它们开始时作为岬角和海崖的一部分与陆地相连，海浪粉碎地侵蚀了较为脆弱的岩石，而把较硬的岩石留在所形成海栈的后面。

They start as part of a headland or sea cliff connected to land. Smashing waves erode the softer rock, leaving harder rock behind in the form of sea stacks.

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作为比较，东亚部分陆地的地表温度与台湾海峡南部、黄海的海表温度及其日变化、季节变化一并进行了分析。

The characteristics of LST in most land of East Asia and that of sea surface temperature(SST) in the south of Taiwan Strait and the Yellow Sea were also analyzed as comparison.

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