IMHE OpenIR  > 成都山地所知识仓储(2009年以前)
The main fetures of mudflow in Jingjia revine
Li Jian; Yuan Jianmo; Bi Cheng; Luo Defu
1983
Source PublicationGeomorphlogie N. F.
ISSN0372-8854
Volume27Issue:30Pages:325-341
Contribution Rank1
AbstractThe mountainous area of southwest China is a region where mudflows generated by heavy rainfall are rather common and frequently cause catastrophic damage to the local settlements and fields. Jiang-jia Ravine has the largest and most hazardous mudflow in this area. Its catchment is only 47.1 Km2, but the maximum mudflow discharge can reach 2420 m3/s. It is known that the mudflow has been causing damage for at least 300 years. In the wet season (May-October) each year, the mudflow may occur from several to several dozen times, and the total volume transported reaches 3-5×10~6 m~3 every year. We describe the staic and dynamic features of the mudflow and its deposits on the basis of observations made over more than 15 years.
Keywordmudflows generated heavy rainfall the mountainous area southwest China
Indexed By其他
Language英语
Document Type期刊论文
Identifierhttp://ir.imde.ac.cn/handle/131551/26472
Collection成都山地所知识仓储(2009年以前)
Corresponding AuthorLi Jian
Recommended Citation
GB/T 7714
Li Jian,Yuan Jianmo,Bi Cheng,et al. The main fetures of mudflow in Jingjia revine[J]. Geomorphlogie N. F.,1983,27(30):325-341.
APA Li Jian,Yuan Jianmo,Bi Cheng,&Luo Defu.(1983).The main fetures of mudflow in Jingjia revine.Geomorphlogie N. F.,27(30),325-341.
MLA Li Jian,et al."The main fetures of mudflow in Jingjia revine".Geomorphlogie N. F. 27.30(1983):325-341.
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