Citations:Koxlax

English citations of Koxlax

						1998	2008 2016 2021
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• [1932 August [1932 March 14], Reginald C. F. Schomberg, “Alleged Changes in the Climate of Southern Turkistan”, in The Geographical Journal‎^[1], volume LXXX, number 2, London: Royal Geographical Society, →ISSN, →OCLC, page 138:

  On the Yurunggash, between the Eghriyar and the Qoshlash langars, was a low ridge of sand, on which were dead, dying, and living toghraqs.]

• [1993, Xuncheng Xia, ‎Chongshun Li, ‎Xingjia Zhou, Desertification and Control of Blown Sand Disasters in Xinjiang‎^[2], Science Press, →ISBN, →OCLC, page 43:

  There also existed on either bank of the lower section of the Hotan River below Kuoshilashi, at 38 ° 45'N, 39 ° 30'N and 39 ° 55'N, 4-5 river courses which ran northward, parallel to the current mainstream of the river, and disappeared into the old river courses in […]]

• 1998, Atlas of the World‎^[3], HarperCollins, →ISBN, →OCLC, page 65:

  Koxlax

  (in sector K5, northeast of Hotan)

• 1998, “Hotan River”, in Saul B. Cohen, editor, The Columbia Gazetteer of the World‎^[4], volume 2, New York: Columbia University Press, →ISBN, →LCCN, →OCLC, page 1313, column 3:

  […] rises in Kunlun mts. in 2 branches — the Karakax (left) and the Yurungkax (right), which form the Hotan R. at Koxlax; […]

• 2008, Saul B. Cohen, editor, The Columbia Gazetteer of the World‎^[5], 2nd edition, Columbia University Press, →ISBN, →LCCN, →OCLC, page 1607, column 2:

  Hotan River, 400 mi/644 km long, S XINJIANG UYGUR AUTONOMOUS REGION, NW CHINA; rises in KUNLUN mountains in two branches—the Karakax (left) and the Yurungkax (right), which form the HOTAN RIVER at Koxlax; flows N, through TAKLIMAKAN DESERT, but rarely reaching the TARIM.

• [2009 July, Lingmei Huang, Lina Wu, Bing Shen, “Quantitative Estimation of Annual Runoff Variation from the Hotan River, China”, in Journal of Sustainable Development‎^[6], volume 2, number 2, →DOI, →ISSN, →OCLC, archived from the original on 28 February 2023, page 120:

  There are two tributaries in the upper reach of the Hotan River. One is the Yulongkashi River; the other is the Kalakashi River. They converge at Kuoshilashi.]

• 2016, Hongwei Guo et al., “Study of suitable oasis scales based on water resource availability in an arid region of China: a case study of Hotan River Basin”, in Environmental Earth Sciences‎^[7], volume 75, →DOI, →ISSN, →OCLC:

  The upper reaches encompass the river source to the mountain pass, and the middle reaches extend from the mountain pass to the intersection (ie, Koxlax) of the two tributaries. The lower reach includes the river section between the Koxlax and Xiaota Hydrologic Stations with a length of 319 km.

• 2021, The Buddha’s Words and Their Interpretations‎^[8], Shin Buddhist Comprehensive Research Institute, →ISBN, →OCLC, archived from the original on 24 October 2021, page 137:

  The waters of two rivers, the Yurungkash or Baiyu he 白玉河 (White Jade River) and the Karakash or Heiyu he 黑玉河 (Black Jade River), were indispensable for establishing human culture in Khotan. These two rivers unite near Koxlax (about 200 km north of Khotan) and together form the Khotan River.