| II.
|
 |
Land and Resources |
The topography of Mongolia consists mainly of a plateau between about 914 and 1,524 m (3,000 and 5,000 ft) in elevation broken by mountain ranges in the north and west. The Altai Mountains in the south-west rise to heights above 4,267 m (14,000 ft). The Gobi covers a wide arid tract in the central and south-eastern areas.
| A.
|
 |
Rivers and Lakes |
The most important rivers in Mongolia are the Selenga and its tributary, the Orhon, in the north. Large lakes include the Har Us, Hyargas, Uvs, and Hövsgöl.
| B.
|
 |
Climate |
Mongolia’s climate is harsh, with temperatures ranging between -15° and -30° C (-5° and -22° F) in winter and 10° and 26.7° C (50° and 80° F) in summer. Winters are dry, and summer rainfall seldom exceeds 380 mm (15 in) in the mountains and 125 mm (5 in) in the desert.
| C.
|
 |
Natural Resources |
Rich prairie land in the north-east and north-west supports large numbers of cattle, sheep, and goats. Mineral resources such as coal, iron, copper, fluorspar, gold, uranium, and silver have not been fully exploited.
| D.
|
 |
Plants and Animals |
Mongolia contains forests of larch, pine, and cedar in the mountains, but these are of little economic importance. Fur-bearing animals, especially marmot and squirrel, are abundant, and the country has a well-developed fur industry.
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