viii ie ty Hitiee Reta i) era iat Cornell University Library The original of this book is in the Cornell University Library. There are no known copyright restrictions in the United States on the use of the text. http://www.archive.org/details/cu31924090934773 CORNELL UNIVERSITY LieRaRy DOC 3 1924 090 934 173 In compliance with current copyright law, Cornell University Library produced this replacement volume on paper that meets the ANSI Standard Z39.48-1992 to replace the irreparably deteriorated original. 2001 Cornell University GLibrary Ithaca, New York BOUGHT WITH THE INCOME OF THE SAGE ENDOWMENT FUND THE GIFT OF HENRY W. SAGE 1891 THE GREAT AFRICAN ISLAND. Ballantyne Dress BALLANTYNE, HANSON AND CO. EDINBURGH AND LONDON Ny 2 ROFIA PALM (Sagus rugia) AND TRAVELLER'S TREE (Urania speciosa). THE GREAT AFRICAN ISLAND. CHAPTERS ON MADAGASCAR. ‘4 POPULAR ACCOUNT OF RECENT RESEARCHES IN THE PHYSICAL GEOGRAPHY, GEOLOGY, AND EXPLORATION OF THE COUNTRY). AND ITS NATURAL HISTORY AND BOTANY ; AND IN THE ORIGIN AND DIVISIONS, CUSTOMS AND LANGUAGE, SUPERSTITIONS, FOLK-LORE, AND RELIGIOUS BELIEFS AND PRACTICES OF THE DIFFERENT TRIBES. TOGETHER WITH ILLUSTRATIONS OF SCRIPTURE AND EARLY CHURCH HISTORY FROM NATIVE HABITS ANI) MISSIONARY EXPERTENCE. BY THE Rev. JAMES SIBREE, Jun., F.R.GS. OF THE LONDON MISSIONARY SOCIETY 5 AUTHOR OF ‘“MADAGASCAR AND ITS PEOPLE.” ETC. WITH PHYSICAL AND ETHNOGRAPAICAL SKETCH-MAPS AND FOUR ILLUSTRATIONS. Pe LONDON: TRUBNER & CO, LUDGATE HILL 1880. | AML rights reserved. ] PREFACE, ALTHOUGH many books have been written about Madagascar during the last twenty years, the majority of these have had reference chiefly to the religious history of the country, and to the political and social changes which have followed upon the acceptance of Christianity by the Government and people of the central provinces. And while much has been written about the Hovas, in the interior of Madagascar, little is still known about the numerous tribes inhabiting other portions of the island. In writing the following pages my object has been to supply information of a more general character than is given in most previous works; and especially to arrange in a systematic form numerous interesting facts which have only recently come to light. During the last nine or ten years many journeys have been made in previously little known, or entirely unknown, parts of Madagascar, so that our knowledge of the various tribes inhabiting the island is greatly increased; and every year continual accessions are being made to our information as to the physical geography and geology of the country, its luxuriant flora, its remarkable and exceptional fauna, and as to the origin and divisions, language and customs, superstitions and folk-lore, and reli- gious beliefs and practices of the Malagasy. For several years past I have been noting down facts of vi PREFACE. interest on these various subjects ; and it will be seen that I have also made extensive use of the volumes of a yearly periodical, printed and published in Madagascar, called The Antaninarivo Annual. This was commenced four years ago at my suggestion, and was designed to be a repository of information on all the points just mentioned with regard to the country and people; and as I edited the first three numbers, and their circulation has been almost entirely con- fined to Madagascar itself, and to those in England who are immediately connected with the island, I have not hesitated to quote largely from it, as well as from other pamphlets and notes of journeys, also published at Antananarivo, and con- sequently almost unknown here in England. It was intended, in the original prospectus of this book, to have added another chapter, giving specimens of the folk- tales and legendary lore of the Malagasy, and of native songs and proverbs, fairy and nursery tales, and traditional history; but this part of the work has had to be relinquished partly owing to the exigencies of space,—for more than one chapter would be required to treat of all these points satisfactorily,— and partly also from the pressure of other work arising from my immediate departure from England; indeed the last sheets of the book have been corrected within a few hours of sailing. I have to acknowledge, with many thanks, the courtesy of Messrs. Macmillan & Co. and of Mr. Alfred Russel Wallace, in allowing a woodcut from Mr. Wallace’s valuable work on The Geographical Distribution of Animals to be used as an illustration for this book. It will be seen that I have derived much help from that work in treating of the animal life of Madagascar. PREFACE. vil I have also to express my thanks to H. W. Bates, Esq., Assistant Secretary of the Royal Geographical Society, and to the Council of that Society, for their readily-accorded permission to use the physical sketch-map of Madagascar from their Proceedings. I must also add that this map has been slightly altered from the original sketch I supplied, and in one or two points is not perfectly correct, particularly in the cross-section. Three or four of the chapters of the book have already appeared as separate papers in the Proceedings and Transac- tions of various societies, the Royal Geographical Society, The Anthropological Institute, The Folk-lore Society, as well as in Nature. Remembering with gratitude the kindly reception given to my former work, Madagascar and its People (R. T. S., 1870), I trust that much of the information given in this second book will not be without interest to many in this and in other countries. J.8. dr Forest Hitz, November 1879. LIST OF ILLUSTRATIONS. SS ROFIA PALM AND TRAVELLER'S TREE, é : Frontispiece. PHYSICAL SKETCH-MAP, . ‘ ' . To face page 32 AYE-AYE, . . . . . . ‘ . ” 42 THREE SPECIES OF CENTETIDA, . ‘ ‘ : 5 64 CHARACTERISTIC FORMS OF ANIMAL AND VEGETABLE LIFE IN MADAGASCAR, : ‘ F : . 84 ETHNOGRAPHICAL SKETCH-MAP, . , ‘ ‘ is 144 CONTENTS. CHAPTER L NAMES, DISCOVERY, EARLY ACCOUNTS, AND MAPS OF MADAGASCAR. PAaGa The names by which the country was known to the Ancients and to Medieval writers—Its discovery by Europeans—Accounts given of it by early voyagers, and first references to it in English litera- ture, together with notices of the maps of the island, ancient and modern, and our knowledge of its geography at the present time, I-21 CHAPTER IL THE PHYSICAL GEOGRAPHY AND GEOLOGY OF MADAGASCAR. Elevated granitic region—Scenery—Rivers and lakes—Lower region and maritime plains—Mountains—Delt of forest—Volcanic dis- turbances—Geology of the chief divisions—Secondary fossils— Recently extinct fauna—Lignite formation—Coral reefs—Metals and minerals—Fertility of soil, . : . : . 22-37 CHAPTER IIL THE ANIMAL LIFE OF MADAGASCAR, Peculiar and specialised character of the fauna—One of the most re- ‘markable geological regions—Lemurs—Aye-aye—Insectivora— Carnivora—Ungulata—Fossil hippopotamus—Rodentia—Remote affinities of the Avi-fauna — Raptores — Water-birds — Perching birds—Cardinal-birds—Sun-birds—Zpyornis and its enormous ega—Reptiles—Scarcity of venomous serpents— Lizards—Gigantic tortoises — Crocodiles — Fishes — Insects —Butterflies—Beetles— Wasps—Fireflies—Mantis—Ants—Locusts—M osquitoes—Spiders —Scorpions and centipedes—An armour-plated creature—Minute and aquatic fauna—Origin and meaning of the specialised fauna of Madagascar—Opinions of eminent naturalists, . Fi - 38-68 CHAPTER IV. NOTES ON THE VEGETABLE PRODUCTIONS OF MADAGASCAR. Forest scenery—Valuable woods—Coast vegetation—Pandanus—Tan- géna poison-tree—Palms—Bark cloth—Bamboos : their applica- x CONTENTS. PAGE tions—Baobab—Mosses, creepers, and lianas—Ferns—Beautifal- leaved plants— Pitcher plants — Vegetation of the interior — Spiny and prickly plants—Grasses—Reeds and rushes— Vegetable foods— Rice and its culture— Roots— Arums — Coffee—Sugar— Spices—Fruits—Bananas—Traveller’s tree—Medicinal Plants— Gourds— Tobacco—Hemp and cotton—Dyes—Lichens—Flowering plants and trees—Orchids—Gums—India-rubber—Lace-leaf plant, 69-101 CHAPTER V. ORIGIN AND DIVISIONS OF THE MALAGASY PEOPLE. Malayo-Polynesian affinities—Alleged connection with African Races —European and Arab elements—African influence on West Coast —Principal divisions of the people—Colour, physique, and lan- age—Difficult problems raised by variations in these respects —Attempted solutions of Energie afforded By Tradition and Philology, . e « 102-122 CHAPTER VL CHARACTERISTICS OF THE DIFFERENT TRIBES INHABITING MADAGASCAR IN ANCIENT AND MODERN TIMES. Hovas—Bétsiléo—Bara—Tanala—Tankay—Sihinaka— Bétsimisaraka and East Coast tribes—Aboriginal peoples before Malay incur- sion: Vazimba—Kimos or Quimos—Kalio or Behosy—Population —Various estimates—Chief towns—Table of ye tribes and their subdivisions, . 2 + 123-144 CHAPTER VIL CURIOSITIES OF THE MALAGASY LANGUAGE: WITH NOTES UPON THE “History,” “POETRY,” AND “MORALITY” EMBODIED IN NATIVE WORDS. Malayan, not African affinities—Oneness over the Island—Musically sounding—Parallelism and rhythmical structure—Curious de- ficiencies and fulness—Preference for passive—Dialects—Diffe- rences between Coast and Hova forms—Tabooed or ‘‘ Fady” words—Obsolete words—Additions from French and English sources — Arabic influence — Examples of the ‘‘ History,” “Poetry,” and ‘‘ Morality” in Malagasy words—Words intro- duced in religious matters—Onomatopoetic words : - 145-164 CHAPTER VIIL CURIOSITIES OF MALAGASY NAMES : PERSONAL, TRIBAL, AND GEOGRAPHICAL, Length—No family names—Personal prefix—Designation from chil- “dren—Unpleasant names—Tabooed words in Chiefs’ rames— Royal names—Sakalava customs—Christian names—Tribal a ap- pellations — Place-names — Foreign Nomenclature in Coast Geography F ‘ 5 ‘ : ‘ + 165-173 CONTENTS. xi CHAPTER IX. CURIOUS AND NOTEWORTHY CUSTOMS AMONG THE DIFFERENT TRIBES. PAGE Roads and travelling—Canoes and boats—Slavery—Ranks of society —Hovas or Commoners—Andrians or Nobles—Royalty—Oaths of allegiance—Royal property—A Malagasy Kabary—Native oratory—Occupations and modes of living—Handicrafts + 174-196 CHAPTER X. CURIOUS AND NOTEWORTHY CUSTOMS AMONG THE DIFFERENT TRIBES —(continued). Houses, their structure and arrangement—The house as a compass and sundial—Towns and villages—Fire by friction—Pottery and substitutes for it—Kissing or nose-rubbing—Tattooing and other adornments—Modes of dressing the hair—Clothing—Use of vegetable fibres for dress— Female adornment— Weapons . 197-216 CHAPTER XL CURIOUS AND NOTEWORTHY CUSTOMS AMONG THE MALAGASY TRIBES —(concluded). Circumcision observances—Brotherhood by blood covenant—Royal ancestor-worship among the Sakalava—Tombs and funeral rites . . ‘ . F . ‘ + 217-242 CHAPTER XIL RELATIONSHIPS, AND THE NAMES USED FOR THEM, AMONG THE PEOPLES OF MADAGASCAR, CHIEFLY THE HOVAS. 243-257 CHAPTER XIIL NOTES UPON MALAGASY ART IN DECORATION AND MANUFACTURE, Hova art: house decoration—Church adornment—Textile fabrics— Straw plaiting-——Metal work—Pottery—Bétsiléo art : Carving on burial memorials—Houses and utensils . 258-2€6 xif CONTENTS. CHAPTER XIV. MALAGASY FOLK-LORE AND POPULAR SUPERSTITIONS. PAGE Animals—Birds—Fabulous animals—Trees and plants—Lucky and unlucky days and times—Ordeals—Folk-lore of home and family life—Lucky and unlucky numbers, actions, etc.—Sickness and death—Witcheraft and charms . 2 ‘ . . 