After a geological and geomorphological description, the distribution in space and time of landslides which occurred in the surroundings of Cortina d'Ampezzo is presented. The type, activity, frequency and, when possible, the age of mass movements
This paper examines the evolution of a large-scale earthflow located in the northern sector of the Marche Region. In this area, mass movements of different typology are particularly frequent since geological and geomorphological conditions often