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古老滑坡往往规模大,变形持续缓慢。通过详实调查研究表明,池头滑坡具有显著的古老滑坡的系列特征。滑坡局部复活主要影响因素是后缘弃土石堆载加压、坡中耕作蓄水、前缘河流侵蚀和强降雨诱发。
Ancient landslides are often large-scale, deformation continued to slow. Through detailed investigation and study, it shows that the landscaped of ChiTou has obvious series of features of ancient landslide. The main factors that affect the local revival of landslide are the loading pressure of trailing edge abandoned earth, plowing and tillage in impoundment, erosion of front river and intense rainfall.