On the basis of the correlation between seismic tectonostratigraphic u
nits, volcanism, and geochemical distribution patterns of sea-floor se
diments on Deception Island (Antarctica), a regional tectonic extensio
n is suggested to explain the sequence of volcanic and hydrothermal ev
ents. The syncollapse caldera episode is composed of five tectonostrat
igraphic units separated by progressively tilted and bent unconformiti
es. Each unit shows a sequence of Quaternary volcanic cones and mound
structures that display high contents of Fe, Mn, and Zn. As-rich activ
e fumaroles and hot-spring areas are associated with the postcollapse
episode and linked to normal faulting and present volcanism.