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《Journal of Glaciology and Geocryology》 1984-02
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Features of Wangfeng Glacial Moraine at the Headwater of Urumqi River in Tianshan

Ma Qiuhua (Lanzhou Institute of Glaciology and Cryopedology, Academia Sinica)  
Distributive boundary line between the Lower Wangfeng and the Upper Wangfeng moraines and the eastern boundary of Lower Wangfeng moraine have been ascertained in this paper according to the features of the cross sections actually surveyed onthespot. Besides, the author has made a detailed study on the macroscopic and microscopic structures of longitudinal section of Wangfeng moraine and conclusions are as follows; 1 ) Laminar structures are found in the moraine; 2 ) The feature of concentrated accumulation exists in the moraine; 3 ) Phenomena of overlapping of overfault and of folded fault in the section are also seen.
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