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 …

Reservoir landslides are typical geohazards with sophisticated thermo‐hydro‐mechanical
interactions. However, direct observations of subsurface multi‐physical processes in bank …

Rock avalanches represent a serious risk for human lives, properties, and infrastructures. On
June 24, 2017, a catastrophic landslide destroyed the village of **nmo (Maoxian County …

The addition of water on or below the earth's surface generates changes in stress that can
trigger both stable and unstable sliding of landslides and faults. While these sliding …

Deformation monitoring of sliding zones or surfaces is of great significance to investigate
evolution stages and triggering factors of landslides. The fiber–optic strain sensing cables …

Episodically to continuously active slow‐moving landslides are driven by precipitation.
Climate change, which is altering both the frequency and magnitude of precipitation …

Strong earthquakes in mountainous areas can trigger a large number of landslides that
generate deposits of loose and unconsolidated debris across the landscape. These deposits …

Temperature fluctuations in landslide shear zones can originate from heat exchanges with
deeper layers as well as with the atmosphere through the landslide body. Shallow …

Abstract On August 28, 2017, a large rock avalanche occurred in Pusa, a village in the
County of Nayong (Guizhou Province, China). About 500,000 m 3 of rock detached from a …

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 …