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• W2056588806 abstract "Research Article| August 01, 2014 Anatomy of an active submarine volcano A.F. Arnulf; A.F. Arnulf 1Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California–San Diego, La Jolla, California 92093, USA Search for other works by this author on: GSW Google Scholar A.J. Harding; A.J. Harding 1Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California–San Diego, La Jolla, California 92093, USA Search for other works by this author on: GSW Google Scholar G.M. Kent; G.M. Kent 2Nevada Seismological Laboratory, 0174, University of Nevada–Reno, Reno, Nevada 89557, USA Search for other works by this author on: GSW Google Scholar S.M. Carbotte; S.M. Carbotte 3Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA Search for other works by this author on: GSW Google Scholar J.P. Canales; J.P. Canales 4Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02540, USA Search for other works by this author on: GSW Google Scholar M.R. Nedimović M.R. Nedimović 3Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA5Department of Earth Sciences, Dalhousie University, Halifax, Nova Scotia B3H4J1, Canada Search for other works by this author on: GSW Google Scholar Author and Article Information A.F. Arnulf 1Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California–San Diego, La Jolla, California 92093, USA A.J. Harding 1Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California–San Diego, La Jolla, California 92093, USA G.M. Kent 2Nevada Seismological Laboratory, 0174, University of Nevada–Reno, Reno, Nevada 89557, USA S.M. Carbotte 3Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA J.P. Canales 4Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02540, USA M.R. Nedimović 3Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA5Department of Earth Sciences, Dalhousie University, Halifax, Nova Scotia B3H4J1, Canada Publisher: Geological Society of America Received: 28 Feb 2014 Revision Received: 12 May 2014 Accepted: 13 May 2014 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2014 Geological Society of America Geology (2014) 42 (8): 655–658. https://doi.org/10.1130/G35629.1 Article history Received: 28 Feb 2014 Revision Received: 12 May 2014 Accepted: 13 May 2014 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation A.F. Arnulf, A.J. Harding, G.M. Kent, S.M. Carbotte, J.P. Canales, M.R. Nedimović; Anatomy of an active submarine volcano. Geology 2014;; 42 (8): 655–658. doi: https://doi.org/10.1130/G35629.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Most of the magma erupted at mid-ocean ridges is stored in a mid-crustal melt lens that lies at the boundary between sheeted dikes and gabbros. Nevertheless, images of the magma pathways linking this melt lens to the overlying eruption site have remained elusive. Here, we have used seismic methods to image the thickest magma reservoir observed beneath any spreading center to date, which is principally attributed to the juxtaposition of the Juan de Fuca Ridge with the Cobb hotspot (northwestern USA). Our results reveal a complex melt body, which is ∼14 km long, 3 km wide, and up to 1 km thick, beneath the summit caldera. The estimated volume of the reservoir is 18–30 km3, more than two orders of magnitude greater than the erupted magma volumes of either the A.D. 1998 or 2011 eruption. Our images show a network of sub-horizontal to shallow-dipping (<30°) features that we interpret as pathways facilitating melt transport from the magma reservoir to the eruption sites. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2056588806 title "Anatomy of an active submarine volcano" @default.
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