孤峰波地型岩溶
又称残丘波地型岩溶。是以溶蚀作用为主形成的岩溶地貌。为碳酸盐岩岩层分布地区，受到长期而强烈的岩溶作用后，形成有孤峰残丘点缀的起伏平缓的波状地形。在低洼地带多为残积—冲积土层覆盖。多具有统一的地下水力面。如广西宾阳、桂林地区为典型的孤峰波地型岩溶地貌。
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Contributor
contributed at 2011-10-12
Classification(s)
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Earth System(in Chinese) Karstology
Detailed Description
| English |
|---|
| Name | isolated peak rolling land type karst |
| Chinese |
|---|
| Name | 孤峰波地型岩溶 |
| Description | 又称残丘波地型岩溶。是以溶蚀作用为主形成的岩溶地貌。为碳酸盐岩岩层分布地区，受到长期而强烈的岩溶作用后，形成有孤峰残丘点缀的起伏平缓的波状地形。在低洼地带多为残积—冲积土层覆盖。多具有统一的地下水力面。如广西宾阳、桂林地区为典型的孤峰波地型岩溶地貌。 |
How to Cite
NNU_Group (2011). 孤峰波地型岩溶, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/4c5cc1c1-28d8-4938-ad9b-1d9d93f3ad58
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