“…1) Rosi and Sbrana, 1987;Barberi et al, 1991;Scandone et al, 1991;Scarpati et al, 1993;Wohletz et al, 1995;Orsi et al, 1996;Florio et al, 1999;Judenherc and Zollo, 2004 Following the NYT eruption, the evolution of the Campi Flegrei was dominated by hydromagmatic activity with occasional plinian phases and minor effusive activity forming lava domes . Several tens of monogenic phreato-magmatic vents including tuff rings, tuff cones, cinder and spatter cones, have been active in the last 15 kyr mostly inside the NYT caldera collapse Di Vito et al, 1999;Insinga et al, 2006;Di Renzo et al, 2011;Fedele et al, 2011). The last event was the Monte Nuovo eruption in 1538 A.D., which occurred after some 100 years of caldera uplift (Parascandola, 1946;Di Vito et al, 1987;Morhange et al, 1999;D'Oriano et al, 2005;Piochi et al, 2005;Bellucci et al, 2006;De Natale et al, 2006).…”