Paraglacial geomorphology is the study of earth-surface processes, sediments, landforms,
landsystems and landscapes that are directly conditioned by former glaciation and …

Assessing initiation of rock-slope deformation and paleo-slip rates of rockslides is important
to understand the impact of climate variability-in particular permafrost changes-on rockslide …

The evidence for the Little Ice Age, the most important fluctuation in global climate in
historical times, is most dramatically represented by the advance of mountain glaciers in the …

The world's coastlines represent a myriad of dynamic and constantly changing
environments. Heavily settled and intensely used areas, they are of enormous importance to …

A guide to the systematic understanding of the geoarchaeological matrix Reconstructing
Archaeological Sites offers an important text that puts the focus on basic theoretical and …

This is a study of the Quaternary alluvial sedimentation and its controls in the piedmont zone
of the Lefka Ori limestone massif in southwestern Crete, Greece. The piedmont was …

Whether rock glaciers are permafrost creep features or may also be related to glaciers in
non-permafrost environments, and whether they should be defined by genesis or …

Landslide dams are a particular kind of natural dam which forms when an earth or rock mass
reaches a river channel causing its complete or partial blockage. Since 1995, the Earth …

Slope deposits are found on slopes or at the base or foot of slopes. Two main groups of
processes are usually involved in the development of a given slope deposit:(i) slope wash …

Debris-flow activity in a watershed is usually defined in terms of magnitude and frequency.
While magnitude–frequency (M–F) relations have long formed the basis for risk assessment …