On August 21, 2020, Fuquan Town, Hanyuan County, Sichuan Province, landslide geological disasters, large rock landslides, landslides, destructive, causing huge losses to the local. This paper collects relevant data through field investigation. The movement and deformation mechanism and causes of Hanyuan landslide are analyzed, and the main results are as follows. 1. In recent years, the local surface of the landslide area has a certain tensile deformation, and the terrain changes greatly in the rear edge of the landslide and the steeper part of the middle and upper part of the landslide, forming a multi-stage dislocation platform. 2 The landslide is a traction landslide induced by rainfall. At present, it is in the stage of creep deformation. The failure mode is that the clay rock of Xigeda Formation is softened after soaking in groundwater, which leads to the decrease of shear strength and the formation of local bedding sliding at the edge of the scarp. 3. The landslide front is saturated, and the landslide is cut out from the shear outlet on the free face of the shear outlet. The transverse cracks at the trailing edge of the landslide continue to widen and deepen. 4. Under the action of continuous heavy rainfall, rainwater infiltrates into the sliding body and sliding surface, and sliding will occur. The landslide coverage directly slides out and accumulates in the valley, and the rare debris flow may occur.