贝窝
又称流痕。由紊流水的溶蚀和侵蚀作用，在洞壁（或洞外岩壁）上贝窝形成的一种波状凹入的形态，常成群出现。其剖面不对称，迎水面缓而较长，背水面陡而较短，故可用以确定形成时水流流向，其波长由1～2厘米至大于1米。其大小与水的流速成反比。
Classification(s)
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Geographic semantic resource library Earth System(in Chinese) Karstology
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| English |
|---|
| Name | scallop solutional ripple, flute |
| Chinese |
|---|
| Name | 贝窝 |
| Description | 又称流痕。由紊流水的溶蚀和侵蚀作用，在洞壁（或洞外岩壁）上贝窝形成的一种波状凹入的形态，常成群出现。其剖面不对称，迎水面缓而较长，背水面陡而较短，故可用以确定形成时水流流向，其波长由1～2厘米至大于1米。其大小与水的流速成反比。 |
{{htmlJSON.HowtoCite}}
NNU_Group (2011). 贝窝, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/3d623bac-a732-43a2-86d1-f824c611139e
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