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Bible Encyclopedias
Burma
1911 Encyclopedia Britannica
or a province of British India, including the former kingdom of independent Burma, as well as British Burma, acquired by the British Indian government in the two wars of 1826 and 1852. It is divided into Upper and Lower Burma, the former being the territory annexed on 1st January 1886. The province lies to the east of the Bay of Bengal, and covers a range of country extending from the Pakchan river in 9° 55' north latitude to the Naga and Chingpaw, or Kachin hills, lying roughly between the 27th and 28th degrees of north latitude; and from the Bay of Bengal on the west to the Mekong river, the boundary of the dependent Shan States on the east, that is to say, roughly, between the 92nd and tooth degrees of east longitude. The extreme length from north to south is almost 1200 m., and the broadest part, which is in about latitude 210 north, is 575 m. from east to west. On the N. it is bounded by the dependent state of Manipur, by the Mishmi hills, and by portions of Chinese territory; on the E. by the Chinese Shan States, portions of the province of Yunnan, the French province of Indo-China, and the Siamese Shan, or Lao States and Siam; on the S. by the Siamese Malay States and the Bay of Bengal; and on the W. by the Bay of Bengal and Chittagong. The coast-line from Taknaf, the mouth of the Naaf, in the Akyab district on the north, to the estuary of the Pakchan at Maliwun on the south, is about 1200 m. The total area of the province is estimated at 238,738 sq. m., of which Burma proper occupies 168,573 sq. m., the Chin hills 10,250 sq. m., and the Shan States, which comprise the whole of the eastern portion of the province, some 59,915 sq. m.
Natural Divisions
The province falls into three natural divisions: Arakan with the Chin hills, the Irrawaddy basin, and the old province of Tenasserim, together with the portion of the Shan and Karen-ni states in the basin of the Salween, and part of Kengtung in the western basin of the Mekong. Of these Arakan is a strip of country lying on the seaward slopes of the range of hills known as the Arakan Yomas. It stretches from Cape Negrais on the south to the Naaf estuary, which divides it from the Chittagong division of Eastern Bengal and Assam on the north, and includes the districts of Sandoway, Kyaukpyu, Akyab and northern Arakan, an area of some 18,540 sq. m. The northern part of this tract is barren hilly country, but in the west and south are rich alluvial plains containing some of the most fertile lands of the province. Northwards lie the Chin and some part of the Kachin hills. To the east of the Arakan division, and separated from it by the Arakan Yomas, lies the main body of Burma in the basin of the Irrawaddy. This tract falls into four subdivisions. First, there is the highland tract including the hilly country at the sources of the Chindwin and the upper waters of the Irrawaddy, the Upper Chindwin, Katha, Bhamo, Myitkyina and Ruby Mines districts, with the Kachin hills and a great part of the Northern Shan states. In the Shan States there are a few open plateaus, fertile and well populated, and Maymyo in the Mandalay district, the hill-station to which in the hot weather the government of Burma migrates, stands in the Pyin-u-lwin plateauYsome 3500 ft. above the sea. But the greater part of this country is a mass of rugged hills cut deep with narrow gorges, within which even the biggest rivers are confined. The second tract is that known as the dry zone of Burma, and includes thewhole of the lowlands lying between the Arakan Yomas and the western fringe of the Southern Shan States. It stretches along both sides of the Irrawaddy from the north of Mandalay to Thayetmyo, and embraces the Lower Chindwin, Shwebo, Sagaing, Mandalay, Kyaukse, Meiktila, Yamethin, Myingyan, Magwe, Pakokku and Minbu districts. This tract consists mostly of undulating lowlands, but it is broken towards the south by the Pegu Yomas, a considerable range of hills which divides the two remaining tracts of the Irrawaddy basin. On the west, between the Pegu and the Arakan Yomas, stretches the Irrawaddy delta, a vast expanse of level plain 12,000 sq. m. in area falling in a gradual unbroken slope from its apex not far south of Prome down to the sea. This delta, which includes the districts of Bassein, Myaungmya, Thongwa, Henzada, Hantha waddy, Tharrawaddy, Pegu and Rangoon town, consists almost entirely of a rich alluvial deposit, and the whole area, which between Cape Negrais and Elephant Point is 137 m. wide, is fertile in the highest degree. To the east lies a tract of country which, though geographically a part of the Irrawaddy basin, is cut off from it by the Yomas, and forms a separate system draining into the Sittang river. The northern portion of this tract, which on the east touches the basin of the Salween river, is hilly; the remainder towards the confluence of the Salween, Gyaing and Attaran rivers consists of broad fertile plains. The whole is comprised in the districts of Toungoo and Thaton, part of the Karen-ni hills, with the Salween hill tract and the northern parts of Amherst, which form the northern portion of the Tenasserim administrative division. The third natural division of Burma is the old province of Tenasserim, which, constituted in 1826 with Moulmein as its capital, formed the nucleus from which the British supremacy throughout Burma has grown. It is a narrow strip of country lying between the Bay of Bengal and the high range of hills which form the eastern boundary of the province towards Siam. It comprises the districts of Mergui and Tavoy and a part of Amherst, and includes also the Mergui Archipelago. The surface of this part of the country is mountainous and much intersected with streams. Northward from this lies the major portion of the Southern Shan States and Karen-ni and a narrowing strip along the Salween of the Northern Shan States.
