黄土峁
黄土高原地区特有的一种地貌形态，呈孤立的黄土丘状，顶部浑圆，坡面向四周倾斜，状如馒头。大多数黄土峁是由黄土梁进一步侵蚀切割形成的，极少数是晚期黄土覆盖在古丘状高地上形成的。黄土峁可见于甘肃环县、永登等地。黄土塬、梁、峁之间的关系基本代表了流水对黄土的侵蚀强度和地貌演化过程。
Classification(s)
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Geographic semantic resource library Earth System(in Chinese) Geology of loess
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| Chinese |
|---|
| Name | loess hillock，loess mao |
| Chinese |
|---|
| Name | 黄土峁 |
| Description | 黄土高原地区特有的一种地貌形态，呈孤立的黄土丘状，顶部浑圆，坡面向四周倾斜，状如馒头。大多数黄土峁是由黄土梁进一步侵蚀切割形成的，极少数是晚期黄土覆盖在古丘状高地上形成的。黄土峁可见于甘肃环县、永登等地。黄土塬、梁、峁之间的关系基本代表了流水对黄土的侵蚀强度和地貌演化过程。 |
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NNU_Group (2011). 黄土峁, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/5f565e55-cbc4-4264-9dee-e3bd99819cff
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