The machanism and types of the hillrockcollapsing forming in Guangdong province

ZHANG Shu-guang; ZHONG Chao-zhang

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The machanism and types of the hillrockcollapsing forming in Guangdong province

- The machanism and types of the hillrockcollapsing forming in Guangdong province
- Bulletin of Soiland Water Conservation Vol. 9, Issue 3, Pages: 8-16(1990)
- 作者机构：
  
  广东省水利水电科学研究所
- 作者简介：
- 基金信息：
- DOI：
  CLC：
- Published：1990
- 稿件说明：
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ZHANG Shu-guang, ZHONG Chao-zhang. The machanism and types of the hillrockcollapsing forming in Guangdong province[J]. Bulletin of Soiland Water Conservation, 1990, 9(3): 8-16.
DOI：

ZHANG Shu-guang, ZHONG Chao-zhang. The machanism and types of the hillrockcollapsing forming in Guangdong province[J]. Bulletin of Soiland Water Conservation, 1990, 9(3): 8-16. DOI：

摘要

崩岗是我国南方一种重要的侵蚀类型

广东省的特点是降水量多、暴雨集中、土质粗、抗冲抗蚀性弱、人为活动强烈。崩岗就是在径流冲刷、崩塌和滑坡、水蚀和重力侵蚀相互作用下形成的。崩岗分为四种类型三个发育阶段。

Abstract

The hillrock collaping is a pricipal type of erosion in the south of China.In Guangdong province it is characterized with great rainfall.intensive storm

rough texture of soil

and weak ability to resist to the scouring and eroding

it is said that that the artificial activity is fierce is the main factor to cause the collapsing of the hillrock

the scouring of runoff

collapsing and slopeslide

water and gravitational erosion are effected each other.The paper divides the hillrock collapsing into fou types and there stages in decelopement.

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