267-296 CHAPTER XV. MALAGASY IDOLATRY AND RELIGIOUS BELIEFS AND OBSERVANCES. Idols and their worship—Sacrifices—Atonement and expiation— Altars and sacred stones and places—Divination—Ambron- drombé, the Malagasy Hades—New Year's festival é » 297-317 CHAPTER XVL NEW LIGHT ON OLD TEXTS: ILLUSTRATIONS OF SCRIPTURE FROM MALAGASY CUSTOMS. Royalty and Government—Family life—Marriage—Benedictions, curses, and salutations—Dress and food—Weapons—Houses and towns—Tombs and burial—Roads and paths—Symbolic acts and figurative language—Agriculture—Slavery—Time . + 318-336 CHAPTER XVII. MALAGASY CHURCH LIFE, AS ILLUSTRATIVE OF THE HISTORY OF THE APOSTOLIC AND EARLY CHURCHES. As regards morals—Rise of superstitious practices and sacramenta- lism—Church divisions—Customs connected with worship— Church offices and Government— Relations between the Church and the State. . . . . . + 337-349 CHAPTER XVIII. THE MADAGASCAR OF TO-DAY: ITS PROGRESS AND PRESENT POSITION, SOCLALLY AND RELIGIOUSLY . * 350-367 INDEX . : : é bs F 368 THE GREAT AFRICAN ISLAND. CHAPTER I. NAMES, DISCOVERY, EARLY ACCOUNTS, AND MAPS OF MADAGASCAR. THE NAMES BY WHICH THE COUNTRY WAS KNOWN TO THE ANCIENTS AND TO MEDIEVAL WRITERS—ITS DISCOVERY BY EUROPEANS—ACCOUNTS GIVEN OF IT BY EARLY VOYAGERS, AND FIRST REFERENCES TO IT IN ENGLISH LITERATURE, TOGETHER WITH NOTICES OF THE MAPS OF THE ISLAND, ANCIENT AND MODERN, AND OUR KNOWLEDGE OF ITS GEOGRAPHY AT THE PRESENT TIME. ALTHOUGH only seen by Europeans within the last 380 years, the ereat African island of Madagascar has been known to the Arabs for many centuries, probably for at least a thousand years past; and also, but perhaps not for so long a time, to the Indian traders of Cutch and Bombay.* The former, indeed, have left ineffaceable traces of their influence in the words they introduced into the Malagasy language, prin- cipally in the names of the days and months, and in those connected with divination and astrology, and also in the various superstitions they engrafted upon the original religious belief and charm-worship of the inhabitants. But even before the Arabian intercourse, it seems probable that the Phcenician traders, in some of those long voyages made by the “ships of Tarshish” (1 Kings x. 22), touched at Madagascar, or at least obtained information about the island. For it is mentioned by some of the classical writers under various names: thus, Ptolemy in his Zabule appears * Sce Sir Bartle Frere’s despatches in Blue-book on the Kast African Slave Trade. t See Rev. L. Dahle in the Antananarivo Annual, No. ii. pp. 75-91. A 2 EARLY NAMES, to refer to it under the name of Menuthias ; * and Pliny writes about an island which, in the opinion of many authors, could hardly be any other than Madagascar, under the name of Cerné.{ And it has been supposed to be obscurely indicated in the book De Mundo ascribed to Aristotle, under the name of Phanbalon. Some other names are also given in early writers; thus, in a quaint old book published in 1609 by Hieronymus Megiserus, entitled Beschreibung der Mechtigen und Weitberhiimbten Insul Madagascar (Altenbourg in Meis- sen), it is stated that Arrian calls it Adenutheseas, Stephanus Byzantinus Menuthis, and Diodorus Siculus Jamboli. Tharetus is also quoted as saying that it was called Pacras on account of the many tortoises found there; afterwards Aldargra, then Manutia-Alphil, and then Magadascar, a corruption of the name of Magadoxo, on the mainland of Africa, whose king is said to have invaded the island. Finally, this word was changed to Madagascar. Soruns the account, some of the particulars of which are probably not very reliable, although they may possess a basis of fact. Madagascar is mentioned by several of the Arabian writers, being known to them also by various names, as Serandah and Chebona ; and by the geographers Edrisi and Abulfeda (twelfth and thirteenth centuries), under the strangely different titles of Phelon (or Phenbalon), Quambalon (or Chambalon), Zaledz (also variously spelt), and Gezirat al-Komr or “Island of the Moon.” * “Huic de processo promontorio hodie Mozambique adjacet ab estivo ortu insula nomine Menuthias ; cujus positio $5 Austral 12.0” (lib. 4, cap. 9). + “Contra Sinum Persicum Cerne, nominetur insula adversa Athiopix, cujus neque magnitudo, neque intervallum a continente constat, Athiopias tantum populos habere traditur” (lib. vi. cap. 31). The bishop appointed to Mada- gascar four years ago has adopted this name Cerné as that of his see on his official seal. + Since writing the above, I have referred to the original texts of some of the classical authors mentioned by the old German writer, as well as to his own book ; and also to a learned French author, Gossellin, who, in his work entitled Récherches sur la Géographie Systématique ct Positive des Anciens (4 vols. Paris, 1813), disputes the opinion of earlier writers that Madagascar was mentioned by classical authors under the names of Cerné and Menuthias (see tom. i. pp. 80, 191-193). With regard to the former of these names, I think his opinion is correct, but I am not so sure about the second. Gossellin maintains that Menu- thias was the name of a very small island in the estuary of one of the great rivers on the East African coast. MARCO POLO. 3 The country was first made known to (modern) European nations by the celebrated Venetian traveller Marco Polo, in the thirteenth century. He, however, did not himself visit the island, but heard various accounts of it during his travels in Asia, under the name of Magaster or Madetgascar. A chapter of his book of travels (33, B. iii. Yule’s ed. pp. 345-354) is devoted to a description of it; but much of what he relates is evidently confused with accounts of Zanzibar and countries on the mainland of Africa, as he says that ivory is one of the chief productions, and that elephants, giraffes, and other animals (which never existed in the island), were numerous. His well-known account of the rukh or gigantic bird, long thought to be entirely fabulous, has during the last few years been discovered to have a basis of fact in the existence of the now-extinct Apyornis, a struthious bird allied to the New Zealand Moa, and which produced the largest of all known eggs. It was not until the commencement of the sixteenth century that Europeans set foot upon the great island. Towards the end of the previous century the adventurous Portuguese navi- gators Bartholomew Diaz and Vasco de Gama reached the scuthernmost portions of Africa and rounded the Cape of Good Hope, thus discovering the sea route to India and the farther East. On the Mozambique coast they found numbers of Arabs trading with India and well acquainted with Mada- gascar. But in 1505 King Manoel of Portugal sent out a great expedition of twenty-two ships to the Indies, under the command of Don Francisco de Almeida, the first viceroy, with orders to build fortresses at Sofala and Quiloa for the pro- tection of the Portuguese commerce in Africa. Juan de Nova, whose name is preserved in that of a small island in the Mozambique Channel, sailed in this expedition. Almeida sent back in the beginning of the following year eight ships loaded with spices to Portugal, under the command of Fernando Soares. On their way they discovered, on the Ist of February 1506, the east coast of Madagascar.* From this * See The Life of Prince Henry of Portugal, surnamed “The Navigator,” Major’s ed., London, 1868, p. 415. 4 4 ITS DISCOVERY. it appears clear that Soares, and not Almeida, as commonly said in histories, was the real discoverer of the island. “In that same year Joio Gomez d’Abreu discovered the west coast of Madagascar on the roth of August, St. Law- rence’s Day, from which circumstance [following the usual custom of the early Spanish and Portuguese navigators] the island received the name of San Lorenco [which it retained for more than a hundred years]. He gave the name of Bahia Formosa, apparently the bay between Point Barrow and Point Croker” [S.W. coast]. The famous navigator Tristan da Cunha, who was sent out to India in the same year, also heard of the island through one of his captains, Rodrigo Pereira Coutinho. This officer had been obliged to take refuge in one of the southern ports of Madagascar from a storm which scattered Da Cunha’s squadron off the Cape of Good Hope. Hearing glowing accounts of the newly-found country from his subordinate, Da Cunha visited various parts of the same coast, making with his own hand a chart of what he discovered, and was accordingly, though of course mis- takenly, celebrated in song by his countryman Caméens in the Lusiad (c. x. s. 39) as the discoverer of Madagascar :-— “ Green Madagascar’s flowery dale shall swell His echoed fame, till ocean’s southmost bound O’er isles and shores unknown his fame resound.” * He reached the northern end of the island on Christmas Day, and accordingly gave it the name of Cape Natal—a name which, however, it has not retained, but has been for long known as Cape Amber or Ambro. The ship of Gomez d’Abreu doubled the northern cape, and running along the east coast, reached the mouth of the river Matitanana in the south-east, where he landed. In a letter dated Mozambique, 8th February 1507, to King Manoel from the celebrated Alfonso d’Albuquerque, who was with * Mickle’s translation of the Lusiad. See Lyons M‘Leod'’s Madagascar and its People, p. 6. The original Portuguese runs thus— “ Pelo cunia tambem, que nunca extinto Serd seu nome em todo o mar que lava As has do Austro, e praias, que se chamam De sa6 LOURENGO, e em todo 0 Sul se affam.” NATIVE NAMES. 5 Da Cunha’s expedition, he speaks of the discovery of the island; so that within a short time several of the most in- trepid Portuguese navigators discovered various portions of the Madagascar coast while on their voyages to or from the far East; in fact, they seem to have almost, if not quite, circumnavigated the island. During the early times of the French intercourse with Madagascar (reign of Henri IV.), they called it by the name of Ile Dauphind, but this appellation was never accepted by other nations. A few worlds may here be said about the name by which the island has been known for the last two hundred years. There is much reason to believe that Aladagascar is not a native name, but one given to the country by foreigners, and has only in modern times been accepted by the inhabitants. The spelling of the word in its present form is opposed to the laws of the native orthography, which do not allow the joining of two such consonants as s and ¢ (¢, moreover, is not used), and all native words end in a vowel. Ndsin-ddmbo, or “Isle of Wild Hogs,” was a name occasionally given to it; but when the Malagasy speak of the whole of the island, they usually call it Lzao rehétra izao, “ This all,” or Lza0 tontdlo izao, “This whole,” thinking, like many insular people, that their own country was the most important part of the world, and that the Arabs and other foreigners who visited their north- west coast came from some insignificant islands across the sea. Another term, somewhat poetical in form, and occa- sionally used by the people, is Wy anivon’ ny riaka, te. “The (land) in the midst of the moving waters,” a term which might be used of any island, but is only applied to Madagascar itself, ndsy being the word employed to denote the small islands off the mainland. This term was engraved on the huge silver coffin of the first Radima, who was there called Tompon’ ny anivon’ ny riaka, “Lord of the island,” as above described. The form of the word,* like the name * By Copland and other writers the island is called Madecassa, which, by substituting & for c, would be a correct enough native word. In many books the people are called Madecasse, but the origin of these forms of the name is obscure. 