Tibet | History, Map, Capital, Population, Language, & Facts

Drainage and soils

The Plateau of Tibet is the principal source of the rivers of East, Southeast, and South Asia. The Indus River, known in Tibet as the Sênggê Zangbo (“Lion Spring”; Chinese: Shiquan He), has its source in western Tibet near Mount Kailas, a mountain sacred to Buddhists and Hindus; it then flows westward across the Kashmir region to Pakistan. Three other rivers also begin in the west: the Xiangquan River (Tibetan: Langqên Kanbab, “Elephant Spring”) flows west to become the Sutlej River in northwestern India and eastern Pakistan; the Mabja Zangbo River flows into the Ghaghara (Nepali: Kauriala) River to eventually join the Ganges (Ganga) River; and the Maquan River (Tibetan: Damqog Kanbab, “Horse Spring”) flows east and, after joining the Lhasa River south of Lhasa, forms the Brahmaputra.

The Salween (Nu) River has its source in east-central Tibet, from where it flows through eastern Tibet and Yunnan and then enters Myanmar. The Mekong River begins in southern Qinghai as two rivers—the Ang and Zha—which join near the Tibet border; the river then flows through eastern Tibet and western Yunnan and enters Laos and Thailand. The source of the Yangtze River (Chang Jiang) rises in southern Qinghai, near the Tibet border; after flowing through southern Qinghai, the Yangtze turns south to form most of the Tibet-Sichuan border.

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Tibet’s three largest lakes are centrally located, northwest of Lhasa: Lakes Dangre Yong (Tibetan: Tangra Yum), Nam, and Siling. South of Lhasa lie two other large lakes, Yamzho Yun (Yangzho Yong) and Puma Yung (Pumo). In western Tibet two adjoining lakes are located near the Nepal border—Lake Mapam, sacred to both Buddhists and Hindus, and Lake La’nga.

Tibetan: Bod (Show more) In full: Tibet Autonomous Region (Show more) Chinese (Pinyin): Xizang Zizhiqu or (Wade-Giles romanization): Hsi-tsang Tzu-chih-ch’ü (Show more) On the Web: College of DuPage Digital Press - The Eastern World: Daily Readings on Geography - East Asia: Regional Example – Tibet (Feb. 03, 2026) (Show more) See all related content

Soils are alluvial and are often composed of sand that is blown by the wind to form a layer above gravels and shingles. Colour varies from light brown to gray, according to the humus content, which is generally poor.