Active volcanoes in Marie Byrd Land

Two volcanoes in Marie Byrd Land, Mounts Berlin and Takahe, can be considered active, and a third, Mount Waesche, may be as well, although the chronology of activity is less well constrained. The records of explosive activity of these three volcanoes is well represented through deposits on the volca...

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Main Authors: N.W. Dunbar, N.A. Iverson, J.L. Smellie, W.C. McIntosh, M.J. Zimmerer, P.R. Kyle
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of London 2021
Subjects:
Online Access:https://dx.doi.org/10.6084/m9.figshare.c.5226158
https://geolsoc.figshare.com/collections/Active_volcanoes_in_Marie_Byrd_Land/5226158
id ftdatacite:10.6084/m9.figshare.c.5226158
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spelling ftdatacite:10.6084/m9.figshare.c.5226158 2023-05-15T13:44:57+02:00 Active volcanoes in Marie Byrd Land N.W. Dunbar N.A. Iverson J.L. Smellie W.C. McIntosh M.J. Zimmerer P.R. Kyle 2021 https://dx.doi.org/10.6084/m9.figshare.c.5226158 https://geolsoc.figshare.com/collections/Active_volcanoes_in_Marie_Byrd_Land/5226158 unknown Geological Society of London https://dx.doi.org/10.1144/m55-2019-29 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Geology FOS Earth and related environmental sciences Collection article 2021 ftdatacite https://doi.org/10.6084/m9.figshare.c.5226158 https://doi.org/10.1144/m55-2019-29 2021-11-05T12:55:41Z Two volcanoes in Marie Byrd Land, Mounts Berlin and Takahe, can be considered active, and a third, Mount Waesche, may be as well, although the chronology of activity is less well constrained. The records of explosive activity of these three volcanoes is well represented through deposits on the volcano flanks, tephra layers found in blue ice areas, as well as by the presence of cryptotephra layers found in West and East Antarctic ice cores. Records of effusive volcanism are found on the volcano flanks, but some deposits may be obscured by pervasive glacerization of the edifices. Based on a compilation of tephra depths/ages in ice cores, the activity patterns of Mounts Takahe and Berlin are dramatically different. Mount Takahe has erupted infrequently over the past 100 ka. Mount Berlin, by contrast, has erupted episodically during this time interval, with the number of eruptions being dramatically higher in the time interval between around 32 to 18 ka. Integration of the Mount Berlin tephra record from ice cores and blue ice areas over a 500 ka time span reveals a pattern of geochemical evolution related to small batches of partial melt being progressively removed from a single source underlying Mount Berlin. Article in Journal/Newspaper Antarc* Antarctic Marie Byrd Land DataCite Metadata Store (German National Library of Science and Technology) Antarctic Byrd Marie Byrd Land ENVELOPE(-130.000,-130.000,-78.000,-78.000) Takahe ENVELOPE(-112.233,-112.233,-76.267,-76.267) Mount Takahe ENVELOPE(166.800,166.800,-77.217,-77.217) Mount Berlin ENVELOPE(-135.867,-135.867,-76.050,-76.050) Mount Waesche ENVELOPE(-126.900,-126.900,-77.167,-77.167)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Geology
FOS Earth and related environmental sciences
spellingShingle Geology
FOS Earth and related environmental sciences
N.W. Dunbar
N.A. Iverson
J.L. Smellie
W.C. McIntosh
M.J. Zimmerer
P.R. Kyle
Active volcanoes in Marie Byrd Land
topic_facet Geology
FOS Earth and related environmental sciences
description Two volcanoes in Marie Byrd Land, Mounts Berlin and Takahe, can be considered active, and a third, Mount Waesche, may be as well, although the chronology of activity is less well constrained. The records of explosive activity of these three volcanoes is well represented through deposits on the volcano flanks, tephra layers found in blue ice areas, as well as by the presence of cryptotephra layers found in West and East Antarctic ice cores. Records of effusive volcanism are found on the volcano flanks, but some deposits may be obscured by pervasive glacerization of the edifices. Based on a compilation of tephra depths/ages in ice cores, the activity patterns of Mounts Takahe and Berlin are dramatically different. Mount Takahe has erupted infrequently over the past 100 ka. Mount Berlin, by contrast, has erupted episodically during this time interval, with the number of eruptions being dramatically higher in the time interval between around 32 to 18 ka. Integration of the Mount Berlin tephra record from ice cores and blue ice areas over a 500 ka time span reveals a pattern of geochemical evolution related to small batches of partial melt being progressively removed from a single source underlying Mount Berlin.
format Article in Journal/Newspaper
author N.W. Dunbar
N.A. Iverson
J.L. Smellie
W.C. McIntosh
M.J. Zimmerer
P.R. Kyle
author_facet N.W. Dunbar
N.A. Iverson
J.L. Smellie
W.C. McIntosh
M.J. Zimmerer
P.R. Kyle
author_sort N.W. Dunbar
title Active volcanoes in Marie Byrd Land
title_short Active volcanoes in Marie Byrd Land
title_full Active volcanoes in Marie Byrd Land
title_fullStr Active volcanoes in Marie Byrd Land
title_full_unstemmed Active volcanoes in Marie Byrd Land
title_sort active volcanoes in marie byrd land
publisher Geological Society of London
publishDate 2021
url https://dx.doi.org/10.6084/m9.figshare.c.5226158
https://geolsoc.figshare.com/collections/Active_volcanoes_in_Marie_Byrd_Land/5226158
long_lat ENVELOPE(-130.000,-130.000,-78.000,-78.000)
ENVELOPE(-112.233,-112.233,-76.267,-76.267)
ENVELOPE(166.800,166.800,-77.217,-77.217)
ENVELOPE(-135.867,-135.867,-76.050,-76.050)
ENVELOPE(-126.900,-126.900,-77.167,-77.167)
geographic Antarctic
Byrd
Marie Byrd Land
Takahe
Mount Takahe
Mount Berlin
Mount Waesche
geographic_facet Antarctic
Byrd
Marie Byrd Land
Takahe
Mount Takahe
Mount Berlin
Mount Waesche
genre Antarc*
Antarctic
Marie Byrd Land
genre_facet Antarc*
Antarctic
Marie Byrd Land
op_relation https://dx.doi.org/10.1144/m55-2019-29
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.6084/m9.figshare.c.5226158
https://doi.org/10.1144/m55-2019-29
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