(pop. about 10,000), 165 m. W.S.W. of El Obeid, is a commercial centre which has sprung into importance since the fall of the dervishes. All the trade with Darfur passes through the town, the chief commerce being in cattle, feathers, ivory and cotton goods. Trade is largely in the hands of Greeks, Syrians, Danagla and Jaalin. Taiara, on the route between El Obeid and the Nile, was destroyed by the dervishes but has been rebuilt and is a thriving mart for the gum trade. El Odoaiya or Eddaiya is the headquarters of the Homr country. It and Baraka in the Muglad district are on the trade road between Nahud and Shakka in Darfur.
Bara is a small town some 50 m. N.N.E. of Obeid. Talodi and Tendek are government stations in the Nuba country. The Nubas have no large towns. They live in villages on the hillsides or summits. The usual habitation built both by Arabs and Nubas is the tukl, a conical-shaped hut made of stone, mud, wattle and daub or straw. The Nuba tukls are the better built. In the chief towns houses are built of mud bricks with flat roofs.
History.—Of the early history of Kordofan there is little record. It never formed an independent state. About the beginning of the 16th century Funj from Sennar settled in the country; towards the end of that century Kordofan was conquered by Suleiman Solon, sultan of Darfur. About 1775 it was conquered by the Funj, and there followed a considerable immigration of Arab tribes into the country. The Sennari however suffered a decisive defeat in 1784 and thereafter under Darfur viceroys the country enjoyed prosperity. In 1821 Kordofan was conquered by Mahommed Bey the defterdar, son-in-law of Mehemet Ali, pasha of Egypt. It remained under Egyptian rule till 1882 when Mahommed Ahmed, the mahdi, raised the country to revolt. It was in Kordofan that Hicks Pasha and his army, sent to crush the revolt, were annihilated (Nov. 1883). The Baggara of Kordofan from that time onward were the chief supporters of the mahdi, and his successor, the khalifa Abdullah, was a Baggara. In Kordofan in 1899 the khalifa met his death, the country having already passed into the hands of the new Sudan government. The chief difficulty experienced by the administration was to habituate the Arabs and Nubas, both naturally warlike, to a state of peace. In consequence of the anti-slave raiding measures adopted, the Arabs of Talodi in May 1906 treacherously massacred the mamur of that place and 40 men of the Sudanese regiment. The promptness with which this disturbance was suppressed averted what otherwise might have been a serious rising. (See Sudan: Anglo-Egyptian, § “History.”)
See The Anglo-Egyptian Sudan, edited by Count Gleichen (London, 1905); H. A. MacMichael, Notes on the History of Kordofan before the Egyptian Conquest (Cairo, 1907); John Petherick, Egypt, the Sudan, and Central Africa (London, 1861); Ignaz Pallme, Beschreibung von Kordofan (Stuttgart, 1843; trans. Travels in Kordofan, London, 1844); Major H. G. Prout, General Report on Province of Kordofan (Cairo, 1877); Ernst Marno, Reise in der egypt. Equat. Provinz (Vienna, 1879); papers (with maps) by Capt. W. Lloyd in the Geog. Journ. (June 1907 and March 1910); and the bibliography given under Sudan: Anglo-Egyptian.
KOREA, or Corea (Ch’ao Hsien, Dai han). Its mainland portion consists of a peninsula stretching southwards from Manchuria, with an estimated length of about 600 m., an extreme breadth of 135 m., and a coast-line of 1740 m. It extends from 34° 18′ to 43° N., and from 124° 36′ to 130° 47′ E. Its northern boundary is marked by the Tumen and Yalu rivers; the eastern boundary by the Sea of Japan; the southern boundary by Korea Strait; and the western boundary by the Yalu and the Yellow Sea. For 11 m. along the Tumen river the north frontier is conterminous with Russia (Siberia); otherwise Korea has China (Manchuria) on its land frontier. Nearly the whole surface of the country is mountainous. (For map, see Japan.)
