Analysis on the Cause of Debris Flow Formation in Sanchahe Valley Along Du-ku Highway of Tianshan Mountains
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Analysis on the Cause of Debris Flow Formation in Sanchahe Valley Along Du-ku Highway of Tianshan Mountains
Bulletin of Soiland Water ConservationVol. 14, Issue 5, Pages: 41-46(1995)
作者机构:
中国科学院兰州冰川冻土研究所,兰州市,730000
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Published:1995
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DENG Xiaofeng, ZHU Shousen. Analysis on the Cause of Debris Flow Formation in Sanchahe Valley Along Du-ku Highway of Tianshan Mountains[J]. Bulletin of Soiland Water Conservation, 1995, 14(5): 41-46.
DOI:
DENG Xiaofeng, ZHU Shousen. Analysis on the Cause of Debris Flow Formation in Sanchahe Valley Along Du-ku Highway of Tianshan Mountains[J]. Bulletin of Soiland Water Conservation, 1995, 14(5): 41-46.DOI:
Analysis on the Cause of Debris Flow Formation in Sanchahe Valley Along Du-ku Highway of Tianshan Mountains
The benefical conditions that debris flow is formed in Sanchahe valley along Du-ku highway of Tianshan mountains are frequent rainstorm
exposed rock and high and precipitous land form in alpine region of the drainage basin. Sustained high air temperature in summer can lead to ice-fall of glacier at backwall of the basin.Then
the ice-fall is melted qulkly and results in formation of glacier flood which the debris flow is simulated.Because the conditions mentioned above are still exist