The Kunlun mountain range () is one of the longest mountain chains in Asia, extending more than 3,000 km.
It runs along the western border of China southwards beside the Pamir range, then curves to the East, to form the border range of northern Tibet. It stretches along the southern edge what is now called the Tarim Basin, the infamous Takla Makan or "sand-buried houses" desert, and the Gobi desert.
The range has over 200 peaks higher than 6,000 metres. The three highest peaks are the Kongur Tagh (7,719m), the Dingbei (7,625m) and the famous Muztagh Ata (7,546m). These highest peaks are in the Arkatag range of the range complex. A number of important rivers flow from it including the Karakash River ('Black Jade River') and the Yurungkash River ('White Jade River') which flow through the Khotan Oasis into the Taklamakan Desert.
A southern branch of the Kunlun Mountains forms the watershed between the catchment basins of China's two longest rivers, the Yangtze River and the Huang He.
The mountain range formed at the northern edges of the Indian Plate during its collision, in the late Triassic, with the Eurasian Plate, which resulted in the closing of the Paleo-Tethys Ocean.
Mountain ranges of Asia | Mountains of China
Kunlun | Kunlun | Kunlun | Kunlun Shan | 쿤룬 산맥 | הרי קונלון | 崑崙山脈 | Kunlunfjellene | 昆仑山脉
This article is licensed under the GNU Free Documentation License.
It uses material from the
"Kunlun Mountains".
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