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The largest deep-ocean silicic volcanic eruption of the past century.
Carey, Rebecca; Soule, S Adam; Manga, Michael; White, James; McPhie, Jocelyn; Wysoczanski, Richard; Jutzeler, Martin; Tani, Kenichiro; Yoerger, Dana; Fornari, Daniel; Caratori-Tontini, Fabio; Houghton, Bruce; Mitchell, Samuel; Ikegami, Fumihiko; Conway, Chris; Murch, Arran; Fauria, Kristen; Jones, Max; Cahalan, Ryan; McKenzie, Warren.
Affiliation
  • Carey R; CODES and School of Physical Sciences, University of Tasmania, Hobart, Tasmania 7001, Australia.
  • Soule SA; Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.
  • Manga M; Department of Earth and Planetary Science, University of California, Berkeley, 307 McCone Hall, Berkeley, CA 94720-4767, USA.
  • White J; Geology Department, University of Otago, Dunedin 9054, New Zealand.
  • McPhie J; CODES and School of Physical Sciences, University of Tasmania, Hobart, Tasmania 7001, Australia.
  • Wysoczanski R; National Institute of Water and Atmospheric Research, Auckland, New Zealand.
  • Jutzeler M; CODES and School of Physical Sciences, University of Tasmania, Hobart, Tasmania 7001, Australia.
  • Tani K; Department of Geology and Paleontology, National Museum of Nature and Science, 4-1-1 Amakubo, Tsukuba-shi, Ibaraki 305-0005, Japan.
  • Yoerger D; Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.
  • Fornari D; Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.
  • Caratori-Tontini F; GNS Science, P.O. Box 30368, Lower Hutt 5010, New Zealand.
  • Houghton B; Geology and Geophysics, University of Hawaii at Manoa, 1680 East-West Road, Honolulu, HI 96825, USA.
  • Mitchell S; Geology and Geophysics, University of Hawaii at Manoa, 1680 East-West Road, Honolulu, HI 96825, USA.
  • Ikegami F; CODES and School of Physical Sciences, University of Tasmania, Hobart, Tasmania 7001, Australia.
  • Conway C; Department of Geology and Paleontology, National Museum of Nature and Science, 4-1-1 Amakubo, Tsukuba-shi, Ibaraki 305-0005, Japan.
  • Murch A; Geology Department, University of Otago, Dunedin 9054, New Zealand.
  • Fauria K; Department of Earth and Planetary Science, University of California, Berkeley, 307 McCone Hall, Berkeley, CA 94720-4767, USA.
  • Jones M; Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.
  • Cahalan R; Massachusetts Institute of Technology/Woods Hole Oceanographic Institution Joint Program in Oceanography/Applied Ocean Science and Engineering, Woods Hole, MA 02543, USA.
  • McKenzie W; School of Earth and Atmospheric Sciences, Georgia Institute of Technology, 311 Ferst Drive, Atlanta, GA 30332, USA.
Sci Adv ; 4(1): e1701121, 2018 01.
Article in En | MEDLINE | ID: mdl-29326974
ABSTRACT
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-km2 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.