The south and west coasts are fringed by about 200 islands (exclusive of islets), two-thirds of which are inhabited; 100 of them are from 100 to 2000 ft. in height, and many consist of bold bare masses of volcanic rock. The most important are Quelpart and the Nan Hau group. The latter, 36 m. from the eastern end of Quelpart, possesses the deep, well-sheltered and roomy harbour of Port Hamilton, which lies between the north points of the large and well-cultivated islands of Sun-ho-dan and So-dan, which have a population of 2000. Aitan, between their south-east points, completes this noble harbour. The east coast of Korea is steep and rock-bound, with deep water and a tidal rise and fall of 1 to 2 ft. The west coast is often low and shelving, and abounds in mud-banks, and the tidal rise and fall is from 20 to 36 ft. Korean harbours, except two or three which are closed by drift ice for some weeks in winter, are ice-free. Among them are Port Shestakov, Port Lazarev, and Wön-san (Gensan), in Broughton Bay;[1] Fusan, Ma-san-po, at the mouth of the Nak-tong, on the south coast; Mok-po, Chin-nampo, near the mouth of the Tai-dong; and Chemulpo, near the mouth of the Han, the port of the capital and the sea terminus of the first Korean railway on the west coast.
Korea is distinctly mountainous, and has no plains deserving the name. In the north there are mountain groups with definite centres, the most notable being Paik-tu San or Pei-shan (8700 ft.) which contains the sources of the Yalu and Tumen. From these groups a lofty range runs southwards, dividing the empire into two unequal parts. On its east, between it and the coast, which it follows at a moderate distance, is a fertile strip difficult of access, and on the west it throws off so many lateral ranges and spurs as to break up the country into a chaos of corrugated and precipitous hills and steep-sided valleys, each with a rapid perennial stream. Farther south this axial range, which includes the Diamond Mountain group, falls away towards the sea in treeless spurs and small and often infertile levels. The northern groups and the Diamond Mountain are heavily timbered, but the hills are covered mainly with coarse, sour grass and oak and chestnut scrub. The rivers are shallow and rocky, and are usually only navigable for a few miles from the sea. Among the exceptions are the Yalu (Amnok), Tumen, Tai-dong, Naktong, Mok-po, and Han. The last, rising in Kang-wön-do, 30 m. from the east coast, cuts Korea nearly in half, reaching the sea on the west coast near Chemulpo; and, in spite of many serious rapids, is a valuable highway for commerce for over 150 miles.
Geology.—The geology of Korea is very imperfectly known. Crystalline schists occupy a large part of the country, forming all the higher mountain ranges. They are always strongly folded and it is in them that the mineral wealth of Korea is situated. Towards the Manchurian frontier they are covered unconformably by some 1600 ft. of sandstones, clay-slates and limestones, which contain Cambrian fossils and are the equivalents of a part of the Sinian system of China. Carboniferous beds, consisting chiefly of slates, sandstones and conglomerates, are found in the south-eastern provinces. They contain a few seams of coal, but the most important coal-bearing deposits of the country belong to the Tertiary period. Recent eruptive and volcanic rocks are met with in the interior of Korea and also in the island of Quelpart. The principal mountain in the latter, Hal-la-san (or Mount Auckland), according to Chinese stories, was in eruption in the year 1007. With this possible exception there are no active volcanoes in Korea, and the region has also been remarkably free from earthquakes throughout historic times.
Climate.—The climate is superb for nine months of the year, and the three months of rain, heat and damp are not injurious to health. Koreans suffer from malaria, but Europeans and their children are fairly free from climatic maladies, and enjoy robust health. The summer mean temperature of Seoul is about 75° F., that of winter about 33°; the average rainfall, 36.3 in. in the year, and of the rainy season 21.86 in. The rains come in July and August on the west and north-east coasts, and from April to July on the south coast, the approximate mean annual rainfall of these localities being 30, 35 and 42 in. respectively. These averages are based on the observations of seven years only.
Flora.—The plants and animals await study and classification. Among the indigenous trees are the Abies excelsa, Abies microsperma, Pinus sinensis, Pinus pinea, three species of oak, five of maple, lime, birch, juniper, mountain ash, walnut, Spanish chestnut, hazel, willow, hornbeam, hawthorn, plum, pear, peach, Rhus vernicifera, (?) Rhus semipinnata, Acanthopanax ricinifolia, Zelkawa, Thuja orientalis, Elaeagnus, Sophora Japonica, &c. Azaleas and rhododendrons are widely distributed, as well as other flowering shrubs and creepers, Ampelopsis Veitchii being universal. Liliaceous plants
- ↑ Named after William Robert Broughton (1762–1821), an English navigator who explored these seas in 1795–1798.
