Contemporary Seismicity in and Around the Yakima Fold-and-Thrust Belt in Eastern Washington

dc.contributor.utaustinauthorTrautman, M.en_US
dc.creatorGomberg, J.en_US
dc.creatorSherrod, B.en_US
dc.creatorTrautman, M.en_US
dc.creatorBurns, E.en_US
dc.creatorSnyder, D.en_US
dc.date.accessioned2016-10-28T19:51:34Z
dc.date.available2016-10-28T19:51:34Z
dc.date.issued2012-02en_US
dc.description.abstractWe examined characteristics of routinely cataloged seismicity from 1970 to the present in and around the Yakima fold-and-thrust belt (YFTB) in eastern Washington to determine if the characteristics of contemporary seismicity provide clues about regional-scale active tectonics or about more localized, near-surface processes. We employed new structural and hydrologic models of the Columbia River basalts (CRB) and found that one-third to one-half of the cataloged earthquakes occur within the CRB and that these CRB earthquakes exhibit significantly more clustered, and swarmlike, behavior than those outside. These results and inferences from published studies led us to hypothesize that clustered seismicity is likely associated with hydrologic changes in the CRB, which hosts the regional aquifer system. While some general features of the regional groundwater system support this hypothesis, seismicity patterns and mapped long-term changes in groundwater levels and present-day irrigation neither support nor refute it. Regional tectonic processes and crustal-scale structures likely influence the distribution of earthquakes both outside and within the CRB as well. We based this inference on qualitatively assessed alignments between the dominant northwest trends in the geologic structure and the seismicity generally and between specific faults and characteristics of the 2009 Wooded Island swarm and aseismic slip, which is the only cluster studied in detail and the most vigorous since regional monitoring began.en_US
dc.description.departmentEarth and Planetary Sciencesen_US
dc.description.sponsorshipUSGS-NAGTen_US
dc.identifierdoi:10.15781/T2G15TD7B
dc.identifier.citationGomberg, J., B. Sherrod, M. Trautman, E. Burns, and D. Snyder. "Contemporary Seismicity in and around the Yakima Fold?and?Thrust Belt in Eastern Washington." Bulletin of the Seismological Society of America , Vol. 102, No. 1 (Feb., 2012): 309-320.en_US
dc.identifier.doi10.1785/0120110065en_US
dc.identifier.issn0037-1106en_US
dc.identifier.urihttp://hdl.handle.net/2152/43250
dc.language.isoEnglishen_US
dc.relation.ispartofen_US
dc.relation.ispartofserialBulletin of the Seismological Society of Americaen_US
dc.rightsAdministrative deposit of works to Texas ScholarWorks: This works author(s) is or was a University faculty member, student or staff member; this article is already available through open access or the publisher allows a PDF version of the article to be freely posted online. The library makes the deposit as a matter of fair use (for scholarly, educational, and research purposes), and to preserve the work and further secure public access to the works of the University.en_US
dc.rights.restrictionOpenen_US
dc.subjectoregonen_US
dc.subjectearthquakesen_US
dc.subjectcaliforniaen_US
dc.subjectswarmsen_US
dc.subjectfaultsen_US
dc.subjectmodelen_US
dc.subjectgeochemistry & geophysicsen_US
dc.titleContemporary Seismicity in and Around the Yakima Fold-and-Thrust Belt in Eastern Washingtonen_US
dc.typeArticleen_US

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