In the most destructive and catastrophic landslide events, rocks, soil and fluids can travel at
speeds approaching several tens of metres per second. However, many landslides …

Assessing initiation of rock-slope deformation and paleo-slip rates of rockslides is important
to understand the impact of climate variability-in particular permafrost changes-on rockslide …

Mapping and monitoring landslides in remote areas with steep and mountainous terrain is
logistically challenging, expensive, and time consuming. Yet, in order to mitigate hazards …

The movement of large, slow-moving, deep-seated landslides is regulated principally by
changes in pore-water pressure in the slope. In urban areas, drastic reorganization of the …

Earthquake triggered landslides often pose a great threat to human life and property.
Emerging research has been devoted to documenting coseismic landslides failed during or …

Heavy rainfall has long been recognized as a key factor in the triggering of landslides, as
large amounts of precipitation generally have strong weakening effects on anti-sliding forces …

Slow‐moving landslides are hydrologically driven. Yet, landslide sensitivity to precipitation,
and in particular, precipitation extremes, is difficult to constrain because landslides occur …

Large slow rock-slope deformations, including deep-seated gravitational slope deformations
and large landslides, are widespread in alpine environments. They develop over thousands …

Catastrophic landslides with basal shear zones usually involve a number of mechanisms
that are poorly understood. One mechanism issue is the transition from slow sliding to fast …

The residual strength of sliding basal soils plays a pivotal role not only in the movement of
bedding landslides controlled by clay-rich interlayers but also in remobilized granular …