海底隆起
- 网络submarine swell;subsea elevation
海底隆起-
地震海啸是当海域发生大地震时，海底隆起和下沉引起的海浪。地震海啸常常具有巨大的摧毁力，会给人类带来巨大的灾难。
The tsunami generated by earthquake is a kind of sea wave directly created by the ocean floor uplifting and subsiding , which usually has great destructive power and could bring huge calamity to human .
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通过计算，展现了滑坡的发展演化过程，并将其分为三个阶段，即轻微隆起阶段、强烈隆起阶段、滑面贯通剪出阶段。二是海底地形隆起与拗陷反差强烈；
E. slight hunch stage , intensive hunch stage and transfixion and fast slippage stage . secondly , a great contrast between apophysis and depression of the seafloor topographty ;