Earthquake and Tsunami Information and Resources for Schools Surviving Great Waves of Destruction
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New Constraints on Coseismic Slip During Southern Cascadia Subduction Zone Earthquakes Over the Past 4600 Years Implied by Tsunami Deposits and Marine Turbidites
W&M ScholarWorks VIMS Articles Virginia Institute of Marine Science 2018 New constraints on coseismic slip during southern Cascadia subduction zone earthquakes over the past 4600 years implied by tsunami deposits and marine turbidites GR Priest RC Witter Yinglong J. Zhang Virginia Institute of Marine Science C Goldfinger KL Wang See next page for additional authors Follow this and additional works at: https://scholarworks.wm.edu/vimsarticles Part of the Aquaculture and Fisheries Commons Recommended Citation Priest, GR; Witter, RC; Zhang, Yinglong J.; Goldfinger, C; Wang, KL; and Allen, JC, "New constraints on coseismic slip during southern Cascadia subduction zone earthquakes over the past 4600 years implied by tsunami deposits and marine turbidites" (2018). VIMS Articles. 734. https://scholarworks.wm.edu/vimsarticles/734 This Article is brought to you for free and open access by the Virginia Institute of Marine Science at W&M ScholarWorks. It has been accepted for inclusion in VIMS Articles by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. Authors GR Priest, RC Witter, Yinglong J. Zhang, C Goldfinger, KL Wang, and JC Allen This article is available at W&M ScholarWorks: https://scholarworks.wm.edu/vimsarticles/734 Nat Hazards (2017) 88:285–313 DOI 10.1007/s11069-017-2864-9 ORIGINAL PAPER New constraints on coseismic slip during southern Cascadia subduction zone earthquakes over the past 4600 years implied by tsunami deposits and marine turbidites 1 2 3 George R. Priest • Robert C. Witter • Yinglong J. Zhang • 4 5 1 Chris Goldfinger • Kelin Wang • Jonathan C. Allan Received: 24 August 2016 / Accepted: 8 April 2017 / Published online: 29 April 2017 Ó Springer Science+Business Media Dordrecht (outside the USA) 2017 Abstract Forecasting earthquake and tsunami hazards along the southern Cascadia sub- duction zone is complicated by uncertainties in the amount of megathrust fault slip during past ruptures. -
The Mw 8.8 Chile Earthquake of February 27, 2010
EERI Special Earthquake Report — June 2010 Learning from Earthquakes The Mw 8.8 Chile Earthquake of February 27, 2010 From March 6th to April 13th, 2010, mated to have experienced intensity ies of the gap, overlapping extensive a team organized by EERI investi- VII or stronger shaking, about 72% zones already ruptured in 1985 and gated the effects of the Chile earth- of the total population of the country, 1960. In the first month following the quake. The team was assisted lo- including five of Chile’s ten largest main shock, there were 1300 after- cally by professors and students of cities (USGS PAGER). shocks of Mw 4 or greater, with 19 in the Pontificia Universidad Católi- the range Mw 6.0-6.9. As of May 2010, the number of con- ca de Chile, the Universidad de firmed deaths stood at 521, with 56 Chile, and the Universidad Técni- persons still missing (Ministry of In- Tectonic Setting and ca Federico Santa María. GEER terior, 2010). The earthquake and Geologic Aspects (Geo-engineering Extreme Events tsunami destroyed over 81,000 dwell- Reconnaissance) contributed geo- South-central Chile is a seismically ing units and caused major damage to sciences, geology, and geotechni- active area with a convergence of another 109,000 (Ministry of Housing cal engineering findings. The Tech- nearly 70 mm/yr, almost twice that and Urban Development, 2010). Ac- nical Council on Lifeline Earthquake of the Cascadia subduction zone. cording to unconfirmed estimates, 50 Engineering (TCLEE) contributed a Large-magnitude earthquakes multi-story reinforced concrete build- report based on its reconnaissance struck along the 1500 km-long ings were severely damaged, and of April 10-17. -
Earthquake Myths
