old San Juan and reassembled on the new site. g, Street scene, Charapan (Sierra). h, Street scene, Tirindaro, Zacapu Basin. i, Plaza at
Charapan
PLATE 3.—House types. a, Front view of troje from inside house lot, Quinceo. b, Back view of troje from the street, Sicuicho. Notethe plank wall (¢ar¢éakata)
to left of house. c, Elaborately carved door, Charapan. d, Planks housed in L-shaped cornerpiece, Cuanajo. e, Notched plank ladder leading to lofto
troje, Charapan. f, Roofed gate, Sicuicho. g, Trojes at Pamatacuaro. Note rail fences.
=~
PLATE 4.—House types. a, Old log struc ture, Zacin. 6, Old wooden troje, Tirindaro. c, Adobe house at Apo. The floor plan and roof are similar to those
of the plank troje. d, Wooden house at Caltzontzin, the refugee pueblo east of Uruapan. These new structures are North American n appearance,
e, Abandoned adobe two-shed house, San Jeronimo, f, Street scene, San Jeronimo. The house at left with the high verandalike front is often seen in
Lake Patzcuaro towns.
—Maize culture. a, The Egyptian plow, still widely used in Mexico (Nurio). Note straight steel tip (reja) which slips over endpiece of plow
yoke and goad near end of tongue; leather strap used to fasten yoke to horns of oxen. 6, Planting maize near Caltzontzin. The first plow, which opens the
furrow, is followed by two small boys, who drop seeds at regular intervals. The second plow covers the seeds. c, Contour plowing near Cuanajo. Field
of youngmaize. d, Hillof maize and beansin hoe land near Chilchota. Plants are about 1 week old. Newly burned desmonte near Apo. Note wood ash,
which will be mixed with underlying soil. f, Platform on which maize fodder (rastrojo) is stored, An
PLATE 6.—Wheat culture. a, Irrigated wheat fields near Chilcota, La Cafiada. 6, Temporal wheat fields on the northern edge of the Sierra, near Tirindaro.
ec, Method of hauling wheat bundles to the threshing floor, Apo. d, Cutting wheat with the sickle, near Pichataro. ¢, Threshing wheat with flails, Sirio.
f, Threshing wheat in the era with horses, at Comanja. The carreta (right) is used in many parts of Tarasca to haul wheat bundles and maize fodder.
Se
2 Peas. ET
PLATE 7.—Horticulture and domestic animals. a, Large plowed ekudiu, San Felipe. Note anima]pen adjoining froje. b, Small patch of cabbage in house lot,
San Felipe. c, Vines of chayoteineckuaiu, Tanaquillo, La Canada. d, Irrigated vegetable plotsalong west shore of Lake Patzcuaro, near Arocutin. e, Ditch
well and palas (t‘aparatarakueca) used to lift water from ditch to irrigate fields. Near Uricho. /, Sheep grazing in harvested maize field, near Tanaco.
g,Herding sheep near summit of Cerro de Patamban. The flock is from the rancho of Uringuitiro. h, Bee hivesin house lot, Azajo.
cay
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See E i aed
PLATE 9.—Ceramics: Pottery making at Cocucho. a, Vessel being started from’a single daub of clay. The vessel is worked on top of the mouth of a broken
olla. 5, and c, Bottom portion of vessel being shaped. d, Piece of clay being rolled out on board. e¢ and f, Sides of vessel are built up by adding pieces of
rolled clay.
PLATE 10.— Ceramics: Pottery making at Cocucho (continued) gand h, Rolled pieces of clay are worked into sides of vessel. i, Sides of vessel are smoothed
with corncob. jand k, Lip of vessel being shaped. /, The finished olla. The vessel was made in about 25 minutes.
PLATE 11.—Textiles. a, Weaving cotton cloth for aprons on the native belt loom, Charapan. 6, Weaving women’s belts (fajas), Azajo. The belts vary in width
from 114 to3 inches, carry various designs, and each is of several brilliant colors. c, Weaving men’s sashes of white cotton thread, Janitzio, C ari is drying
on the petate, lower right. d, Weaving a mor of agave fiber, Tarecuato. e, Stretching woven pieces of agave fiber, Tarecuato. Each piece is doubled
over to make a morral. /, Weaving agave fiber on the belt loom, Tarecuato. g, Spinning agave fiber witb the malacate, Tarecuato.
7) Pe A
4 Pisgh en oe
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aks aia
PLATE 12.—Textiles. a, A milpa of tule along the shore of Lake Patzcuaro, between San Jer6énimo and San Andrés. Many petate makers own their own milpas,
but sometimes portions of the brakes are leased to tule sellers, who harvest the reeds and distribute them to various villages around the lake. b, Harvesting
tule, Jaracuaro Island, Lake Patzeuaro. After partially drying in the sun, the reeds are bundled into manojas and stz 1in shocks. c, Weaving petates,
Thuatzio. Note the wooden mallet on the mat near the man’s hands. d, Making capotes, Arantepacua. Work is done je the kichen. Note the hearth,
lower left. Palm leaves are kept moist by dipping them in the batea of water at left. e, Embroidering a huipil, or blouse, Tarecuato. f, Baskets woven at
Ihuatzio. The large one (left), called @uite, is used to carry bread and fruit. It is usually transported on the back in the ayate. The flat round basket is
called ¢‘Akiata and is used to carry fish and tamales. The twilled basket is a tlascal (the Tarascans call it ‘‘tascile’’) for tortillas. The handled basket at
the right (simply named ‘‘canasta’’) is for carrying eggs, piloncillo, and often fish.
3.—Woodwork. a, Gouging tools, Pamatacuaro. 6, Wooden spoons and ladles, Pamatacuaro. c, Modern electrically powered lathe shop, Paracho.
urned objects made at Paracho. e, Cabinetmaker’s shop in house lot, Corupo. f, Making molinillos with the bow lathe, Paracho. g, Nest of wooden
boxes, Cuanajo. h, Small (2 feet high) folding chair commonly made in Cuanajo. i, Bateas made at Sirio.
1 ey wears
ao plainer
*LATE 14.—Markets and transport. a, The Sunday firewood and fish market, Erongaricuaro. The wood vendor at left has already bartered a pile of pinesticks
for a few fish in the basket
of burros bringing pimu palm leaves from the tierra
, Pottery section of the Sunday market at Uruapan.
caliente to Ario de Rosales
c, The bread section of the Erongaricuaro market on the plaza. d, A train
e, Boats from Janitzio landing on the mud flats at Erongaricuaro for the
Sunday market. /, Hauling disassembled chairs and tables from Corupo to the Uruapan market
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