“…The geomorphology of volcanoes has long been used to investigate volcanic development and activity (Thouret, 1999). Digital topography has been used to classify volcano morphology (e.g., Euillades et al, 2013;Favalli et al, 1999;Grosse et al, 2014;Pedersen & Grosse, 2014;Prima & Yoshida, 2010), identify and assess eruptive deposits and structures (e.g., Csatho et al, 2008;Hofton et al, 2006;Hutchison et al, 2015;Zouzias et al, 2011), and evaluate ongoing volcanic hazards (e.g., Favalli et al, 2005;Córdoba et al, 2015;Stefanescu et al, 2012). Many studies have used the morphometry of lava flow deposits (e.g., Nomikou et al, 2014;Pyle & Elliott, 2006;Tarquini et al, 2012;Ventura & Vilardo, 2007), cones (e.g., Fornaciai et al, 2012;Kervyn et al, 2012), and other deposits (e.g., Jessop et al, 2012) to investigate their rheology and dynamics of emplacement.…”