Establishing landslide chronologies is essential both for understanding causes of mass movements as part of fundamental geomorphological research, and for the assessment of landslide hazards as part of applied geomorphology. The AA. discuss
The aim of this paper is to ascertain precisely the roles played both by permanent conditions (geological structure, geomorphological setting, angles of slope) and triggering factors (anthropogenic interference, rainfall) in the occurrence
Deep-seated mass-movements of different types affect the Pizzotto-Greci slope in northwest Calabria, Italy. The main aspects of the geological and geomorphological studies and some preliminary geotechnical data are presented here, along