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Research Article| March 01, 2006 Holocene tsunamis in the southwestern Bering Sea, Russian Far East, and their tectonic implications Joanne Bourgeois; Joanne Bourgeois 1Department of Earth and Space Sciences 351310, University of Washington, Seattle, Washington 98195-1310, USA Search for other works by this author on: GSW Google Scholar Tatiana K. Pinegina; Tatiana K. Pinegina 2Institute of Volcanology and Seismology, Piip Boulevard 9, Petropavlovsk-Kamchatsky, 683006, Russia Search for other works by this author on: GSW Google Scholar Vera Ponomareva; Vera Ponomareva 2Institute of Volcanology and Seismology, Piip Boulevard 9, Petropavlovsk-Kamchatsky, 683006, Russia Search for other works by this author on: GSW Google Scholar Natalia Zaretskaia Natalia Zaretskaia 3Geological Institute, Pyzhevsky per., 7, Moscow, 119017, Russia Search for other works by this author on: GSW Google Scholar Author and Article Information Joanne Bourgeois 1Department of Earth and Space Sciences 351310, University of Washington, Seattle, Washington 98195-1310, USA Tatiana K. Pinegina 2Institute of Volcanology and Seismology, Piip Boulevard 9, Petropavlovsk-Kamchatsky, 683006, Russia Vera Ponomareva 2Institute of Volcanology and Seismology, Piip Boulevard 9, Petropavlovsk-Kamchatsky, 683006, Russia Natalia Zaretskaia 3Geological Institute, Pyzhevsky per., 7, Moscow, 119017, Russia Publisher: Geological Society of America Received: 21 Sep 2004 Revision Received: 28 Jul 2005 Accepted: 16 Aug 2005 First Online: 08 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (2006) 118 (3-4): 449–463. https://doi.org/10.1130/B25726.1 Article history Received: 21 Sep 2004 Revision Received: 28 Jul 2005 Accepted: 16 Aug 2005 First Online: 08 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Joanne Bourgeois, Tatiana K. Pinegina, Vera Ponomareva, Natalia Zaretskaia; Holocene tsunamis in the southwestern Bering Sea, Russian Far East, and their tectonic implications. GSA Bulletin 2006;; 118 (3-4): 449–463. doi: https://doi.org/10.1130/B25726.1 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 SocietyGSA Bulletin Search Advanced Search Abstract The Bering Sea coast of Kamchatka overlies a boundary between the proposed Okhotsk and Bering blocks, or (micro)plates, of the North American plate in the Russian Far East. A history of tsunamis along this coast for the past 4000 yr indicates that the zone north of the Kuril-Kamchatka subduction zone produces tsunamigenic earthquakes every few centuries. Such a record is consistent with convergence of the proposed Okhotsk and Bering blocks along the Bering Sea coast of Kamchatka. A tsunami deposit from the 1969 Mw 7.7 Ozernoi earthquake helps us interpret older tsunami deposits. Newly studied tephra layers from Shiveluch volcano as well as previously established marker tephra layers in northern Kamchatka provide age control for historic and prehistoric tsunami deposits. Based on >50 measured sections along 14 shoreline profiles, tsunami-deposit frequencies in the southwestern Bering Sea are about five per thousand years for tsunamis generated north of the Kuril-Kamchatka trench. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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