6 EARLY ACCOUNTS. of the inhabitants of the country, Malagasy (also probably not a native name), seems to indicate an African origin, so that pos- sibly there may be some foundation of truth in the accounts given by the German writer already quoted from. Ma, it is well known, is a frequent prefix to words indicating tribal names on the African continent, as Makololo, Matabele, &c. The early accounts given of Madagascar by voyagers and other writers are full of glowing and extravagant praises of its fertility and natural wealth. But in all this, of course, it formed no exception to other newly-found countries, for the imagination of the people of the sixteenth and seventeenth centuries invested with a halo of beauty and mystery all the strange new lands which were being yearly discovered by the bold seamen of Portugal and Spain, and of England and Holland. The luxuriance of the tropical vegetation of the New World and the far Eastern Archipelago, and the undoubted wealth in precious metals of some of those regions, made every fresh addition to their geography a possible El Dorado, with gold and gems waiting to be collected in every stream, and precious spices to be gathered from every tree. Even the title-pages of some of the early books upon Madagascar are eloquent panegyrics upon the resources and wealth of the island; while their quaint descriptions, as well as the strong religious feelings so many of them evince, make them by no means uninteresting reading. Although the Portuguese discovered the island, they made no lengthened occupation of any part of it. Probably they found that their extensive possessions in South America and Africa and the Malay Archipelago demanded all their strength to occupy; and accordingly their colony was soon abandoned. For a few years towards the close of the sixteenth century (1595-98), the Dutch had some little intercourse with Madagascar, but were not much impressed in its favour ; for they lost through sickness so many of their number that an "island where they landed was called “The Dutchmen’s Grave- yard.” A book written by Johan Hugen von Lindschot (1628) describes these voyages, and it is evident that they paid some considerable attention to the country, for two of the very earliest books upon Madagascar were published at HIERONYMUS MEGISERUS. 7 Amsterdam in 1603, both of them giving vocabularies of Malagasy words (see chapter on the language). As the Portuguese discovered Madagascar, probably the earliest descriptions of the country are to be found in Portu- guese books, notably in the Commentarios do grande Afonso D Alboquerque (Lisbon, 1576, fol.), but this book contains little of interest beyond the mere fact of the discovery of the island. Next in date come the two Dutch linguistic works already mentioned, and then the little German work of Hieronymus Megiserus, from which quotations have been made as to the early names of the island. The title-page of this book pro- mises to give us— A GENUINE, THOROUGH, AND AMPLE, as well as HISTORICAL AND CHRONOGRAPHICAL DESCRIPTION of the EXCEEDINGLY RICH, POWERFUL, AND FAMOUS ISLAND OF MADAGASCAR, called also St. LAWRENCE ; Together with an Account of all its Qualities, Peculiarities, Inhabitants, Animals, Fruits and Vegetables. Also A History of what has happened there before and since its Discovery. The title-page, like those of other books we shall have occasion to mention, leads one therefore to expect much valuable information; but except some curious particulars about the names given to the island at that period, there is little of value about either country or people, while some of the same mistakes are made as to the productions as are found in Marco Polo’s account. At the end is added “A Dictionary and Dialogues of the Madagascar Language, collected with special industry from the Portuguese, Italian, and Latin Histories and Geographies;” and this portion, more than half of the whole book, has considerable interest, the greater part of the words being easily recognisable. It has 8 WALTER HAMOND. a small map, and seven or eight engravings of the people, and of the animal and vegetable productions. The earliest English book upon Madagascar of which I have any knowledge is by one Walter Hamond, surgeon, and published in 1640, entitled “A Paradox: Proving the Inhabitants of the Island called Madagascar, or St. Law- rence (in Things temporal), to be the happiest People in the World.” * This work may be almost regarded as a satire upon the extravagance and luxury of the times, for its gene- ral purport is to show that the inhabitants of Madagascar, in their poverty and ignorance, are much better off than civilised peoples, being not much troubled with clothing or ornaments, or with the fatigues of commerce, navigation, and civilisation, the varieties of food and drink, and the evils arising from the use of gunpowder and the arms of European nations. All this is argued out in a comically serious style. Possibly a diligent search in the larger libraries would dis- cover earlier books, or at least pamphlets or tracts on Mada- gascar ; and doubtless there are many notices of the country to be found in the narratives of the early English voyagers. The same author published three years later (1643) another book, whose title-page may be given in full, as it is curious from its quaintness, and as showing the great expecta- tions formed of the island. It is as follows :— MADAGASCAR, The Richest and most Frvitefvll Island In the World. Wherein the Temperature of the Clymate, the Nature of the Inhabitants, the Commodities of the Countrie, and the facility and benefit of a Planta- tion by our People there, are compendiously and truely described. * Reprinted in the Harleian Miscellany, a Collection of Scarce, Curious, and Entertaining Pamphlets and V'racts, as well in Manuscript as in Print. London, 1808. DESCRIPTION OF THE ISLAND. 9 Dedicated To THE HONOURABLE IOHN BOND, Governour of the Island, whose proceeding is Authorized for this Expedition, both by the King and Parliament. By WALTER HAMOND. Lonpon: Printed for NICHOLAS BouRNE, and are to bee sold at his Shop, at the South Entrance of the Royall Exchange. 1643. [4to.] The promise of the title-page (as in the case of the Ger- man book already described) is hardly borne out by the book itself, which does not contain much of value, except some information about the author’s experiences with the people, chiefly those about St. Augustine’s Bay on the south-west coast. He seems to have been greatly impressed by the honesty and good faith of the inhabitants; again and again is this mentioned in such words as “in all our trayding with them we never sustained so much as the losse of one bead.” He even says, “they retaine the first incorrupt innocence of man,” and are “a people approaching in some degree neere Adam, naked without guilt, and innocent, not by a forc’t vertue, but by ignorance of evill, and the creatures as inno- cent and serviceable to man as they were before his trans- gression.” (How wofully, according to all accounts, must they have depreciated since then!) We find, however, in the book, that among these innocent people wars were going on be- tween them and the neighbouring tribes, as there still are, and probably always have been. There is a notice of some of the valuable trees of the country, ebony, tamarind, and others, and of a remarkable tree he calls the “flesh-tree,” probably a dragon-tree, yielding a sanguine-coloured sap. The book contains an urgent appeal to the writer's countrymen to “go in and possess the land,’ which “doth here by me friendly and lovingly invite our nation to take some compassion of her nakednesse, her poverty, and her simplicity, both corporall and spirituall, and doth earnestly and affectionately even beg of us to redeeme her out of her miserable thraldome under the tyranny of Satan [curiously inconsistent this with the pre- 10 RICHARD BOOTHBY. ceding eulogy of the people], to be united with us into the fellowship of the sons of God by our union in Christ Jesus.” Who this Hon. John Bond, “ Governour and Captaine-Generall of Madagascar,” was, I have been unable to discover, or to find what claim he had to such large powers in the great island. In the same decade of the seventeenth century other books on Madagascar were also published, the next in date being one with an extremely long title, which is also perhaps worth quoting nearly in full, not only for its quaint language but as affording additional evidence of the sanguine expecta- tions formed respecting the island. It runs thus :— A BREIFE DISCOVERY or DESCRIPTION Of the most Famous Island of MADAGASCAR or ST. LAWRENCE in Asia neere unto East India. With relation of the Healthfulness, Pleasure, Fertility, and Wealth of that Country, comparable if not transcending all the Easterne parts of the World, a very Earthly Paradise ; a most fitting and desirable place to settle an English Colony and Plantation there, rather than in any other parte of the knowne World. Also the condition of the Natives, there inhabiting, their Affability, Habit, Weapons, and Manner of living, the plenty and cheapnesse of Food, Flesh, Fish, and Fowle, Oringes and Lemonds, Amber-Greece, Gold, Tortle-Shels, and Drugs, and many other Commodities fit for trade and commerce, to be had and gotten there at cheaper Rates than in India or elsewhere. Also trading from Port to Port all India and Asia over, and the great profit gained thereby ; The chiefest place in the World to inrich men by Trade, to and from India, Persia, Moco, Achine, China, and other rich Easterne Kingdoms. It being the fittest place for a Magazine or Store-house of Trade between Europe and Asia, farre exceeding all other Plantations in America or elsewhere, Also the excellent meanes and accommodation to fit the planters there, with all things needfull and superfluous for back and belly (out of India neere adjacent, at one fourth part of the price, and cheaper then it will cost in England ; yea, Fat Bullocks, Sheep, Goats, Swine, Poultry, Rice (and Wheat and Barley reasonable, &c.) exceeding cheape, for the value of 12 pence or one shilling English will purchase or buy of the Natives PROFECTED ENGLISH COLONY. MI as much as 5, 6, 7 pounds or more in England, in this famous Island at their first arrivall, which no other country hath afforded. By RICHARD BOOTHBY, Merchant. Lonvon : Printed by E. G. for JOHN HARDESTY ad the Signe of the Black- Spread Eagle in Duck Lane, 1646. It seems from the preface to Boothby’s work, which is a small octavo of seventy-two pages, that two years previous to the publication of this book there had been a project to found an English plantation in Madagascar, Prince Rupert having been named at the Privy Council board as Viceroy for King Charles I., from whom he was to have had twelve men-of-war and thirty merchantmen to form the colony. The Governor and Committee of the East India Company were also ordered to give all possible assistance to the enterprise. Rupert, how- ever, going away to the Continent, the Earl of Arundel, Earl Marshal of England, was