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 …

Geophysical monitoring of landslides can provide insights into spatial and temporal
variations of subsurface properties associated with slope failure. Recent improvements in …

Ambient-noise-based seismic monitoring of the near surface often has limited
spatiotemporal resolutions because dense seismic arrays are rarely sufficiently affordable …

Records of Alpine microseismicity are a powerful tool to study landscape-sha** processes
and warn against hazardous mass movements. Unfortunately, seismic sensor coverage in …

In the context of in-situ geophysical methods the Electrical Resistivity Tomography (ERT) is
widely used for the near-surface exploration of landslide areas characterized by a complex …

We retrieve P diving waves by applying seismic interferometry to ambient‐noise records
observed at Long Beach, California, and invert travel times of these waves to estimate 3‐DP …

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

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 …

Environmental seismology consists in studying the mechanical vibrations that originate from,
or that have been affected by external causes, that is to say causes outside the solid Earth …

Landslides (LS) represent geomorphological processes that can induce changes over time
in the physical, hydrogeological, and mechanical properties of the involved materials. For …