Unexpected response of mt. wrangell volcano, alaska, to the shaking from a large regional earthquake: a puzzle for intermediate-term earthquake-volcanoes interactions

On November 3, 2002 three segments of the Denali fault in interior Alaska ruptured during a Mw 7.9 earthquake, offering a unique opportunity to study earthquake-volcano interactions. Out of the 24 volcanoes that are seismically monitored by the Alaska Volcano Observatory (AVO) only Mt. Wrangell, the...

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Autores:
Sánchez, John J.
McNutt, Stephen R.
Tipo de recurso:
Article of journal
Fecha de publicación:
2004
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/34061
Acceso en línea:
https://repositorio.unal.edu.co/handle/unal/34061
http://bdigital.unal.edu.co/24141/
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Atribución-NoComercial 4.0 Internacional
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spelling Atribución-NoComercial 4.0 InternacionalDerechos reservados - Universidad Nacional de Colombiahttp://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Sánchez, John J.e874e927-e762-4ae4-b6be-719d91212d01300McNutt, Stephen R.b1f2d83d-d039-4aeb-b717-04d01992de5d3002019-06-27T23:11:29Z2019-06-27T23:11:29Z2004https://repositorio.unal.edu.co/handle/unal/34061http://bdigital.unal.edu.co/24141/On November 3, 2002 three segments of the Denali fault in interior Alaska ruptured during a Mw 7.9 earthquake, offering a unique opportunity to study earthquake-volcano interactions. Out of the 24 volcanoes that are seismically monitored by the Alaska Volcano Observatory (AVO) only Mt. Wrangell, the closest volcano to the epicenter (247 km), showed a clear response to the shaking in the intermediate-term (weeks to months) time scale. The response was unexpected because it consisted of a decline by at least 50% in the volcano's seismicity rate (mostly low-frequency events) that lasted for five months. Because most well documented previous instances of short-term (minutes to days) responses of volcanic centers to the passing waves of distant earthquakes, have all been seismicity increases, the decline in seismicity at Mt. Wrangell poses a controversial puzzle. By using several independent methods to measure the seismicity rate at the volcano from before to after the main shock, and applying rigorous statistical testing, we conclude that the change in seismicity at the volcano was a real effect of the Denali earthquake. We suggest that a depressurization of the volcanic plumbing system took place either as a result of sudden decompression (static stress changes) or because of creation of new pathways resulting from the strong shaking (dynamic stresses). At present we cannot distinguish between these two possibilities.application/pdfspaUNIVERSIDAD NACIONAL DE COLOMBIAhttp://revistas.unal.edu.co/index.php/esrj/article/view/21259Universidad Nacional de Colombia Revistas electrónicas UN Earth Sciences Research JournalEarth Sciences Research JournalEarth Sciences Research Journal; Vol. 8, núm. 1 (2004); 34-44 Earth Sciences Research Journal; Vol. 8, núm. 1 (2004); 34-44 2339-3459 1794-6190Sánchez, John J. and McNutt, Stephen R. (2004) Unexpected response of mt. wrangell volcano, alaska, to the shaking from a large regional earthquake: a puzzle for intermediate-term earthquake-volcanoes interactions. Earth Sciences Research Journal; Vol. 8, núm. 1 (2004); 34-44 Earth Sciences Research Journal; Vol. 8, núm. 1 (2004); 34-44 2339-3459 1794-6190 .Unexpected response of mt. wrangell volcano, alaska, to the shaking from a large regional earthquake: a puzzle for intermediate-term earthquake-volcanoes interactionsArtículo de revistainfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a85Texthttp://purl.org/redcol/resource_type/ARTORIGINAL21259-72222-1-PB.pdfapplication/pdf747080https://repositorio.unal.edu.co/bitstream/unal/34061/1/21259-72222-1-PB.pdfd9d1f20f1b817aacb6a631246986a5a4MD51THUMBNAIL21259-72222-1-PB.pdf.jpg21259-72222-1-PB.pdf.jpgGenerated Thumbnailimage/jpeg7869https://repositorio.unal.edu.co/bitstream/unal/34061/2/21259-72222-1-PB.pdf.jpg0c86f0bba46edfc9d3353a436a2e15c8MD52unal/34061oai:repositorio.unal.edu.co:unal/340612023-12-24 23:05:37.962Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co
