“…While in central volcanoes it is generally assumed that future eruptions will occur through the same vents that have been active in the past, in monogenetic systems forecasting the position of new vents is much more challenging due to this lack of a permanent shallow stress configuration. Spatial analysis addressed to infer the location of future vents (volcanic susceptibility, see Martí and Felpeto, 2010) in monogenetic volcanism generally assumes that the next eruption will occur close to the location of the previous ones (Connor, 1990;Connor et al, 1992Ho, 1992Ho, , 1995Martin et al, 1994;Ho and Smith, 1998;Alberico et al, 2002;Martí and Felpeto, 2010;Bebbington and Cronin, 2011;Cappello et al, 2012;Selva et al, 2012;Bartolini et al, 2013;Becerril et al, 2013a;Le Corvec et al, 2013a;Bevilacqua et al, 2015). The reason to make this assumption is based on the fact that in last eruptive episodes volcanoes had formed near previous ones (forming a cluster), so we assume that this behavior will continue.…”