Geologic Hazards in WA

Total Page:16

File Type:pdf, Size:1020Kb

Geologic Hazards in WA Geologic Hazards in WA Maximilian Dixon – Earthquake Program Manager July 28, 2018 Washington’s Earthquake Hazard . According to the Federal Emergency Management Agency (FEMA), Washington State has 2nd highest earthquake risk in the United States. More than 2,500 earthquakes occur in Washington each year. Estimated Probability of Approximate Earthquake Source and Example Events Occurrence in 50 Years Recurrence Interval Deep Earthquakes • 2001 Nisqually, M6.8 84 Percent 30 – 50 Years • 1965 Seattle-Tacoma, M6.5 • 1949 Olympia, M6.8 Cascadia Subduction Zone 10 – 20 Percent 200 – 600 Years • 1700 January 26 Event, M9.0 (est.) Shallow/Crustal Earthquakes 5 Percent 1,000 Years • Seattle Fault, M6.5 or greater • Random 6.5 or greater 15 Percent 333 Years Deep (Benioff Zone) Fault Earthquakes • Nisqually Earthquake in 2001 • Magnitude 6.8 • 11 miles northeast of Olympia, Washington • 31.6 miles deep • Amazingly, there were no deaths, ~400 injuries • Estimated losses of $1 - $4 billion Deep EQ: Less damage to Infrastructure and fewer aftershocks Courtesy: USGS, Shallow / Crustal Fault Earthquakes • Seattle Fault • Magnitude 7.2 • At least 4 earthquakes within the last 8,000 years. The most recent was 1,100 years ago. Shallow EQ: More intense shaking, heavy infrastructure damage and more aftershocks Summary of significant losses in the M7.2 Seattle fault earthquake scenario. Among the counties most likely to be affected are King, Kitsap, Mason, Pierce, Snohomish, and Thurston. Shallow / Crustal Fault Earthquakes South Whidbey Island Fault • Magnitude 7.4 • At least four earthquakes in the last 16,000 years. The most recent was less than 2,700 years ago. Shallow EQ: More intense shaking, heavy infrastructure damage and more aftershocks Summary of significant losses in the magnitude 7.4 southern Whidbey Island earthquake scenario. The counties most likely to be affected are Island, King, Pierce, San Juan, Skagit, Snohomish, and Whatcom. Shallow / Crustal Fault Earthquakes Devils Mountain Fault • Magnitude 7.1 • At least 2 earthquakes: 1,100 – 2,200 years ago; and 100-500 years ago. Shallow EQ: More intense shaking, heavy infrastructure damage and more aftershocks Devils Mountain Fault Impacts Summary of significant losses in the magnitude 7.1 Darrington - Devils Mountain Fault earthquake scenario. The counties most likely to be affected are Island, Jefferson, King, San Juan, Skagit, Snohomish, and Whatcom. A M9.0 Cascadia earthquake is estimated to cost $49 Billion These large quakes recur every 200–600 years The last one was AD 1700 (318 years ago) Landslide damage is usually not covered by insurance Landslides are one of the most frequent natural hazards, but are difficult to predict or quantify 13 What is ShakeAlert? • The ShakeAlert system detects an earthquake and rapidly disseminates warnings to end users in potentially affected areas. • The system currently operates as a production prototype in California, Oregon, and Washington. • ShakeAlert does not yet support public warnings. How ShakeAlert works: P-waves S-waves What is Earthquake Early Warning (EEW)? In the U.S., EEW is the combination of: • ShakeAlert system technology • Recommended protective messages communicated to end users • The outreach, education, training, and other risk reduction activities required to fully implement EEW What could we do with EEW? • Slow down trains so they don’t derail • Stop elevators at the nearest floor and open the doors so people can escape • Notify people so they can move away from hazards and protect themselves • Automatically divert inbound aircraft away from an airport that might be