MongoliaGeography
Landforms
Figure 4. Topography and Drainage
The terrain is one of mountains and rolling plateaus, with a
high degree of relief
(see
fig. 4). Overall, the land slopes from
the high Altai Mountains of the west and the north to plains and
depressions in the east and the south. Hutyen Orgil (sometimes
called Nayramadlin Orgil--Mount Friendship) in extreme western
Mongolia, where the Mongolian, the Soviet, and the Chinese
borders meet, is the highest point (4,374 meters). The lowest is
560 meters, an otherwise undistinguished spot in the eastern
Mongolian plain. The country has an average elevation of 1,580
meters. The landscape includes one of Asia's largest freshwater
lakes (Hovsgol Nuur), many salt lakes, marshes, sand dunes,
rolling grasslands, alpine forests, and permanent montane
glaciers. Northern and western Mongolia are seismically active
zones, with frequent earthquakes and many hot springs and extinct
volcanoes.
Mongolia has three major mountain ranges. The highest is the
Altai Mountains, which stretch across the western and the
southwestern regions of the country on a northwest-to-southeast
axis. The Hangayn Nuruu, mountains also trending northwest to
southeast, occupy much of central and north-central Mongolia.
These are older, lower, and more eroded mountains, with many
forests and alpine pastures. The Hentiyn Nuruu, mountains near
the Soviet border to the northeast of Ulaanbaatar, are lower
still. Much of eastern Mongolia is occupied by a plain, and the
lowest area is a southwest-to-northeast trending depression that
reaches from the Gobi region in the south to the eastern
frontier. The rivers drain in three directions: north to the
Arctic Ocean, east to the Pacific, or south to the deserts and
the depressions of Inner Asia. Rivers are most extensively
developed in the north, and the country's major river system is
that of the Selenge-Moron, which drains into Lake Baykal. Some
minor tributaries of Siberia's Yenisey River also rise in the
mountains of northwestern Mongolia. Rivers in northeastern
Mongolia drain into the Pacific through the Argun and Amur
(Heilong Jiang) rivers, while the few streams of southern and
southwestern Mongolia do not reach the sea but run into salt
lakes or deserts.
Data as of June 1989
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