Rainfall-initiated landslides continue to inflict damages and loss of life throughout the world.
Processes and mechanisms revealed from hydrological, geomorphic, geotechnical …

Rockslides in alpine areas can reach large volumes and, owing to their position along
slopes, can either undergo large and rapid evolution originating large rock avalanches or …

Understanding and quantifying the evolution of landslides are research topics that have
always engaged researchers. Indeed, scientific literature provides a large number of …

Landslides are common features found on steep slopes on Mars and the role of water in
their formation is an open question. Our study focuses on three young martian landslides …

The prediction of landslide movement acceleration is a complex problem, among others
identified for deep-seated landslides, and represents a crucial step for risk assessment …

This paper deals with the applicability of electrical resistivity tomography (ERT) for the
recognition of large landslide structures at depths, which have never previously been …

Rainfall is one of the major triggering factors of landslides, and its pattern controls their
temporal behaviour. Characterization of the groundwater processes and possible …

Clay shale landscapes are sensitive to landslide, erosion, and re‐sedimentation processes.
In this context, tectonized clay shales have peculiar hydrological and mechanical …

Among the processes controlling landslide dynamics, piezometry plays a major role. The
characterization of a landslide's aquifer recharge (= inflows) is thus indispensable for …

Onshore slides are driven by gravitational forces that are either related to a basal or a
surface slope. Resisting these driving forces are the friction at the base of the slide, and the …