The Bontoc Igorot Part 1

The Bontoc Igorot.

by Albert Ernest Jenks.

Preface

After an expedition of two months in September, October, and November, 1902, among the people of northern Luzon it was decided that the Igorot of Bontoc pueblo, in the Province of Lepanto-Bontoc, are as typical of the primitive mountain agriculturist of Luzon as any group visited, and that ethnologic investigations directed from Bontoc pueblo would enable the investigator to show the culture of the primitive mountaineer of Luzon as well as or better than investigations centered elsewhere.

Accompanied by Mrs. Jenks, the writer took up residence in Bontoc pueblo the 1st of January, 1903, and remained five months. The following data were gathered during that Bontoc residence, the previous expedition of two months, and a residence of about six weeks among the Benguet Igorot.

The accompanying ill.u.s.trations are mainly from photographs. Some of them were taken in April, 1903, by Hon. Dean C. Worcester, Secretary of the Interior; others are the work of Mr. Charles Martin, Government photographer, and were taken in January, 1903; the others were made by the writer to supplement those taken by Mr. Martin, whose time was limited in the area. Credit for each photograph is given with the halftone as it appears.

I wish to express my grat.i.tude for the many favors of the only other Americans living in Bontoc Province during my stay there, namely, Lieutenant-Governor Truman K. Hunt, M.D.; Constabulary Lieutenant (now Captain) Elmer A. Eckman; and Mr. William F. Smith, American teacher.

In the following pages native words have their syllabic divisions shown by hyphens and their accented syllables and vowels marked in the various sections wherein the words are considered technically for the first time, and also in the vocabulary in the last chapter. In all other places they are unmarked. A later study of the language may show that errors have been made in writing sentences, since it was not always possible to get a consistent answer to the question as to what part of a sentence const.i.tutes a single word, and time was too limited for any extensive language study. The following alphabet has been used in writing native words.

A as in FAR; Spanish RAMO A as in LAW; as O in French OR AY as AI in AISLE; Spanish HAY AO as OU in OUT; as AU in Spanish AUTO B as in BAD; Spanish BAJAR CH as in CHECK; Spanish CHICO D as in DOG; Spanish DAR E as in THEY; Spanish HALLE E as in THEN; Spanish COMEN F as in FIGHT; Spanish FIRMAR G as in GO; Spanish GOZAR H as in HE; Tagalog BAHAY I as in PIQUE; Spanish HIJO I as in PICK K as in KEEN L as in LAMB; Spanish LENTE M as in MAN; Spanish MENOS N as in NOW; Spanish JABON NG as in FINGER; Spanish LENGUA O as in NOTE; Spanish NOSOTROS OI as in BOIL P as in POOR; Spanish PERO Q as CH in German ICH S as in SAUCE; Spanish SORDO SH as in SHALL; as CH in French CHARMER T as in TOUCH; Spanish TOMAR U as in RULE; Spanish UNO U as in BUT U as in German KUHL V as in VALVE; Spanish VOLVER W as in WILL; nearly as OU in French OUI Y as in YOU; Spanish YA

It seems not improper to say a word here regarding some of my commonest impressions of the Bontoc Igorot.

Physically he is a clean-limbed, well-built, dark-brown man of medium stature, with no evidence of degeneracy. He belongs to that extensive stock of primitive people of which the Malay is the most commonly named. I do not believe he has received any of his characteristics, as a group, from either the Chinese or j.a.panese, though this theory has frequently been presented. The Bontoc man would be a savage if it were not that his geographic location compelled him to become an agriculturist; necessity drove him to this art of peace. In everyday life his actions are deliberate, but he is not lazy. He is remarkably industrious for a primitive man. In his agricultural labors he has strength, determination, and endurance. On the trail, as a cargador or burden bearer for Americans, he is patient and uncomplaining, and earns his wage in the sweat of his brow. His social life is lowly, and before marriage is most primitive; but a man has only one wife, to whom he is usually faithful. The social group is decidedly democratic; there are no slaves. The people are neither drunkards, gamblers, nor "sportsmen." There is little "color" in the life of the Igorot; he is not very inventive and seems to have little imagination. His chief recreation -- certainly his most-enjoyed and highly prized recreation -- is head-hunting. But head-hunting is not the pa.s.sion with him that it is with many Malay peoples.

His religion is at base the most primitive religion known -- animism, or spirit belief -- but he has somewhere grasped the idea of one G.o.d, and has made this belief in a crude way a part of his life.

