资源环境科技发展态势分析平台

Post-seismic debris flows are an important hazard following large earthquakes, propagating destruction downstream from hillslopes where coseismic landslides occur and extending damage for years after shaking stops. Data sets of post-seismic debris flows are necessary to predict initiation and runout characteristics but are presently scarce. We used satellite imagery supplemented by field observations to compile an inventory of >1,000 debris flows associated with the 2015 Gorkha Earthquake in Nepal. We identified two distinct debris flow types: (1) Material from a coseismic landslide was remobilized in a steep channel during a later monsoon; and (2) a new post-seismic hillslope failure occurred in saturated conditions and became fluidized and channelized. Runout distance was constrained by channel confluences and may be related to confluence geometry. Unstable landslide debris was largely flushed from steep channels during the first monsoon following the earthquake, and the rate of new hillslope failures tailed off over a few years.

Plain Language Summary Debris flows-rapidly flowing slurries of rock, mud, and water-are common in many steep mountain ranges and are deadly hazards to communities that lie in their paths. They are also important erosional mechanisms. Large earthquakes destabilize hillsides and cause landslides, providing abundant opportunities for debris flows to form. Here we mapped and categorized debris flows associated with the 2015 Gorkha Earthquake in Nepal. We identified two main mechanisms for debris flow formation in the wake of the earthquake, and our results suggest that distinguishing these mechanisms may help in post-earthquake hazard assessment. Loose landslide deposits that were generated during the earthquake and that were vulnerable to forming debris flows did so almost exclusively during the first monsoon following the earthquake. Debris flows flowed out to distances influenced by tributary junctions they encountered.