Relevant bibliographies by topics / Cascadia subduction zone

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Cascadia subduction zone'

Author: Grafiati
Published: 4 June 2021
Last updated: 26 July 2025

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Journal articles on the topic "Cascadia subduction zone"

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Gao, Haiying, and Maureen D. Long. "Tectonics and Geodynamics of the Cascadia Subduction Zone." Elements 18, no. 4 (2022): 226–31. http://dx.doi.org/10.2138/gselements.18.4.226.

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The Cascadia subduction zone, where the young and thin oceanic Juan de Fuca plate sinks beneath western North America, represents a thermally hot endmember of global subduction systems. Cascadia exhibits complex and three-dimensional heterogeneities including variable coupling between the overriding and downgoing plates, the amount of water carried within and released by the oceanic plate, flow patterns within the mantle wedge and backarc, and the continuity and depth extent of the subducting slab. While recent research has benefitted from extensive onshore and offshore deployments of geophysi
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Kent, Adam J. R., and Josef Dufek. "Cascadia: Subduction and People." Elements 18, no. 4 (2022): 221–25. http://dx.doi.org/10.2138/gselements.18.4.221.

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The well-studied Cascadia subduction zone has enriched our general understanding of global subduction zones. This Elements issue explores the interconnected set of processes that link geodynamics, tectonics, and magmatism at depth and the surface expressions of these processes, which shape the landscape and give rise to natural hazards in the Cascadia region. This issue also addresses the impact of subduction zone processes on human populations using cultural records, and reviews the state of knowledge of Cascadia while highlighting some key outstanding research questions.
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Rogers, Garry C. "An assessment of the megathrust earthquake potential of the Cascadia subduction zone." Canadian Journal of Earth Sciences 25, no. 6 (1988): 844–52. http://dx.doi.org/10.1139/e88-083.

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The active tectonic setting of the southwest coast of Canada and the Pacific northwest coast of the United states is dominated by the Cascadia subduction zone. The zone can be divided into four segments where oceanic lithosphere is converging independently with the North American plate: the Winona and the Explorer segments in the north, the larger Juan de Fuca segment that extends into both Canada and the United States, and the Gorda segment in the south. The oceanic lithosphere entering the Cascadia subduction zone in all segments is extremely young, less than 10 Ma. Of the other six zones ar
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Schmalzle, Gina M., Robert McCaffrey, and Kenneth C. Creager. "Central Cascadia subduction zone creep." Geochemistry, Geophysics, Geosystems 15, no. 4 (2014): 1515–32. http://dx.doi.org/10.1002/2013gc005172.

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Janiszewski, Helen A., James B. Gaherty, Geoffrey A. Abers, Haiying Gao, and Zachary C. Eilon. "Amphibious surface-wave phase-velocity measurements of the Cascadia subduction zone." Geophysical Journal International 217, no. 3 (2019): 1929–48. http://dx.doi.org/10.1093/gji/ggz051.

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SUMMARY A new amphibious seismic data set from the Cascadia subduction zone is used to characterize the lithosphere structure from the Juan de Fuca ridge to the Cascades backarc. These seismic data are allowing the imaging of an entire tectonic plate from its creation at the ridge through the onset of the subduction to beyond the volcanic arc, along the entire strike of the Cascadia subduction zone. We develop a tilt and compliance correction procedure for ocean-bottom seismometers that employs automated quality control to calculate robust station noise properties. To elucidate crust and upper
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Moore, Nicole E., and Lynn Robinson. "The Role of Subduction Zone Processes in the Cultural History of the Cascade Region." Elements 18, no. 4 (2022): 246–50. http://dx.doi.org/10.2138/gselements.18.4.246.

