Chapter 7.1 Deception Island

Author:

Geyer A.1ORCID,Pedrazzi D.1ORCID,Almendros J.2ORCID,Berrocoso M.34,López-Martínez J.5ORCID,Maestro A.6ORCID,Carmona E.2ORCID,Álvarez-Valero A. M.7ORCID,de Gil A.34

Affiliation:

1. Geosciences Barcelona, GEO3BCN - CSIC, Lluis Sole i Sabaris s/n, 08028 Barcelona, Spain

2. Andalusian Institute of Geophysics, University of Granada, Granada, Spain

3. Laboratory of Astronomy, Geodesy and Cartography, Department of Mathematics, Faculty of Sciences, University of Cádiz, 11510 Puerto Real (Cádiz), Spain

4. Instituto Universitario de Investigación Marina (INMAR), Universidad de Cádiz, Campus de Excelencia Internacional del Mar (CEIMAR), Campus Universitario de Puerto Real, 11510 Puerto Real, Cádiz, Spain

5. Department of Geology and Geochemistry, Faculty of Sciences, University Autónoma of Madrid, 28049 Madrid, Spain

6. Geological and Mining Institute of Spain, C/Calera, 1, 28760 Tres Cantos, Madrid, Spain

7. Department of Geology, University of Salamanca, 37008 Salamanca, Spain

Abstract

AbstractDeception 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.

Funder

Ministerio de Ciencia e Innovación

Ministerio de Economía y Competitividad

Agència de Gestió d’Ajuts Universitaris i de Recerca

Ministerio de Economía, Industria y Competitividad, Gobierno de España

Ministerio de Ciencia, Innovación y Universidades

Ministerio de Educación y Ciencia

Publisher

Geological Society of London

Subject

Geology

Reference177 articles.

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2. Years to weeks of seismic unrest and magmatic intrusions precede monogenetic eruptions

3. Recent tectonic and morphostructural evolution of Byers Peninsula (Antarctica): insight into the development of the South Shetland Islands and Bransfield Basin;Journal of Iberian Geology,2010

4. Observations of volcanic earthquakes and tremor at Deception Island – Antarctica;Annali di Geofisica,1999

5. Array tracking of the volcanic tremor source at Deception Island, Antarctica

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