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    Debris flow propagation and deposition: from the field scale of the Giampilieri alluvial event (Messina, Italy) to the laboratory scale

    Dott.ssa Laura Maria Stancanelli (Universitą di Catania) 7 giugno 2017, ore 15:30 Aula Beltrami - Edificio 5 - piano terra - Campus Leonardo

    Debris flows are rapid, gravity-induced mass movements consisting of sediment-liquid mixtures, which propagate along channels carved into mountain slopes or debris fans. These movements represent a serious natural hazard due to the high velocity, the large volumes of mobilized sediment, and the highimpact forces exerted on any obstacle they come across. ...

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