Formation of Stanley Patch volcanic cone: New insights into the evolution of Deception Island caldera (Antarctica)

Deception Island (South Shetland Islands) is one of the most active volcanoes in Antarctica, with more than 20 explosive eruptive events registered over the past centuries. Recent eruptions (1967, 1969, and 1970) and volcanic unrest episodes (1992, 1999, and 2014–2015) demonstrate that volcanic activity is likely occurring in the future. This is of special concern for scientists, logistic personnel, and tourists, since the South Shetland Islands are an important tourist destination and host numerous year-round and seasonal scientific stations and base camps. Significant efforts have been made to understand the complex magmatic and volcanic evolution of Deception Island with special interest on its subaerial part. However, studies on submerged volcanic cones within Port Foster, the sea-flooded part of Deception Island's caldera depression, are comparatively scarce. Here, we provide a full characterization of Stanley Patch volcano, the largest of these volcanic edifices. Estimated morphometric parameters based on new multibeam bathymetric data, supported by petrographic and chemical observations from rock samples collected on the crater rim, reveal that Stanley Patch volcano grew in a subaerial environment. This result, combined with previous findings and new sedimentological evidence from our ultra-high resolution seismic profiles, allow to further detail the island's geologic evolution since the caldera collapse. We conclude that the complete flooding of Port Foster could have only occurred after the formation of Stanley Patch volcano, i.e. during the last ~2000 years, and in a time period of a few days or less.

Saved in:
Bibliographic Details
Main Authors: Hopfenblatt, Joaquin, Geyer, Adelina, Aulinas, M., Álvarez-Valero, A. M., Gisbert, G., Kereszturi, G., Ercilla, Gemma, Gomez-Ballesteros, María, Márquez, Alvaro, García-Castellanos, Daniel, Pedrazzi, Dario, Sumino, H., Hoskuldsson, Armann, Giralt, Santiago, Angulo-Preckler, Carlos
Other Authors: Ministerio de Economía y Competitividad (España)
Format: artículo biblioteca
Language:English
Published: Elsevier 2021-04
Subjects:Seismic profiles, Caldera evolution, Caldera flooding, Antarctic volcanism, South Shetland Islands, Deception Island,
Online Access:http://hdl.handle.net/10261/240383
http://dx.doi.org/10.13039/501100003329
http://dx.doi.org/10.13039/501100011033
Tags: Add Tag
No Tags, Be the first to tag this record!
id dig-icm-es-10261-240383
record_format koha
institution ICM ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-icm-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del ICM España
language English
topic Seismic profiles
Caldera evolution
Caldera flooding
Antarctic volcanism
South Shetland Islands
Deception Island
Seismic profiles
Caldera evolution
Caldera flooding
Antarctic volcanism
South Shetland Islands
Deception Island
spellingShingle Seismic profiles
Caldera evolution
Caldera flooding
Antarctic volcanism
South Shetland Islands
Deception Island
Seismic profiles
Caldera evolution
Caldera flooding
Antarctic volcanism
South Shetland Islands
Deception Island
Hopfenblatt, Joaquin
Geyer, Adelina
Aulinas, M.
Álvarez-Valero, A. M.
Gisbert, G.
Kereszturi, G.
Ercilla, Gemma
Gomez-Ballesteros, María
Márquez, Alvaro
García-Castellanos, Daniel
Pedrazzi, Dario
Sumino, H.
