Landslides are natural hazards that may show diverse and complicated triggering and failure processes, such as advancing, enlarging, progression, and retrogression, due to varying soil properties, slope geometry or environments, etc (Varnes, 1958). Among the different failure patterns, retrogressive failure is characterized by a series of rearward-advancing disruptions of a slope after triggering by a small initial failure at the toe. The sequential failure can spread miles away from the starting point, as reported by Locat et al. (2011). In literature, retrogressive slope failures are mostly observed and discussed in relation to the failure of sensitive clay (