Debris floods are geophysical phenomena that are difficult to quantify in mountain streams because they turn otherwise peaceful waters into powerful torrents capable of overtopping their banks and reorganizing landforms along their channel boundaries in often poorly predictable ways (Figure 1). Debris floods are conventional water floods that are sufficiently powerful to mobilize all erodible materials on the stream bed and along its banks and can carry very large volumes of sediment.Costa (1984, 1988) has defined severe sediment transporting events in steep channels as "water floods," "hyperconcentrated flows," (or "mud floods") and "debris flow." Hungr et al. ( 2014) and Wilford et al. ( 2004) have popularized the term "debris flood" describing severe floods involving exceptionally high rates of transport of coarse sediments, usually occurring in steep channels. Church and Jakob (2020) recently proposed subdividing debris floods into three categories: those triggered by a supra-critical bed shear stress ratio (Type 1), those that form by dilution from debris flows (Type 2), and those resulting from outbreak floods (Type 3).All three debris flood types are associated with large-scale bed mobilization and may therefore cause extensive and rapid bank erosion (Church & Jakob, 2020) and deep scour (Theule et al., 2015;de Haas & van Woerkom, 2016). Bank erosion can lead to building collapse and severing of roads and other linear infrastructure that typically follows valleys (e.g., Arnaud-Fassetta et al., 2005;Jakob et al., 2017). The geomorphic effect of a debris flood depends on the channel gradient, the water depth, and the length of time during which a critical bed shear stress is exceeded (Church & Jakob, 2020).