Debris flows are one of the most frequent mass movement processes which develop on the
mountain river network. With high flow velocity, long run-out, and high impacts, they are
one of the most hazardous types of landslide. The material involved is heterometric debris
with an extremely heterogeneous grain size distribution. The present research is focused on
the interaction between the potential debris flow deposits from Rio Conzen and Canalone
Andrea rivers with one of the four settling slag basins created during mining operations in
the Cave del Predil mine (Tarvisio, Friuli Venezia Giulia, NE Italy). The mine is historical,
the first written record of its existence dates back to 800BC. It remained active for a long
period, and was the cause of dispute between the Italians and Austrians during WWI when
the Austrians used a tunnel to transport troops and war material. After 1991 when the mine
was closed, some levels were partially flooded in order to grant stability to the mine. The
latter was later converted into a touristic area that along with the whole Val Canale valley
was hit by an extremely intense alluvial event in August 2003 when more than 100 debris
flows occurred. The valley is orthogonal to Val Canale where more intense damages
occurred, but the possibility of the occurrence of new events (return period of 300y) is still
high. The aim of this study was to create a possible scenario of the event, using FLO-2D
software. The scenario obtained allow to study the interactions between debris flow
deposits and the slag basins, and provide an understanding of the possibility of a river
interruption. Scenarios can be considered extremely useful data to assist in informed future
territorial planning of the area providing a good indication for hazard definition.
