THE ORIGIN AND CHARACTERISTICS OF THE GLACIAL DEBRIS FLOW IN THE DUKU HIGHWAY OF TIANSHAN MOUNTAINS, CHINA
THE ORIGIN AND CHARACTERISTICS OF THE GLACIAL DEBRIS FLOW IN THE DUKU HIGHWAY OF TIANSHAN MOUNTAINS,作者机构:Department of GeographyXinjiang UniversityUrumqi830046PRC Department of GeographyPeking UniversityBeijing 100871PRC Institute of Botanythe Chinese Academy of SciencesBeijing 100039PRC
出 版 物:《Chinese Geographical Science》 (中国地理科学(英文版))
年 卷 期:1996年第6卷第3期
页 面:282-288页
核心收录:
学科分类:08[工学] 083304[工学-城乡发展历史与遗产保护规划] 0833[工学-城乡规划学]
主 题:debris flow natural hazard Tianshan Mountains
摘 要:Debris flow is one of the most serious natural hazards in the TianshanMountains. According to trigger agent, the debris flow can be divided into stormtype which is caused by flood, and glacial type which is caused by flood from meltingof snow and glacier in hot weather. At present, debris flow causes damage mainly totransportation, sometimes to mining and residents in mountainous area. The catastrophic process and the forming condition of the debris flow show regional regularity,therefore, the research of its distribution, processes, and environmental condition isuseful in mitigating the natural hazard.