Recent studies have pointed out a similarity between tectonics and slope tectonic-induced
structures. Numerous studies have demonstrated that structures and fabrics previously …

Landslides are among the most frequent secondary disasters caused by earthquakes in
areas prone to seismic activity. Given the necessity of assessing the current seismic …

Landslide early warning systems (EWSs) have to be implemented in areas with large risk for
populations or infrastructures when classical structural remediation measures cannot be set …

Large catastrophic rock slope failures are difficult to predict because the underlying
mechanisms causing slope accelerations are difficult to study under in-situ conditions. For …

For quantitative hazard assessment it is necessary to define the magnitude–frequency
distribution and a temporal model of the landslide frequency. This is often complicated for …

This paper describes a newly designed, experimental, and affordable rock slope monitoring
system. This system is being used to monitor three rock slopes in Czechia for a period of up …

The basal sliding surfaces in large rockslides are often composed of several surfaces and
possess a complex geometry. The exact morphology and location in three dimensions of the …

The unstable rock slope, Stampa, above the village of Flåm, Norway, shows signs of both
active and postglacial gravitational deformation over an area of 11km2. Detailed structural …

Sackung is a widespread post-glacial morphological feature affecting Alpine mountains and
creating characteristic geomorphological expression that can be detected from topography …

Abstract The Eastern Betic Cordillera (Spain) exemplifies at the Sierra de Aitana an
impressive case of lateral spreading which involves a mountain anticline ridge dislodged by …