“…In addition, earthquake loading can influence the shape of failure surface, particularly when tension cracks are present. Earthquake-induced landslides are among the most destructive slope movements and there is a large body of literature on limit analysis or other methods applied on landslides triggered by seismic activities (Chang et al, 1984, Ling and Leshchinsky, 1995, Crespellani et al, 1998, Cao and Zaman, 1999, You and Michalowski, 1999, Loukidis et al, 2003, Chen and Liu, 1990, Yang and Chi, 2014. Seismic shaking can directly trigger slope failures and at the same time cause damage within the slope material, predisposing it to successive failures under different triggering factors or earthquakes of smaller magnitude.…”