流水波痕
由单向水流作用于非粘质沉积物表面形成。波脊线形态的变化(据Allen，1968补充)波长小于0.6米，波高0.3～6厘米，波痕指数大于5，多数在8～15之间，流水波痕脊线的形态随水流速度、水深变化而改变。水深减少和流速加快，其脊线由平直变成波状和舌状。
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contributed at 2011-09-27
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Earth System(in Chinese) Sedimentology and sedimentary petrology
Detailed Description
| English |
|---|
| Name | current ripples |
| Chinese |
|---|
| Name | 流水波痕 |
| Description | 由单向水流作用于非粘质沉积物表面形成。波脊线形态的变化(据Allen，1968补充)波长小于0.6米，波高0.3～6厘米，波痕指数大于5，多数在8～15之间，流水波痕脊线的形态随水流速度、水深变化而改变。水深减少和流速加快，其脊线由平直变成波状和舌状。 |
How to Cite
NNU_Group (2011). 流水波痕, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/60e1546f-8e4d-40c0-a721-0d5ab7dbd473
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