Mountains
Burma proper is encircled on three sides by a wall of mountain ranges. The Arakan Yomas starting from Cape Negrais extend northwards more or less parallel with the coast till they join the Chin and Naga hills. They then form part of a system of ranges which curve north of the sources of the Chindwin river, and with the Kumon range and the hills of the Jade and Amber mines, make up a highland tract separated from the great Northern Shan plateau by the gorges of the Irrawaddy river. On the east the Kachin, Shan and Karen hills, extending from the valley of the Irrawaddy into China far beyond the Salween gorge, form a continuous barrier and boundary, and tail off into a narrow range which forms the eastern watershed of the Salween and separates Tenasserim from Siam. The highest peak of the Arakan Yomas, Liklang, rises nearly io,000 ft. above the sea, and in the eastern Kachin hills, which run northwards from the state of Meng Mit to join the high range dividing the basins of the Irrawaddy and the Salween, are two peaks, Sabu and Worang, which rise to a height of 11,200 ft. above the sea. The Kumon range running down from the Hkamti country east of Assam to near Mogaung ends in a peak known as Shwedaunggyi, which reaches some 5750 ft. There are several peaks in the Ruby Mines district which rise beyond 7000 ft. and Loi Ling in the Northern Shan States reaches woo ft. Compared with these ranges the Pegu Yomas assume the proportions of mere hills. Popa, a detached peak in the Myingyan district, belongs to this system and rises to a height of nearly 5000 f t., but it is interesting mainly as an extinct volcano, a landmark and an object of superstitious folklore, throughout the whole of Central Burma. Mud volcanoes occur at Minbu, but they are not in any sense mountains, resembling rather the hot springs which are found in many parts of Burma. They are merely craters raised above the level of the surrounding country by the gradual accretion of the soft oily mud, which overflows at frequent intervals whenever a discharge of gas occurs. Spurs of the Chin hills run down the whole length of the Lower Chindwin district, almost to Sagaing, and one hill, Powindaung, is particularly noted on account of its innumerable cave temples, which are said to hold no fewer than 446,444 images of Buddha. Huge caves, of which the most noted are the Farm Caves, occur in the hills near Moulmein, and they too are full of relics of their ancient use as temples, though now they are chiefly visited in connexion with the bats, whose flight viewed from a distance, as they issue from the caves, resembles a cloud of smoke.
Rivers
Of the rivers of Burma the Irrawaddy is the most important. It rises possibly beyond the confines of Burma in the unexplored regions, where India, Tibet and China meet, and seems to be formed by the junction of a number of considerable streams of no great length. Two rivers, the Mali and the N'mai, meeting about latitude 25° 45' some 150 m. north of Bhamo, contribute chiefly to its volume, and during the dry weather it is navigable for steamers up to their confluence. Up to Bhamo, a distance of 900 m. from the sea, it is navigable throughout the year, and its chief tributary in Burma, the Chindwin, is also navigable for steamers for 300 in. from its junction with the Irrawaddy at Pakokku. The Chindwin, called in its upper reaches the Tanai, rises in the hills south-west of Thama, and flows due north till it enters the southeast corner of the Hukawng valley, where it turns north-west and continues in that direction cutting the valley into two almost equal parts until it reaches its north-west range, when it turns almost due south and takes the name of the Chindwin. It is a swift clear river, fed in its upper reaches by numerous mountain streams. The Mogaung river, rising in the watershed which divides the Irrawaddy and the Chindwin drainages, flows south and south-east for 180 m. before it joins the Irrawaddy, and is navigable for steamers as far as Kamaing for about four months in the year. South of Thayetmyo, where arms of the Arakan Yomas approach the river and almost meet that spur of the Pegu Yomas which formed till 1886 the northern boundary of British Burma, the valley of the Irrawaddy opens out again, and at Yegin Mingyi near Myanaung the influence of the tide is first felt, and the delta may be said to begin. The so-called rivers of the delta, the Ngawun, Pyamalaw, Panmawaddy, Pyinzalu and Pantanaw, are simply the larger mouths of the Irrawaddy, and the whole country towards the sea is a close network of creeks where there are few or no roads and boats take the place of carts for every purpose. There is, however, one true river of some size, the Hlaing, which rises near Prome, flows southwards and meets the Pegu river and the Pazundaung creek near Rangoon, and thus forms the estuary which is known as the Rangoon river and constitutes the harbour of Rangoon. East of the Rangoon river and still within the deltaic area, though cut off from the main delta by the southern end of the Pegu Yomas, lies the mouth of the Sittang. This river, rising in the Sham-Karen hills, flows first due north and then southward through the Kyaukse, Yamethin and Toungoo districts, its line being followed by the Mandalay-Rangoon railway as far south as Nyaunglebin in the Pegu district. At Toungoo it is narrow, but below Shwegyin it widens, and at Sittang it is half a mile broad. It flows into the Gulf of Martaban, and near its mouth its course is constantly changing owing to erosion and corresponding accretions. The second river in the province in point of size is the Salween, a huge river, believed from the volume of its waters to rise in the Tibetan mountains to the north of Lhasa. It is in all probability actually longer than the Irrawaddy, but it is not to be compared to that river in importance. It is, in fact, walled in on either side, with banks varying in British territory from 3000 to 6000 ft. high and at present unnavigable owing to serious rapids in Lower Burma and at one or two places in the Shan States, but quite open to traffic for considerable reaches in its middle course. The Gyaing and the Attaran rivers meet the Salween at its mouth, and the three rivers form the harbour of Moulmein, the second seaport of Burma.
Lakes
The largest lake in the province is Indawgyi in the Myitkyina district. It has an area of nearly too sq. m. and is surrounded on three sides by ranges of hills, but is open to the north where it has an outlet in the Indaw river. In the highlands of the Shan hills there are the Inle lakes near Yawnghwe, and in the Katha district also there is another Indaw which covers some 60 sq. m. Other lakes are the Paunglin lake in Minbu district, the Inma lake in Prome, the Tu and Duya in Henzada, the Shahkegyi and the Inyegyi in Bassein, the sacred lake at Ye in Tenasserim, and the Nagamauk, Panzernyaung and Walonbyan in Arakan. The Meiktila lake covers an area of some 5 sq. m., but it is to some extent at least an artificial reservoir. In the heart of the delta numerous large lakes or marshes abounding in fish are formed by the overflow of the Irrawaddy river during the rainy season, but these either assume very diminutive proportions or disappear altogether in the dry season.
Climate
The climate of the delta is cooler and more temperate than in Upper Burma, and this is shown in the fairer complexion and stouter physique of the people of the lower province as compared with the inhabitants of the drier and hotter upper districts as far as Bhamo, where there is a great infusion of other types of the TibetoBurman family. North of the apex of the delta and the boundary between the deltaic and inland tracts, the rainfall gradually lessens as far as Minbu, where what was formerly called the rainless zone commences and extends as far as Katha. The rainfall in the coast districts varies from about 200 in. in the Arakan and Tenasserim divisions to an average of 90 in Rangoon and the adjoining portion of the Irrawaddy 'delta. In the extreme north of Upper Burma the rainfall is rather less than in the country adjoining Rangoon, and in the dry zone the annual average falls as low as 20 and 30 in.
The temperature varies almost as much as the rainfall. It is highest in the central zone, the mean of the maximum readings in such districts as Magwe, Myingyan, Kyaukse, Mandalay and Shwebo in the month of May being close on 100° F., while in the littoral and sub-montane districts it is nearly ten degrees less. The mean of the minimum readings in December in the central zone districts is a few degrees under 60° F. and in the littoral districts a few degrees over that figure. In the hilly district of Mogok (Ruby Mines) the December mean minimum is 36.8° and the mean maximum 79°. The climate of the Chin and Kachin hills and also of the Shan States is temperate. In the shade and off the ground the thermometer rarely rises above 80° F. or falls below 25° F. In the hot season and in the sun as much as 150° F. is registered, and on the grass in the cold weather ten degrees of frost are not uncommon. Snow is seldom seen either in the Chin or Shan hills, but there are snow-clad ranges in the extreme north of the Kachin country. In the narrow valleys of the Shan hills, and especially in the Salween valley, the shade maximum reaches 100° F. regularly for several weeks in April. The rainfall in the hills varies very considerably, but seems to range from about 60 in. in the broader valleys to about 100 in. on the higher forest-clad ranges.
Geology
Geologically, British Burma consists of two divisions, an eastern and a western. The dividing line runs from the mouth of the Sittang river along the railway to Mandalay, and thence continues northward, with the same general direction but curving slightly towards the east. West of this line the rocks are chiefly Tertiary and Quaternary; east of it they are mostly Palaeozoic or gneissic. In the western mountain ranges the beds are thrown into a series of folds which form a gentle curve running from south to north with its convexity facing westward. There is an axial zone of Cretaceous and Lower Eocene, and this is flanked on each side by the Upper Eocene and the Miocene, while the valley of the Irrawaddy is occupied chiefly by the Pliocene. Along the southern part of the Arakan coast the sea spreads over the western Miocene zone. The Cretaceous beds have not yet been separated from the overlying Eocene, and the identification of the system rests on the discovery of a single Cenomanian ammonite. The Eocene beds are marine and contain nummulites. The Miocene beds are also marine and are characterized by an abundant molluscan fauna. The Pliocene, on the other hand, is of freshwater origin, and contains silicified wood and numerous remains of Mammalia. Flint chips, which appear to have been fashioned by hand, are said to have been found in the Miocene beds, but to prove the existence of man at so early a period would require stronger evidence than has yet been brought forward.
The older rocks of eastern Burma are very imperfectly known. Gneiss and granite occur; Ordovician fossils have been found in the Upper Shan States, and Carboniferous fossils in Tenasserim and near Moulmein. Volcanic rocks are not common in any part of Burma, but about 50 m. north-north-east of Yenangyaung the extinct volcano of Popa rises to a height of 3000 ft. above the surrounding Pliocene plain. Intrusions of a serpentine-like rock break through the Miocene strata north of Bhamo, and similar intrusions occur in the western ranges. Whether the mud " volcanoes" of the Irrawaddy valley have any connexion with volcanic activity may be doubted. The petroleum of Burma occurs in the Miocene beds, one of the best-known fields being that of Yenangyaung. Coal is found in the Tertiary deposits in the valley of the Irrawaddy and in Tenasserim. Tin is abundant in Tenasserim, and lead and silver have been worked extensively in the Shan States. The famous ruby mines of Upper Burma are in metamorphic rock, while the jadeite of the Bhamo neighbourhood is associated with the Tertiary intrusions of serpentine-like rock already noticed.' Population. - The total population of Burma in 1901 was 10,490,624 as against 7,722,053 in 1891; but a considerable portion of this large increase was due to the inclusion of the Shan States and the Chin hills in the census area. Even in Burma proper, however, there was an increase during the decade of 1,530,822, or 19.8%. The density of population per square mile is 44 as compared with 167 for the whole of India and S52 for the Bengal Delta. England and Wales have a population more than twelve times as dense as that of Burma, so there is still room for expansion. The chief races of Burma are Burmese (6,508,682), Arakanese (405,143), Karens (717,859), Shans (787,087), Chins (179,292), Kachins (64,405) and Talaings (321,898); but these totals do not include the Shan States and Chin hills. The Burmese in person have the Mongoloid characteristics common to the Indo-Chinese races, the Tibetans and tribes of the Eastern Himalaya. They may be generally described as of a stout, active, well-proportioned form; of a brown but never of an intensely dark complexion, with black, coarse, lank and abundant hair, and a little more beard than is possessed by the Siamese. Owing to their gay and lively disposition the Burmese have been called " the Irish of the East," and like the Irish they are somewhat inclined to laziness. Since the advent of the British power, the immigration of Hindus with a lower standard of comfort and of Chinamen with a keener business instinct has threatened the economic independence of the Burmese in their own country. As compared with the Hindu, the Burmese wear silk instead of cotton, and eat rice instead of the cheaper grains; they are of an altogether freer and less servile, but also of a less practical character. The Burmese women have a keener business instinct than the men, and serve in some degree to redress the balance. The Burmese children are adored by their parents, and are said to be the happiest and merriest children in the world.
Language and Literature
The Burmese are supposed by modern philologists to have come, as joint members of a vast Indo-Chinese immigration swarm, from western China to the head waters of the Irrawaddy and then separated, some to people Tibet and Assam, the others to press southwards into the 1 See also, for geology, W. Theobald, " On the Geology of Pegu." Mem. Geol. Surv. India, vol. x. pt. ii. (1874); F. Noetling, " The Development and Subdivision of the Tertiary System in Burma," Rec. Geol. Surv. India, vol. xxviii. (1895), pp. 5986, pl. ii.; F. Noetling, " The Occurrence of Petroleum in Burma, and its Technical Exploitation," Mem. Geol. Surv. India, vol. xxvii. pt. ii. (1898).
plains of Burma. The indigenous tongues of Burma are divided into the following groups: - (a) The Burmese group.
(b) The Kachin group.
(c) The Kuki-Chin group.
(d) The Tai group.
(e) - The Karen group.
(f) The Upper Middle Mekong or Wa Palaung group.
(g) The North Cambodian group.
B. Malay family (h) The Selung language.
Burmese, which was spoken by 7,006,495 people in the province in 1901, is a monosyllabic language, with, according to some authorities, three different tones; so that any given syllable may have three entirely different meanings only distinguishable by the intonation when spoken, or by accents or diacritical marks when written. There are, however, very many weighty authorities who deny the existence of tones in the language. The Burmese alphabet is borrowed from the Aryan Sanskrit through the Pali of Upper India. The language is written from left to right in what appears to be an unbroken line. Thus Burma possesses two kinds of literature, Pali and Burmese. The Pali is by far the more ancient, including as it does the Buddhist scriptures that originally found their way to Burma from Ceylon and southern India. The Burmese literature is for the most part metrical, and consists of religious romances, chronological histories and songs. The Maha Yazawin or " Royal Chronicle," forms the great historical work of Burma. This is an authorized history, in which everything unflattering to the Burmese monarchs was rigidly suppressed. After the Second Burmese War no record was ever made in the Yazawin that Pegu had been torn away from Burma by the British. The folk songs are the truest and most interesting national literature. The Burmese are fond of stage-plays in which great licence of language is permitted, and great liberty to " gag " is left to the wit or intelligence of the actors.
Government
The province as a division of the Indian empire is administered by a lieutenant-governor, first appointed 1st May 1897, with a legislative council of nine members, five of whom are officials. There are, besides, a chief secretary, revenue secretary, secretary and two under-secretaries, a public works department secretary with two assistants. The revenue administration of the province is superintended by a financial commissioner, assisted by two secretaries, and a director of land records and agriculture, with a land records departmental staff. There is a chief court for the province with a chief justice and three justices, established in May 1900. Other purely judicial officers are the judicial commissioner for Upper Burma, and the civil judges of Mandalay and Moulmein. There are four commissioners of revenue and circuit, and nineteen deputy commissioners in Lower Burma, and four commissioners and seventeen deputy commissioners in Upper Burma. There are two superintendents of the Shan States, one for the northern and one for the southern Shan States, and an assistant superintendent in the latter; a superintendent of the Arakan hill tracts and of the Chin hills, and a Chinese political adviser taken from the Chinese consular service. The police are under the control of an inspector-general, with deputy inspector-general for civil and military police, and for supply and clothing. The education department is under a director of public instruction, and there are three circles - eastern, western and Upper Burma, each under an inspector of schools.
