| Geology
Mongolia is a huge, landlocked
country about 3 times the size of France, squashed between China and Russia.
It was immeasurably bigger during the period of Mongol conquest under Genghis
Khan and Kublai Khan. Until the 20th century Mongolia was twice its present
size and included a large chunk of Siberia and Inner Mongolia (now controlled
by China).Mongolia has a 3,000km (1,864ml) border with the Russian Federation in the north and a
4,670km (2,901ml) border with China in the south. From north to south it can
be divided into four areas: mountain-forest steppe, mountain steppe and, in
the extreme south, semi-desert and desert (the latter being about 3% of the
entire territory).
Mongolia is one of the highest countries in the world, with an average
elevation of 1,580m (5,180ft). Its highest mountains are in the far west. The
Mongol Altai Nuruu are permanently snowcapped, and their highest peak,
Tavanbogd Mountain (4,370m/14,350ft), has a magnificent glacier that towers over
Mongolia, Russia and China. Between the peaks are stark deserts where rain
almost never falls. The lowest point, Khuch Lake, in the east, lies at
560m (1,820ft). The
extensive grasslands of the steppes covering the center and eastern part
of the land with a 360° view are the heart of Mongolia. The south is the
domain of the Gobi
Desert
(extending down to China) with large sand dune
areas and canyons in Eastern Gobi, the "dinosaur graveyard". Much of the rest of Mongolia is grassland, home to Mongolia's
famed takhi horses, which Genghis Khan used so successfully in his wars
of conquest. Mongolia is dotted with about 4,000 lakes (one of which is
Lake
Huvsgul, which contains 2% of the
world's fresh water) and rivers where fishing is abundant.
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