“…In particular, the landscape is the result of the mantling of preexisting volcanic edifices by the 15 ka Neapolitan Yellow Tuff (Deino, Orsi, De Vita, & Piochi, ), of the collapse of the related caldera (PF depression) and, between 15 and 3.8 ka, of the accumulation of products from at least 70 explosive eruptions of variable magnitude which generated variably dispersed pyroclastic deposits and formed tuff cones, tuff rings, and lava domes (Di Vito et al., ). These morphologies are cut by SW‐NE and NE‐SW fault scarps, widely spread in the study area (Amato et al., ; Cinque et al., ; Romano et al., ) due to the intense volcano‐tectonics (Fig. ) detected within the PF caldera, the Bay of Naples, and the Campania Plain (Bruno, Rapolla, & Di Fiore, ; Cinque et al., ; Di Vito et al., ).…”