Part 1 (1/2)
Pagan Tribes of Borneo.
by Hose & McDougall.
Preface
In writing this book we have aimed at presenting a clear picture of the pagan tribes of Borneo as they existed at the close of the nineteenth century. We have not attempted to embody in it the observations recorded by other writers, although we have profited by them and have been guided and aided by them in making our own observations. We have rather been content to put on record as much information as we have been able to obtain at first hand, both by direct observation of the people and of their possessions, customs, and manners, and by means of innumerable conversations with men and women of many tribes.
The reader has a right to be informed as to the nature of the opportunities we have enjoyed for collecting our material, and we therefore make the following personal statement. One of us (C. H.) has spent twenty-four years as a Civil Officer in the service of the Rajah of Sarawak; and of this time twenty-one years were spent actually in Sarawak, while periods of some months were spent from time to time in visiting neighbouring lands -- Celebes, Sulu Islands, Ternate, Malay Peninsula, British North Borneo, and Dutch Borneo. Of the twenty-one years spent in Sarawak, about eighteen were pa.s.sed in the Baram district, and the remainder mostly in the Rejang district. In both these districts, but especially in the Baram, settlements and representatives of nearly all the princ.i.p.al peoples are to be found; and the nature of his duties as Resident Magistrate necessitated a constant and intimate intercourse with all the tribes of the districts, and many long and leisurely journeys into the far interior, often into regions which had not previously been explored. Such journeys, during which the tribesmen are the magistrate's only companions for many weeks or months, and during which his nights and many of his days are spent in the houses of the people, afford unequalled opportunities for obtaining intimate knowledge of them and their ways. These opportunities have not been neglected; notes have been written, special questions followed up, photographs taken, and sketches made, throughout all this period.
In the years 1898 -- 9 the second collaborator (W. McD.) spent the greater part of a year in the Baram district as a member of the Cambridge Anthropological Expedition, which, under the leaders.h.i.+p of Dr. A. C. Haddon, went out to the Torres Straits in the year 1897. During this visit we co-operated in collecting material for a joint paper on the animal cults of Sarawak;[1] and this co-operation, having proved itself profitable, suggested to us an extension of our joint program to the form of a book embodying all the information already to hand and whatever additional information might be obtainable during the years that one of us was still to spend in Borneo. The book therefore may be said to have been begun in the year 1898 and to have been in progress since that time; but it has been put into shape only during the last few years, when we have been able to come together for the actual writing of it.
During the year 1899 Dr. A. C. Haddon spent some months in the Baram district, together with other members of the Cambridge Expedition (Drs. C. G. Seligmann, C. S. Myers, and Mr. S. Ray); and we wish to express our obligation to him for the friendly encouragement in, and stimulating example of, anthropological field work which he afforded us during that time, as well as for later encouragement and help which he has given us, especially in reading the proofs of the book and in making many helpful suggestions. We are indebted to him also for the Appendix to this book, in which he has stated and discussed the results of the extensive series of physical measurements of the natives that he made, with our a.s.sistance, during his visit to Sarawak.
We have pleasure in expressing here our thanks to several other gentlemen to whom we are indebted for help of various kinds -- for permission to reproduce several photographs, to Dr. A. W. Nieuwenhuis, the intrepid explorer of the interior of Dutch Borneo, who in his two fine volumes (QUER DURCH BORNEO) has embodied the observations recorded during two long journeys in the interior; to Mr. H. Ling Roth for the gift of the blocks used in the preparation of his well-known work, THE NATIVES OF SARAWAK AND BRITISH NORTH BORNEO, many of which we have made use of; to Dr. W. H. Furness, author of THE HOME LIFE OF BORNEO HEAD-HUNTERS (1902), for several photographic plates made by him during his visits to the Baram in the years 1897 and 1898; to Drs. C. G. Seligmann and C. S. Myers for permission to reproduce several photographs; to Mr. R. Shelford, formerly Curator of the Sarawak Museum, for his permission to incorporate a large part of a paper published jointly with one of us (C. H.) on tatu in Borneo, and for measurements of Land Dayaks made by him; to Mr. R. S. Douglas, formerly a.s.sistant Officer in the Baram district and now Resident of the Fourth Division of Sarawak, for practical help genially afforded on many occasions.
