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 …

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 …

Globally, glacial and paraglacial environments in mountains are vulnerable to the effects of
ongoing contemporary climate change (global warming), but monitoring of such systems …

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

On the 20th September 2012, a large debris slide occurred in the Móafellshyrna Mountain in
the Tröllaskagi peninsula, central north Iceland. Our work describes and discusses the …

The temporal pattern of rock‐slope failures (RSFs) following Late Pleistocene deglaciation
on tectonically stable terrains is controversial: previous studies variously suggest (1) a rapid …

Landslides are important components of global geoheritage, but awareness of their
significance and value in such terms seems scanty in the scientific community. Landslides …

In de‐glaciated areas, para‐glaciation (ie the conditioning of landscapes by prior glaciation)
has often been considered a major predisposing factor in landslide occurrence; its …

Two main ways in which the progress of deglaciation in mountains can be identified and
monitored are through (a) meltwater loss over time as glaciers and permafrost melt and (b) …

Most studies focusing on landslide spatial analysis have considered the relationships
between predictors and landslide occurrence as fixed effects. Yet spatially varying …