低山沟谷型岩溶
以溶蚀侵蚀作用形成的岩溶地貌。指在碳酸盐岩岩层分布地区，地表水流以机械侵蚀作用为主，形成相对高差200～500米的低山，地下溶蚀作用较显著，溶洞常在河谷地带出露。北京附近碳酸盐岩构成的低山地带，多形成这类岩溶地貌。
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contributed at 2011-10-12
Classification(s)
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Earth System(in Chinese) Karstology
Detailed Description
| English |
|---|
| Name | low mountainvalley type karst |
| Chinese |
|---|
| Name | 低山沟谷型岩溶 |
| Description | 以溶蚀侵蚀作用形成的岩溶地貌。指在碳酸盐岩岩层分布地区，地表水流以机械侵蚀作用为主，形成相对高差200～500米的低山，地下溶蚀作用较显著，溶洞常在河谷地带出露。北京附近碳酸盐岩构成的低山地带，多形成这类岩溶地貌。 |
How to Cite
NNU_Group (2011). 低山沟谷型岩溶, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/050a3b6d-3313-46fb-8110-17a024579c97
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