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The Cascadia subduction zone continuously shapes the landscape of the Pacific Northwest of North America and the cultures of its inhabitants. The impacts of subduction processes on Pacific Northwest societies and cultures are varied, but Native Americans and European settler cultures alike have described geological processes through oral histories and have relied on resources provided by the subduction zone. Indigenous peoples focus many aspects of their religious practices and art around the geohazards of the Cascadia region, and our melded modern cultures continue to take part in storytellin
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Li, Duo, and Yajing Liu. "Cascadia megathrust earthquake rupture model constrained by geodetic fault locking." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 379, no. 2196 (2021): 20200135. http://dx.doi.org/10.1098/rsta.2020.0135.

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Paleo-earthquakes along the Cascadia subduction zone inferred from offshore sediments and Japan coastal tsunami deposits approximated to M9+ and ruptured the entire margin. However, due to the lack of modern megathrust earthquake records and general quiescence of subduction fault seismicity, the potential megathrust rupture scenario and influence of downdip limit of the seismogenic zone are still obscure. In this study, we present a numerical simulation of Cascadia subduction zone earthquake sequences in the laboratory-derived rate-and-state friction framework to investigate the potential infl
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Farahbod, Amir Mansour, Andrew J. Calvert, John F. Cassidy, and Camille Brillon. "CodaQin the Northern Cascadia Subduction Zone." Bulletin of the Seismological Society of America 106, no. 5 (2016): 1939–47. http://dx.doi.org/10.1785/0120160058.

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Minor, Rick, and Wendy C. Grant. "Earthquake-Induced Subsidence and Burial of Late Holocene Archaeological Sites, Northern Oregon Coast." American Antiquity 61, no. 4 (1996): 772–81. http://dx.doi.org/10.2307/282017.

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Fire hearths associated with prehistoric Native American occupation lie within the youngest buried lowland soil of the estuaries along the Salmon and Nehalem rivers on the northern Oregon coast. This buried soil is the result of sudden subsidence induced by a great earthquake about 300 years ago along the Cascadia subduction zone, which extends offshore along the North Pacific Coast from Vancouver Island to northern California. The earthquake 300 years ago was the latest in a series of subsidence events along the Cascadia subduction zone over the last several thousand years. Over the long term
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Westby, Elizabeth G., Andrew Meigs, and Chris Goldfinger. "Volcano, Earthquake, and Tsunami Hazards of the Cascadia Subduction Zone." Elements 18, no. 4 (2022): 251–56. http://dx.doi.org/10.2138/gselements.18.4.251.

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Subduction zones produce some of Earth’s most devastating geological events. Recent eruptions of Mount St. Helens and great earthquakes and tsunamis in Japan and Sumatra provide stark examples of the destructive power of subduction-related hazards. In the Cascadia subduction zone, large earthquakes, tsunamis, and volcanic eruptions have occurred in the past and geologic records imply that these events will occur in the future. As the population and infrastructure increase in the region, resilience to these natural hazards requires a detailed scientific understanding of the geologic forces and
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Dissertations / Theses on the topic "Cascadia subduction zone"

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Dehler, Sonya Astrid. "Integrated geophysical modelling of the northern Cascadia subduction zone." Thesis, University of British Columbia, 1991. http://hdl.handle.net/2429/30798.

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The northern Cascadia subduction zone involves convergence of the Explorer Plate and northern part of the Juan de Fuca Plate with the North American Plate along a margin lying west of Vancouver Island, Canada. A wide accretionary complex which underlies the continental slope and shelf has been formed. Two allochthonous terranes, the Crescent Terrane of Eocene oceanic crustal volcanics and the Pacific Rim Terrane of Mesozoic melange sedimentary rocks and volcanics, lie against the Wrangellia Terrane backstop beneath the west coast of Vancouver Island and outcrop on the southern tip of the islan
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Matharu, Gian. "Crustal anisotropy in a subduction zone forearc : Northern Cascadia." Thesis, University of British Columbia, 2014. http://hdl.handle.net/2429/46496.

