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《Journal of Glaciology and Geocryology》 1981-02
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DISCUSSION ON THE GLACIAL CHANGES SINCE WRM ICE AGE IN THE MOUNT SUZHULIAN, QILIAN SHAN

Qin Dahe (Department of Geology & Geography, Lanzhou University)  
The glaciations and the glacial changes since Wurm Glacial in the Suz-hulian Feng have been studied on the basis of glacial landform in this paper. The results of study show that the snow line in the Wurm Glacial. Neoglaciation and Little Ice Ages,was about 590-630, 230-360, 140-150 meters lower than that at present, temperature being 4℃, 1.5-2.5℃, 1℃ lower than that at present near the snow line. The conditons of the development of glacier in Wurm have been researched. The characteristics and patterns of glaciers during that time have been deduced, and the map of distribution of glacier in Wurm was compiled.
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