Initiation processes for run-off generated debris flows in the Wenchuan earthquake area of China

The frequency of huge debris flows greatly increased in the epicenter area of the Wenchuan earthquake. Field investigation revealed that runoff during rainstorm played a major role in generating debris flows on the loose deposits, left by coseismic debris avalanches. However, the mechanisms of these...

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Veröffentlicht in:	Geomorphology (Amsterdam, Netherlands) Netherlands), 2016-01, Vol.253, p.468-477
Hauptverfasser:	Hu, W., Dong, X.J., Xu, Q., Wang, G.H., van Asch, T.W.J., Hicher, P.Y.
Format:	Artikel
Sprache:	eng
Schlagworte:	Channels Damming and breaching effect Debris Debris flow Earthquakes Erosion Fluidization Flumes Geomorphology Run-off Runoff Slopes Three dimensional
Online-Zugang:	Volltext
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