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Hazard characteristics and mechanism are important for landslide analysis�� To analyze the threat to the humans and the cultural relics��we studied the landslides in the Beishan temple slope area��which shows several landslides developed in this slope area��i��e��the old landslide��forest farm new landslide I��Sanqing temple new landslide II and deep potential landslide�� The information of the shape��length��width and depth of each landslide is investigated and obtained�� The old landslide��forest farm new landslide I and Sanqing temple new landslide II belong to shallow types��and the slip surface is the creep surface between the colluvium and the bed rocks�� The development and generation of the deep landslides depend on the following steps: uploading rebound��slip of the front area along the potential soft surface �� tension and deformation of the trailing area �� extension of the pressure crack �� generation and connection of the deep potential slip surface��