湖泊地貌
在内动力或外动力地质作用下，陆地上形成的积水凹地形态。湖盆受地质条件、气候条件等因素的控制，因此，湖泊地貌与湖盆成因关系很大。如断陷湖，湖岸多为平直陡峻；火口湖，因位于火山体顶端，一般高出地表，水体受火山口规模的限制；风蚀湖常呈新月形湖盆等。
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contributed at 2011-10-11
Classification(s)
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Earth System(in Chinese) Geomorphology
Detailed Description
| English |
|---|
| Name | landform of lake |
| Chinese |
|---|
| Name | 湖泊地貌 |
| Description | 在内动力或外动力地质作用下，陆地上形成的积水凹地形态。湖盆受地质条件、气候条件等因素的控制，因此，湖泊地貌与湖盆成因关系很大。如断陷湖，湖岸多为平直陡峻；火口湖，因位于火山体顶端，一般高出地表，水体受火山口规模的限制；风蚀湖常呈新月形湖盆等。 |
How to Cite
NNU_Group (2011). 湖泊地貌, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/eb187f70-59e0-4f66-aadc-2fa1f15d0244
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