impacted • Shut down industrial processes to protect property • Suspend or initiate financial or critical data transfers and save vital data • Stop surgeries What is a Successful EEW System? • The ShakeAlert system adequately detected an earthquake and rapidly disseminated warnings to end users in potentially affected areas • The end users received the warnings and took the recommended protective measures • The receipt of the warning and resulting protective actions (individual and automated responses) enhanced public safety What is a Tsunami? Distant vs Local Tsunamis Local Tsunamis: The first waves could reach the Washington coast within 15 to 20 minutes. • Cascadia Subduction Zone Fault • Seattle and Tacoma Faults Distant Tsunamis: Waves higher than 3 feet could reach the Washington coast within 3 hours or more. • Alaska 1964 • Tohoku 2011 Waves only a couple feet high… Tsunamis can be generated across the Pacific or locally A tsunami from a Cascadia earthquake will hit Seattle in <2.5 hours and be up to 6' tall 2011 Tohoku tsunami (Japan) ~$300B damage 15,894 fatalities Cascadia Subduction Zone – L1 2 Tsunami Warning Centers Pacific National Tsunami Tsunami Warning Warning Center Center (Honolulu, HI) (Palmer, AK) Role of the National Tsunami Warning Center Process for Issuing a Tsunami Warning Page 30 During a Disaster First Local Disaster Response Local EOC Mutual Aid Occurs Arrives at Activated Requested Scene State Proclamation County EOC Activated President State EOC Declares Activated Disaster Preliminary Damage Assessment Recommendation FEMA FEMA Director Evaluates Presidential Disaster Reports To Reports To Reviews Damage & Declaration Requested Request Requirements Tsunami Alerts NOAA Weather Radio • 16 Stations in Washington • Warning Alarm Feature • NWS Portal into the Emergency Alert System (EAS) Wireless Emergency Alerts All Hazard Alert Broadcast Sirens • OUTDOOR Tsunami Warning System • Activated upon receipt of a Tsunami WARNING from the NTWC • Wailing Tone followed by verbal warning in English and Spanish • Coverage areas focus on major population centers WA AHAB Sirens Regular Siren Tests Stay Informed 40404 “Follow NWS_NTWC” [email protected] https://www.facebook.com/NWSNTWC Tsunami.gov • Visually displays which coasts are impacted • List ALL tsunami alert messages (public bulletins) • In chronological order • Only look for messages titled AK/BC/US West Coast • As of result of Jan 23rd event, NOAA has dedicated more servers to support event spike traffic 7/30/2018 It could save your life! Get Off and Stay Off the beach Guidance for Safe Minimum Offshore Depth for Vessel Movement Distant Source Local Source (ships State/Territory Notes (ships in harbor)* at sea)* Evaluated; may add potential safe areas within large bays 30 fathoms 100 fathoms California and ports Evaluated, but is re-evaluating based on new data; also 30 fathoms 100 fathoms Oregon evaluating Columbia River Evaluated; ships should be at least 1/2 mile from shore for 30 fathoms 100 fathoms Alaska all scenarios Washington 30 fathoms 100 fathoms Evaluated; special conditions exist inside Puget Sound Evaluated; implemented in Coast Guard plan in some 50 fathoms 50 fathoms Hawaii locations * Ships also recommended to be a minimum of ½ mile from shore or fringing reef Plan to be on your own Help will be slow in coming Know the ‘natural warning signs’ FEEL, SEE, HEAR, RUN!! Know what areas are at risk Practice evacuations (Walking) Know your evacuation routes, Have multiple routes, Walk the routes Do not count on being able to drive Be prepared to be on your own for a while! • mil.wa.gov/preparedness • geologyportal.dnr.wa.gov • www.tsunami.gov • earthquake.usgs.gov/ens/register.
