Deep seated gravitational slope deformations (DSGSD) are widespread phenomena,
recognized in different mountain ranges worldwide. The distribution of such phenomena at …

Deep-seated gravitational slope deformations (DSGSDs) are slow moving, hillslope-scale
mass movements featuring characteristic landforms such as double-crested ridges and …

The ages of 31 postglacial rock-slope failures (RSFs) in Scotland and NW Ireland, derived
from 89 cosmogenic isotope exposure ages, are employed to analyse the temporal pattern …

Large landslides and deep-seated gravitational slope deformations (DSGSD) represent an
important geo-hazard in relation to the deformation of large structures and infrastructures …

Recent progress of dating techniques has greatly improved the age determination of various
types of landslides. Since the turn of the 21st century, the number of dated landslides …

This paper presents a detailed analysis of a dramatic rock slope acceleration that occurred
in fall 2016 at the Moosfluh Landslide, located at the glacier tongue of the Great Aletsch …

Reconstructing the ages and magnitudes of prehistoric extreme events that are recorded in
landforms and sediments allows us to capture the full range of frequency-magnitudes and …

Climatic factors are considered major causes and triggers of slope instability, but the
palaeoclimatic implications of landslides have not yet been systematically reviewed. As …

Rock slopes next to the tongue of the Great Aletsch Glacier, Switzerland are characterized
by rapid environmental adjustment to non-glacial conditions. This study investigates and …

Rock slope failure (RSF) occurs in different contexts but is typically reported either as (i)
single-category inventories or (ii) single-site geotechnical monographs. Few studies have …