The Kumamoto Earthquake Investigation: a Preliminary Report
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19-20 March, 2018 Kobe, Japan Agenda Book Ver.2.0
#6 CHIKYU IODP BOARD MEETING 19-20 March, 2018 Kobe, Japan Agenda book Ver.2.0 #6 CIB Meeting Agenda Book ver.2 revision summary as of 16 March 2018 Agenda Item Sub Item Action taken Material 2 Revision List of Participants 2 Insertion Wireless LAN connection information 3 Revision Draft Agenda ver.1.5 6 Insertion CIB message to Riser proposal lead proponents 7 e Insertion MEXT Report 9 a Revision Overall Chikyu Operation 11 a Insertion Proposal 866-Full2_Strasser cover sheet 15 Revision Safety Review Committee Update 16 a Revision Main Points of JFY2017 Review Agenda Item 1 Welcome Remarks Agenda Item 2 Introductions and Logistics Welcome and meeting logistics 1)Meeting Logistics 2)List of Participants 3)Emergency Escape Route Chikyu IODP Board #6 Meeting Logistics 19-20 March 2018 Kobe, JAPAN MEETING DATES & TIMES: Monday, 19 March 09:00 - 17:30 Tuesday, 20 March 09:00 - 17:30 MEETING LOCATION: Chikyu IODP Board (CIB) will be held at the Takigawa Memorial Hall, Rokkodai Campus, Kobe University Access: http://www.kobe-u.ac.jp/en/campuslife/campus_guide/campus/rokkodai2.html SOCIAL EVENT: *Details to be announced later. 1) Field Trip: Sunday, 18 March 08:30- : Nojima Fault Preservation Museum 2) Ice breaker: Sunday, 18 March 19:00-21:00: TBD Not an official event 3) Reception: Monday, 19 March 18:30-20:30: ANA CROWNE PLAZA KOBE Lavender (9th floor of the Hotel) http://www.anacrowneplaza-kobe.jp/en/banquet/space/medium/ Free of charge RECOMMENDED HOTEL AND LODGING RESERVATIONS (Important Deadline Information): There is a block of rooms at “ANA CROWNE PLAZA KOBE” at a rate of ¥15,120 per night for 18, 19, 21 March, and ¥23,760 per night for 17, 20 March. -
Veourstofa Islands Report
VeOurstofa islands Report BarOi ~orkelsson (editor) The second EU-Japan workshop on seismie risk Destructive earthquakes: Understanding crustal proeesses leading to destructive earthquakes Reykjavik, Iceland, June 23-27, 1999 Vi-G99012..JA04 Reykjavik June 1999 r Vedurstofa Islands Report Baråi ~orkelsson (editor) The second EU-Japan workshop on seismie risk Destructive earthquakes: Understanding crustal proeesses leading to destructive earthquakes Reykjavik, Iceland, June 23-27, 1999 Vf-G99012-JA04 Reykjavik June 1999 THE SECOND EU-JAPAN WORKSHOP ON SEISMIC RISK DESTRUCTIVE EARTHQUAKES: Understanding Crustal Proeesses Leading to Destructive Earthquakes Reykjavfk, Iceland, June 23-27, 1999 Supported by: European Commission OG XII Organized by: Icelandic Meteorological Office Programme Abstracts List of participants Organizing committee: I I~,--------------------- Dr. R. Stefansson (Icelandic Meteorological Office), chairman Mr. B. Porkelsson (Icelandic Meteorological Office) Prof. P. Einarsson (University of Iceland) Scientific and technical advisory committee: Dr. R. Stefansson (Icelandic Meteorological Office) Dr. A. Ghazi (Europan Commission OG XII) Dr. N. Kamaya (Japanese Science and Technology Agency) Mr. R. Burmanjer (European Commission OG XII) Mrs. M. Yeroyanni (European Commission OG XII) Objectives of the workshop I I~,------------------------ The scientific objectives aim to reinforce EU-Japan cooperation in earthquake research. The main contribution of the earth sciences to mitigate seismic risks is to provide better understanding of where, how and when destructive earthquakes will strike. The better the scientists can answer such questions the better will be the basis for mitigating risks. It concerns actions taken by society, engineers, city planners and rescue teams. Multidisciplinary approach is necessary to answer the questions above, involving seismologists, geophysicists and geologists. Multinational approach is necessary for integration of experience and knowhow. -
Earthquake Hazard
SUB-SECTION 4G.2 PUYALLUP TRIBE ALL HAZARD MITIGATION PLAN EARTHQUAKE HAZARD Table of Contents TABLE OF CONTENTS ............................................................................................... 1 IDENTIFICATION DESCRIPTION ................................................................................ 2 DEFINITION ............................................................................................................. 2 TYPES .................................................................................................................... 2 SECONDARY HAZARDS: ................................................................................................ 3 PROFILE ................................................................................................................... 5 LOCATION AND EXTENT ............................................................................................... 5 VULNERABILITY ....................................................................................................... 15 IMPACTS ............................................................................................................... 16 RESOURCE DIRECTORY .......................................................................................... 24 REGIONAL ............................................................................................................. 24 NATIONAL ............................................................................................................. 24 ENDNOTES ............................................................................................................ -
