Discovery of the Largest Historic Silicic Submarine Eruption

It was likely twice the size of the renowned Mount St. Helens eruption of 1980 and perhaps more than 10 times bigger than the more recent 2010 Eyjafjallajökull eruption in Iceland. However, unlike those two events, which dominated world news headlines, in 2012 the daylong submarine silicic eruption...

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Published in:Eos, Transactions American Geophysical Union
Main Authors: Carey, Rebecca J., Wysoczanski, Richard, Wunderman, Richard, Jutzeler, Martin
Format: Article in Journal/Newspaper
Language:unknown
Published: 2014
Subjects:
Online Access:http://hdl.handle.net/10088/25645
https://doi.org/10.1002/2014EO190001
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spelling ftsmithonian:oai:repository.si.edu:10088/25645 2023-05-15T16:09:28+02:00 Discovery of the Largest Historic Silicic Submarine Eruption Carey, Rebecca J. Wysoczanski, Richard Wunderman, Richard Jutzeler, Martin 2014 http://hdl.handle.net/10088/25645 https://doi.org/10.1002/2014EO190001 unknown EOS, Transactions American Geophysical Union Carey, Rebecca J., Wysoczanski, Richard, Wunderman, Richard, and Jutzeler, Martin. 2014. "Discovery of the Largest Historic Silicic Submarine Eruption." EOS, Transactions American Geophysical Union . 95 (19):157–159. https://doi.org/10.1002/2014EO190001 2324-9250 http://hdl.handle.net/10088/25645 121052 doi:10.1002/2014EO190001 Journal Article 2014 ftsmithonian https://doi.org/10.1002/2014EO190001 2020-09-09T18:34:42Z It was likely twice the size of the renowned Mount St. Helens eruption of 1980 and perhaps more than 10 times bigger than the more recent 2010 Eyjafjallajökull eruption in Iceland. However, unlike those two events, which dominated world news headlines, in 2012 the daylong submarine silicic eruption at Havre volcano in the Kermadec Arc, New Zealand (Figure 1a; ~800 kilometers north of Auckland, New Zealand), passed without fanfare. In fact, for a while no one even knew it had occurred. NH-Mineral Sciences NMNH Peer-reviewed Article in Journal/Newspaper Eyjafjallajökull Iceland Unknown Havre ENVELOPE(-71.417,-71.417,-69.333,-69.333) New Zealand Eos, Transactions American Geophysical Union 95 19 157 159
institution Open Polar
collection Unknown
op_collection_id ftsmithonian
language unknown
description It was likely twice the size of the renowned Mount St. Helens eruption of 1980 and perhaps more than 10 times bigger than the more recent 2010 Eyjafjallajökull eruption in Iceland. However, unlike those two events, which dominated world news headlines, in 2012 the daylong submarine silicic eruption at Havre volcano in the Kermadec Arc, New Zealand (Figure 1a; ~800 kilometers north of Auckland, New Zealand), passed without fanfare. In fact, for a while no one even knew it had occurred. NH-Mineral Sciences NMNH Peer-reviewed
format Article in Journal/Newspaper
author Carey, Rebecca J.
Wysoczanski, Richard
Wunderman, Richard
Jutzeler, Martin
spellingShingle Carey, Rebecca J.
Wysoczanski, Richard
Wunderman, Richard
Jutzeler, Martin
Discovery of the Largest Historic Silicic Submarine Eruption
author_facet Carey, Rebecca J.
Wysoczanski, Richard
Wunderman, Richard
Jutzeler, Martin
author_sort Carey, Rebecca J.
title Discovery of the Largest Historic Silicic Submarine Eruption
title_short Discovery of the Largest Historic Silicic Submarine Eruption
title_full Discovery of the Largest Historic Silicic Submarine Eruption
title_fullStr Discovery of the Largest Historic Silicic Submarine Eruption
title_full_unstemmed Discovery of the Largest Historic Silicic Submarine Eruption
title_sort discovery of the largest historic silicic submarine eruption
publishDate 2014
url http://hdl.handle.net/10088/25645
https://doi.org/10.1002/2014EO190001
long_lat ENVELOPE(-71.417,-71.417,-69.333,-69.333)
geographic Havre
New Zealand
geographic_facet Havre
New Zealand
genre Eyjafjallajökull
Iceland
genre_facet Eyjafjallajökull
Iceland
op_relation EOS, Transactions American Geophysical Union
Carey, Rebecca J., Wysoczanski, Richard, Wunderman, Richard, and Jutzeler, Martin. 2014. "Discovery of the Largest Historic Silicic Submarine Eruption." EOS, Transactions American Geophysical Union . 95 (19):157–159. https://doi.org/10.1002/2014EO190001
2324-9250
http://hdl.handle.net/10088/25645
121052
doi:10.1002/2014EO190001
op_doi https://doi.org/10.1002/2014EO190001
container_title Eos, Transactions American Geophysical Union
container_volume 95
container_issue 19
container_start_page 157
op_container_end_page 159
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