冰锥
又称泉冰锥(ice cone from natural spring)。承压水通过地层、河湖冰面的裂隙流出地表，逐层冻结成冰，成为形似尖顶向上的锥体。冰锥与冰丘不同，前者是水流至地表冻结成冰，后者是水流在地下冻结成冰核。
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Contributor
contributed at 2011-12-23
Classification(s)
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Earth System(in Chinese) Glacial geology
Detailed Description
| English |
|---|
| Name | ice cone |
| Chinese |
|---|
| Name | 冰锥 |
| Description | 又称泉冰锥(ice cone from natural spring)。承压水通过地层、河湖冰面的裂隙流出地表，逐层冻结成冰，成为形似尖顶向上的锥体。冰锥与冰丘不同，前者是水流至地表冻结成冰，后者是水流在地下冻结成冰核。 |
How to Cite
NNU_Group (2011). 冰锥, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/de141a32-7deb-475e-a5c7-44d35611d75f
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