appointed; and it appears that that nobleman had also written a book on the subject, urging the desirability of forming a magazine or victualling station on the island. However, the calling of the parliament im- mediately preceding the Long Parliament, and the political troubles’ which soon ensued, put a stop to this projected English colony in Madagascar. It is stated in Boothby’s book that the island had been previously visited by other dis- tinguished Englishmen, viz. the ambassadors from Charles I. to the King of Persia, who landed there on their way to the East. The appointment of Prince Rupert called forth another book upon the island, but this time in the shape of a poem, by Sir William Davenant, entitled “Madagascar, with other Poems, by W. Davenant, Knight ” (London, 1648). This pro- duction occupies only twenty-one pages of print, and gives no information whatever about Madagascar itself, being simply a complimentary effusion, “written to the most illustrious Prince Rupert.” Following the strange conceits common to the literary productions of the time, such as are seen in Beaumont and Fletcher, Donne, Herbert, and other writers, the poem is in the form of a dream, in which the country 12 DAVENANT’S POEM. where the Prince was going is described in an inflated style, with extravagant laudation of Rupert, so that even the sun is described as being absorbed in contemplating what the Prince is supposed to have conquered :— , : “ The good old planet’s business is Of late only to visit what is his ;” while as to the government of the Prince, “ Chronologers pronounce his style The first true monarch of the golden isle ; An isle so seated for predominance, Where naval strength its power can so advance,” The supposed riches of the country are next described, the colonists employing themselves “Tn virgin mines, where shining gold they spy, Some root up coral trees, where mermaids lie Sighing beneath those precious boughs, and die.” Some from “old oysters” rifle pearls, “ Whose ponderous size sinks weaker divers ; Their weight would yoke a tender lady’s neck.” Some “ Search the rocks till each have found e A saphyr, ruby, and a diamond.” The poem is a poor enough production in itself, but has a certain interest as showing the extravagant notions then entertained about the wealth of distant countries. But it nevertheless met with great commendation from the poet’s contemporaries, Endymion Porter saying that it was a “ Poem in so sweet a style As never yet was lauded in this isle,” Another of the poet’s friends, Sir John Suckling, Comptroller of the Household to King Charles I., wrote a sonnet entitled, “To my friend Will Davenant, on his Poem of Madagascar,” which is perhaps amusing enough to be quoted in full, espe- cially as he concludes by a sly hit at his friend for having nothing but words to show in proof of the enormous wealth he describes :— STR FOHN SUCKLING. 13 “What mighty princes poets are! Those things The great ones stick at, and our very kings Lay down, they venture on ; and with great ease Discover, conquer, what and where they please. Some phlegmatic sea-captain would have staid For money now, or victuals ; not have weigh’d Anchor without ’em : Thou (Will) dost not stay So much as for a wind, but go’st away, Land’st, view’st the country ; fight’st, put’st all to rout Before another could be setting out ; And now the news in town is, ‘Davenant’s come From Madagascar, fraught with laurel, home ;’ And welcome (Will) for the first time, but prithee, In thy next voyage, bring the gold with thee.” The fifth decade of the seventeenth century was thus, it appears, most prolific in works upon the great African island. Towards the end of the century an account was written (but not published until some years later) of the adventures and extreme hardships suffered by an English sailor upon a small island off the western coast of Madagascar. This was entitled— “A Relation of Three Years’ Sufferings of Robert Everard upon the Island of Assada, near Madagascar, in a Voyage to India, in the year 1686, and of his Wonderful Preservation and Deliverance and arrival at London, Anno 1693.”* This account, which occupies twenty-three pages of small folio print, contains several interesting particulars of the customs of the people, amongst which is the statement that on one occasion twenty children were circumcised by the women. The writer had evidently a hard time during his three years’ residence; for, although he made shot for the king, because he could not also find gun-flints he was turned out of doors and left to shift for himself. He obtained food in the shape of fruit and roots, shell-fish and turtles, but he had to lodge under a tree only, for two years and nine months, although on one occasion, he says, it rained continuously for three months. As he was quite naked, he kept a fire burning * Pages 259-282 in vol. vi. of A Collection of Voyages and Travels, some now first printed from the Original Manuscripts, &c. London, Churchill, 1732. 14 DRURY’ S NARRATIVE. for warmth, not being allowed to enter the houses. Jven- tually he became (no wonder) very ill, and at his request was bought by an Arab, and at last taken to India, where he obtained his liberty. This island of “Assada” is probably one of those numerous ones off the north-west coast of Mada- gascar. . The last of these early books which can be here noticed is that by Robert Drury, an English lad, who, at the commence- ment of the last century, went as a passenger to the East on board an Indiaman named the Degrave. On their homeward voyage the vessel was wrecked on the south-west coast of Madagascar, and owing to imprudent conduct and collisions with the natives, the whole of the ship’s company and pas- sengers were eventually killed, with the exception of Drury and another lad, whose lives were spared. He thus became a slave, and remained as such in the island for fifteen years (1702-17), meeting with varied experience and many hard- ships, and occasionally being harshly treated, and narrowly escaping being killed. At last, however, he obtained his liberty, and returned to England, afterwards writing the book describing his adventures, or possibly had it written from his dictation. Drury being comparatively uneducated, the narra- tive is in a most artless style, with an evident impress of truth, and, from its undoubted genuineness, is a very valuable record of the customs of some of the Malagasy tribes at that period, and throws important light upon many questions con- nected with their customs, superstitions, and beliefs. He describes their ancient and patriarchal system of worship in connection with the ddy, or household gods; and we see the political state of that part of the island, really unaltered to the present time, in which the different tribes are constantly engaged in warfare, making raids on each others’ cattle, and capturing slaves. There is added to the book a pretty full vocabulary, which is one of the most valuable portions of it, the great majority of the words being easily recognisable as identical with those in the Hova dialect, and thus giving another proof of the substantial unity of the language over portions of the island far distant from one another. Curi- ously enough, he gives a decidedly “Cockney ” pronunciation MADAGASCAR AND THE FRENCH. 15 and spelling to his list of Malagasy words; héna (meat) he calls “henar;” vdla, money, “voler;” and andro, day, “hawndro;” &c. From the year 1651, when a work describing a voyage to Madagascar by one Frangois Cauche, of Rouen, was issued, a considerable number of books upon Madagascar have been published in the French language. A list of between thirty and forty of these is given by M. Barbié du Bocage in a book entitled, Madagascar: Possession frangaise depuis 1642, the title of which work explains the interest taken in the island by the French. But it is quite an unfounded assumption to call Madagascar a French possession, and is warranted neither by conquest or treaty, or by any other claim or right; and although it is quite true that the French have for two cen- turies past been attempting to gain power in the country, their colonies, or rather, military posts, have never been per- manent, nor have they been able to maintain their hold upon any portion of the mainland. They have, however, seized the small island of St. Marie’s, off the eastern coast, and they have also possession of the island of Noésibé, on the north- west coast. This latter was ceded to them in 1840 by the Sakalava inhabitants of that portion of Madagascar. Turning now to the Maps of Madagascar, and our present knowledge of the geography of the island, it may be affirmed that a considerable portion of the country is still a terra incognita to us; and notwithstanding all that has been done of late years to increase our knowledge of it, there are exten- sive regions still unknown and unexplored. Among them may be mentioned the greater part of the triangle formed by the northern portion of the island, from Antsihanaka to Cape Amber at the apex of the triangle; almost all the Sakalava country on the western seaboard; large portions of the eastern side, from the central plateaux to the sea; and, lastly, an extensive district to the south of the Bétsiléo province, from the Bara country to the southern Cape of St. Mary. The earliest map of Madagascar which I have discovered is one in the British Museum, and is an extremely curious specimen of chartography. The outline of the island there given is so different from the reality, that it would hardly be 16 EARLY MAPS. = recognised but for the name, “8S. Lorenzo,” which is marked upon it. The towns shown on the map, six in number, are true medieval strongholds, with walls and gates, and crowded with spires and towers, one of them boasting of a grand © cathedral !