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海积夷平岸
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海积夷平岸
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理学
〔海岸分类〕
释
coast planation by marine deposition
海积夷平岸
在海水淹没的平原上,由于海岸带物质来源多,水下岸坡平缓,海岸海湾地区以堆积作用为主,在水下岸坡下部会发生冲刷,冲刷产物沿岸坡上移,形成水下堤、离岸堤、海滩等,最终使海岸因堆积而夷平。
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