The feature of landslide time space movement was a geological process of landslide geological mass from a state to a other state under internal and external factors action.
滑坡时空运动特征是滑坡地质体在内因和外因共同作用下，自一种状态向另一种状态转化的地质过程。
By analyzing the geological condition in the area of the potential landslide, the contributing factor of potential landslide mass is put forward and its stability is checked.
通过对潜滑体区域地质情况的分析，指出了潜滑体的成因，并对其稳定性进行了验算，根据分析结果提出了相应的防治措。
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