—while they are all on such a scale that they would be disproportionately large even if the island were only two or three miles wide. Similarly gigantic ships, with banks of oars, are depicted along the coast, and strange sea- monsters are here and there seen emerging from the waves around the island. From its very incorrect outline I am strongly inclined to think that it is of considerably earlier date than that given in the catalogue, viz, 1570 * (Venice), the more so as another map, also Venetian, and dated three years earlier (1567), is far more correct in outline, and the principal capes, bays, and rivers can be recognised, and are tolerably accurate, as far as regards the coast-line. Another very curious old map, to a small scale, is given in the quaint German work of Megiser’s already referred to. But I find that it is taken from an earlier book, a neat little atlas of maps, with descriptions of the different countries, entitled Thresor de Chartes, and dated 1602. A glance at several of the numerous maps of Madagascar that have been published since these dates would lead one to suppose that what is stated above as to the incompleteness of our knowledge of the country was all a mistake. On many of these we find the so-called provinces defined with a minute- ness resembling that of the divisions of the counties on an Ordnance map of England; the rivers, with their tributaries, are all unhesitatingly laid down, and mountain chains of sin- gular regularity and wall-like straightness cross the country in all directions. Far from imitating the ineenuous confessions of ignorance shown on some maps, where— “Geographers on pathless downs Put elephants instead of towns,” many of these early maps of Madagascar are, strange to say, * T am confirmed in this opinion by a further reference to the catalogue, in which a note of interrogation is affixed both to the date and the placo of pub- lishing. ROCHON’S MAP. 17 the most minute and exact in their fulness of detail; and knowing how little certainly was then ascertained as to the interior of the island, we look at them with a feeling of wonder as to whence their information could have been derived. One of the most curious of these early maps is that prefixed to an English edition of the Abbé Rochon’s book entitled, A Voyage to Madagascar and the East Indies (Lon- don, 1793). According to this map, no part of the island would appear to have been unknown to the map-maker; the rivers with their tributaries have a picturesque symme- try resembling that of stately trees, and the mountains a re- gular cone-like outline only possessed by mountains seen on a map. But on examining this map more minutely to find out well-known places in the interior, we are puzzled to find that neither the central and most important province of Imérina, nor the capital city, Antananarivo, are shown; and it is the same with the important province of Bétsiléo and its chief towns; while some other places are strangely transposed. Clearly this map owes more of its filling-in to a lively imagination than to any exploration of the country, notwithstanding the somewhat ambiguous assurance in its title that it is “from the original design, drawn on the spot ;” but what and where “the spot ” was, is not specified.* Again, take a very pretentious-looking map published by Arrowsmith, and purporting to be “Madagascar, from Original Drawings, Sketches, and Oral Information, by J. A. Lloyd, ERS. &., &c., Surveyor-General of the Mauritius.” The last edition I have seen is dated 1850. In a journey to the south-east part of Madagascar in 1876 I consulted this on many occasions, but found that not the slightest reliance was to be placed upon it. But subsequently meeting with a pamphlet read by Colonel Lloyd before the Royal Geogra- phical Society upon Madagascar (10th December 1849), I discovered a clue to the reason for all this; for at page 22, in a few remarks upon the map accompanying his paper (a * Since writing the above, I find that Rochon’s map is little more than a copy of that given in Flacourt’s Histoire de la Grande Isle de Madagascar, published in 1661, a hundred and thirty years before Rochon’s book. B 18 FRENCH MAPS. reduced copy of the above-mentioned map), Colonel Lloyd makes this ingenuous admission: “For the detail of the interior I cannot claim the slightest pretensions to correctness. It is only an attempt to form approximately some foundation for future inquiries and more correct and extensive research.” And yet this map, confessedly so problematical, appears to have been the source of most subsequent maps of the island as given in English books or published separately. The coast-line of Madagascar, with a narrow strip of country bordering the sea, was accurately surveyed by Cap- tain W. F. W. Owen, R.N., of H.M.S. Leven and Barracouta, about forty-seven years ago. This survey was published by the Admiralty, and Captain Owen described his experiences in a book entitled Narrative of Voyages to Explore the Shores of Africa, Arabia, and Madagascar, gc. (London, 1833). With regard to the later French maps of Madagascar, they also appear to have been chiefly constructed from verbal information, with an occasional itinerary of a priest, or naturalist, or trader; for the interior detail of most of them prior to 1870 seems little more reliable than that given in the English maps. (The island has been crossed in various directions by a good many travellers, as shown in a valuable list of routes compiled by M. Grandidier, and given in a paper published in the Bulletin de la Société de Géographie [Avril 1872, pp. 408-411]; but very few of these travellers have left any accurate observations or scien- tific surveys of the line of country they traversed.) How some of these French maps have been constructed is amusingly described by M. Grandidier in a paper upon the island before the Paris Geographical Society. Speaking of a book by a M. Leguevel de Lacombe, entitled Voyage @ Madagascar, he says: “This writer relates that he has ‘at different periods traversed the island from north to south, from east to west; he gives the most precise details of his journeys. M. de Lacombe has told me, and I am myself well assured of it, with his book in my hand, that he has never left the east coast! It is from his imagination that he has drawn the accounts, to which geographers have attached so much impor- GRANDIDIER’S MAP. 19 tance that the maps of Madagascar have to the present day been constructed upon the topographical data taken from his work.” * To a French traveller, however, we owe the most accurate general map of the island yet produced. M. Alfred Gran- didier, who explored the country from 1865 to 1870, pub- lished in 1871 a sketch-map (Esquwisse d’un Carte de lIle de Madagascar). It is somewhat roughly lithographed, and was merely intended to illustrate the brief summary of his travels and explorations read before the Paris Geographical Society ; but from the prospectus of his magnificent work on the island and its natural history, botany, ethnology, &c., now in process of publication in twenty-eight quarto volumes, a much more complete map may be expected. Meanwhile, this preliminary map has already done much to clear away some traditional mistakes, and to establish two or three facts of great interest in the physical geography of the country, namely, the existence in the island of two strongly contrasted regions: the elevated granitic district, and the low mari- time plains region to the west and south, of Secondary and Tertiary formation; t and also the existence of a belt of forest surrounding the whole island. On this map most of the Hova military stations and the more important places in the interior are laid down; and having had opportunities of testing its accuracy in more than one direction, I feel confident that it is by far the most trustworthy map of the island yet published. Indeed, no previous traveller has been so thoroughly prepared by scientific knowledge and with full appliances to make an accurate survey of the country; and as many hundreds of principal points were fixed astronomi- cally, a reliable basis has been formed for future work. It must, however, be remembered that M. Grandidier has not traversed the island in every direction, and, as already remarked, extensive portions of it have still to be explored, * Bulletin de la Société de Géographie, Aout 1871, p. 82. + M. Grandidier says: ‘‘ Je vais maintenant tacher de tracer en quelques mots la physionomie générale que présente Madagascar. Cette fle comprend deux parties bien distinctes : la partie nord et est qui est toute montagneuses, et la partie sud et ouest qui est rélativement plate.”—Bull. de la Soc. de Géog., Aout 1871, p 100. 20 DR. MULLENS’S MAP. so that there is still much to be added to this map of the French traveller and savant. Far surpassing everything else previously attempted as a delineation of the interior must be mentioned the map of The Central Provinces of Madagascar, by the Rev. Dr. Mullens,* published, together with his book entitled Twelve Months in Madagascar,in 1875. Stretching over five degrees of lati- tude, from the Antsihinaka province in the north to Imaha- zony in Southern Bétsiléo, it depicts on a scale of twelve miles to the inch the physical features of the central portion of the island and the sites of the chief towns and most impor- tant villages. The late Mr. James Cameron had previously fixed astronomically some of the chief points in Imérina, and measured a base-line from which the triangulation was con- structed, so that a reliable foundation for the map was pro- vided, and the series of angles was extended right down into the Bétsiléo province. This map is a great gain to our know- ledge of the interior, and is full of detail; it is, however, im- perfect in many directions, and plenty of room is still left for additions and improvements. Since Dr. Mullens’s visit several important contributions have been made towards a fuller geographical knowledge of various portions of the island not previously mapped. Among these are sketch-maps illustrating journeys, made chiefly by members of the London Missionary Society and the Friends’ Mission Association, into the Sakalava country, the Bara province in the south, to the Southern Tanala or forest. tribes, and the south-east coast, the north-east coast, and northern central portions of the island, and to the north-west and extreme north.t The results of these journeys are embodied in a map prepared by Mr. W. Johnson of the Friends’ Mission, and lithographed at their press in Antandnarivo, the work being done by native lads. The same gentleman has * Since the above was written, I deeply regret to add that Dr. Mullens’s name must now be prefixed by the word ‘“‘late.” He died at Mpwapwa on July 10, 1879, having nobly volunteered to head a party to relieve the Central African Mission of the London Missionary Socicty. Had his life been spared, he would doubtless have done something in Africa, as in Madagascar, to add to our geographical knowledge of the country he traversed. t See Proc. Roy. Geog. Soc., January 17, 1877. RECENT RESULTS. 21 also published a very minute and complete map of the south- western portions of the central province. ° In the year 1877 a journey was made by Rev. J. Richard- son from the Bétsiléo province to St. Augustine’s Bay on the south-west coast, across new ground, and thus much light has been thrown upon the northern portion of that extensive tract of Southern Madagascar, which is still largely an un- known region. The results of all these recent additions to our knowledge of the geography of Madagascar have been embodied in a very fine general map prepared by Dr. Mullens and published in May last. This is the largest inap of the island yet con- structed, being on the same scale as those of the central provinces and Southern Madagascar. These are included in it without much alteration, but three or four other routes are also laid down, Grandidier’s sketch-map forming the authority for other parts of the country. There is still, however, much to be done in all directions before we can be said to have a tolerably complete general map of the island, while of course there is ample room for hundreds of more detailed maps of special portions of the country. An island nearly a thousand miles long and three hundred and fifty at its greatest breadth gives “ample space and verge” for map-making. Still, so far, every journey lately made appears to confirm the general truth of M. Gran- didier’s sketch-map as to the broad outlines of the elevated mountainous and granitic region in the northern and eastern central portion of the island; but we still need much infor- mation as to the contour of this in various directions, and the steps by which it rises from the plains on all sides. From the usually brilliantly clear and pure atmosphere, and the large number of