吹蚀作用
风蚀作用的一种方式，由于风的吹刮，将大量物质运移去使地面遭受破坏的作用。多见于干燥和缺乏植物的地区，如荒漠、海滩、湖岸及干涸的河床、湖底等。吹蚀作用形成的地貌景观有吹蚀盆地、戈壁、风蚀垅槽(即雅丹)等。
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Contributor
contributed at 2011-10-12
Classification(s)
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Earth System(in Chinese) External dynamic geology
Detailed Description
| English |
|---|
| Name | deflation |
| Chinese |
|---|
| Name | 吹蚀作用 |
| Description | 风蚀作用的一种方式，由于风的吹刮，将大量物质运移去使地面遭受破坏的作用。多见于干燥和缺乏植物的地区，如荒漠、海滩、湖岸及干涸的河床、湖底等。吹蚀作用形成的地貌景观有吹蚀盆地、戈壁、风蚀垅槽(即雅丹)等。 |
How to Cite
NNU_Group (2011). 吹蚀作用, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/83224e3d-86d0-4324-9500-57a828614617
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