KMS Institute of Mountain Hazards and Environment,CAS
The main fetures of mudflow in Jingjia revine | |
Li Jian; Yuan Jianmo; Bi Cheng; Luo Defu | |
1983 | |
Source Publication | Geomorphlogie N. F.
![]() |
ISSN | 0372-8854 |
Volume | 27Issue:30Pages:325-341 |
Contribution Rank | 1 |
Abstract | The 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. |
Keyword | mudflows generated heavy rainfall the mountainous area southwest China |
Indexed By | 其他 |
Language | 英语 |
Document Type | 期刊论文 |
Identifier | http://ir.imde.ac.cn/handle/131551/26472 |
Collection | 成都山地所知识仓储(2009年以前) |
Corresponding Author | Li 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. |
Files in This Item: | ||||||
File Name/Size | DocType | Version | Access | License | ||
1563180560425.pdf(4970KB) | 期刊论文 | 出版稿 | 开放获取 | CC BY-NC-SA | View Application Full Text |
Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.
Edit Comment