Figure 6From: Key factors influencing the mechanism of rapid and long runout landslides triggered by the 2008 Wenchuan earthquake, ChinaA complex slide (rockslide–debris flow) occurred in Donghekou Village, Qingchuan County during the Wenchuan Earthquake. (a) Photo of the region before the earthquake, taken by the local people and (b) Photo 2 months (July 2008) after the earthquake by the first author. The flow-path was considered to be fully saturated.Back to article page