Earthquake-induced landslides, also called seismic landslides (SLs), are some of the most
catastrophic natural hazards on the Tibetan Plateau (TP). They have frequently caused …

Strong earthquakes, especially on mountain slopes, can generate large amounts of
unconsolidated deposits, prone to remobilization by aftershocks and rainstorms. Assessing …

The Wenchuan earthquake triggered numerous landslides and damaged vast areas of
vegetation. Strong mountain earthquakes have long-term impacts on the activities of …

Modern satellite networks with rapid image acquisition cycles allow for near-real-time
imaging of areas impacted by natural hazards such as mass wasting, flooding, and volcanic …

Frequent geohazards have knock-on effects on ecological quality. Timely and dynamically
monitoring the damage of geohazards to ecological quality is important to the geological …

Coseismic landslides are a major hazard associated with large earthquakes in mountainous
regions. Despite growing evidence for their widespread impacts and persistence, current …

Debris flow activity increased after the Wenchuan earthquake, and many debris flows
continue to occur. Recently, a catastrophic debris flow event was triggered by strong rainfall …

A major earthquake can trigger numerous landslides, which exert severe impacts on
regional vegetation coverage. In some years following an earthquake, rainstorms can easily …

Catastrophic earthquakes that occur in mountainous areas always trigger a large number of
co-seismic geohazards, which exerts a negative impact on the geological environment and …

It is widely recognized that post-seismic mass movements amplify and decay. Previous
studies have found that most post-seismic mass movement is concentrated in the first few …