Mantle updrafts and mechanisms of oceanic volcanism

Lord Kelvin’s name is associated with the laws of thermodynamics and the cooling Earth hypothesis. The widely accepted mantle plume conjecture has been justified by experiments and calculations that violate the laws of thermodynamics for an isolated cooling planet. Hotspots such as Hawaii, Samoa, Ic...

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Published in:Proceedings of the National Academy of Sciences
Main Authors: Anderson, Don L., Natland, James H.
Format: Text
Language:English
Published: National Academy of Sciences 2014
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4205608
http://www.ncbi.nlm.nih.gov/pubmed/25201992
https://doi.org/10.1073/pnas.1410229111
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spelling ftpubmed:oai:pubmedcentral.nih.gov:4205608 2023-05-15T16:48:51+02:00 Mantle updrafts and mechanisms of oceanic volcanism Anderson, Don L. Natland, James H. 2014-10-14 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4205608 http://www.ncbi.nlm.nih.gov/pubmed/25201992 https://doi.org/10.1073/pnas.1410229111 en eng National Academy of Sciences http://www.ncbi.nlm.nih.gov/pmc/articles/PMC http://www.ncbi.nlm.nih.gov/pubmed/25201992 http://dx.doi.org/10.1073/pnas.1410229111 Freely available online through the PNAS open access option. PNAS Plus Text 2014 ftpubmed https://doi.org/10.1073/pnas.1410229111 2014-11-09T01:09:51Z Lord Kelvin’s name is associated with the laws of thermodynamics and the cooling Earth hypothesis. The widely accepted mantle plume conjecture has been justified by experiments and calculations that violate the laws of thermodynamics for an isolated cooling planet. Hotspots such as Hawaii, Samoa, Iceland, and Yellowstone are due to a thermal bump in the shallow mantle, a consequence of the cooling of the Earth. They are not due to ∼100- to 200-km-wide tubes extending upward from fixed points near the Earth’s core. Seismic imaging shows that features associated with hotspots are thousands of kilometers across, and inferred ascent rates are low. Plate tectonic-induced updrafts and a cooling planet explain hotspots and the volcanoes at oceanic ridges. Text Iceland PubMed Central (PMC) Proceedings of the National Academy of Sciences 111 41 E4298 E4304
institution Open Polar
collection PubMed Central (PMC)
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language English
topic PNAS Plus
spellingShingle PNAS Plus
Anderson, Don L.
Natland, James H.
Mantle updrafts and mechanisms of oceanic volcanism
topic_facet PNAS Plus
description Lord Kelvin’s name is associated with the laws of thermodynamics and the cooling Earth hypothesis. The widely accepted mantle plume conjecture has been justified by experiments and calculations that violate the laws of thermodynamics for an isolated cooling planet. Hotspots such as Hawaii, Samoa, Iceland, and Yellowstone are due to a thermal bump in the shallow mantle, a consequence of the cooling of the Earth. They are not due to ∼100- to 200-km-wide tubes extending upward from fixed points near the Earth’s core. Seismic imaging shows that features associated with hotspots are thousands of kilometers across, and inferred ascent rates are low. Plate tectonic-induced updrafts and a cooling planet explain hotspots and the volcanoes at oceanic ridges.
format Text
author Anderson, Don L.
Natland, James H.
author_facet Anderson, Don L.
Natland, James H.
author_sort Anderson, Don L.
title Mantle updrafts and mechanisms of oceanic volcanism
title_short Mantle updrafts and mechanisms of oceanic volcanism
title_full Mantle updrafts and mechanisms of oceanic volcanism
title_fullStr Mantle updrafts and mechanisms of oceanic volcanism
title_full_unstemmed Mantle updrafts and mechanisms of oceanic volcanism
title_sort mantle updrafts and mechanisms of oceanic volcanism
publisher National Academy of Sciences
publishDate 2014
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4205608
http://www.ncbi.nlm.nih.gov/pubmed/25201992
https://doi.org/10.1073/pnas.1410229111
genre Iceland
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op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC
http://www.ncbi.nlm.nih.gov/pubmed/25201992
http://dx.doi.org/10.1073/pnas.1410229111
op_rights Freely available online through the PNAS open access option.
op_doi https://doi.org/10.1073/pnas.1410229111
container_title Proceedings of the National Academy of Sciences
container_volume 111
container_issue 41
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