Shiquanhe aka森格possession cloth, the upper reaches of the Indian River. Northwest drought and cold running through Tibetan areas with a total length of 430 km, 27,000 square kilometers of drainage areas, the annual runoff of about 700 million cubic meters. Gangrenbeiji originated in the north peak, 5,164 meters above sea level at its source, periglacial areas downstream into the desert area. Via Ge'gyai, such as the town of Shiquanhe, in the Tashi Kong and the tributaries Burning Tibetan cloth convergence. After entering Kashmir from India said the river. Tibet is the least rainfall in the region, the only precipitation in the 50-80 mm. - Gully mainly to the coastal terrain, swamps and distribution of hot springs. Hot Springs for more than igneous rock fissures in the ground diving, not only supplies the river, raising the temperature of the river, and to make some little frozen river in winter. As is located in arid zone, not Shiquanhe water development, the average runoff of only 25 mm, annual runoff of about 700 million cubic meters, is the outflow of a river in Tibet smallest river runoff. Nevertheless, it is still a dry climate, the scarcity of fresh water on the plateau hinterland of the valuable water resources.
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