“…These local, intense, convective rainfalls (Underwood et al, submitted) produce abundant runoffs at the feet of rocky headwater walls that are able to entrain large quantities of sediments and debris flows. Runoffgenerated debris flows, initially observed in laboratory facilities (Gregoretti, 2000a,b;Tognacca et al, 2000), are common both in the Alpine region (Berti and Simoni, 2005;Gregoretti and Dalla Fontana, 2008;Theule et al, 2012;Tiranti and Deangeli, 2015) and in other mountainous regions such as the Pyrenees (Hurlimann et al, 2014), Japan Alps (Imaizumi et al, 2006;Okano et al, 2012), Colorado and California (Cannon et al, 2008;Coe et al, 2008;Kean et al, 2012). The routing of debris flow in settled areas can cause damage and casualties.…”