Water Supply Forum Resiliency Project, Water Quality Assessment
Water Supply Forum Regional Water Supply Resiliency Project Water Quality Resiliency Assessment Technical Memorandum Snohomish, King, and Pierce Counties, Washington May 6, 2016 This page is intentionally left blank. Water Quality Resiliency Assessment Contents 1.0 Introduction ............................................................................................................ 1 1.1 Description of Risk ....................................................................................................... 1 1.2 Objectives .................................................................................................................... 1 2.0 Methodology .......................................................................................................... 1 2.1 Multibarrier Approach ................................................................................................... 1 2.2 Risk Event Prioritization ............................................................................................... 3 3.0 Results .................................................................................................................. 4 3.1 Risk Event Prioritization ............................................................................................... 4 3.2 Mitigation Measures ..................................................................................................... 6 4.0 Detailed Review of Risk Events ........................................................................... 11 4.1 Wildfire ........................................................................................................................11 -
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). -
IJURCA: International Journal of Undergraduate Research & Creative Activities
IJURCA: International Journal of Undergraduate Research & Creative Activities Volume 13 Article 6 MAY 17, 2021 Modeling Tsunamis in Washington State and Integrating Universal Design: Incorporating Universal Design into Tsunami Modeling Results for Cascadia Subduction Zone Faults to Create and Inundation and Universal Design Evacuation Map for Washington State Hannah Spero Boise State University, Department of Geosciences, Undergraduate Dr. Breanyn MacInnes Central Washington University, Department of Geology, Research Mentor (Geosciences/GeoClaw) Dr. Naomi Jeffery Petersen Central Washington University, Department of Educational Foundations and Curriculum, Research Mentor (Universal Design) Abstract Current tsunami hazard inundation and evacuation maps in the Puget Sound are based primarily on Cascadia and Seattle fault tsunamis. The standard evaluation process for tsunami impacts focuses on elevation and hypothetical fault rupture of known and predicted earthquakes. However, there are several known tsunami deposits in the Puget Sound that are not from Cascadia or Seattle fault tsunamis, potentially from other faults within the region, that could affect tsunami mitigation. Work to understand newly discovered crustal deformation and faults in Puget Sound is ongoing, therefore evacuation and inundation maps need to be updated to include these new faults and integrate universal design more broadly. Methods involved using GeoClaw software to map tsunamis from the Cascadia Subduction Zone (CSZ), Leech River fault (LRF), and Utsalady Point fault (UPF). Modeled tsunamis determined the overall inundation of Port Angeles, Washington through a wide range of earthquake inputs of magnitude, proximity, and recurrence. The output simulations were evaluated with key components of universal design to create a new tsunami hazard map. Comparison between the universal design-based map to current the tsunami hazard map allowed for an evaluation of the current evacuation map. -
Hanford Sitewide Probabilistic Seismic Hazard Analysis 2014