Recommended publications
  • Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information
    Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information Index Abancay Deflection, 201, 204–206, 223 Allmendinger, R. W., 206 Abant, Turkey, earthquake of 1957 Ms 7.0, 286 allochthonous terranes, 26 Abdrakhmatov, K. Y., 381, 383 Alpine fault, New Zealand, 482, 486, 489–490, 493 Abercrombie, R. E., 461, 464 Alps, 245, 249 Abers, G. A., 475–477 Alquist-Priolo Act, California, 75 Abidin, H. Z., 464 Altay Range, 384–387 Abiz, Iran, fault, 318 Alteriis, G., 251 Acambay graben, Mexico, 182 Altiplano Plateau, 190, 191, 200, 204, 205, 222 Acambay, Mexico, earthquake of 1912 Ms 6.7, 181 Altunel, E., 305, 322 Accra, Ghana, earthquake of 1939 M 6.4, 235 Altyn Tagh fault, 336, 355, 358, 360, 362, 364–366, accreted terrane, 3 378 Acocella, V., 234 Alvarado, P., 210, 214 active fault front, 408 Álvarez-Marrón, J. M., 219 Adamek, S., 170 Amaziahu, Dead Sea, fault, 297 Adams, J., 52, 66, 71–73, 87, 494 Ambraseys, N. N., 226, 229–231, 234, 259, 264, 275, Adria, 249, 250 277, 286, 288–290, 292, 296, 300, 301, 311, 321, Afar Triangle and triple junction, 226, 227, 231–233, 328, 334, 339, 341, 352, 353 237 Ammon, C. J., 464 Afghan (Helmand) block, 318 Amuri, New Zealand, earthquake of 1888 Mw 7–7.3, 486 Agadir, Morocco, earthquake of 1960 Ms 5.9, 243 Amurian Plate, 389, 399 Age of Enlightenment, 239 Anatolia Plate, 263, 268, 292, 293 Agua Blanca fault, Baja California, 107 Ancash, Peru, earthquake of 1946 M 6.3 to 6.9, 201 Aguilera, J., vii, 79, 138, 189 Ancón fault, Venezuela, 166 Airy, G.
    [Show full text]
  • What's Shaking
    ISSUE 03 - February 2016 WHAT’S SHAKING newsletter of the THE NEVADA SEISMOLOGICAL LABORATORY Earthquake Update NEVADA Carson RENO City Maps of earthquakes located by the Nevada Seismo- logical Laboratory (NSL) between 1/1/16 and 1/31/16, within the NSL network (right). Truckee Meadows region (above), Hawthorne, Nevada area (bottom left) and the area surrounding Las Vegas, Nevada (bottom right). HAWTHORNE Earthquakes located by the NSL (1/1/16-1/31/16) ML Quantity 4.0+ 1 3.0-3.9 2 2.0-2.9 67 Nevada 1.0-1.9 478 National ML < 1.0 809 Security Site Total 1357 eismicity during January included a small sequence near Haw- Sthorne, Nevada (above), and a notable sequence near Enter- LAS VEGAS prise, Utah (right). The largest of these Hawthorne events measured M3.2, and several events greater than M2.0 were also recorded. An event (M4.3) that occurred near Enterprise, Utah shook several eastern Nevada communities on January 15, 2016. The Sheldon Sequence also continues to be active in northwestern Nevada. Maps compiled by D. Molisee (2016) www.graphicdiffer.comwww.seismo.unr.edu @NVSeismoLab1 DEVELOPMENTS NSL Graduate Students Leverage Funding from the National Science Foundation unding for Steve Angster and will focus on the Agai-Pai, Indian FIan Pierce has come from Head, Gumdrop, Benton Springs, a National Science Foundation and Petrified fault systems, while grant (Steve Wesnousky, lead PI) Ian will study the Tahoe, Carson, focused on the deformation pat- Antelope Valley, Smith Valley, Ma- tern and kinematics of the Walker son Valley, and Walker Lake fault Lane.
    [Show full text]
  • Geologic History of Siletzia, a Large Igneous Province in the Oregon And
    Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Wells, R., Bukry, D., Friedman, R., Pyle, D., Duncan, R., Haeussler, P., & Wooden, J. (2014). Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot. Geosphere, 10 (4), 692-719. doi:10.1130/GES01018.1 10.1130/GES01018.1 Geological Society of America Version of Record http://cdss.library.oregonstate.edu/sa-termsofuse Downloaded from geosphere.gsapubs.org on September 10, 2014 Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Ray Wells1, David Bukry1, Richard Friedman2, Doug Pyle3, Robert Duncan4, Peter Haeussler5, and Joe Wooden6 1U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025-3561, USA 2Pacifi c Centre for Isotopic and Geochemical Research, Department of Earth, Ocean and Atmospheric Sciences, 6339 Stores Road, University of British Columbia, Vancouver, BC V6T 1Z4, Canada 3Department of Geology and Geophysics, University of Hawaii at Manoa, 1680 East West Road, Honolulu, Hawaii 96822, USA 4College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, 104 CEOAS Administration Building, Corvallis, Oregon 97331-5503, USA 5U.S. Geological Survey, 4210 University Drive, Anchorage, Alaska 99508-4626, USA 6School of Earth Sciences, Stanford University, 397 Panama Mall Mitchell Building 101, Stanford, California 94305-2210, USA ABSTRACT frames, the Yellowstone hotspot (YHS) is on southern Vancouver Island (Canada) to Rose- or near an inferred northeast-striking Kula- burg, Oregon (Fig.
