“…Notoriously, the landslide occurrence can be controlled by several factors, which can be subdivided into predisposing and triggering factors. The former include intrinsic factors that make an area prone to slope instability such as slope (Dai, Lee, & Ngai, 2002;Guzzetti, Reichenbach, Ardizzone, Cardinali, & Galli, 2006), lithology (Duman et al, 2005;Chacón, Irigaray, Fernandez, & El Hamdouni, 2006), aspect (Calvello, Cascini, & Mastroianni, 2013;Guzzetti, 2005), land use (Cevasco, Pepe, & Brandolini, 2014;Glade, 2003;Matthews, Brunsden, Frenzel, Glaser, & Weiß, 1997;Van Beek & Van Asch, 2004), vegetation cover (Cammeraat, van Beek, & Kooijman, 2005;Gonzalez-Ollauri & Mickovski, 2017), distance from rivers and roads (Bordoni et al, 2018;Donnini et al, 2017). The latter are represented by factors that actually trigger the landslide such as intense or prolonged rainfall, earthquakes, rapid snow melting and human activities (Anderson & Holcombe, 2013;Corominas et al, 2014;Crosta, Agliardi, Frattini, & Sosoi, 2012).…”