Debris flow and debris flood phenomena threat the life of thousands of citizens living in
mountain areas and endanger buildings and infrastructure worldwide. The assessment of …

Debris flows have been always a serious problem in the mountain areas. Research on the
assessment of debris flows susceptibility (DFS) is useful for preventing and mitigating debris …

Land use and land cover change can increase or decrease landslide susceptibility (LS) in
the mountainous areas. In the hilly and mountainous part of southwestern China, land use …

In the Dolomitic region, abundant coarse hillslope sediment is commonly found at the toe of
rocky cliffs. Ephemeral channels originate where lower permeability bedrock surfaces …

A large amount of debris was generated by the co-seismic mass wasting associated with the
2008 M w 7.9 Wenchuan earthquake. The abundance of this loose material along the slopes …

The landslide susceptibility (LS) of any mountainous region is significantly affected by the
land-use land-cover (LULC) change. Recently, LULC change effects on landslides have …

Debris flows are common geological hazards in mountainous regions worldwide. The scale
of debris flows can be significantly enhanced by basal erosion and bank collapse in the …

Debris flows can grow greatly in size by entrainment of bed material, enhancing their runout
and hazardous impact. Here, we experimentally investigate the effects of debris‐flow …

A large and catastrophic rock avalanche occurred at the Xinmo village in the Maoxian
county of the Sichuan province of China on June 24, 2017. The avalanche destroyed 64 …

A solid physical understanding of debris‐flow erosion is needed for both hazard prediction
and understanding landscape evolution. However, the processes and forces involved in …