He is a very likable man, and there is little about his primitiveness that is repulsive. He is of a kindly disposition, is not servile, and is generally trustworthy. He has a strong sense of humor. He is decidedly friendly to the American, whose superiority he recognizes and whose methods he desires to learn. The boys in school are quick and bright, and their teacher p.r.o.nounces them superior to Indian and Mexican children he has taught in Mexico, Texas, and New Mexico.[1]

Briefly, I believe in the future development of the Bontoc Igorot for the following reasons: He has an exceptionally fine physique for his stature and has no vices to destroy his body. He has courage which no one who knows him seems ever to think of questioning; he is industrious, has a bright mind, and is willing to learn. His inst.i.tutions -- governmental, religious, and social -- are not radically opposed to those of modern civilization -- as, for instance, are many inst.i.tutions of the Mohammedanized people of Mindanao and the Sulu Archipelago -- but are such, it seems to me, as will quite readily yield to or a.s.sociate themselves with modern inst.i.tutions.

I recall with great pleasure the months spent in Bontoc pueblo, and I have a most sincere interest in and respect for the Bontoc Igorot as a man.

Introduction

The readers of this monograph are familiar with the geographic location of the Philippine Archipelago. However, to have the facts clearly in mind, it will be stated that the group lies entirely within the north torrid zone, extending from 4[degree] 40' northward to 21[degree]

3' and from 116[degree] 40' to 126[degree] 34' east longitude. It is thus about 1,000 miles from north to south and 550 miles from east to west. The Pacific Ocean washes its eastern sh.o.r.es, the Sea of Celebes its southern, and the China Sea its western and northern sh.o.r.es. It is about 630 kilometers, or 400 miles, from the China coast, and lies due east from French Indo-China. The Batanes group of islands, stretching north of Luzon, has members nearer Formosa than Luzon. On the southwest Borneo is sighted from Philippine territory.

Briefly, it may be said the Archipelago belongs to Asia -- geologically, zoologically, and botanically -- rather than to Oceania, and that, apparently, the entire Archipelago has shared a common origin and existence. There is evidence that it was connected with the mainland by solid earth in the early or Middle Tertiary. For a long geologic time the land was low and swampy. At the end of the Eocene a great upheaval occurred; there were foldings and crumplings, igneous rock was thrust into the distorted ma.s.s, and the islands were considerably elevated above the sea. During the latter part of the Tertiary period the lands seem to have subsided and to have been separated from the mainland.

About the close of the subsidence eruptions began which are continued to the present by such volcanoes as Taal and Mayon in Luzon and Apo in Mindanao. No further subsidence appears to have occurred after the close of the Tertiary, though the gradual elevation beginning then had many lapses, as is evidenced by the numerous sea beaches often seen one above the other in horizontal tiers. The elevation continues to-day in an almost invisible way. The Islands have been greatly enlarged during the elevation by the constant building of coral around the submerged sh.o.r.es.

It is believed that man had appeared in the great Malay Archipelago before this elevation began. It is thought by some that he was in the Philippines in the later Tertiary, but there are no data as yet throwing light on this question.

To-day the Archipelago lies like a large net in the natural pathway of people fleeing themselves from the supposed birthplace of the primitive Malayan stock, namely, from Java, Sumatra, and the adjacent Malay Peninsula, or, more likely, the larger mainland. It spreads over a large area, and is well fitted by its numerous islands -- some 3,100 -- and its innumerable bays and coastal pockets to catch up and hold a primitive, seafaring people.

There are and long have been daring Malayan pirates, and there is to-day among the southern islands a numerous cla.s.s -- the Samal -- living most of the time on the sea, yet they all keep close to land, except in time of calm, and when a storm is brewing they strike out straight for the nearest sh.o.r.e like scared children. The ocean currents and the monsoons have been greatly instrumental in driving different people through the seas into the Philippine net.[2] The Tagakola on the west coast of the Gulf of Davao, Mindanao, have a tradition that they are descendants of men cast on their present sh.o.r.es from a distant land and of the Man.o.bo women of the territory. The Bagobo, also in the Gulf of Davao, claim they came to their present home in a few boats generations ago. They purposely left their former land to flee from head-hunting, a practice in their earlier home, but one they do not follow in Mindanao. What per cent of the people coming originally to the Archipelago was castaway, nomadic, or immigrant it is impossible to judge, but there have doubtless also been many systematic and prolonged migrations from nearby lands, as from Borneo, Celebes, Sangir, etc.

Primitive man is represented in the Philippines to-day not alone by one of the lowest natural types of savage man the historic world has looked upon -- the small, dark-brown, bearded, "crisp-woolly"-haired Negritos -- but by some thirty distinct primitive Malayan tribes or dialect groups, among which are believed to be some of the lowest of the stock in existence.