The Burma forests are divided into three circles each under a conservator, with twenty-one deputy conservators. There are also a deputy postmaster-general, chief superintendent and four superintendents of telegraphs, a chief collector of customs, three collectors and four port officers, and an inspector-general of jails. At the principal towns benches of honorary magistrates, exercising powers of various degrees, have been constituted. There are forty-one municipal towns, fourteen of which are in Upper Burma. The commissioners of division are ex officio sessions judges in their several divisions, and also have civil powers, and powers as revenue officers. They are responsible to the lieutenant-governor, each in his own division, for the working of every department of the public service, except the military department, and the branches of the administration directly under the control of the supreme government. The deputy commissioners perform the functions of district magistrates, district judges, collectors and registrars, besides the miscellaneous duties which fall to the principal district officer as representative of government. Subordinate to the deputy commissioners are assistant commissioners, extra-assistant commissioners and myooks, who are invested with various magisterial, civil and revenue powers, and hold charge of the townships, as the units of regular civil and revenue jurisdiction are called, and the sub-divisions of districts, into which most of these townships are grouped. Among the salaried staff of officials, the townships officers are the ultimate representatives of government who come into most direct contact with the people. Finally, there are the village headmen, assisted in Upper Burma by elders, variously designated according to old custom. Similarly in the towns, there are headmen of wards and elders of blocks. In Upper Burma these headmen have always been revenue collectors. The system under which in towns headmen of wards and elders of blocks are appointed is of comparatively recent origin, and is modelled on the village system.
The Shan States were declared to be a part of British India by notification in 1886. The Shan States Act of 1888 vests the civil, criminal and revenue administration in the chief of the The Shan state, subject to the restrictions specified in the sanad States. or patent granted to him. The law to be administered in each state is the customary law of the state, so far as it is in accordance with the justice, equity and good conscience, and not opposed to the spirit of the law in the rest of British India. The superintendents exercise general control over the administration of criminal justice, and have power to call for cases, and to exercise wide revisionary powers. Criminal jurisdiction in cases in which either the complainant or the defendant is a European, or American, or a government servant, or a British subject not a native of a Shan State, is withdrawn from the chiefs and vested in the superintendents and assistant superintendents. Neither the superintendents nor the assistant superintendents have power to try civil suits, whether the parties are Shans or not. In the Myelat division of the southern Shan States, however, the criminal law is practically the same as the law in force in Upper Burma, and the ngwegunhmus, or petty chiefs, have been appointed magistrates of the second class. The chiefs of the Shan States are of three classes: - (1) sawbwas; (2) myosas; (3) ngwegunhmus. The last are found only in the Myelat, or border country between the southern Shan States and Burma. There are fifteen sawbwas, sixteen myosas and thirteen ngwegunhmus in the Shan States proper. Two sawbwas are under the supervision of the commissioner of the Mandalay division, and two under the commissioner of the Sagaing division. The states vary enormously in size, from the 12,000 sq. m. of the Trans-Salween State of Keng Tung, to the 3.95 sq. m. of Nam Hkem in the Myelat. The latter contained only 41 houses with 210 inhabitants in 1897 and has since been merged in the adjoining state. There are five states, all sawbwaships, under the supervision of the superintendent of the northern Shan States, besides an indeterminate number of Wa States and communities of other races beyond the Salween river. The superintendent of the southern Shan States supervises thirty-nine, of which ten are sawbwaships. The headquarters of the northern Shan States are at Lashio, of the southern Shan States at Taung-gyi.
The states included in eastern and western Karen-ni are not part of British India, and are not subject to any of the laws in force in the Shan States, but they are under the supervision of the superintendent of the southern Shan States.
