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Korea

coast, mountain, country, sea, ft, yalu and boundary

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KOREA, a country of Further Asia consisting of a peninsula and about 200 islands. The peninsula stretches southwards from Manchuria, and has an estimated length of about 600 m., an ex treme breadth of 135 m., a coast-line of 1,740 m. and an area of 86,000 sq.m. It extends from 34° 18' to 43° N., and from 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) ; other wise Korea has Manchuria on its land frontier. Nearly the whole surface of the country is mountainous. (For map, see JAPAN.) One native name for the country is Chosyon from the Chinese Ch`ao Hsien. It is also called Dai Han. Of the islands, two-thirds are inhabited, 1 oo are from ioo to 2,000 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, excellent harbour of Port Hamilton, which lies between the north points of the large and well-cultivated islands of Sun-ho-dan and So-dan. 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 are nearly all ice-free ; the most important are Fusan (the landing point from Japan), Chemulpho, Mokpo, Chin-nampo and Gen-san.

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 (8,700 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 per ennial 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 navi gable 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-won-do, 3o m. from the east coast, cuts Korea nearly in half, reaching the sea on the west coast near Chemulpho; and, in spite of many serious rapids, is a valuable highway for commerce for over i5o miles.

Geology.

Crystalline schists occupy a large part of the coun try, 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 1,600 f t. 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, con sisting 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 be long 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 records, was in eruption in the year 1007.

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 ; although there is some malaria. The summer mean tem perature 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.

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