construction and repair shops here), the Chicago, Rock Island & Pacific, and the Toledo, Peoria & Western (Pennsylvania system) railways; and has an extensive river commerce. The river is spanned here by the Chicago, Burlington & Quincy railway bridge. Many of the residences are on bluffs commanding beautiful views of river scenery; and good building material has been obtained from the Burlington limestone quarries. Crapo Park, of 100 acres, along the river, is one of the attractions of the city. Among the principal buildings are the county court house, the free public library, the Tama building, the German-American savings bank building and the post office. Burlington has three well-equipped hospitals. Among the city's manufactures are lumber, furniture, baskets, pearl buttons, cars, carriages and wagons, Corliss engines, waterworks pumps, metallic burial cases, desks, boxes, crackers, flour, pickles and beer. The factory product in 1905 was valued at $5,779,337, or 29.9% more than in 1900. The first white man to visit the site of Burlington seems to have been Lieutenant Zebulon M. Pike, who came in 1805 and recommended the erection of a fort. The American Fur Company established a post here in 1829 or earlier, but settlement really began in 1833, after the Black Hawk War, and the place had a population of 1200 in 1838. It was laid out as a town and named Flint Hills (a translation of the Indian name, Shokokon) in 1834; but the name was soon changed to Burlington, after the city of that name in Vermont. Burlington was incorporated as a town in 1837, and was chartered as a city in 1838 by the territory of Wisconsin, the city charter being amended by the territory of Iowa in 1839 and 1841. The territorial legislature of Wisconsin met here from 1836 to 1838 and that of Iowa from 1838 to 1840. In 1837 a newspaper, the Wisconsin Territorial Gazette, now the Burlington Evening Gazette, and in 1839 another, the Burlington Hawk Eye, were founded; the latter became widely known in the years immediately following 1872 from the humorous sketches contributed to it by Robert Jones Burdette (b. 1844), an associate editor, known as the "Burlington Hawk Eye Man," who in 1903 entered the Baptist ministry and became pastor of the Temple Baptist church in Los Angeles, California, and among whose publications are Hawkeyetems (1877), Hawkeyes (1879), and Smiles Yoked with Sighs (1900).
BURLINGTON, a city of Burlington county, New Jersey, U.S.A., on the E. bank of the Delaware river, 18 m. N.E. of Philadelphia. Pop. (1890) 7264; (1900) 7392, of whom 636 were foreign-born and 590 were of negro descent; (1905) 8038; (1910) 8336. It is served by the Pennsylvania railway, and by passenger and freight steamboat lines on the Delaware river, connecting with river and Atlantic coast ports. Burlington is a pleasant residential city with a number of interesting old mansions long antedating the War of Independence, some of them the summer homes of old Philadelphia families. The Burlington Society library, established in 1757 and still conducted under its original charter granted by George II., is one of the oldest public libraries in America. At Burlington are St Mary's Hall (1837; Protestant Episcopal), founded by Bishop G.W. Doane, one of the first schools for girls to be established in the country, Van Rensselaer Seminary and the New Jersey State Masonic home. In the old St Mary's church (Protestant Episcopal), which was built in 1703 and has been called St Anne's as well as St Mary's, Daniel Coxe (1674-1739), first provincial grand master of the lodge of Masons in America, was buried; a commemorative bronze tablet was erected in 1907. Burlington College, founded by Bishop Doane in 1864, was closed as a college in 1877, but continued as a church school until 1900; the buildings subsequently passed into the hands of an iron manufacturer. Burlington's principal industries are the manufacture of shoes and cast-iron water and gas pipes. Burlington was settled in 1677 by a colony of English Quakers. The settlement was first known as New Beverly, but was soon renamed after Bridlington (Burlington), the Yorkshire home of many of the settlers. In 1682 the assembly of West Jersey gave to Burlington "Matinicunk Island," above the town, "for the maintaining of a school for the education of youth"; revenues from a part of the island are still used for the support of the public schools, and the trust fund is one of the oldest for educational purposes in the United States. Burlington was incorporated as a town in 1693 (re-incorporated, 1733), and became the seat of government of West Jersey. On the union of East and West Jersey in 1702, it became one of the two seats of government of the new royal province, the meetings of the legislature generally alternating between Burlington and Perth Amboy, under both the colonial and the state government, until 1790. In 1777 the New Jersey Gazette, the first newspaper in New Jersey, was established here; it was published (here and later in Trenton) until 1786, and was an influential paper, especially during the War of Independence. Burlington was chartered as a city in 1784.
