海蚀台
又称浪蚀台。在地壳稳定的条件下，海蚀崖长期受携带泥沙的激浪的磨蚀而不断后退，并在其前方形成一个向海微斜的近似平坦的基岩台地。其上常覆有砂、砾等海积物，或残留有较坚硬岩石形成的海蚀柱和海蚀残丘等。低潮时部分出露海面，高潮时则海蚀台柱没于海面之下。中国基岩海蚀崖前大都有海蚀台出现。由于陆地上升或海面下降，可被抬升而形成海蚀阶地。
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Contributor
contributed at 2011-10-13
Classification(s)
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Earth System(in Chinese) Marine geology
Detailed Description
| English |
|---|
| Name | wave cut bench, marine bench |
| Chinese |
|---|
| Name | 海蚀台 |
| Description | 又称浪蚀台。在地壳稳定的条件下，海蚀崖长期受携带泥沙的激浪的磨蚀而不断后退，并在其前方形成一个向海微斜的近似平坦的基岩台地。其上常覆有砂、砾等海积物，或残留有较坚硬岩石形成的海蚀柱和海蚀残丘等。低潮时部分出露海面，高潮时则海蚀台柱没于海面之下。中国基岩海蚀崖前大都有海蚀台出现。由于陆地上升或海面下降，可被抬升而形成海蚀阶地。 |
How to Cite
NNU_Group (2011). 海蚀台, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/74cd90c5-38bb-4df9-ab06-106e497e7899
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