Finally, it is our agreeable duty to acknowledge our obligation to H.H. the Rajah of Sarawak, who welcomed to his country the members of the Cambridge Anthropological Expedition, and without whose enlightened encouragement of scientific work on the part of his officers this book would never have been written.
C. H.
W. McD.
JULY 1912.
Supplementary Preface by one of the Authors
I feel that it is necessary to supplement our joint-preface with some few words of apology for, and explanation of, the appearance of my name on the t.i.tle-page of this book. For the book is essentially an attempt to set forth in condensed form the ma.s.s of knowledge of the tribes of Borneo acquired by Dr. Hose in the course of a quarter of a century's intimate study of, and sympathetic companions.h.i.+p with, the people of the interior. My own part in its production has been merely that of a midwife, though I may perhaps claim to have helped in the was.h.i.+ng and dressing of the infant as well as in its delivery, and even to have offered some useful advice during the long years of pregnancy. And, since it is more difficult to present a brief and popular account of any complex subject the more intimate is one's knowledge of it, I may fairly hope that my superficial acquaintance with the pagan tribes of Borneo has been a useful ally to Dr. Hose's profound and extensive knowledge of them; I have therefore gladly accepted my friend's generous invitation to place my name beside his as joint-author of this work.
W. McD.
CHAPTER 1
Geography of Borneo
Borneo is one of the largest islands of the world. Its area is roughly 290,000 square miles, or about five times that of England and Wales. Its greatest length from north-east to south-west is 830 miles, and its greatest breadth is about 600 miles. It is crossed by the equator a little below its centre, so that about two-thirds of its area lie in the northern and one-third lies in the southern hemisphere. Although surrounded on all sides by islands of volcanic origin, Borneo differs from them in presenting but small traces of volcanic activity, and in consisting of ancient ma.s.ses of igneous rock and of sedimentary strata.
The highest mountain is Kinabalu, an isolated ma.s.s of granite in the extreme north, nearly 14,000 feet in height. With this exception the princ.i.p.al mountains are grouped in several ma.s.sive chains, which rise here and there to peaks about 10,000 feet above the sea. The princ.i.p.al of these chains, the Tibang-Iran range, runs south-westward through the midst of the northern half of the island and is prolonged south of the equator by the Schwaner chain. This median south-westerly trending range forms the backbone of the island. A second much-broken chain runs across the island from east to west about 1[degree]
north of the equator. Besides these two princ.i.p.al mountain chains which determine the main features of the river-system, there are several isolated peaks of considerable height, and a minor ridge of hills runs from the centre towards the south-cast corner. With the exception of the northern extremity, which geographically as well as politically stands apart from the rest of the island, the whole of Borneo may be described as divided by the two princ.i.p.al mountain chains into four large watersheds. Of these, the north-western basin, the territory of Sarawak, is drained by the Rejang and Baram, as well as by numerous smaller rivers. Of the other three, which const.i.tute Dutch Borneo, the north-eastern is drained by the Batang Kayan or Balungan river; the south-eastern by the Kotei and Banjermasin rivers; and the south-western by the Kapuas, the largest of all the rivers, whose course from the centre of the island to its south-west corner is estimated at 700 miles. Although the point of intersection of the two princ.i.p.al mountain chains lies almost exactly midway between the northern and southern and the eastern and western extremities of the island, the greater width of the southern half of the island gives a longer course to the rivers of that part, in spite of the fact that all the six princ.i.p.al rivers mentioned above have their sources not far from this central point. The princ.i.p.al rivers thus radiate from a common centre, the Batang Kayan flowing east-north-east, the Kotei south-east by east, the Banjermasin south, the Kapuas a little south of west, the Rejang west, and the Baram north-west. This radiation of the rivers from a common centre is a fact of great importance for the understanding of the ethnography of the island, since the rivers are the great highways which movements of the population chiefly follow.