See Henry Armitt Brown, The Settlement of Burlington (Burlington, 1878); George M. Hills, History of the Church in Burlington (Trenton, 1885); and Mrs A.M. Gummère, Friends in Burlington (Philadelphia, 1884).
BURLINGTON, a city, port of entry and the county-seat of Chittenden county, Vermont, U.S.A., on the E. shore of Lake Champlain, in the N.W. part of the state, 90 m. S.E. of Montreal, and 300 m. N. of New York. It is the largest city in the state. Pop. (1880) 11,365; (1890) 14,590; (1900) 18,640, of whom 3726 were foreign-born; (1910, census) 20,468. It is served by the Central Vermont and the Rutland railways, and by lines of passenger and freight steamboats on Lake Champlain. The city is attractively situated on an arm of Lake Champlain, being built on a strip of land extending about 6 m. south from the mouth of the Winooski river along the lake shore and gradually rising from the water's edge to a height of 275 ft.; its situation and its cool and equable summer climate have given it a wide reputation as a summer resort, and it is a centre for yachting, canoeing and other aquatic sports. During the winter months it has ice-boat regattas. Burlington is the seat of the university of Vermont (1791; non-sectarian and co-educational), whose official title in 1865 became "The University of Vermont and State Agricultural College." The university is finely situated on a hill (280 ft. above the lake) commanding a charming view of the city, lake, the Adirondacks and the Green Mountains. It has departments of arts, sciences and medicine, and a library of 74,800 volumes and 32,936 pamphlets housed in the Billings Library, designed by H.H. Richardson. The university received the Federal grants under the Morrill acts of 1862 and 1890, and in connexion with it the Vermont agricultural experiment station is maintained. At Burlington are also the Mt St Mary's academy (1889, Roman Catholic), conducted by the Sisters of Mercy; and two business colleges. Among the principal buildings are the city hall, the Chittenden county court house, the Federal and the Y.M.C.A. buildings, the Masonic temple, the Roman Catholic cathedral and the Edmunds high school. Burlington's charitable institutions include the Mary Fletcher hospital, the Adams mission home, the Lousia Howard mission, the Providence orphan asylum, and homes for aged women, friendless women and destitute children. The Fletcher free public library (47,000 volumes in 1908) is housed in a Carnegie building. In the city are two sanitariums. The city has two parks (one, Ethan Allen Park, is on a bluff in the north-west part of the city, and commands a fine view) and four cemeteries; in Green Mount Cemetery, which overlooks the Winooski valley, is a monument over the grave of Ethan Allen, who lived in Burlington from 1778 until his death. Fort Ethan Allen, a United States military post, is about 3 m. east of the city, with which it is connected by an electric line. Burlington is the most important manufacturing centre in the state; among its manufactures are sashes, doors and blinds, boxes, furniture and wooden-ware, cotton and woollen goods, patent medicines, refrigerators, house furnishings, paper and machinery. In 1905 the city's factory products were valued at $6,355,754, three-tenths of which was the value of lumber and planing mill products, including sashes, doors and blinds. The Winooski river, which forms the boundary between Burlington and the township of Colchester and which enters Lake Champlain N.W. of the city,
furnishes valuable water-power, but most of the manufactories are operated by steam. Quantities of marble were formerly taken from quarries in the vicinity. The city is a wholesale distributing centre for all northern Vermont and New Hampshire, and is one of the principal lumber markets in the east, most of the lumber being imported from Canada. It is the port of entry for the Vermont customs district, whose exports and imports were valued respectively in 1907 at $8,333,024 and $5,721,034. A charter for a town to be founded here was granted by the province of New Hampshire in 1763, but no settlement was made until 1774. Burlington was chartered as a city in 1865.
BURMA, 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 100th degrees of east longitude. The extreme length from north to south is almost 1200 m., and the broadest part, which is in about latitude 21° 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 Yornas, 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 plateau, some 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 the whole 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, Kyauksè, Meiktila, Yamèthin, Myingyan, Magwe, Pakôkku 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, Thôngwa, Henzada, Hanthawaddy, 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 10,000 ft. above the sea, and in the eastern Kachin hills, which run northwards from the state of Möng 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 9000 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 ft., 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 m. from its junction with the Irrawaddy at Pakôkku. 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 south-east 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 Kyauksè, Yamèthin and Toungoo districts, its line being followed by the Mandalay-Rangoon railway as far south as Nyaunglèbin 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.