Hanford Sitewide Probabilistic Seismic Hazard Analysis 2014 Contents 4.0 The Hanford Site Tectonic Setting ............................................................................................... 4.1 4.1 Tectonic Setting.................................................................................................................... 4.1 4.2 Contemporary Plate Motions and Tectonic Stress Regime .................................................. 4.11 4.3 Late Cenozoic and Quaternary History ................................................................................ 4.16 4.3.1 Post-CRB Regional Stratigraphy ............................................................................... 4.17 4.3.2 Summary of Late Miocene, Pliocene and Quaternary History .................................. 4.19 4.4 Seismicity in the Hanford Site Region ................................................................................. 4.21 4.4.1 Crustal Seismicity ..................................................................................................... 4.21 4.4.2 Cascadia Subduction Zone Seismicity ...................................................................... 4.26 4.5 References ............................................................................................................................ 4.28 4.i 2014 Hanford Sitewide Probabilistic Seismic Hazard Analysis Figures 4.1 Plate tectonic setting of the Hanford Site .................................................................................... 4.1 4.2 Areal extent -
Geology and Earthquakes in Japan Worksheet Example Answers
Name: ____________________________Example Answers____________________ Date: ______________________ Class: _________________ Geology and Earthquakes in Japan Worksheet Objective: Investigate the geologic conditions that make Japan a frequent location for large- magnitude earthquakes. Materials: Work in pairs sharing one computer with Internet access. Engage: Take a moment to think about what you already know about Japan. 1. Where is it located? Example answers: Japan is an island off the coast of the Asian continent. Japan is located in the Pacific Ocean/ 2. What do you know about the geology of Japan? Students might not know much about the geology, but expect them to know that Japan is an island. Japan also has volcanic activity and an active fault. 3. Have you heard of earthquakes in the Japan area? Possible answers: The 2011 Fukushima earthquake, which caused a tsunami, resulted in a nuclear disaster. Japan has had several other historic earthquakes, including one in 1995. Explore: Navigate to the Earthquakes Living Lab at http://www.teachengineering.org/livinglabs/earthquakes/. 4. Notice the four main focus regions in the Earthquakes Living Lab, each based on one of four historic earthquakes. For this activity, select the third option, the “Japan” box. Then follow the link on the right side of the page: “Why did the earthquake happen at Kobe? What were the short- and long-term effects of the earthquake?” 5. Read the screen information about “Why did the earthquake happen here?” Explain: Record the following information in your journal: 6. Draw a labeled sketch of the plate tectonics present in the Kobe region. Include the name of the fault, crusts and plates. -
OUGS Journal 26(2) © Copyright Reserved Symposium Edition 2005 Email: [email protected] Cover Illustration: Thin Sections of Several Different Habits of Barite
Open University Geological Society Journal Symposium Edition 2005 The Gathering Stirling University 1-3 July 2005 Contents Terrane spotting in the Himalaya 1 Professor Nigel Harris, Open University New light on the Neoproterozoic evolution of the Moine supergroup: an exotic taerrane 5 within the Scottish Caledonides? Dr Rob Strachan, University of Portsmouth Caledonian granite dating, Scottish accretion and the weather 8 Dr Grahame Oliver, University of St Andrews The geology of the Caledonian Foreland and Moine Thrust Belt: new thoughts on old rocks 18 Iain Allison1 & John Mendum2. 1 University of Glasgow, 2 British Geological Survey, Edinburgh The Southern Uplands: new perspectives on an old terrane 25 Dr James D Floyd, British Geological Survey, Edinburgh Tracking Dinosaurs in Scotland 30 Dr Neil D L Clark, Hunterian Museum, University of Glasgow The Caledonian architecture of East Greenland 72°-75°N 36 Dr A Graham Leslie1 & A K Higgins2.1British Geological Survey, Edinburgh 2Geological Survey of Denmark and Greenland, Copenhagen ********* The crater lake lahar hazard on Mount Ruapehu 42 Philip Clark An assessment of the geohazard potential of earthquakes in the Tacoma area of Southern 48 Puget Lowland, Washington State Josephine Brown Book reviews 4, 7, 17, 24, 29, 35, 62 It is the responsibility of authors to obtain the necessary permission to reproduce any copyright material they wish to use in their articles. The views expressed in this Journal are those of the individual author and do not represent those of the Open University Geological Society. In the opinion of the authors the descriptions of venues are accurate at the time of going to press; the Open University Geological Society does not accept responsibility for access, safety considerations or adverse conditions encountered by those visiting the sites. -