Hoskuldsson, Armann
Giralt, Santiago
Angulo-Preckler, Carlos
Formation of Stanley Patch volcanic cone: New insights into the evolution of Deception Island caldera (Antarctica)
description Deception Island (South Shetland Islands) is one of the most active volcanoes in Antarctica, with more than 20 explosive eruptive events registered over the past centuries. Recent eruptions (1967, 1969, and 1970) and volcanic unrest episodes (1992, 1999, and 2014–2015) demonstrate that volcanic activity is likely occurring in the future. This is of special concern for scientists, logistic personnel, and tourists, since the South Shetland Islands are an important tourist destination and host numerous year-round and seasonal scientific stations and base camps. Significant efforts have been made to understand the complex magmatic and volcanic evolution of Deception Island with special interest on its subaerial part. However, studies on submerged volcanic cones within Port Foster, the sea-flooded part of Deception Island's caldera depression, are comparatively scarce. Here, we provide a full characterization of Stanley Patch volcano, the largest of these volcanic edifices. Estimated morphometric parameters based on new multibeam bathymetric data, supported by petrographic and chemical observations from rock samples collected on the crater rim, reveal that Stanley Patch volcano grew in a subaerial environment. This result, combined with previous findings and new sedimentological evidence from our ultra-high resolution seismic profiles, allow to further detail the island's geologic evolution since the caldera collapse. We conclude that the complete flooding of Port Foster could have only occurred after the formation of Stanley Patch volcano, i.e. during the last ~2000 years, and in a time period of a few days or less.
author2 Ministerio de Economía y Competitividad (España)
author_facet Ministerio de Economía y Competitividad (España)
Hopfenblatt, Joaquin
Geyer, Adelina
Aulinas, M.
Álvarez-Valero, A. M.
Gisbert, G.
Kereszturi, G.
Ercilla, Gemma
Gomez-Ballesteros, María
Márquez, Alvaro
García-Castellanos, Daniel
Pedrazzi, Dario
Sumino, H.
Hoskuldsson, Armann
Giralt, Santiago
Angulo-Preckler, Carlos
format artículo
topic_facet Seismic profiles
Caldera evolution
Caldera flooding
Antarctic volcanism
South Shetland Islands
Deception Island
author Hopfenblatt, Joaquin
Geyer, Adelina
Aulinas, M.
Álvarez-Valero, A. M.
Gisbert, G.
Kereszturi, G.
Ercilla, Gemma
Gomez-Ballesteros, María
Márquez, Alvaro
García-Castellanos, Daniel
Pedrazzi, Dario
Sumino, H.
Hoskuldsson, Armann
Giralt, Santiago
Angulo-Preckler, Carlos
author_sort Hopfenblatt, Joaquin
title Formation of Stanley Patch volcanic cone: New insights into the evolution of Deception Island caldera (Antarctica)
title_short Formation of Stanley Patch volcanic cone: New insights into the evolution of Deception Island caldera (Antarctica)
title_full Formation of Stanley Patch volcanic cone: New insights into the evolution of Deception Island caldera (Antarctica)
title_fullStr Formation of Stanley Patch volcanic cone: New insights into the evolution of Deception Island caldera (Antarctica)
title_full_unstemmed Formation of Stanley Patch volcanic cone: New insights into the evolution of Deception Island caldera (Antarctica)
title_sort formation of stanley patch volcanic cone: new insights into the evolution of deception island caldera (antarctica)
publisher Elsevier
publishDate 2021-04
url http://hdl.handle.net/10261/240383
http://dx.doi.org/10.13039/501100003329
http://dx.doi.org/10.13039/501100011033
work_keys_str_mv AT hopfenblattjoaquin formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
AT geyeradelina formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
AT aulinasm formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
AT alvarezvaleroam formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
AT gisbertg formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
AT kereszturig formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
AT ercillagemma formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
AT gomezballesterosmaria formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
AT marquezalvaro formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
AT garciacastellanosdaniel formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
AT pedrazzidario formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
AT suminoh formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
AT hoskuldssonarmann formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
AT giraltsantiago formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
