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 …

Monitoring landslides is essential to understand their dynamics and to reduce the risk of
human losses by raising warnings before a failure. A decade ago, a decrease of apparent …

In tectonically active mountain belts, landslides contribute significantly to erosion. Statistical
analysis of regional inventories of earthquake-triggered-landslides after large earthquakes …

Slow-moving landslides are widespread in many landscapes with significant impacts on the
topographic relief, sediment transfer and human settlements. Their area-wide mapping and …

The Sentinel-2 optical satellites provide a global coverage of land surfaces with a 5-day
revisit time at the Equator. We investigate the ability of these freely available optical images …

In mountainous environments, slow‐moving landslides (velocities< 100 m/year) are a major
concern for local populations. Rainfall is often the dominant forcing, and often result in major …

Slow-moving landslides are numerous in mountainous areas and pose a large threat to
populations. Many observations show that their kinematics is driven by climatic forcings and …

Major earthquakes in mountainous areas often trigger rapid landslides. Some observations
also suggest that earthquakes can damage landslide prone areas or cause slow-moving …

In this study, on the basis of the image correlation technique and the time-series images of
Landsat-8 (L8), Sentinel-2 (S2), and GaoFen-2 (GF2), a systematic technical process is …

Landslides are the main secondary effects of earthquakes in mountainous areas. The spatial
distribution of these landslides is controlled by the local seismic ground motion and the local …