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《Journal of Glaciology and Geocryology》 1982-04
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ON THE REMNANTS OF QUATERNARY GLACIATION IN ERASHAN, HAINAN, QINGHAI

Guo Penfei ( 00926 Department of PLA )  
The Era Shan is located in the northeast part of Qing-Zang Plateau an easterly extended part of Bulhanbuda Shan in the eastern section of Kunlun Shan.The Quaternary glaciation is distributed on its northern and southern slopes.According to the characteristics of geomorphological form in Era Shan, the glacial remnants can be divided into following forms: the cirque, the glacial valley, the platform of glacial drift, and the piedmont moraine ridge. There was a glacial age in the early mid-pleistocene in the area of Era Shan and was called the Era Shan Glacial Age; then in the late Pleistocene there appeared a long interglacial age and was called the Dahouba Intergla-cial Age.
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