冰水平原
又称外冲平原。在冰水扇外发育的辫状水系所形成的沉积平原。常见于大陆冰川和山麓冰泛的外围。冰水平原从外形上可划分为两大类，即平坦的冰水平原和凸凹不平的平原，后者主要分布有被埋藏的死冰融化后产生的巨大锅穴。
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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 | outwash plain,sandur |
| Chinese |
|---|
| Name | 冰水平原 |
| Description | 又称外冲平原。在冰水扇外发育的辫状水系所形成的沉积平原。常见于大陆冰川和山麓冰泛的外围。冰水平原从外形上可划分为两大类，即平坦的冰水平原和凸凹不平的平原，后者主要分布有被埋藏的死冰融化后产生的巨大锅穴。 |
How to Cite
NNU_Group (2011). 冰水平原, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/4aba4980-b9f3-4fc7-9b4e-0a2af297d125
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