prominent and lofty hills all over the central regions of the island, Madagascar offers especial facilities for map-making, as some well-known points can almost always be seen, from which to get good bearings. What is most wanted is that a few more of these be exactly fixed by astronomical observations. (22°) CHAPTER II. THE PHYSICAL GEOGRAPHY AND GEOLOGY OF MADAGASCAR. ELEVATED GRANITIC REGION—SCENERY—RIVERS AND LAKES—LOWER REGION AND MARITIME PLAINS—MOUNTAINS—BELT OF FOREST—VOLCANIC DIS- TURBANCES—GEOLOGY OF THE CHIEF DIVISIONS—SECONDARY FOSSILS— RECENTLY EXTINCT FAUNA—LIGNITE FORMATION—CORAL REEFS—METALS AND MINERALS—FERTILITY OF SOIL. ALTHOUGH Madagascar is known to be the third largest island in the world, its actual size and extent is not very generally understood. And it is easy to see how misconception on this point arises, for in maps the island is usually seen only in connection with Africa, and that continent is of such immense extent that it dwarfs by comparison with itself everything in its near neighbourhood ; so that the really large island shel- tering under its south-eastern side appears but an incon- siderable appendage to its vast neighbour. If, however, we take a good-sized map of Madagascar, and put by its side the outline, to the same scale, of another country with whose dimensions we are familiar—such, for instance, as England— we begin to realise how important an island it is as regards size, being nearly 1000 miles long* by about 250 in average breadth, and reaching to 350 miles at its widest part. It has, therefore, an area of about 230,000 square miles, so that it is nearly four times as large as England and Wales. During the last ten years much light has been thrown upon the physical geography of Madagascar, principally through the researches of M. Alfred Grandidier, and the numerous exploratory journeys made in various parts of the country by missionaries and others. Until a very recent period there was no reliable map of the island, and the physical geography was completely misunderstood. But it is * More exactly, 975 miles. MOUNTAINOUS REGION. 23 now quite clear that, instead of a “central mountain chain,” as described in most histories and gazetteers, there is an elevated mountainous region, which, however, does not occupy the centre of the island, but is more to the east and north, leaving a considerable extent of country to the west, and all beyond the twenty-third parallel of south latitude, at a much lower level above the sea. Broadly speaking, therefore, Mada- gascar consists of two great divisions, viz—(1) An elevated interior region raised some 3000 to 5000 feet above the sea-level, and (2) a comparatively level country surrounding it, and not much exceeding 400 or 500 feet of elevation, but most extensive on the west and south. The elevated region is largely composed of Primary and crystalline rocks. Lines of hills traverse it in all directions, but they do not rise to a very great height; the highest points in the island, the peaks of the Ankaratra group of hills, being a little under 9000 feet above the sea-level. A very large extent of this portion of Madagascar is covered with bright red clay, through which the granite and basaltic rocks pro- trude. But there are also extensive rice plains, especially in the neighbourhood of the capital cities of the two chief pro- vinces, where there is a rich black alluvial soil; and it can hardly be doubted that some at least of these plains, from their perfect level, out of which the red clay hills rise like islands, have formerly been the beds of extensive lakes, sub- sequently drained, possibly by slight changes in the level through subterranean action. A good deal of this portion of Madagascar is bare and somewhat dreary-looking country. The long rolling moor- like hills are only covered with a coarse grass, which becomes very brown and dry towards the end of the seven months’ rainless season; but the hollows and river valleys are often filled with a luxuriant tropical vegetation, and, wherever there is population, with the bright green of the rice-fields. There is, nevertheless, an element of grandeur in the landscape, from the great extent of country visible from many points in the clear pure atmosphere, which renders very distant objects wonderfully sharp and distinct. And many portions of the central region possess still greater claims to admiration from 24 THE WATERSHED. the picturesque mountain scenery. In the Southern Bétsiléo country the grand and varied forms of the mountains filled me with an exultant kind of delight. To the south was a crowd of mountain-tops, peak beyond peak, with the greatest variety of outline: one had the appearance of a colossal trun- cated spire; another had a jagged saw-like ridge; another . was a pyramid with successive steps; and another an enor- mous dome. Their summits were never long free from clouds, and many of the peaks must be at least 3000 feet above the plain. Sections taken by the aneroid across this elevated region from east to west, at the latitude of the capital, show that it has a depression in the centre, the edges on either side being considerably higher than the country between them. At some points this height of 4000 or 5000 feet is gained by a series of steps from the maritime plains, each range of hills rising higher and higher; while at other points it descends almost at one steep slope for nearly 3000 feet. The watershed is not near the centre of the island, but is much more towards the eastern side. Through the eastern wall many of the rivers cut their way by magnificent gorges, amidst dense forest, finding their way to the sea by a suc- cession of rapids and cataracts, and occasionally by stupen- dous falls, as in the case of the Matitanana, which descends at one plunge 500 or 600 feet. Some of the western rivers also are said to form grand waterfalls, particularly that of the Mania, whose sound is reported to be heard at a distance of two days’ journey, 7.¢., from forty to fifty miles. The largest river in Madagascar is probably the Bétsibika, which, with its affluent the Ikiopa, is the great drain of the central province of Imérina, and falls into the Bay of Bem- batoka. It is about 300 miles long. Many other rivers of considerable size flow to the west, the Mania and Matsiatra being almost as large as the Bétsiboka, but few are navigable for vessels of large size. The Bétsibdka could be ascended by steamers of light draught for about ninety miles from its mouth, and perhaps also several others of those which fall into the Mozambique Channel. The eastern rivers are almost all blocked at their outlets by a sandy bar LAGOONS. 25 thrown up by the ever-restless surf driven by the strong south-east trade winds. This contest between the fresh and the salt water has given rise to one of the most curious geographical features of the east coast, namely, the long chain of lagoons which stretch for several hundred miles along the shore. Many of these look like a river following the coast-line, but often they spread out into extensive sheets of water and form large lakes. So short is the distance between the detached links, that by cutting about thirty miles of canal to connect them, a continuous waterway could be formed for 260 miles along the eastern coast, a circumstance which will no doubt at some future day be taken advantage of for commercial purposes, as it would be a most valuable means of communi- cation between distant portions of this side of the island. Except these lagoons, there are few lakes in Madagascar, although, as already noticed, there were probably some very extensive ones in a recent geological period. Of one of the largest of these, the lake Aladtra in the Sihanaka province is the relic; this sheet of water is about twenty-five miles long, and from four to five miles wide, spreading out at the northern end into a hammer-head shape. The next in size is Itasy in Imérina, which is about eight miles long; and there is another of some extent in the south-western part of the island. The lower region of Madagascar consists of extensive plains only a few hundred feet above the sea-level, but there are at least three prominent chains of hills traversing it from north to south, one of which appears nearly continuous in a very straight line for above 600 miles. The eastern side of the island is, for the greater part of its extent, without any bay or indentation; indeed, for 500 miles, from Foule Pointe to Fort Dauphin, the coast forms almost a straight line. North of the first-named of these two places there is a deep inlet forming the Bay of Antongil, and protected by the mountainous peninsula of Maréa. Close to the northern point of the island is one of the finest harbours in the world, that of Diego Suarez or British Sound; and the north- western side is deeply indented with large bays, into which 26 ROCK FORTRESS. some of the chief rivers fall. All this part of the coast is bold and mountainous; and some of the finest scenery in Madagascar is to be found here, as the northern extremity of the volcanic region forms several very grand mountains, particularly the one called Amber or Ambohitra. This is said to be about 6000 feet high, and, from its isolated position in the low country surrounding it, is a remarkably majestic hill as seen from every direction, as well as from far out to sea.* It has three summits, and its sides are clothed with impene- trable woods. South-west of this mountain is a remarkable rock fortress of the tribe inhabiting this part of the country, who are called Antankarana, that is, “the people of the rocks.” It is an enormous lofty and precipitous rock, having an eleva- tion of nearly 1000 feet, and covering an area of about eight square miles. Its sides are so precipitous that they cannot be climbed unless artificial means are used, and it is thickly wooded wherever trees can possibly grow. The only entrance into the interior of the rock, which is full of caves, is by means of a subterranean passage, a portion of which is extremely narrow, allowing only a single person to pass along it at a time, and has on each side of it deep water. The other principal group of mountains in Madagascar is the great mass of elevated peaks called Ankaratra, in the central province. This has hardly the grand appearance of Mount Amber (although it considerably exceeds the latter in absolute height), since it rises from the elevated region of Imérina, which is at the capital about 4000 feet above the sea-level. Ankdratra is, nevertheless, a noble group of hills, and is the most conspicuous feature of the landscape over a considerable portion of the central regions of the island. There are five or six principal peaks, and these are in two ranges, lying in the form of a cross. They vary from 8000 to 9000 feet in height, the most lofty one, a peak called Tsidfajavona (“that which the mists cannot climb ”), being 8950 feet above the sea-level, and so is the highest point in the whole country. * According to a French engineer’s estimate, it considerably exceeds the above-given altitude, being—so he says—2700 metres hich. VIRGIN FOREST. 