AT anguloprecklercarlos formationofstanleypatchvolcanicconenewinsightsintotheevolutionofdeceptionislandcalderaantarctica
_version_ 1777667439458254848
spelling dig-icm-es-10261-2403832021-10-20T09:51:49Z Formation of Stanley Patch volcanic cone: New insights into the evolution of Deception Island caldera (Antarctica) Hopfenblatt, Joaquin Geyer, Adelina Aulinas, M. Álvarez-Valero, A. M. Gisbert, G. Kereszturi, G. Ercilla, Gemma Gomez-Ballesteros, María Márquez, Alvaro García-Castellanos, Daniel Pedrazzi, Dario Sumino, H. Hoskuldsson, Armann Giralt, Santiago Angulo-Preckler, Carlos Ministerio de Economía y Competitividad (España) Agencia Estatal de Investigación (España) Geyer, Adelina [0000-0002-8803-6504] Giralt, Santiago [0000-0001-8570-7838] Hopfenblatt, Joaquin [0000-0003-4235-8302] García-Castellanos, Daniel [0000-0001-8454-8572] Pedrazzi, Dario [0000-0002-6869-1325] Seismic profiles Caldera evolution Caldera flooding Antarctic volcanism South Shetland Islands Deception Island Deception Island (South Shetland Islands) is one of the most active volcanoes in Antarctica, with more than 20 explosive eruptive events registered over the past centuries. Recent eruptions (1967, 1969, and 1970) and volcanic unrest episodes (1992, 1999, and 2014–2015) demonstrate that volcanic activity is likely occurring in the future. This is of special concern for scientists, logistic personnel, and tourists, since the South Shetland Islands are an important tourist destination and host numerous year-round and seasonal scientific stations and base camps. Significant efforts have been made to understand the complex magmatic and volcanic evolution of Deception Island with special interest on its subaerial part. However, studies on submerged volcanic cones within Port Foster, the sea-flooded part of Deception Island's caldera depression, are comparatively scarce. Here, we provide a full characterization of Stanley Patch volcano, the largest of these volcanic edifices. Estimated morphometric parameters based on new multibeam bathymetric data, supported by petrographic and chemical observations from rock samples collected on the crater rim, reveal that Stanley Patch volcano grew in a subaerial environment. This result, combined with previous findings and new sedimentological evidence from our ultra-high resolution seismic profiles, allow to further detail the island's geologic evolution since the caldera collapse. We conclude that the complete flooding of Port Foster could have only occurred after the formation of Stanley Patch volcano, i.e. during the last ~2000 years, and in a time period of a few days or less. This research was supported by the Spanish Government RECALDEC (CTM2009-05919-E/ANT), PEVOLDEC (CTM2011-13578-E/ANT), POSVOLDEC (CTM2016-79617-P)(AEI/FEDER, UE), VOLGASDEC (PGC2018-095693-B-I00), USAL-2019 project (Programa Propio - mod. 1B) and the GALIEO-IHM Program. A.G. is grateful for her Ramón y Cajal contract (RYC-2012-11024), and A.M.A-V for the grant under the “JSPS invitation fellowship” program (S18113). D.P. is grateful for his Beatriu de Pinós (2016 BP 00086) and Juan de la Cierva (IJCI-2016-30482) contracts. We thank all the military staff of the Spanish Antarctic Base “Gabriel de Castilla”, BIO Hespérides oceanographic cruise and the Marine Hydrographic Institute, for their constant help and logistic support. This research is part of POLARCSIC and PTI VOLCAN activities. English editing by Grant George Buffett (www.terranova.barcelona). We thank the Editor, J.L. Macías, and both reviewers A. Di Roberto and P. Nomikou for their constructive comments that have allowed improving a previous version of this manuscript. This work acknowledges the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S) to ICM-CSIC Peer reviewed 2021-05-11T07:56:16Z 2021-05-11T07:56:16Z 2021-04 artículo http://purl.org/coar/resource_type/c_6501 Journal of Volcanology and Geothermal Research, 415: 107249 (2021) 0377-0273 CEX2019-000928-S http://hdl.handle.net/10261/240383 10.1016/j.jvolgeores.2021.107249 http://dx.doi.org/10.13039/501100003329 http://dx.doi.org/10.13039/501100011033 en #PLACEHOLDER_PARENT_METADATA_VALUE# #PLACEHOLDER_PARENT_METADATA_VALUE# #PLACEHOLDER_PARENT_METADATA_VALUE# #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CTM2009-05919-E/ANT info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CTM2016-79617-P info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CTM2011-13578-E/ANT info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/PGC2018-095693-B-I00 Publisher's version https://doi.org/10.1016/j.jvolgeores.2021.107249 Sí open Elsevier