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debris slide
泻溜
在陡峭的坡面上,由于冷热干湿交替变化,表层物质严重风化,造成土石体表面松散和内聚力降低,形成与母岩体接触不稳定的碎屑物质,这些岩土碎屑在重力作用下时断时续地沿斜坡坡面或沟坡坡面下泻的现象。
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