27 Another interesting physical feature of Madagascar, which has only been made clear very recently, is the existence of an almost continuous belt of virgin forest all round the island, and generally following the coast-line. This forest divides into two belts on the eastern side of the country, leaving a long narrow valley about 250 miles long between the two lines. The uppermost of these clothes the slopes which form the edge of the upper plateau of the island. North of this valley the two lines unite, and here is the widest portion of the forest, it being about forty miles across. The average breadth is from fifteen to twenty miles. On the north-west side the two lines overlap each other nearly 100 miles, leaving an opening about seventy miles wide. The total length of this forest must be about 2300 miles, and much of this is yet un- explored, so that there is doubtless still much of interest in botanical science awaiting research. Besides the forest belt, a good deal of the country to the west and south is well wooded. A third fact of interest in the physical geography of Mada- gascar is the extensive evidence of recent volcanic action throughout a great part of the country. It has been known for several years that there were signs of this on the north- west coast, and that in the island of Nosibé and the adja- cent mainland there are numerous extinct craters and much igneous rock. A few years ago the Rev. T. Campbell, of the Church Missionary Society, pointed out evident traces of volcanic agency in the district near the Ankaratra hills. He says: “It seemed as if the whole place were once a great smeltery, from the enormous number of clinkers lying about. There were altogether five mountains, all near to each other, which have been active volcanoes at some remote period; each has one of its sides melted down, and the inside hollowed out. The flow of lava looks as if it had been some immense reservoir bursting its banks, and the water dashing and foam- ing through, bearing everything away with it, or covering the plain beneath.” In a journey I took to the lake Itasy in 1866, I was struck with the number of truncated cones in the hills sur- rounding the lake. But extensive journeys made more recently in various directions have revealed the existence of 28 EXTINCT VOLCANOES. a very widespread and powerful subterranean action through- out a great part of the island, probably extending almost unbroken from the south-east to the north-west and extreme north. There seems reason to believe that this volcanic belt is part of a line which has its eastern extremity in the island of Réunion, where there is a volcano still showing occasional sions of activity; while the other (north-western) extremity passes through the Comoro group (the islands of which consist of grand masses of lofty volcanic mountains), and terminates in the island of Great Comoro, where also, as in Réunion, is a still active volcano. It would seem as if the subterranean forces had expended their energy in the intermediate space, for there is no active voleano in Madagascar, while at each end of the line their presence is still occasionally felt. There are, however, signs of not altogether extinct forces in the slight earthquake-shocks which are felt almost every year, and in the hot springs of various kinds which occur in many parts of the country. A large number of extinct volcanoes are found west of Lake Itasy. These are thus described by Dr. Mullens: “When we ascended the lofty hill overhanging the western end of the lake, crater after crater met cur astonished gaze. Some were of enormous size, some were small; some were cones, others were hollow, or were horseshoe in shape, and had long ridges of lava running out from the open side. There were forty craters in all, of which we were sure; we think there were others beyond to the north.” “ Fifty miles farther south we came on the volcanoes again. We climbed a lofty rounded hill called Ivéko, and then found that we were on the crater wall. The inner hollow was a quarter of a mile wide, the height of the wall above the level country outside was 1000 feet. Two lava streams went out towards the south and west; three small craters were at the foot, and others, large and conspicuous, were around us on every side. Close by, another huge crater, Iatsifitra, had its opening to- wards the north, and the lava that had issued from it was fresh, black, and sharp, as if broken yesterday. But stranger still, at its eastern side was a plain a mile square, covered with heaps of lava like stone cottages, fortresses, ruined VOLCANIC ACTION. 29 palaces. I counted thirty greater piles and noted numberless smaller ones; it was clear that at one time the entire plain had been on fire, that a hundred jets of fire and flame and molten lava had spouted from its surface. The heaps were now old and moss-grown, but we were informed of a vague tradition among the people that their ancestors had seen these flames bursting forth. Altogether, in that important journey, we saw and counted a hundred extinct craters, ex- tending over an are of ninety miles, not reckoning the central mass of Ankaratra, round one side of which that arc bends.”’* In a journey to the south-east of Madagascar I discovered traces of volcanic action in many places, in some parts shown in the deposits of rolled pebbles of lava, and in others in the streams of lava rock running into the sea and forming reefs which are being gradually broken up by the surf. And in the very opposite part of the island, on the extreme north- west coast, opposite the Minnow group of islets, Bishop Kestell- Cornish observes: “This coast is the most distinctly volcanic that I have seen in Madagascar; at one point the lava must have run down to be quenched in the sea, and it looked as if this had taken place only last year.” t In the Antsihanaka province also the same plutonic agency is distinctly visible. A great part of this region consists of an immense marshy plain, about thirty-five miles long by fifteen wide, with the lake Aladtra at its north-east corner and sur- rounded by hills; and it has evidently been the seat of some powerful subterranean force by which this depression was caused. This is clear from the fact that the lines of hills which are seen on both sides of the Antsihanaka plain do not run in the same direction as the main valley or depression of the country, but cut it at an angle of about 45°; so that while the general direction of the valley is N.N.E. and 8.8. W., the lines of hills on either side have a bearing of N.N.W. and S.S.E. Many of the ridges seem to be broken off more or less abruptly by the level ground for several miles, and then are continued on the other side of the plain. It was impos- sible to avoid the conclusion that by some great convulsion * Proc. Roy. Geog. Soc., January 25, 1875. + Antandnarivo Annual, No. iii. p. 22. 30 A PLUTONIC VALLEY. a vast rent and depression had been made across the lines of hills in a diagonal direction; while the water-worn and wasted remains of some few of these towards the south, forming a line of low detached hills, suggested that probably the action of water, either as an arm of the sea or a great river, had completed what was commenced by more violent agencies, The evidence of former volcanic action in the presence of extinct craters and lava streams to the west, north, and north-east of the plain, gives considerable support to this supposition. About a hundred miles north of the Antsihanaka pro- vince there seem to be further traces of volcanic action. The Rev. J. A. Houlder thus describes a remarkable valley called Mandritsira, which, until he saw it in 1876, was unknown to Europeans even by name, and not marked upon any map: “Tt is a great basin, or rather a mighty elongated pit, sunk deep down among the surrounding heights. It is about thirty miles long, and nearly 2000 feet below the level of the country east and west of it. Dante would have imagined it, not a ‘circle’ certainly, but a remnant of some region of the horrible pit itself, which for a wise and gracious purpose had been gently touched by the cooling breath of heaven. There had evidently been a great commotion going on there in the ages gone by, for all the long valley was dotted with rounded hills, giving it the look of boiling water or bubbling pitch, which by some strange process had suddenly become congealed.” It will therefore be seen that igneous agency has been a powerful factor in shaping the physical geography of many portions of Madagascar, and that in few places could that agency have been present on a grander scale than in the great volcanic region of which Madagascar is the centre, and the Comoro and Mascarene groups the extreme points in either direction. An attempt has been made in the accompanying sketch- map to show the prominent features in the physical geography of the island already noted. Probably closer examination would show that the detached groups of extinct craters are | all connected by intermediate links, so as to form a continuous GLOLOGICAL FORMATION. 31 line of igneous disturbance from the extreme northern point of Madagaséar to at least as far south as the twenty-third parallel; and from the appearance of a line of hills seen at a distance south of this latitude, I am strongly inclined to believe that there has been subterranean agency at work even beyond the upper granitic plateaux, but no examination has yet been made of this southernmost region. With regard to the geology of Madagascar, but little is at present known with any exactness, for no competent geolo- gist has yet made a systematic examination of the country. There are, however, a few facts of a general character which have been noted by various observers, and these may be here collected together as a slight contribution to a knowledge of this subject, pending a more complete and scientific treatment of it. As already mentioned, the elevated region which forms so large a part of the central, northern, and eastern portions of the island is largely composed of Primary and igneous rocks. Granite, gneiss, and basalt are present almost all through this high region, and generally form the loftiest points in the country. In a single hill there is often a considerable variety of rock both in colour and texture—granite of various shades of grey, red, and rose-colour, with the constituent parts both fine and coarse. Veins of quartz, running both through these and the clays by which they are overlaid, are often met with, and very fine specimens of rock-crystal are frequently found. A hard, whitish, and durable stone, which has some resem- blance to the Yorkshire stone called Bramley Fall, is used in Antananarivo for public buildings, as well as for the native tombs. The lower hills, as well as the high moors, are usually com- posed of a bright red clay, but below the surface this often seems to pass into a light pink or white earth, resembling kaolin or china clay. This frequent change of colour would lead one to infer that atmospheric influences had something to do with the difference between the surface clay and that exposed in the numerous precipitous clefts which the rains excavate on the hillsides. In many places the material found amongst the rock seems exactly like granite in its con- 32 LIME AND SLATE, stituent parts, but without the cementing element, so that it can be cut quite easily by a spade. The red clay is some- times varied by a light brown clay on the hills, while the plains and valleys are filled with rich alluvial clays, blue and black in colour. In all these