Pyroclastic deposits at the base of dacitic dome (grey in color). Photo ID 640
Pyroclastic deposits at the base of dacitic dome (grey in color). Photo ID 640
Photograph: Alessandro Da Mommio
Reference: The transition from subduction arc to slab tearing: Evidence from Capraia Island, northern Tyrrhenian Sea. Massimo Gasparona, Gideon Rosenbauma, Jan Wijbransb, Piero Manetti