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

Glacial cirques are armchair-shaped erosional hollows, typified by steep headwalls and,
often, overdeepened floors. They reflect former regions of glacier initiation, and their …

This review provides a synthesis of the evolution of the Pyrenees since~ 84 Ma and is
uniquely focused on analysing jointly and comparatively its peripheral pro-foreland, retro …

Moderate-relief landscapes, such as the Czech Flysch Outer Western Carpathians (COWC),
in comparison with alpine regions are rarely subject to extensive landslide inventory …

Hydrothermal systems involving dormant faults within orogenic belts are rarely targeted for
geothermal exploration, partly because of the complexity of the 3‐D topography, the …

Rockfalls are very rapid and damaging slope instability processes that affect mountainous
regions, coastal cliffs and slope cuts. This contribution focuses on fragmental rockfalls in …

The rock masses of hydro-fluctuation belt experience seepage pressure following
impoundment in the Three Gorges Reservoir; its creep behaviors are significant for reservoir …

It has been proposed that most cirques are source‐area depressions of large, deep‐seated
rock‐slope failures. Yet the close relation between cirques and climate is convincing …

Oversteepened valley walls in western Norway have high recurrences of Holocene rock-
slope failure activity causing significant risk to communities and infrastructure. Deposits from …

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) …