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Natural environment in Central Asia
The natural environment in Central Asia is dominated by plains and hills.

Central Asia is the abbreviation of Central Asia, which refers to the inland areas of Central Asia. This concept was first put forward by German alexander von humboldt in 1843, and its scope has many definitions. In a narrow sense, it is generally limited to "five Central Asian countries". "Five Central Asian countries" refer to Kazakhstan, Kyrgyzstan, Tajikistan and Uzbekistan.

Geographically, Central Asia is located at the junction of Asia and Europe, in the middle of Russian, China, Indian, Iranian, Pakistani and other big countries or regional powers. It is a transportation hub that runs through Asia and Europe. It has always been the only place that passes through the east, west, north and south, and the ancient Silk Road passes through here. After the end of the Cold War, Central Asia became an important strategic buffer zone.

Introduction to the overall topography and environment of Central Asia

Generally speaking, it is high in the southeast and low in the northwest. In Pamir region of Tajikistan and Tianshan region of western Kyrgyzstan, the mountains are high and steep, with an altitude of 4,000-5,000 meters, among which the Communist Peak at an altitude of 7,495 meters and lenin peak at an altitude of 7 1.34 meters are world-famous peaks. In the vast area between east and west, deserts and oases are between 200 and 400 meters above sea level.

The elevation of hills and grasslands is between 300-500m, and that of eastern mountainous areas is about1000m. There are more than 4,000 glaciers in Central Asia, with a total area of 1 1 1,000 square kilometers. The largest Philippine Decenco Glacier is 7 1 km long, including 33 tributaries, covering an area of 900 square kilometers, but at the foot of the mountain is an endless dry and hot desert.

The above contents refer to Baidu Encyclopedia-Central Asia.