摘要：Geomorphological investigations in the area ofCortina d’Ampezzo (Dolomites, Italy) have beencarried out since the 1980s mainly within nationaland European research projects. This has enabledthe researchers to define, on the one hand, thegeomorphological evolution of the area and, on theother hand, the spatial and temporal occurrence oflandslides, that are the most spread geomorphologicalfeature of the studied area.
