Citations:Sogo Nur

English citations of Sogo Nur

• 1993 August, Miao Wang, Shi Bao Xiu, “A Detour Through the Desert to Etzina”, in Tu Nai Hsien, editor, From the Pamirs to Beijing: Tracing Marco Polo's Northern Route‎^[1], Hong Kong: HK China Tourism Press, →ISBN, →OCLC, page 94, columns 1, 2:

  When we were in Zhangye we consulted a map and saw that the Ruoshui River has its source in the Qilian Mountains, then winds north through the Hexi Corridor and into the desert. It then flows through the forests of Ejin Banner and pours into two lakes — the Gaxun Nur and the Sogo Nur.[...]
  The Mongolian woman told us that in recent years the water flowing from the south has seldom reached the lakes here, and consequently the Gaxun Nur had dried up. This summer, less water than usual had poured into the Sogo Nur, so it too was almost empty.[...]
  Next, we headed northeast to visit Sogo Nur. After two hours of driving through willow bushes no more than two feet in height, we saw the white surface of a lake. A solitary thatched cottage stood by the road leading to the lake, and the sound of our engine brought a middle-aged Mongolian man out to greet us. After a short conversation, she^{[sic – meaning he]} told us that the lake had dried up just ten days earlier.

• 1996, Zhou Zhiyi, W. T. Dean, editors, Phanerozoic Geology of Northwest China‎^[2], Beijing: Science Press, →OCLC, page 216‎^[3]:

  In the Badain Jaran District (Fig. 15-1, II-8-2), marine Lower Carboniferous strata occur at Sogo Nur, in the western part of the northern area, and rest disconformably on Upper Devonian.

• 2004 January, Jin Heling et al., “Vicissitude of Sogo Nur and environmental-climatic change during last 1500 years”, in Science China Earth Sciences‎^[4], →DOI, →ISSN, →OCLC, archived from the original on 22 August 2022‎^[5]:

  Lakes in arid zone are sensitive to climatic changes. The lacustrine sediment sequence in Sogo Nur has well and truly recorded climatic events such as the Sui-Tang Dynasty Warm Period, the Song-Liao Dynasty Cold Period, the Medieval Warm Period, the Little Ice Age and the 20th Century Warm Period.

• 2008, Robert Jellison, William D. Williams, Brian Timms, Javier Alcocer, Nikolay V. Aladin, “Salt lakes: values, threats and future”, in Nicholas V. C. Polunin, editor, Aquatic Ecosystems: Trends and Global Prospects‎^[6], Cambridge University Press, →ISBN, →LCCN, →OCLC, page 99, column 2:

  On the Alxa Plateau of Inner Mongolia, Gaxun Nur Lake (262 km²) dried in the 1970s and the Sogo Nur Lake in the 1980s.

• 2009, K. Hartmann, B. Wünnemann, H. Zhang, “Neotectonic impact and Palaeohydrology of Gaxun Nur Basin (NW China) during the Late Quaternary”, in Geophysical Research Abstracts‎^[7], volume 11, →ISSN, →OCLC, archived from the original on 13 August 2017:

  The Gaxun Nur Basin – enclosed by the Tibetan Plateau in the south and the Gobi Altay in the north – has continuously evolved as a strong continental endorheic depositional environment for the last 250,000 years. The Hei River drainage system originates in the Qilian Shan (>5,000 m a.s.l.) fed a crescent-shaped series of terminal lakes at its far end (Gaxun Nur, Sogo Nur and Juyanze).