Large earthquakes initiate chains of surface processes that last much longer than the brief
moments of strong shaking. Most moderate‐and large‐magnitude earthquakes trigger …

Landslide deformations involve approximately all geological materials (natural rocks, soil,
artificial fill, or combinations of these materials) and can occur and develop in a large variety …

In the French Alps, Séchilienne rockslide is one of the natural phenomena that presents one
of the highest levels of risk in terms of socioeconomical outcomes. This rockslide has been …

Although, thanks to the new developments in investigation techniques, modeling, and data
analyses, much progress has been made in our understanding of collateral seismic hazards …

The influence of site effects on landslide triggering during earthquakes has been inferred in
several studies, but its evaluation is made difficult by the complexity of factors controlling the …

Earthquake induced slope failures are responsible for a significant amount of life loss and
damage, and their effective mitigation requires further advancements in our comprehension …

The Séchilienne rockslide, in the French Alps, has recently been instrumented with three
seismic arrays. This network has recorded numerous rockfalls and local microearthquakes …

A variety of methods (detailed geomorphological surveys, geotechnical investigations, local
instrumentation, satellite data, and radar interferometry) along with geophysical techniques …

Situated in an active tectonic region, Santiago de Chile, the country's capital with more than
six million inhabitants, faces tremendous earthquake risk. Macroseismic data for the 1985 …

Landslide phenomena involve the northern coast of Malta, affecting in particular the urban
area of Xemxija. Limestones overlying a clayey formation represent the shallower lithotypes …