Evidence of an active volcanic heat source beneath the Pine Island Glacier

The West Antarctic Ice Sheet sits atop an extensional rift system with volcano-like features, yet we do not know if any of these volcanoes are active, because identifying subglacial volcanism remains a challenge. Here, the authors find evidence in helium isotopes that a large volcanic heat source is...

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Autores principales:	Brice Loose, Alberto C. Naveira Garabato, Peter Schlosser, William J. Jenkins, David Vaughan, Karen J. Heywood
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/ac5f35edc4084065a2ea8d1450bdbf4d
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spelling	oai:doaj.org-article:ac5f35edc4084065a2ea8d1450bdbf4d2021-12-02T16:49:34ZEvidence of an active volcanic heat source beneath the Pine Island Glacier10.1038/s41467-018-04421-32041-1723https://doaj.org/article/ac5f35edc4084065a2ea8d1450bdbf4d2018-06-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-04421-3https://doaj.org/toc/2041-1723The West Antarctic Ice Sheet sits atop an extensional rift system with volcano-like features, yet we do not know if any of these volcanoes are active, because identifying subglacial volcanism remains a challenge. Here, the authors find evidence in helium isotopes that a large volcanic heat source is emanating from beneath the fast-melting Pine Island Ice Glacier.Brice LooseAlberto C. Naveira GarabatoPeter SchlosserWilliam J. JenkinsDavid VaughanKaren J. HeywoodNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-9 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Brice Loose Alberto C. Naveira Garabato Peter Schlosser William J. Jenkins David Vaughan Karen J. Heywood Evidence of an active volcanic heat source beneath the Pine Island Glacier
description	The West Antarctic Ice Sheet sits atop an extensional rift system with volcano-like features, yet we do not know if any of these volcanoes are active, because identifying subglacial volcanism remains a challenge. Here, the authors find evidence in helium isotopes that a large volcanic heat source is emanating from beneath the fast-melting Pine Island Ice Glacier.
format	article
author	Brice Loose Alberto C. Naveira Garabato Peter Schlosser William J. Jenkins David Vaughan Karen J. Heywood
author_facet	Brice Loose Alberto C. Naveira Garabato Peter Schlosser William J. Jenkins David Vaughan Karen J. Heywood
author_sort	Brice Loose
title	Evidence of an active volcanic heat source beneath the Pine Island Glacier
title_short	Evidence of an active volcanic heat source beneath the Pine Island Glacier
title_full	Evidence of an active volcanic heat source beneath the Pine Island Glacier
title_fullStr	Evidence of an active volcanic heat source beneath the Pine Island Glacier
title_full_unstemmed	Evidence of an active volcanic heat source beneath the Pine Island Glacier
title_sort	evidence of an active volcanic heat source beneath the pine island glacier
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/ac5f35edc4084065a2ea8d1450bdbf4d
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Evidence of an active volcanic heat source beneath the Pine Island Glacier

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