The landslide happened in the southwest of Yushan Village in Zoucheng of Shandong in 1950s, some farmland was destroyed. It was a shallow soil landslide, the landslide mass was mainly pebbly-clay; the sliding zone was located in the pebbly-clay and bedrock contact zone. Due to the artificial slope cutting, the sliding zone in the front had been exposed, and the sliding bed was underlying strong weathered diorite. In recent years, frequent human engineering activities may lead to the landslide reoccurring. In order to eliminate the risks of geological disasters, the combined control plan with cantilever retaining wall and water interception & drainage system was taken to achieve the control effect.