The largest deep-ocean silicic volcanic eruption of the past century
Author(s) -
Rebecca Carey,
S. A. Soule,
Michael Manga,
James D. L. White,
Jocelyn McPhie,
Richard Wysoczański,
Martin Jutzeler,
Kenichiro Tani,
D. Yoerger,
Daniel J. Fornari,
Fabio Caratori Tontini,
B. F. Houghton,
S. J. Mitchell,
Fumihiko Ikegami,
Chris E. Conway,
Arran Murch,
Kristen E. Fauria,
Max P. Jones,
Ryan Cahalan,
Warren McKenzie
Publication year - 2018
Publication title -
science advances
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 5.928
H-Index - 146
ISSN - 2375-2548
DOI - 10.1126/sciadv.1701121
Subject(s) - geology , pumice , submarine volcano , effusive eruption , dense rock equivalent , volcano , lava , silicic , vulcanian eruption , magma , peléan eruption , seafloor spreading , explosive eruption , submarine , lateral eruption , volcanology , geochemistry , paleontology , oceanography
The 2012 submarine eruption of Havre volcano in the Kermadec arc, New Zealand, is the largest deep-ocean eruption in history and one of very few recorded submarine eruptions involving rhyolite magma. It was recognized from a gigantic 400-km pumice raft seen in satellite imagery, but the complexity of this event was concealed beneath the sea surface. Mapping, observations, and sampling by submersibles have provided an exceptionally high fidelity record of the seafloor products, which included lava sourced from 14 vents at water depths of 900 to 1220 m, and fragmental deposits including giant pumice clasts up to 9 m in diameter. Most (>75%) of the total erupted volume was partitioned into the pumice raft and transported far from the volcano. The geological record on submarine volcanic edifices in volcanic arcs does not faithfully archive eruption size or magma production.
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