The Plateau of Tibet
This great upland massif occupies about one-fourth of the country’s area. A large part of the plateau lies at elevations above 13,000 to 16,500 feet (4,000 to 5,000 metres). The border ranges of the plateau (the Kunlun Mountains and the Himalayas) are even higher, with individual peaks rising to heights of 23,000 to 26,000 feet (7,000 to 8,000 metres) and higher. As a rule, the interior (i.e., Tibet-side) slopes of these border mountains are gentle, while the exterior slopes are precipitous. The plateau’s eastern and southern periphery is the source of many of the world’s great rivers, including the Yangtze, Huang He, Mekong, Salween, Indus, and Brahmaputra. Only in the low valleys, chiefly along the Brahmaputra valley, are there centres of human settlement.
Stupa on the bank of the Yarlung Zangbo (Brahmaputra) River, southern Tibet Autonomous Region, China.© Naomi Duguid/Asia Access
The Qaidam (Tsaidam) Basin, occupying the northwestern portion of the Plateau of Tibet, is the largest, as well as the lowest, depression in the plateau. The broad northwestern part of the basin lies at elevations between approximately 8,800 and 10,000 feet (2,700 and 3,000 metres), and the narrow southeastern part is slightly lower. Gravel, sandy and clay deserts, semideserts, and salt wastes predominate within the basin.