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S-wave splitting analyses using high signal-to-noise ratio low frequency earthquake (LFE) templates at 3-component stations across southern Vancouver Island (SVI) and northern Washington indicate the presence of a heterogeneous distribution of crustal anisotropy in the North American plate. For SVI, we investigate the contribution to anisotropy from the Leech River Complex (LRC), an allochthonous terrane comprised of strongly foliated greenschist facies phyllites and amphibolite facies schists with steeply dip- ping foliations striking E-W. On SVI, estimates of initial S-wave polarization dire
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Henton, Joseph Alan. "GPS studies of crustal deformation in the northern Cascadia subduction zone." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0020/NQ48226.pdf.

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Rondenay, Stéphane. "Teleseismic imaging of the southeastern Canadian Shield and Cascadia subduction zone." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2001. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/NQ61166.pdf.

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Boyarko, Devin C. "SPATIAL AND TEMPORAL PATTERNS OF NON-VOLCANIC TREMOR ALONG THE SOUTHERN CASCADIA SUBDUCTION ZONE." Miami University / OhioLINK, 2009. http://rave.ohiolink.edu/etdc/view?acc_num=miami1259983250.

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Burgette, Reed Joel. "Uplift in response to tectonic convergence : the Kyrgyz Tien Shan and Cascadia subduction zone /." Connect to title online (ProQuest), 2008. http://proquest.umi.com/pqdweb?did=1616709721&sid=1&Fmt=2&clientId=11238&RQT=309&VName=PQD.

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Thesis (Ph. D.)--University of Oregon, 2008.<br>Typescript. Includes vita and abstract. Includes bibliographical references (leaves 225-242). Also available online in ProQuest, free to University of Oregon users.
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VanDecar, John Callaway. "Upper-mantle structure of the Cascadia subduction zone from non-linear teleseismic travel-time inversion /." Thesis, Connect to this title online; UW restricted, 1991. http://hdl.handle.net/1773/6804.

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Doyle, Debra Lee. "Beach Response to Subsidence Following a Cascadia Subduction Zone Earthquake Along the Washington-Oregon Coast." PDXScholar, 1996. https://pdxscholar.library.pdx.edu/open_access_etds/5072.

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Beach shoreline retreat induced by coseismic subsidence in the Cascadia subduction zone is an important post-earthquake hazard. Sand on a beach acts as a buffer to wave attack, protecting dunes, bluffs and terraces. The loss of sand from a beach could promote critical erosion of the shoreline. This study was initiated in order to estimate the potential amount of post subsidence shoreline retreat on a regional scale in the Central Cascadia Margin. The study area is a 331 km stretch of coastline from Copalis, Washington to Florence, Oregon. Several erosion models were evaluated, and the Bruun mo
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Michel, Lorenz [Verfasser], and Todd [Akademischer Betreuer] Ehlers. "Exhumation Processes at Orogenic Syntaxes : Insights from the Cascadia Subduction Zone (USA) / Lorenz Michel ; Betreuer: Todd Ehlers." Tübingen : Universitätsbibliothek Tübingen, 2020. http://d-nb.info/1204422125/34.

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Michel, Lorenz Verfasser], and Todd [Akademischer Betreuer] [Ehlers. "Exhumation Processes at Orogenic Syntaxes : Insights from the Cascadia Subduction Zone (USA) / Lorenz Michel ; Betreuer: Todd Ehlers." Tübingen : Universitätsbibliothek Tübingen, 2020. http://d-nb.info/1204422125/34.

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Books on the topic "Cascadia subduction zone"

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Wang, Kelin. The Cascadia subduction zone and related subduction systems: Seismic structure, intraslab earthquakes and processes, and earthquake hazards. U.S. Department of the Interior, U.S. Geological Survey, 2002.

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Geist, Eric L. Local tsunami hazards in the Pacific Northwest from Cascadia subduction zone earthquakes. U.S. Dept. of the Interior, U.S. Geological Survey, 2005.

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Geological Survey (U.S.), ed. Turbidite event history: Methods and implications for Holocene paleoseismicity of the Cascadia subduction zone. U.S. Dept. of the Interior, U.S. Geological Survey, 2012.