dc.title.spa.fl_str_mv Unexpected response of mt. wrangell volcano, alaska, to the shaking from a large regional earthquake: a puzzle for intermediate-term earthquake-volcanoes interactions
title Unexpected response of mt. wrangell volcano, alaska, to the shaking from a large regional earthquake: a puzzle for intermediate-term earthquake-volcanoes interactions
spellingShingle Unexpected response of mt. wrangell volcano, alaska, to the shaking from a large regional earthquake: a puzzle for intermediate-term earthquake-volcanoes interactions
title_short Unexpected response of mt. wrangell volcano, alaska, to the shaking from a large regional earthquake: a puzzle for intermediate-term earthquake-volcanoes interactions
title_full Unexpected response of mt. wrangell volcano, alaska, to the shaking from a large regional earthquake: a puzzle for intermediate-term earthquake-volcanoes interactions
title_fullStr Unexpected response of mt. wrangell volcano, alaska, to the shaking from a large regional earthquake: a puzzle for intermediate-term earthquake-volcanoes interactions
title_full_unstemmed Unexpected response of mt. wrangell volcano, alaska, to the shaking from a large regional earthquake: a puzzle for intermediate-term earthquake-volcanoes interactions
title_sort Unexpected response of mt. wrangell volcano, alaska, to the shaking from a large regional earthquake: a puzzle for intermediate-term earthquake-volcanoes interactions
dc.creator.fl_str_mv Sánchez, John J.
McNutt, Stephen R.
dc.contributor.author.spa.fl_str_mv Sánchez, John J.
McNutt, Stephen R.
description On November 3, 2002 three segments of the Denali fault in interior Alaska ruptured during a Mw 7.9 earthquake, offering a unique opportunity to study earthquake-volcano interactions. Out of the 24 volcanoes that are seismically monitored by the Alaska Volcano Observatory (AVO) only Mt. Wrangell, the closest volcano to the epicenter (247 km), showed a clear response to the shaking in the intermediate-term (weeks to months) time scale. The response was unexpected because it consisted of a decline by at least 50% in the volcano's seismicity rate (mostly low-frequency events) that lasted for five months. Because most well documented previous instances of short-term (minutes to days) responses of volcanic centers to the passing waves of distant earthquakes, have all been seismicity increases, the decline in seismicity at Mt. Wrangell poses a controversial puzzle. By using several independent methods to measure the seismicity rate at the volcano from before to after the main shock, and applying rigorous statistical testing, we conclude that the change in seismicity at the volcano was a real effect of the Denali earthquake. We suggest that a depressurization of the volcanic plumbing system took place either as a result of sudden decompression (static stress changes) or because of creation of new pathways resulting from the strong shaking (dynamic stresses). At present we cannot distinguish between these two possibilities.
publishDate 2004
dc.date.issued.spa.fl_str_mv 2004
dc.date.accessioned.spa.fl_str_mv 2019-06-27T23:11:29Z
dc.date.available.spa.fl_str_mv 2019-06-27T23:11:29Z
dc.type.spa.fl_str_mv Artículo de revista
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http://bdigital.unal.edu.co/24141/
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dc.relation.ispartof.spa.fl_str_mv Universidad Nacional de Colombia Revistas electrónicas UN Earth Sciences Research Journal
Earth Sciences Research Journal
dc.relation.ispartofseries.none.fl_str_mv Earth Sciences Research Journal; Vol. 8, núm. 1 (2004); 34-44 Earth Sciences Research Journal; Vol. 8, núm. 1 (2004); 34-44 2339-3459 1794-6190
dc.relation.references.spa.fl_str_mv Sánchez, John J. and McNutt, Stephen R. (2004) Unexpected response of mt. wrangell volcano, alaska, to the shaking from a large regional earthquake: a puzzle for intermediate-term earthquake-volcanoes interactions. Earth Sciences Research Journal; Vol. 8, núm. 1 (2004); 34-44 Earth Sciences Research Journal; Vol. 8, núm. 1 (2004); 34-44 2339-3459 1794-6190 .
dc.rights.spa.fl_str_mv Derechos reservados - Universidad Nacional de Colombia
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