The long-travelling motion of debris agitated and saturated with water is called a``debris flow''. Debris flows can develop during heavy rainfall, when a debris slide changes into a debris flow. They can travel several kilometres from their source and inundate a large area ...
CITATION STYLE
Sassa, K., & Wang, G. hui. (2007). Mechanism of landslide-triggered debris flows: Liquefaction phenomena due to the undrained loading of torrent deposits. In Debris-flow Hazards and Related Phenomena (pp. 81–104). Springer Berlin Heidelberg. https://doi.org/10.1007/3-540-27129-5_5
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