The largest terrestrial coalescent landslide areas of the Earth, spanning hundreds to
thousands of square kilometres, occur along the fringes of relatively low-relief sedimentary …

Sedimentary and volcanic tablelands host the world's largest landslide areas, sometimes
spanning hundreds of kilometers along escarpments. This study, employing new remote …

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

Establishing regional landslide chronologies is necessary to advance from hazard
recognition to risk assessment, and to understand the evolution of landslide-prone terrain …

Hundreds of basaltic plateau margins east of the Patagonian Cordillera are undermined by
numerous giant slope failures. However, the overall extent of this widespread type of plateau …

High Anatolian orographic margins have large variations in terms of topographic relief,
precipitation, and uplift rate. These variations lead to the dynamics of mass movements and …

Slow-moving landslides are often the dominant process that shapes hillslopes and delivers
sediment to channels in weak lithologies. Understanding what controls their velocities is …

Documenting spatial and temporal patterns of past landsliding is a challenging step in
quantifying the effect of landslides on landscape evolution. While landslide inventories can …

The recent launch of national-scale LiDAR-derived topographic data provides an
opportunity for (re) evaluating the geomorphic imprint of landslides in forested mountains. A …

Although the dynamics of individual rock-slope failures above recently shrinking glaciers
have received increasing study, less is known about the spatial distribution of landslides in …