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Janiszewski, Helen A. New Insights on the Structure of the Cascadia Subduction Zone from Amphibious Seismic Data. [publisher not identified], 2018.

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Obermeier, Stephen F. Preliminary estimates of the strength of prehistoric shaking in the Columbia River Valley and the southern half of coastal Washington, with emphasis for a Cascadia subduction zone earthquake about 300 years ago. U.S. Dept. of the Interior, U.S. Geological Survey], 1995.

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R, Toppozada Tousson, and California. Division of Mines and Geology., eds. Planning scenario in Humboldt and Del Norte counties, California, for a great earthquake on the Cascadia subduction zone. California Dept. of Conservation, Division of Mines and Geology, 1995.

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Geological Survey (U.S.), ed. The Cascadia Subduction Zone and Related Subduction Systems--Seismic Structure, etc., U.S. Geological Survey, U.S. Geological Survey Open-File Report-02-328, etc., 2002, (CD-ROM). s.n., 2003.

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D, Peterson Curt, ed. Estimates of coastal subsidence from great earthquakes in the Cascadia subduction zone, Vancouver Island, B.C., Washington, Oregon, and northernmost California. State of Oregon, Dept. of Geology and Mineral Industries, 1997.

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R, Priest George, and Oregon. Dept. of Geology and Mineral Industries., eds. Cascadia subduction zone tsunamis: Hazard mapping at Yaquina Bay, Oregon : final technical report to the National Earthquake Hazard Reduction Program. State of Oregon, Dept. of Geology and Mineral Industries, 1997.

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R, Nelson Alan, Personius Stephen F, Rogers A. M, and Geological Survey (U.S.), eds. Earthquake hazards in the Pacific Northwest of the United States.: An overview of recent coastal geologic studies and their bearing on segmentation of Holocene ruptures, central Cascadia subduction zone. U.S. Geological Survey, 1991.

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Book chapters on the topic "Cascadia subduction zone"

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Heaton, Thomas H., and Stephen H. Hartzell. "Estimation of Strong Ground Motions from Hypothetical Earthquakes on the Cascadia Subduction Zone, Pacific Northwest." In Subduction Zones Part II. Birkhäuser Basel, 1989. http://dx.doi.org/10.1007/978-3-0348-9140-0_6.

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Goldfinger, Chris, LaVerne D. Kulm, Robert S. Yeats, et al. "Oblique Strike-Slip Faulting of the Cascadia Submarine Forearc: The Daisy Bank Fault Zone off Central Oregon." In Subduction Top to Bottom. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm096p0065.

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Cramer, Lori A., Daniel Cox, and Haizhong Wang. "Enhancing a Culture of Preparedness for the Next Cascadia Subduction Zone Tsunami." In Coastal Heritage and Cultural Resilience. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99025-5_11.

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Raghukumar, Kaustubha, Katherine Heal, Frank Spada, et al. "Acoustic Measurements During a Seismic Airgun Survey: The Case of the Cascadia Subduction Zone." In The Effects of Noise on Aquatic Life. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-10417-6_131-1.

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Raghukumar, Kaustubha, Katherine Heal, Frank Spada, et al. "Acoustic Measurements During a Seismic Airgun Survey: The Case of the Cascadia Subduction Zone." In The Effects of Noise on Aquatic Life. Springer International Publishing, 2024. http://dx.doi.org/10.1007/978-3-031-50256-9_131.

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Petersen, Mark D., Chris H. Cramer, and Arthur D. Frankel. "Simulations of Seismic Hazard for the Pacific Northwest of the United States from Earthquakes Associated with the Cascadia Subduction Zone." In Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part I. Birkhäuser Basel, 2002. http://dx.doi.org/10.1007/978-3-0348-8203-3_15.

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McPherson, Robert C. "SEISMICITY AND STRESS AT THE SOUTHERN END OF THE CASCADIA SUBDUCTION ZONE." In Field Guide to the Late Cenozoic Subduction Tectonics & Sedimentation of Northern Coastal California. The Pacific Section American Association of Petroleum Geologist, 1992. http://dx.doi.org/10.32375/1992-gb71.3.

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Underwood, M., and M. Torres. "Data Report: Composition of Clay Minerals from Hemipelagic Sediments at Hydrate Ridge, Cascadia Subduction Zone." In Proceedings of the Ocean Drilling Program, 199 Scientific Results. Ocean Drilling Program, 2006. http://dx.doi.org/10.2973/odp.proc.sr.204.127.2006.

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NELSON, ALAN R. "HOLOCENE TIDAL-MARSH STRATIGRAPHY IN SOUTH-CENTRAL OREGON-EVIDENCE FOR LOCALIZED SUDDEN SUBMERGENCE IN THE CASCADIA SUBDUCTION ZONE." In Quaternary Coasts of the United States. SEPM (Society for Sedimentary Geology), 1992. http://dx.doi.org/10.2110/pec.92.48.0287.

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Nelson, C. Hans, Chris Goldfinger, Joel E. Johnson, and Gita Dunhill. "Variation of Modem Turbidite Systems Along the Subduction Zone Margin of Cascadia Basin and Implications for Turbidite Reservoir Beds." In Deep-Water Reservoirs of the World: 20th Annual. SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS, 2000. http://dx.doi.org/10.5724/gcs.00.15.0714.

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Conference papers on the topic "Cascadia subduction zone"

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Grant, Alex R., Joseph Wartman, Alison R. Duvall, and Sean Richard LaHusen. "CASCADIA SUBDUCTION ZONE LANDSLIDE HAZARD FORECASTING." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-305393.

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McPherson, Bob, Mark Hemphill-Haley, Stewart Smith, Todd Williams, and Ian Pryor. "COMPLICATED KINEMATICS IN THE SOUTHERN CASCADIA SUBDUCTION ZONE." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-299252.

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Hardin, Kellyn. "CASCADIA SUBDUCTION ZONE (CSZ) HAZARDS NGSS PERFORMANCE TASK." In GSA Connects 2024 Meeting in Anaheim, California. Geological Society of America, 2024. http://dx.doi.org/10.1130/abs/2024am-405393.

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Byram, Aspen Samantha, and Elizabeth M. Higgins. "THE CASCADIA SUBDUCTION ZONE: TSUNAMI MITIGATION IN GRAYS HARBOR, WASHINGTON." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283749.

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Stern, Robert J. "EOCENE INITIATION OF THE CASCADIA SUBDUCTION ZONE: A SECOND EXAMPLE OF PLUME-INDUCED SUBDUCTION INITIATION?" In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-297662.

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Bilek, Susan L., Emily A. Morton, and Charlotte A. Rowe. "NEWLY DETECTED CASCADIA SUBDUCTION ZONE EARTHQUAKES OFFSHORE CENTRAL OREGON USING THE CASCADIA INITIATIVE AMPHIBIOUS DATASE." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-300009.

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LeVeque, Randall J., Paul Bodin, Geoffrey Cram, et al. "Developing a Warning System for Inbound Tsunamis from the Cascadia Subduction Zone." In OCEANS 2018 MTS/IEEE Charleston. IEEE, 2018. http://dx.doi.org/10.1109/oceans.2018.8604709.

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Peck, Erin, Thomas P. Guilderson, Maureen H. Walczak, Emerson Webb, and Robert A. Wheatcroft. "RATE OF SALT MARSH REEMERGENCE FOLLOWING THE 1700 CASCADIA SUBDUCTION ZONE EARTHQUAKE." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-356037.

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Dasho, Oluwaseyi, Ashutosh Tiwari, and Manoochehr Shirzaei. "MAPPING VERTICAL LAND MOTION AND FLOODING HAZARDS ALONG THE CASCADIA SUBDUCTION ZONE." In GSA Connects 2024 Meeting in Anaheim, California. Geological Society of America, 2024. http://dx.doi.org/10.1130/abs/2024am-400649.

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Nisar, Ahmed, Ryan M. Nelson, Christopher Hitchcock, Vladimir Calugaru, and Michael W. Greenfield. "Vulnerability Assessment of Portland Water System in an M9 Cascadia Subduction Zone Earthquake." In Lifelines 2022. American Society of Civil Engineers, 2022. http://dx.doi.org/10.1061/9780784484432.040.

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Reports on the topic "Cascadia subduction zone"

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Rutherford, J., and J. F. Cassidy. Comparing felt intensity patterns for crustal earthquakes in the Cascadia and Chilean subduction zones, offshore British Columbia, United States, and Chile. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330475.

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In this study, we utilize US Geological Survey citizen science earthquake felt intensity data to investigate whether , crustal earthquakes in the Chilean Subduction Zone show similar, "felt intensity" distributions to events of the same magnitude and depths within the Cascadia Subduction Zone (Quitoriano &amp;amp; Wald, 2020; USGS Earthquake Hazards Program, 2020). In a companion article (Rutherford &amp;amp; Cassidy, 2022) we examine intraslab deep earthquake intensity patterns for the Chile and Cascadia subduction zones. Building on from the intraslab companion article, the goal of this comp
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Rondenay, S., and M. G. Bostock. An image of the Cascadia subduction zone across central Oregon. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/222512.

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Cassidy, J. F., and F. Waldhauser. Precise relocations of slab seismicity in the northern Cascadia subduction zone. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/222514.

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Kirby, S., K. Wang, and S. Dunlop. The Cascadia subduction zone and related subduction systems - seismic structure, intraslab earthquakes and processes, and earthquake hazards. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/222383.

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Abrahamson, Norman, Nicolas Kuehn, Zeynep Gulerce, et al. Update of the BC Hydro Subduction Ground-Motion Model using the NGA- Subduction Dataset. Pacific Earthquake Engineering Research Center, University of California, Berkeley, CA, 2018. http://dx.doi.org/10.55461/oycd7434.

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An update to the BCHydro ground-motion model for subduction earthquakes has been developed using the 2018 PEER NGA-SUB dataset. The selected subset includes over 70,000 recordings from 1880 earthquakes. The update modifies the BCHydro model to include regional terms for the VS30 scaling, large distance (linear R) scaling, and constant terms, which is consistent with the regionalization approach used in the NGA-W2 ground-motion models. A total of six regions were considered: Cascadia, Central America, Japan, New Zealand, South America, and Taiwan. Region- independent terms are used for the smal
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Shragge, J., M. Bostock, and G. C. Rogers. Modeling post-critical Moho reflections from intraslab earthquakes in the Cascadia subduction zone. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/222495.

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Douglas, K., M. Coté, M. Riedel, A. Podhorodeski, and K. Obana. 2023003PGC cruise report: northern Cascadia Subduction Zone international research expedition, offshore British Columbia. Natural Resources Canada/CMSS/Information Management, 2024. http://dx.doi.org/10.4095/332361.

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Adams, J. Turbidites Off the Oregon-Washington Margin Record Paleo-Earthquakes On the Cascadia Subduction Zone. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127523.

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Doyle, Debra. Beach Response to Subsidence Following a Cascadia Subduction Zone Earthquake Along the Washington-Oregon Coast. Portland State University Library, 2000. http://dx.doi.org/10.15760/etd.6948.

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10

Paul, C., and J. F. Cassidy. Seismic hazard investigations at select DND facilities in Southwestern British Columbia: subduction, in-slab, and crustal scenarios. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/331199.

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Abstract:
Southwest British Columbia has some of the highest seismic hazard in Canada and is home to facilities owned by the Department of National Defence which support operations on the west coast of Canada. The potential impact of seismic hazards on these government facilities are investigated here. The hazard is from three primary sources: subduction interface, crustal and in-slab earthquakes. NRCan, in consultation with DRDC have produced representative earthquake scenarios for each of these sources. The subduction scenario we constructed was an M8.9 earthquake extending along the entire Cascadia S
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