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Baisuntau

Mountain range in southeastern Uzbekistan From Wikipedia, the free encyclopedia

The Baisuntau mountain range (Uzbek: Boysuntogʻ; Russian: Байсунтау) is the southwestern continuation of the Gissar Mountains, in southeastern Uzbekistan. This in turn continues in a southwesterly direction with the Kugitangtau chain.

Geography

The Baisuntau extends for a length of approximately 150 km (93 mi) in a northeast/southwest direction. It culminates at an elevation of 4,424 m (14,514 ft).[1] From its northwestern and northern slopes arise several left-hand tributaries of the Kashkadarya River, including the Akdarya. The south-eastern slope of the mountain range is drained by the Surkhandarya river system.[1]

Geology

The mountain range is made up of limestone, sandstone, and clay. The lower slopes are covered by semi-desert type vegetation; higher up there are juniper forests and alpine meadows.[1]

At the southern end of the mountain range is the Teshik-Tash cave, a famous archaeological site. Other caves in the region are:

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