In northern Luzon is the Igorot, a typical primitive Malayan. He is a muscular, smooth-faced, brown man of a type between the delicate and the coa.r.s.e. In Mindoro the Mangiyan is found, an especially lowly Malayan, who may prove to be a true savage in culture. In Mindanao is the slender, delicate, smooth-faced brown man of which the Subano, in the western part, is typical. There are the Bagobo and the extensive Man.o.bo of eastern Mindanao in the neighborhood of the Gulf of Davao, the latter people following the Agusan River practically to the north coast of Mindanao. In southeastern Mindanao, in the vicinity of Mount Apo and also north of the Gulf of Davao, are the Ata. They are a scattered people and evidently a Negrito and primitive Malayan mixture. In Nueva Vizcaya, Nueva Ecija, Isabela, and perhaps Principe, of Luzon, are the Ibilao. They are a slender, delicate, bearded people, with an artistic nature quite different from any other now known in the island, but somewhat like that of the Ata of Mindanao. Their artistic wood productions suggest the incised work of distant dwellers of the Pacific, as that of the people of New Guinea, Fiji Islands, or Hervey Islands. The seven so-called Christian tribes,[3] occupying considerable areas in the coastwise lands and low plains of most of the larger islands of the Archipelago, represent migrations to the Archipelago subsequent to those of the Igorot and comparable tribes.

The last migrations of brown men into the Archipelago are historic. The Spaniard discovered the inward flow of the large Samal Moro group -- after his arrival in the sixteenth century. The movement of this nomadic "Sea Gipsy" Samal has not ceased to-day, but continues to flow in and out among the small southern islands.

Besides the peoples here cited there are a score of others scattered about the Archipelago, representing many grades of primitive culture, but those mentioned are sufficient to suggest that the Islands have been very effective in gathering up and holding divers groups of primitive men.[4]

PART 1

The Igorot Culture Group

Igorot land

Northern Luzon, or Igorot land, is by far the largest area in the Philippine Archipelago having any semblance of regularity. It is roughly rectangular in form, extending two and one-half degrees north and south and two degrees east and west.

There are two prominent geographic features in northern Luzon. One is the beautifully picturesque mountain system, the Caraballos, the most important range of which is the Caraballos Occidentales, extending north and south throughout the western part of the territory. This range is the famous "Cordillera Central" for about three-quarters of its extent northward, beyond which it is known as "Cordillera del Norte." The other prominent feature is the extensive drainage system of the eastern part, the Rio Grande de Cagayan draining northward into the China Sea about two-thirds of the territory of northern Luzon. It is the largest drainage system and the largest river in the Archipelago.

The surface of northern Luzon is made up of four distinct types. First is the coastal plain -- a consistently narrow strip of land, generally not over 3 or 4 miles wide. The soil is sandy silt with a considerable admixture of vegetable matter. In some places it is loose, and s.h.i.+fts readily before the winds; here and there are stretches of alluvial clay loam. The sandy areas are often covered with coconut trees, and the alluvial deposits along the rivers frequently become beds of nipa palm as far back as tide water. The plain areas are generally poorly watered except during the rainy season, having only the streams of the steep mountains pa.s.sing through them. These river beds are broad, "quicky," impa.s.sable torrents in the rainy season, and are shallow or practically dry during half the year, with only a narrow, lazy thread flowing among the bowlders.

This plain area on the west coast is the undisputed dwelling place of the Christian Ilokano, occupying pueblos in Union, Ilokos Sur, and Ilokos Norte Provinces. Almost nothing is known of the eastern coastal plain area. It is believed to be extremely narrow, and has at least one pueblo, of Christianized Tagalog -- the famous Palanan, the scene of Aguinaldo's capture.

The second type of surface is the coastal hill area. It extends from the coastal plain irregularly back to the mountains, and is thought to be much narrower on the eastern coast than on the western -- in fact, it may be quite absent on the eastern. It is the remains of a tilted plain sloping seaward from an alt.i.tude of about 1,000 feet to one of, say, 100 feet, and its hilly nature is due to erosion. These hills are generally covered only with gra.s.ses; the sheltered moister places often produce rank growths of tall, coa.r.s.e cogon gra.s.s.[5]

The soil varies from dark clay loam through the sandy loams to quite extensive deposits of coa.r.s.e gravel. The level stretches in the hills on the west coast are generally in the possession of the Christian peoples, though here and there are small pueblos of the large Igorot group. The Igorot in these pueblos are undergoing transformation, and quite generally wear clothing similar to that of the Ilokano.

The third type of surface is the mountain country -- the "temperate zone of the Tropics"; it is the habitat of the Igorot. From the western coastal hill area the mountains rise abruptly in parallel ranges lying in a general north and south direction, and they subside only in the foothills west of the great level bottom land bordering the Rio Grande de Cagayan. The Cordillera Central is as fair and about as varied a mountain country as the tropic sun s.h.i.+nes on. It has mountains up which one may climb from tropic forest jungles into open, pine-forested parks, and up again into the dense tropic forest, with its drapery of vines, its varied hanging orchids, and its graceful, lilting fern trees. It has mountains forested to the upper rim on one side with tropic jungle and on the other with st.u.r.dy pine trees; at the crest line the children of the Tropics meet and intermingle with those of the temperate zone. There are gigantic, rolling, bare backs whose only covering is the carpet of gra.s.s periodically green and brown. There are long, rambling, skeleton ranges with here and there pine forests gradually creeping up the sides to the crests. There are solitary volcanoes, now extinct, standing like things purposely let alone when nature humbled the surrounding earth. There are sculptured lime rocks, cities of them, with gray hovels and mansions and cathedrals.