    [Show full text]
  • Constraining the Holocene Extent of the Northwest Meers Fault, Oklahoma Using High-Resolution Topography and Paleoseismic Trenching
    Portland State University PDXScholar Dissertations and Theses Dissertations and Theses Summer 9-8-2017 Constraining the Holocene Extent of the Northwest Meers Fault, Oklahoma Using High-Resolution Topography and Paleoseismic Trenching Kristofer Tyler Hornsby Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geology Commons, and the Geomorphology Commons Let us know how access to this document benefits ou.y Recommended Citation Hornsby, Kristofer Tyler, "Constraining the Holocene Extent of the Northwest Meers Fault, Oklahoma Using High-Resolution Topography and Paleoseismic Trenching" (2017). Dissertations and Theses. Paper 3890. https://doi.org/10.15760/etd.5778 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Constraining the Holocene Extent of the Northwest Meers Fault, Oklahoma Using High-Resolution Topography and Paleoseismic Trenching by Kristofer Tyler Hornsby A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science In Geology Thesis Committee: Ashley R. Streig, Chair Scott E.K. Bennett Adam M. Booth Portland State University 2017 ABSTRACT The Meers Fault (Oklahoma) is one of few seismogenic structures with Holocene surface expression in the stable continental region of North America. Only the ~37 km- long southeastern section of the ~55 km long Meers Fault is interpreted to be Holocene- active. The ~17 km-long northwestern section is considered to be Quaternary-active (pre- Holocene); however, its low-relief geomorphic expression and anthropogenic alteration have presented difficulties in evaluating the fault length and style of Holocene deformation.
    [Show full text]
  • Diverse Rupture Modes for Surface-Deforming Upper Plate Earthquakes in the Southern Puget Lowland of Washington State
    Diverse rupture modes for surface-deforming upper plate earthquakes in the southern Puget Lowland of Washington State Alan R. Nelson1,*, Stephen F. Personius1, Brian L. Sherrod2, Harvey M. Kelsey3, Samuel Y. Johnson4, Lee-Ann Bradley1, and Ray E. Wells5 1Geologic Hazards Science Center, U.S. Geological Survey, MS 966, PO Box 25046, Denver, Colorado 80225, USA 2U.S. Geological Survey at Department of Earth and Space Sciences, University of Washington, Box 351310, Seattle, Washington 98195, USA 3Department of Geology, Humboldt State University, Arcata, California 95521, USA 4Western Coastal and Marine Geology Science Center, U.S. Geological Survey, 400 Natural Bridges Drive, Santa Cruz, California 95060, USA 5Geology, Minerals, Energy, and Geophysics Science Center, U.S. Geological Survey, 345 Middlefi eld Road, MS 973, Menlo Park, California 94025, USA ABSTRACT earthquakes. In the northeast-striking Saddle migrating forearc has deformed the Seto Inland Mountain deformation zone, along the west- Sea into a series of basins and uplifts bounded Earthquake prehistory of the southern ern limit of the Seattle and Tacoma fault by faults. One of these, the Nojima fault, pro- Puget Lowland, in the north-south com- zones, analysis of previous ages limits earth- duced the 1995 Mw6.9 Hyogoken Nanbu (Kobe) pressive regime of the migrating Cascadia quakes to 1200–310 cal yr B.P. The prehistory earthquake, which killed more than 6400 peo- forearc, refl ects diverse earthquake rupture clarifi es earthquake clustering in the central ple, destroyed the port of Kobe, and caused modes with variable recurrence. Stratigraphy Puget Lowland, but cannot resolve potential $100 billion in damage (Chang, 2010).