clays there is an apparently total absence of all organic remains, either animal or vege- table, so that it is not an easy task to determine their geolo- gical age; and there is little sign of stratification, although I have detected some appearance of this in the rocks, with tilting of the strata. In this elevated region there seem to be few, if any, sedimentary rocks of a more recent age than the Primary ones which are so prominent a feature of it. A soft dark- red stone is found in some places, but this appears to be only a hardened clay. Columnar basalt has been noticed at some points, as well as extensive beds of volcanic ash, decomposed lava, scoria, and lava rock of all varieties of hardness, in some of which crystals of olivine are found in abundance. At one point, however, in the upper region of the island, a limestone deposit occurs. This is at Sirabé, to the south-west of the Ankaratra mountains; and from the pits dug here most of the lime used for building in the central province is procured. It has not yet been examined by any one with competent scientific knowledge, but it appears to be a sulphate of lime, and is probably only a local deposit and not a stratified rock, and most likely is connected with the subterranean action so visible all around the district. Jets of carbonic acid gas are found in the plain among the lime, and from one of the springs which rise up to the surface a rock has been deposited with stalactite caves in its sides. Clay-slate is met with in the southern part of this elevated region, and in the Bétsiléo country a valuable slate, suitable both for building and for writing upon, is found, although it has not yet been worked to any extent. The royal chapel at Antananarivo is roofed with this native slate. According to some accounts, greywacke or whinstone, silex, and chert, with chalcedony, are also met with in the southern highlands. From certain of the facts above given, as well as from other considerations, it appears highly probable that this FOSSILS. 33 extensive elevated region of Madagascar is very ancient land, and has probably remained for many ages above the waters of the Indian Ocean ; otherwise some trace of marine deposits would surely be found in portions of this great extent of country. I may, however, here note the fact that there are in some places such rounded boulder-like masses of blue basalt rock, sometimes on the surface, and sometimes partially embedded in the soil, that did these occur in the temperate region one would certainly ascribe them to glacial action ; but the point requires fuller investigation, and possibly some other solution may be given to the rather puzzling inquiry suggested. But in travelling to the north-west coast, as we got near the sea-level on the banks of the Bétsibdka, we met with rounded boulders composed of rock which certainly does not exist im situ anywhere near the spot where these boulders occur, but has come from far away in the interior. With regard to the lower region of Madagascar—the extensive plains to the west and south of the island, as well as the narrower extent of country on the east coast—we have a little more definite information as to the geology of some portions of it. This division of the country is at a much less elevation above the sea, being only as many hundreds of feet above it as the granitic region is thousands of feet. Here we find not only deposits of the later Tertiary epochs, con- taining fossils of animals but recently extinct, but also fossils of the Secondary age. This fact was first pointed out by M. Grandidier, who, in speaking of the south and west portions of the country, says: “Nerinea and other charac- teristic fossils of the Jurassic formation which I have there collected prove the existence of Secondary strata which cover a vast extent of this island” (Bull. de la Soc. de Géog., Aovt 1871, p. 88). In a later number of the same publication (Avril 1872) he also speaks of an extensive “terrain num- mulitique parfaitement charactérisé par des Neritina schmi- deliana, et pétri de foraminiféres appartenant aux genres Alveolina, Orbitoides, Triloculina,” &c. This is confirmed by the fossils discovered in the south-west of Madagascar, in the upper part of the valley of the St. Augustine River, by the Rev. J. Richardson in 1877. These occur in vast numbers, Cc 34 SANDSTONE. and from a drawing he gives of them appear to belong to the Neocomian formation, and are species of the genera Ammonites, Terebratula, Nerinea or Turritella, Einoceramus, and Rhyn- conella, together with an Echinoderm. It is evident, also, that there are deposits of a much later date than the above, for in the south-west of Madagascar M. Grandidier discovered the fossil remains of a hippopotamus (a pachyderm not now found living in the island), of gigantic tortoises (which are now only found in the little island of Aldebra to the north of Madagascar), and of the probably very recently-extinct struthious bird, the “pyornis maximus, whose egg (124 in. x 9} in.) so far exceeds that of any other known bird. It seems highly probable, therefore, that a systematic examination of these less elevated portions of Madagascar would reveal the existence of much that is in- teresting and valuable both in paleontology and geology, and so light would be thrown upon many problems connected with the anomalous animal life of the country and of neigh- bouring islands in the Indian Ocean. It is evident that these maritime plains were under water during portions at least of the Secondary period, at which epoch the high grani- tic region alone formed the island of Madagascar, then a country probably only a third of its present extent.* Dr. Auguste Vinson speaks of seeing yellow sandstone on the eastern coast, and he also describes the plain between the two eastern lines of forest as being composed of beds of sedimentary formations, “rich in fossil remains.” Unfor- tunately he gives no particulars as to these alleged extinct organisms, sc we are still in the dark as to the geological age of these formations. In sailing down the river Bétsibdka to the north-west coast, I noticed at one point that for a con- siderable distance the river bank was formed by layers of yellowish sandstone closely resembling a wall of masonry. Some of the courses appeared much weathered, while others had a smooth face, as if of much harder material. * This is confirmed by what is said in a ‘‘ Notice sur une Exploration Géolo- zique de Madagascar, par M. Ed. Guillemin,” in Annales des Mines, 6me séric, t. x., 1806, pp. 277-319, who speaks of fiaznienis of basalt being found far from the sea, at the foot of the mountains and many metres above the sea-level, with sea-shells, apparently of a recent date, attached. LIGNITE. 35 From the account given by an intelligent native of some rocks in the western part of Madagascar, and a little to the south of the centre, a conglomerate seems to be found there, for he describes hard rocks of great size as being filled as thickly as possible with rolled pebbles of all dimensions and shapes. He also mentions that near the sea he found a hard black stone which rang like iron when struck. This occurred in large, flat masses, scattered over the plain, and was full of shells in good preservation. But here, again, no specimens were brought for examination. A little more information as to the geology of Madagascar is found in papers contributed to scientific periodicals in England and France several years ago. The earliest of these is by the late Dr. Buckland, who, in a “ Notice on the Geolo- gical Structure of a Part of the Island of Madagascar” * (Port Louquez, near the northern extremity), describes a sandstone without fossils, which he compares to the New Red Sandstone, and in which are intercalated trap rocks similar to those of Antrim in Ireland. As to the north-west side of Madagascar, in the Annales des Mines (1854, 5me série, t. vi. pp. 570-576) there is an account of the discovery of beds of lignite, both in the island of Nosibé and at two points on the neighbouring coast. In the opinion of the officers who made the exploration, the beds of this combustible are more ancient than the Tertiary forma- tion. It is contained in layers of sandstone and clay schists, is fibrous and shining, and burns readily with a long and white flame, leaving little ash. If beds of this lignite should be discovered in greater thickness, it would therefore be valu- able both as steam coal and for use in the industrial arts. In the same French publication of a little later date (5me série, t. vili, 1856) there is an “Essai sur la Géologie de Nosibé,” in which the soil of that island is described as con- sisting of three different groups of strata: (1) Granitic rock, gneiss, mica schist, slaty schist, and plastic clay; (2) red and yellow sandstones, traversed by veins of gneiss and quartz; while (3) is essentially volcanic, consisting of basaltic and trap lavas, overlaid in some places by beds of sandy material, * Trans. Geol. Soc., London, vol. v. p. 478. 36 CORAL AND MINERALS. tuffs, and volcanic rappilis. This essay is accompanied by a complete geological map of Nosibé. Since the date of this last paper some further attention has been paid to this part of the country, in connection with the French company promoted by M. Lambert (see Annales des Mines, Ome série, t. x. pp. 277-319), but hardly anything more has been done towards a scientific examination of other portions of Madagascar, except a notice of the peninsula en- closing Antongil Bay on the north-east coast (Bull. de la Soe. de Géoq., Sept. et Oct. 1867), although probably M. Grandidier will have some fuller information in his great work now in progress. It may be here observed that a (barrier?) reef of coral extends from 200 to 300 miles along the south-east coast of Madagascar, varying in its distance from the land from a yuarter of a mile to three or four miles; while fringing reefs surround the northern end of the island, extending for 250 miles along its western side, and for 400 miles down its eastern side, and are also found on the south-west coast. Mr. Darwin gives in his work on “The Structure and Distribu- tion of Coral Reefs” (pp. 104, 105) some facts showing the wonderfully rapid growth of various species of coral on the east. coast of Madagascar. The northern extremity of the country is said by Captain Owen to be formed of madre- poritic rock. With regard to minerals, Madagascar is tolerably rich in some of the most useful metals. Iron is found in great abundance in Imé¢rina, sometimes almost in a pure state. In some of the hills it is so plentiful that it is difficult to get a bearing with a compass from the deflection caused by the iron in the ground. Copper and silver have also been discovered, and from the geological structure of the country it is highly probable that gold would also be found in some of the ravines of the granitic highlands; but as it is at present a serious offence against the native laws to search for the precious metals, hardly anything has been done in this direction, Rock-salt is found near the coast, and nitre is also met with. Iron pyrites, from which sulphur is extracted, is also found in abundance; and in the northern part of the island RAINFALL, 37 antimony seems to be plentiful; and oxide of manganese has been found about fifty miles south of the capital.