The mountains present one interesting geologic feature. The "hiker" is repeatedly delighted to find his trail pa.s.sing quite easily from one peak or ascent to another over a natural connecting embankment. On either side of this connecting ridge is the head of a deep, steep-walled canyon; the ridge is only a few hundred feet broad at base, and only half a dozen to twenty feet wide at the top. These ridges invariably have the appearance of being composed of soft earth, and not of rock. They are appreciated by the primitive man, who takes advantage of them as of bridges.

The mountains are well watered; the summits of most of the mountains have perpetual springs of pure, cool waters. On the very tops of some there are occasional perpetual water holes ranging from 10 to 100 feet across. These holes have neither surface outlet nor inlet; there are two such within two hours of Bontoc pueblo. They are the favorite wallowing places of the carabao, the so-called "water buffalo,"[6]

both the wild and the half-domesticated animals.

The mountain streams are generally in deep gorges winding in and out between the sharp folds of the mountains. Their beds are strewn with bowlders, often of immense size, which have withstood the wearing of waters and storms. During the rainy season the streams racing between the bases of two mountain ridges are maddened torrents. Some streams, born and fed on the very peaks, tumble 100, 500, even 1,500 feet over precipices, landing white as snow in the merciless torrent at the mountain base. During the dry season the rivers are fordable at frequent intervals, but during the rainy season, beginning in the Cordillera Central in June and lasting well through October, even the natives hesitate often for a week at a time to cross them.

The absence of lakes is noteworthy in the mountain country of northern Luzon -- in fact, in all of northern Luzon. The two large lakes frequently shown on maps of Cagayan Province, one east and one west of the Rio Grande de Cagayan near the eighteenth parallel, are not known to exist, though it is probable there is some foundation for the Spaniards' belief in the existence of at least the eastern one. In the bottom land of the Rio Grande de Cagayan, about six hours west of Cabagan Nuevo, near the provincial border of Cagayan and Isabela, there were a hundred acres of land covered with shallow water the last of October, 1902, just at the end of the dry season of the Cagayan Valley. The surface was well covered with rank, coa.r.s.e gra.s.ses and filled with aquatic plants, especially with lilies. Apparently the waters were slowly receding, since the earth about the margins was supporting the short, coa.r.s.e gra.s.ses that tell of the gradual drying out of soils once covered with water. In the mountains near Sagada, Bontoc Province, there is a very small lake, and one or two others have been reported at Bontoc; but the mountains must be said to be practically lakeless.

Another mountain range of northern Luzon, of which practically no details are known, is the Sierra Madre, extending nearly the full length of the country close to the eastern coast. It seems to be an unbroken, continuous range, and, as such, is the longest mountain range in the Archipelago.

The fourth type of surface is the level areas. These areas lie mainly along the river courses, and vary from a few rods in width to the valley of the Rio Grande de Cagayan, which is often 50 miles in width, and probably more. There are, besides these river valleys, varying tracts of level plains which may most correctly be termed mountain table-lands. The limited mountain valleys and table-lands are the immediate home of the Igorot. The valleys are worn by the streams, and, in turn, are built up, leveled, and enriched by the sand and alluvium deposited annually by the floods. They are generally open, gra.s.s-covered areas, though some have become densely forested since being left above the high water of the streams.

The broad valley of the Rio Grande de Cagayan is not occupied by the Igorot. It is too poorly watered and forested to meet his requirements. It is mainly a vast pasture, supporting countless deer; along the foothills and the forest-grown creek and river bottoms there are many wild hogs; and in some areas herds of wild carabaos and horses are found. Near the main river is a numerous population of Christians. Many are Ilokano imported originally by the tobacco companies to carry on the large tobacco plantations of the valley, and the others are the native Cagayan.

The table-lands were once generally forested, but to-day many are deforested, undulating, beautiful pastures. Some were cleared by the Igorot for agriculture, and doubtless others by forest fires, such as one constantly sees during the dry season destroying the mountain forests of northern Luzon.

General observations have not been made on the temperature and humidity of much of the mountain country of northern Luzon. However, scientific observations have been made and recorded for a series of about ten years at Baguio, Benguet Province, at an alt.i.tude of 4,777 feet, and it is from the published data there gathered that the following facts are gained.[7] The temperature and rainfall are the average means deduced from many years' observations: