Bangor Co
Sentinel-2 image (2021)
Bangor Co is located in Tibet
Bangor Co
Bangor Co
LocationXainza County, Nagqu, Tibet, China
Coordinates31°44′16.5″N 89°28′35.8″E / 31.737917°N 89.476611°E / 31.737917; 89.476611

Bangecuo (also spelled as Bangor Co, Tibetan: བྲང་ཁོག་མཚོ, Wylie: brang khog mtsho, ZYPY: Drangkhok Tso; Chinese: 班戈错; pinyin: Bāngēcuò) is a graben basin salt lake[1][2] on the Tibetan Plateau in Xainza County within Nagqu in the Tibet Autonomous Region of China.

It was reported in 2003 that the water levels of Siling Lake and Bangecuo had increased by 19.34% since 1969.[3]

Siling Lake is another nearby salt lake located west of Bangecuo,[4] around four miles away.

See also

References

  1. Meng, Kai and Shi, Xuhua and Wang, Erchie (February 2011). "High-altitude salt lake elevation changes and glacial ablation in Central Tibet, 2000–2010". Chinese Science Bulletin. 57 (5): 525–534. doi:10.1007/s11434-011-4849-5. S2CID 53638685.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  2. Wang, Can; Wang, Hailei; Song, Gao; Zheng, Mianping (February 2019). "Grain size of surface sediments in Selin Co (central Tibet) linked to water depth and offshore distance". Journal of Paleolimnology. 61(2):1-13. DOI:10.1007/s10933-018-0054-8
  3. Yong, Qu. Shelincuo and Bangecuo extensional lake basins in the northern pa rt of Tibet and present chasmic activities. Semantic Scholar. S2CID 131135903.
  4. Doin, Marie-Pierre; Twardzik, Cédric; Ducret, Gabriel; Lasserre, Cécile; Guillaso, Stéphane; Jianbao, Sun (2015). "InSAR measurement of the deformation around Siling Co Lake: Inferences on the lower crust viscosity in central Tibet". Journal of Geophysical Research: Solid Earth. American Geophysical Union (AGU). 120 (7): 5290–5310. Bibcode:2015JGRB..120.5290D. doi:10.1002/2014jb011768. ISSN 2169-9313. S2CID 128466292.

Further reading

  • Lv, P., Qu, Y. G., Li, W. Q., & Wang, H. S. (2003). "Shelincuo and Bangecuo extensional lake basins in the northern part of Tibet and present chasmic activities." Jilin Geol, 22, 15–19.


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