“…Severe retreat processes, mainly occurring with landslides and erosion, are affecting, for instance, many of the coastal cliffs forming the rocky Italian coastline in various geological contexts (Iadanza et al, 2009;Furlani et al, 2014). Here, failures may affect cliff formed by carbonate rocks (e.g., Andriani and Walsh, 2007;Ferlisi et al, 2012), arenaceous-pelitic or calcareous-pelitic flysch (e.g., Budetta et al, 2000;De Vita et al, 2012), sandstones (e.g., Sciarra et al, 2015), shales (e.g., Raso et al, 2017), or volcanic rocks (e.g., Barbano et al, 2014).…”