    [Show full text]
  • Cascadia Low Frequency Earthquakes at the Base of an Overpressured Subduction Shear Zone ✉ Andrew J
    ARTICLE https://doi.org/10.1038/s41467-020-17609-3 OPEN Cascadia low frequency earthquakes at the base of an overpressured subduction shear zone ✉ Andrew J. Calvert 1 , Michael G. Bostock 2, Geneviève Savard 3 & Martyn J. Unsworth4 In subduction zones, landward dipping regions of low shear wave velocity and elevated Poisson’s ratio, which can extend to at least 120 km depth, are interpreted to be all or part of the subducting igneous oceanic crust. This crust is considered to be overpressured, because fl 1234567890():,; uids within it are trapped beneath an impermeable seal along the overlying inter-plate boundary. Here we show that during slow slip on the plate boundary beneath southern Vancouver Island, low frequency earthquakes occur immediately below both the landward dipping region of high Poisson’s ratio and a 6–10 km thick shear zone revealed by seismic reflections. The plate boundary here either corresponds to the low frequency earthquakes or to the anomalous elastic properties in the lower 3–5 km of the shear zone immediately above them. This zone of high Poisson’s ratio, which approximately coincides with an electrically conductive layer, can be explained by slab-derived fluids trapped at near-lithostatic pore pressures. 1 Department of Earth Sciences, Simon Fraser University, 8888 University Drive, Burnaby, BC V5A 1S6, Canada. 2 Department of Earth, Ocean and Atmospheric Sciences, 2207 Main Mall, University of British Columbia, Vancouver, BC V6T 1Z4, Canada. 3 Department of Geosciences, University of Calgary, 2500 University Drive NW, Calgary, AB T2N 1N4, Canada. 4 Department of Physics, University of Alberta, Edmonton, AB T6G 2E9, Canada.
    [Show full text]
  • Deep-Water Turbidites As Holocene Earthquake Proxies: the Cascadia Subduction Zone and Northern San Andreas Fault Systems
    University of New Hampshire University of New Hampshire Scholars' Repository Faculty Publications 10-1-2003 Deep-water turbidites as Holocene earthquake proxies: the Cascadia subduction zone and Northern San Andreas Fault systems Chris Goldfinger Oregon State University C. Hans Nelson Universidad de Granada Joel E. Johnson University of New Hampshire, Durham, [email protected] Follow this and additional works at: https://scholars.unh.edu/faculty_pubs Recommended Citation Goldfinger, C. Nelson, C.H., and Johnson, J.E., 2003, Deep-Water Turbidites as Holocene Earthquake Proxies: The Cascadia Subduction Zone and Northern San Andreas Fault Systems. Annals of Geophysics, 46(5), 1169-1194. http://dx.doi.org/10.4401%2Fag-3452 This Article is brought to you for free and open access by University of New Hampshire Scholars' Repository. It has been accepted for inclusion in Faculty Publications by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. ANNALS OF GEOPHYSICS, VOL. 46, N. 5, October 2003 Deep-water turbidites as Holocene earthquake proxies: the Cascadia subduction zone and Northern San Andreas Fault systems Chris Goldfinger (1),C. Hans Nelson (2) (*), Joel E. Johnson (1)and the Shipboard Scientific Party (1) College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon, U.S.A. (2) Department of Oceanography, Texas A & M University, College Station, Texas, U.S.A. Abstract New stratigraphic evidence from the Cascadia margin demonstrates that 13 earthquakes ruptured the margin from Vancouver Island to at least the California border following the catastrophic eruption of Mount Mazama. These 13 events have occurred with an average repeat time of ¾ 600 years since the first post-Mazama event ¾ 7500 years ago.
    [Show full text]
  • New Stratigraphic Evidence from the Cascadia Margin Demonstrates That
    Agency: U. S. Geological Survey Award Number: 03HQGR0059 Project Title: Holocene Seismicity of the Northern San Andreas Fault Based on Precise Dating of the Turbidite Event Record. Collaborative Research with Oregon State University and Granada University. End Date: 12/31/2003 Final Technical Report Keywords: Paleoseismology Recurrence interval Rupture characteristics Age Dating Principle Investigators: Chris Goldfinger College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon 97331; email: [email protected] C. Hans Nelson Now at Instituto Andaluz de Ciencias de la Tierra, CSIC, Universidad de Granada, Campus de Fuente Nueva s/n ,Granada,18071 Graduate Student: Joel E. Johnson College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon 97331; email: [email protected] Northern San Andreas Seismotectonic Setting The San Andreas Fault is probably the best-known transform system in the world. Extending along the west cost of North America, from the Salton Sea to Cape Mendocino, it is the largest component of a complex and wide plate boundary that extends eastward to encompass numerous other strike-slip fault strands and interactions with the Basin and Range extensional province. The Mendocino Triple junction lies at the termination of the northern San Andreas, and has migrated northward since about 25-28 Ma. As the triple junction moves, the former subduction forearc transitions to right lateral transform motion. West of the Sierra Nevada block, three main fault systems accommodate ~75% of the Pacific-North America plate motion, distributed over a 100 km wide zone (Argus and Gordon, 1991). The remainder is carried by the Eastern California Shear Zone (Argus and Gordon, 1991; Sauber, 1994).
    [Show full text]
  • Policing Priorities Affecting Enforcement of City Noise Limit
    JUNE 2019 POLICING PRIORITIES AFFECTING ENF ORCEMENT OF CITY NOISE LIMIT By Judy Pickens Last summer, the City Council was finally able to pass a vehicle-exhaust noise ordinance - legislation that Fauntleroy and other neighborhoods had been seeking for some time. Police officers can now issue a $135 citation to drivers for muffler and engine noise that’s clearly audible by a person of normal hearing at a distance of 75 feet or more from the vehicle. Because of our ferry traffic, FCA worked with Councilwoman Lisa Herbold to add Fauntleroy to the list of neighborhoods where vehicle noise was affecting public PLANNING STARTS WITH LOOK safety and health. Forty-three percent of residents responding to FCA’s 2018 community survey mentioned AT ‘REASONABLE’ ALTERNATIVES vehicle noise as an issue. The ordinance requires the Seattle Police Department By Frank Immel to report quarterly on the location, demographics, and As outlined in Washington State Ferries’ long-range disposition of noise citations. In her first report, issued in plan, work on the “SR160/Fauntleroy Terminal - Trestle April, Chief Carmen Best emphasized that the and Transfer Span department’s initial focus was on training officers and Replacement Project” is issuing warnings. Enforcement over the winter was also under way. scant because of tasks associated with closure of the An engineering firm has Alaskan Way viaduct and the need to shift some traffic- started preliminary design enforcement resources to patrols. and environmental Best noted that training had to factor in state law assessment. This work will prohibiting officers from targeting motorcyclists without a include identifying and legal basis.
    [Show full text]
  • Western Limits of the Seattle Fault Zone and Its Interaction with the Olympic Peninsula, Washington
    Western limits of the Seattle fault zone and its interaction with the Olympic Peninsula, Washington A.P. Lamb1, L.M. Liberty1, R.J. Blakely2, T.L. Pratt3, B.L. Sherrod3, and K. van Wijk1 1Department of Geosciences, Boise State University, 1910 University Drive, Boise, Idaho 83725, USA 2U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025, USA 3U.S. Geological Survey, School of Oceanography, Box 357940, University of Washington, Seattle, Washington 98195, USA ABSTRACT INTRODUCTION preted north-dipping backthrusts that are in part beneath the Seattle metropolitan area (Fig. 1). We present evidence that the Seattle fault Oblique subduction of the Juan de Fuca plate The shallow portion of this fault zone is com- zone of Washington State extends to the west beneath the North American continent results in posed of a monocline that bounds the southern edge of the Puget Lowland and is kinemati- northeast migration of coastal regions of Wash- margin of the Seattle Basin, and mapped faults cally linked to active faults that border the ington State relative to stable North America. and folds in the hanging wall just south of the Olympic Massif, including the Saddle Moun- This northeast motion is resisted by Mesozoic monocline. The Seattle fault zone may extend tain deformation zone. Newly acquired high- and older rocks that form the stable craton of to the east beyond the boundaries of the Seattle resolution seismic reflection and marine southwest Canada, resulting in shortening Basin to merge with the active South Whidbey magnetic data suggest that the Seattle fault of the Puget Lowland region of Washington Island fault (Fig.
    [Show full text]
  • Cascadia Subduction Zone Earthquake Scenario
    CCaassccaaddiiaa SSuubbdduuccttiioonn ZZoonnee EEaarrtthhqquuaakkeess:: AA MMaaggnniittuuddee 99..00 EEaarrtthhqquuaakkee SScceennaarriioo Update, 2013 Cascadia Region Earthquake Workgroup Also available as Washington Division of Geology and Earth Resources Information Circular 116, Oregon Department of Geology and Mineral Industries Open-File Report 0-13-22, and British Columbia Geological Survey Information Circular 2013-3 Cascadia Region Earthquake Workgroup (CREW) CREW is a non-profit coalition of business people, emergency managers, scientists, engineers, civic leaders, and government officials who are working together to reduce the effects of earthquakes in the Pacific Northwest. Executive Board President: John Schelling, Washington Emergency Management Division Vice President: Michael Kubler, Emergency Management, Providence Health & Services, Portland, OR Past President: Cale Ash, Degenkolb Engineers Secretary: Teron Moore, Emergency Management, British Columbia Treasurer: Timothy Walsh, State of Washington Department of Natural Resources Executive Director: Heidi Kandathil Board of Directors Steven Bibby, Security and Emergency Services, BC Housing Josh Bruce, Oregon Partnership for Disaster Resilience Kathryn Forge, Public Safety Canada Jere High, Oregon State Public Health Division Andre LeDuc, University of Oregon Charlie Macaulay, Global Risk Consultants Ines Pearce, Pearce Global Partners Althea Rizzo, Oregon Emergency Management Bill Steele, University of Washington, Pacific Northwest Seismic Network Yumei Wang, Oregon Department of Geology and Mineral Industries Supporting members Tamra Biasco, FEMA, Region X Craig Weaver, U.S. Geological Survey Joan Gomberg, U.S. Geological Survey Nate Wood, U.S. Geological Survey Acknowledgments CREW would like to thank Tamra Biasco and Joan Gomberg for overseeing the development of this updated edition of Cascadia Subduction Zone Earthquakes: A Magnitude 9.0 Earthquake Scenario. We would also like to thank everyone who shared information and materials or contributed their time and expertise to this project.
    [Show full text]
  • Preliminary Estimates of Future Earthquake Losses
    Earthquake damage in Oregon: Preliminary estimates of future earthquake losses Cascadia Subduction lone earthquake model: Least dangerous areas are yellow, most dangerous are darkest red. 500 year recurrence interval model (including many earth quakes): Least dangerous areas are yellow, most dangerous are darkest red. - l Special Paper 29 by Yumei Wang and J. L. Clark Oregon Department of Geology and Mineral Industries 1999 Oregon Department of Geology and Mineral Industries Special Papers, JSSN 0278-3703 PUblished in conformance with ORS 516.030 This report is a summay of a more complete description of a Deportment of Geology and Minerallndus1ries study. Open-File Report 0-98-3, which contains details about vaious types of acceleration and ground motion and is targeted to scientific and engineering users. as well as emergency planners. For copies of these publications or other information about Oregon's geology and natural resources. contact: Nature of the Northwest Information Center 800 NE Oegon Street #5 Portland. Oegon 972':!2. (503) 872-275) http:/ /www.naturenw.org SPECIAL PAPER 29 EARTHQUAKE DAMAGE IN OREGON: Preliminary estimates of future earthquake losses by Yumei Wang and J.L Clark Oregon Department of Geology and Mineral Industries 1999 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES Donald A. Hull. State Geologist Table of Contents Executive summary ................... ... ......................................................... ............... ............ ......... 1 Introduction ................. .. .......
    [Show full text]