Deception Island (South Shetland Islands) is one of the most active volcanoes in Antarctica, with more than 15 explosive eruptive events registered over the past two centuries. Recent eruptions (1967, 1969 and 1970) and volcanic unrest episodes in 1992, 1999 and 2014–15 demonstrate that the occurrence of future volcanic activity is a valid and pressing concern for scientists, logistic personnel and tourists that are visiting or are working on or near the island. Over the last few decades, intense research activity has been carried out on Deception Island to decipher the origin and evolution of this very complex volcano. To that end, a solid integration of related scientific disciplines, such as tectonics, petrology, geochemistry, geophysics, geomorphology, remote sensing, glaciology, is required. A proper understanding of the island's evolution in the past, and its present state, is essential for improving the efficiency in interpreting monitoring data recorded during volcanic unrest periods and, hence, for future eruption forecasting. In this chapter, we briefly present Deception Island's most relevant tectonic, geomorphological, volcanological and magmatic features, as well as the results obtained from decades of monitoring the island's seismic activity and ground deformation.

Plan research projects: CGL2007-28855-E, CTM2008- 03062-E, CTM2009-07705-E, CTM2009-08085-E, CTM2010- 11740-E, CTM2011-16049-E,CTM2014-57119-R, CTM2014-60451- C2-2-P, BRAVOSEIS (CTM2016-77315-R), CORSHET (POL2006- 08663), RECALDEC (CTM2009-05919-E/ANT), PEVOLDEC (CTM2011-13578-E/ANT), POSVOLDEC (CTM2016-79617-P) (AEI/FEDER, UE) and VOLGASDEC (PGC2018-095693-B-I00) (AEI/FEDER, UE). A. Geyer is grateful for her Ramón y Cajal contract (RYC-2012-11024). D. Pedrazzi is grateful for his Beatriu de Pinós (2016 BP 00086) and Juan de la Cierva (IJCI-2016-30482) contracts.

Peer reviewed