▪ Abstract Field observations, laboratory experiments, and theoretical analyses indicate that
landslides mobilize to form debris flows by three processes:(a) widespread Coulomb failure …

Rainfall‐triggered landslides are among the most widespread hazards in the world. The
hydrology in and around a landslide area is key to pore pressure buildup in the soil skeleton …

Coseismic landslides pose immediate and prolonged hazards to mountainous communities,
and provide a rare opportunity to study the effect of large earthquakes on erosion and …

Catastrophic collapse of large rock slopes ranks as one of the most hazardous natural
phenomena in mountain landscapes. The cascade of events, from rock-slope failure, to rock …

Steep, soil‐mantled hillslopes evolve through the downslope movement of soil, driven
largely by slope‐dependent transport processes. Most landscape evolution models …

The slope stability issues concerning rainfall induced slope failures are investigated and
presented. Specifically, the effect of both negative and positive pore water pressures on the …

Movements and failure of cuts and natural slopes constitute an important geotechnical
problem that involves a variety of geomaterials in a variety of geological and climatic …

Soil moisture is a critical component of the earth system and plays an integrative role among
the various subfields of physical geography. This paper highlights not just how soil moisture …

Predicting debris flow runout is of major importance for hazard mitigation. Apart from
topography and volume, runout distance and area depends on debris flow composition and …

Several multivariate statistical analyses have been performed to identify the most influential
geological and geomorphological parameters on shallow landsliding and to quantify their …