Basin Shear-Wave Velocities Beneath Seattle, Washington, from Noise-Correlation Rayleigh Waves by Andrew A
Bulletin of the Seismological Society of America, Vol. 101, No. 5, pp. 2162–2175, October 2011, doi: 10.1785/0120100260 Ⓔ Basin Shear-Wave Velocities beneath Seattle, Washington, from Noise-Correlation Rayleigh Waves by Andrew A. Delorey and John E. Vidale Abstract Tomography with short-period Rayleigh waves, extracted using noise interferometry, can refine S-wave velocity (VS) models in urban areas with dense arrays of short-period and broadband instruments. We apply this technique to the Seattle area to develop a new shallow VS model for use in seismic-hazard assessment. Continuous data from the Seismic Hazards in Puget Sound (SHIPS) array and local broadband stations have interstation distances of 90 km or less. This spacing allows us to extract Rayleigh waves with periods between 2 and 10 s that are sensitive to shallow-basin structure. This new VS model for the Seattle basin is constructed using direct observations rather than using P-wave velocity (VP) observations and a VP=VS ratio as all previous 3D models at this scale have been constructed. Our results reveal greater detail in the upper 3.5 km than previous models. Earthquake simulations calculated using our new model better predict peak ground velocities (PGV) at periods between 1 and 2 s for two local earthquakes than the previous model used to calculate Seattle’s seismic-hazard map (Frankel et al., 2007). We collected data from two local earthquakes and ran finite-difference simulations using our new velocity model as well as the previous velocity model used in devel- opment of the Seattle seismic-hazard maps to assess how well our model predicts ground motions relative to the previous model. -
Puget Sound Tsunami Sources—2002 Workshop Report
PugetPuget SoundSound TsunamiTsunami SourcesSources 20022002 WorkshopWorkshop ReportReport A JointJoint SpecialSpecial ReportReport National Oceanic and Atmospheric Administration United States Geological Survey Washington State Department of Natural Resources Washington State Military Department Emergency Management Division On the cover: Puget Sound has a history of tsunamis that includes water waves generated by this landslide at the Tacoma Narrows. The slide occurred three days after the magnitude-7.1 Olympia earthquake of April 13, 1949. It generated a tsunami that reflected off the opposite shore and propagated back to the coast on which the landslide occurred. NOAA OAR Special Report Puget Sound Tsunami Sources—2002 Workshop Report A contribution to the Inundation Mapping Project of the U.S. National Tsunami Hazard Mitigation Program Workshop Report Committee: Frank I. Gonz´alez, compiler, with contributions from Brian L. Sherrod, Brian F. Atwater, Arthur P. Frankel, Stephen P. Palmer, Mark L. Holmes, Robert E. Karlin, Bruce E. Jaffe, Vasily V. Titov, Harold O. Mofjeld, and Angie J. Venturato Sponsored by: National Oceanic and Atmospheric Administration U.S. Geological Survey Washington State Department of Natural Resources Washington State Military Department Emergency Management Division Workshop Organizing Committee: G. Crawford, F. Gonz´alez (Chair), M. Holmes, H. Mofjeld, B. Sherrod, V. Titov, A. Venturato, T. Walsh, C. Weaver June 2003 Contribution 2526 from NOAA/Pacific Marine Environmental Laboratory NOTICE Mention of a commercial company or product does not constitute an endorsement by NOAA/OAR. Use of information from this publication concerning proprietary products or the tests of such products for publicity or advertising purposes is not authorized. Contribution No. 2526 from NOAA/Pacific Marine Environmental Laboratory For sale by the National Technical Information Service, 5285 Port Royal Road Springfield, VA 22161 ii Contents iii Contents PugetSoundTsunamiSourcesWorkshopHistory........ -
Earthquake Hazards Program Coordinator U.S
Proceedings of the 7th U.S. / Japan Natural Resources (UJNR) Panel on Earthquake Research Compiled by Shane T. Detweiler and William L. Ellsworth Open-File Report 2008-1335 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia 2008 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Detweiler, Shane T., and Ellsworth, William L., 2008, Compilers, Proceedings of the 7th U.S. / Japan Natural Resources (UJNR) Panel on Earthquake Research: U.S. Geological Survey Open-File Report 2008-1335, 99 p. [http://pubs.usgs.gov/of/2008/1335/]. The abstracts in this volume are published as they were submitted. Abstracts authored entirely by non-USGS authors do not represent the views or position of the U.S. Geological Survey or the U.S. government and are published solely as part of the Proceedings volume. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Proceedings of the 7th U.S.