Jinsha River

Jinsha
Yangtze (长江)
Jinsha flowing along the bottom of Tiger Leaping Gorge
Map of the Jinsha River drainage basin
EtymologyChinese: "Gold Dust River"[1]
Native name金沙江
Location
CountryChina
StateQinghai, Tibet Autonomous Region, Yunnan, Sichuan
CitiesLijiang, Yunnan, Panzhihua
Physical characteristics
SourceTongtian River
 • locationConfluence of the Tongtian and Batang Rivers, Qinghai
 • coordinates34°5′38.8″N 92°54′46.1″E / 34.094111°N 92.912806°E / 34.094111; 92.912806
 • elevation4,500 m (14,800 ft)
MouthYangtze River
 • location
Confluence with Min Jiang at Yibin, Sichuan
 • coordinates
28°46′13.4″N 104°37′58.1″E / 28.770389°N 104.632806°E / 28.770389; 104.632806
 • elevation
300 m (980 ft)
Length
  • 2,290 km (1,420 mi)approx.
  • 3,292 km (2,046 mi) total length including Tongtian River
Basin size485,000 km2 (187,000 sq mi)approx.
Discharge 
 • average4,471 m3/s (157,900 cu ft/s)
 • maximum35,000 m3/s (1,200,000 cu ft/s)
Basin features
ProgressionYangtzeEast China Sea
River systemYangtze River basin
Tributaries 
 • leftBeilu River, Yalong River
 • rightPudu River, Dadan River, Xiaojiang River, Niulan River

The Jinsha River (Chinese: 金沙江; pinyin: Jīnshājiāng; lit. 'Gold Sand River',[1] Tibetan: Dri Chu, འབྲི་ཆུ, Yi: ꀉꉷꏁꒉ, romanized: Axhuo Shyxyy) or Lu river, is the Chinese name for the upper stretches of the Yangtze River. It flows through the provinces of Qinghai, Sichuan, and Yunnan in western China. The river passes through Tiger Leaping Gorge.

It is sometimes grouped together with the Lancang (upper Mekong) and Nu (upper Salween) as the Sanjiang ("Three Rivers") area,[2] part of which makes up the Three Parallel Rivers of Yunnan Protected Areas.

The river is important in generating hydroelectric power, and several of the world's largest hydroelectric power stations are on the Jinsha river.

  1. ^ a b Little, Archibald. The Far East, p. 63. 1905. Reprint: Cambridge Univ. Press (Cambridge), 2010. Accessed 13 August 2013.
  2. ^ E.g., in the "Annual Report of the Chinese Academy of Geological Research", p. 24. Geological Publishing House, 1994.