In almost all parts of the island, the land adjoining the coast is a low-lying swampy belt consisting of the alluvium brought down by the many rivers from the central highlands. This belt of alluvium extends inland in many parts for fifty miles or more, and is especially extensive in the south and south-east of the island.
Between the swampy coast belt and the mountains intervenes a zone of very irregular hill country, of which the average height above the sea-level is about one thousand feet, with occasional peaks rising to five or six thousand feet or more.
There seems good reason to believe that at a comparatively recent date Borneo was continuous with the mainland of Asia, forming its south-eastern extremity. Together with Sumatra and Java it stands upon a submarine bank, which is nowhere more than one hundred fathoms below the surface, but which plunges down to a much greater depth along a line a little east of Borneo (Wallace's line). The abundance of volcanic activity in the archipelago marks it as a part of the earth's crust liable to changes of elevation, and the acc.u.mulation of volcanic matter would tend to make it an area of subsidence; while the north-east monsoon, which blows with considerable violence down the China Sea for about four months of each year, may have hastened the separation of Borneo from the mainland. That this separation was effected in a very recent geological period is shown by the presence in Borneo of many species of Asiatic mammals both large and small, notably the rhinoceros (R. BORNIENSIS, closely allied to R. SUMATRa.n.u.s); the elephant (E. INDICUS, which, however, may have been imported by man); the wild cattle (BOS SONDIACUS, which occurs also in Sumatra); several species of deer and pig (some of which are found in Sumatra and the mainland); several species of the cat tribe, of which the tiger-cat (FELIS NEBULOSA) is the largest; the civet-cat (VIVERRA) and its congeners HEMIGALE, PARADOXURUS, and ARCTOGALE; the small black bear (URSUS MALAYa.n.u.s); the clawless otter (LUTRA CINEREA); the bear-cat (ARCTICTIS BINTURONG); the scaly ant-eater (MANIS JAVANICUS); the lemurs (TARSIUS SPECTRUM and NYCTICEBUS TARDIGRADUS); the flying lemur (GALEOPITHECUS VOLANS); the porcupine (HYSTRIX CRa.s.sISPINIS); numerous bats, squirrels, rats and mice; the big shrew (GYMNURA); several species of monkeys, and two of the anthropoid apes. The last are of peculiar significance, since they are incapable of crossing even narrow channels of water, and must be regarded as products of a very late stage of biological evolution. Of these two anthropoid species, the gibbon (HYLOBATES MULLERI) is closely allied to species found in the mainland and in Sumatra, while the MAIAS or orang-utan (SIMIA SALYRUS) is found also in Sumatra and, though not now surviving on the continent, must be regarded as related to anthropoids whose fossil remains have been discovered there.[2]
The zoological evidence thus indicates a recent separation of Borneo and Sumatra from the continent, and a still more recent separation between the two islands.
The climate of the whole island is warm and moist and very equable. The rainfall is copious at all times of the year, but is rather heavier during the prevalence of the north-east monsoon in the months from October to February, and least during the months of April and May. At Kuching, during the last thirty years, the average yearly rainfall has been 160 inches, the maximum 225, and the minimum 102 inches; the maximum monthly fall recorded was 69 inches, and the minimum .66, and the greatest rainfall recorded in one day was 15 inches. The temperature hardly, if ever, reaches 100[degree] F.; it ranges normally between 70[degree] and 90[degree]
F.; the highest reading of one year (1906) at Kuching was 94[degree], the lowest 69[degree]. Snow and frost are unknown, except occasionally on the summits of the highest mountains. Thunder-storms are frequent and severe, but wind-storms are not commonly of any great violence.