EARTHQUAKE MYTHS FICTION: California will fall into the ocean. FACT: The ocean is not a great hole into which California can fall, but it is itself land at a somewhat lower elevation with water above it. It’s absolutely impossible that California will be swept out to sea. Instead, southwestern California is moving horizontally northward towards Alaska as it slides past central and eastern California. The dividing point is the San Andreas fault system, which extends from the Salton Sea in the south to Cape Mendocino in the north. This 800 mile long fault is the boundary between the Pacific Plate and North American Plate. The Pacific Plate is moving to the northwest with respect to the North American Plate at approximately two inches per year (the rate your fingernails grow). At this rate, Los Angeles and San Francisco will one day (about 15 million years from now) be next-door neighbors, and in an additional 70 million years, Los Angeles residents will find themselves with an Alaska zip code! FACT VS. FICTION FICTION: It’s been raining a lot, or very hot--it must be earthquake weather! FACT: Many people believe that earthquakes are more common in certain kinds of weather. In fact, no correlation with weather has been found. Earthquakes begin many kilometers (miles) below the region affected by surface weather. People tend to notice earthquakes that fit the pattern and forget the ones that FICTION: During an earthquake you should head for the don't. doorway. FICTION: My house will be swallowed up during an FACT: That’s outdated advice. -
Global Navigation Satellite System Enhancement for Tsunami Early
1 Global Navigation Satellite System Enhancement for Tsunami Early Warning Systems Editors: John LaBrecque, Center for Space Research University of Texas Austin, Texas USA John Rundle, Earth and Planetary Science Department University California Davis, California, USA Gerald Bawden, Earth Surface and Interior Focus Area Science Mission Directorate, NASA Washington, DC USA 2 Click on Highlighted Text Below to View Agenda and Proceedings of the GTEWS 2017 Workshop • Motivation and Support GTEWS Clip: • GTEWS Development History GEONET Captures the Tohoku-oki Earthquake & • GTEWS: Tsunami Early Warning Technology Tsunami • GTEWS Requirements • Prototype GTEWS Networks • Workshop Findings and Recommendations • Bibliography 3 Motivation and Support With little to no warning more than 230,000 lives were lost to the Great Indian Ocean Tsunami of December 26, 2004 (Figure 1). The lack of warning was attributed to several failures including the absence of a proper tsunami Figure 1: Tourists become aware of the first of six tsunami waves at Hat Rai Lay Beach, near Krabi in southern Thailand, December 26, 2004. (GettyImages) warning system for the Indian Ocean as well as inadequate sensing technology and analysis systems for large earthquakes and the resulting tsunamis. The devastating loss of life focused the efforts of scientists, engineers and politicians to establish the Indian Ocean Tsunami Warning System and improve the sensor networks for more accurate and rapid estimates of tsunami potential. A combined network of seismic and geodetic sensors quickly emerged as an accurate, efficient, and cost-effective enhancement to tsunami early warning systems for those communities nearest the earthquake epicenter. Geophysicists demonstrated the potential value of the regional network of the Global Positioning System (GPS) receivers of the Global Geodetic Observing System (GGOS) in providing rapid and accurate tsunami warning and tracking. -
A Review of Geological Records of Large Tsunamis at Vancouver Island, British Columbia, and Implications for Hazard John J
Quaternary Science Reviews 19 (2000) 849}863 A review of geological records of large tsunamis at Vancouver Island, British Columbia, and implications for hazard John J. Clague! " *, Peter T. Bobrowsky#, Ian Hutchinson$ !Depatment of Earth Sciences and Institute for Quaternary Research, Simon Fraser University, Burnaby, BC, Canada V5A 1S6 "Geological Survey of Canada, 101 - 605 Robson St., Vancouver, BC, Canada V6B 5J3 #Geological Survey Branch, P.O. Box 9320, Stn Prov Govt, Victoria, BC, Canada V8W 9N3 $Department of Geography and Institute for Quaternary Research, Simon Fraser University, Burnaby, Canada BC V5A 1S6 Abstract Large tsunamis strike the British Columbia coast an average of once every several hundred years. Some of the tsunamis, including one from Alaska in 1964, are the result of distant great earthquakes. Most, however, are triggered by earthquakes at the Cascadia subduction zone, which extends along the Paci"c coast from Vancouver Island to northern California. Evidence of these tsunamis has been found in tidal marshes and low-elevation coastal lakes on western Vancouver Island. The tsunamis deposited sheets of sand and gravel now preserved in sequences of peat and mud. These sheets commonly contain marine fossils, and they thin and "ne landward, consistent with deposition by landward surges of water. They occur in low-energy settings where other possible depositional processes, such as stream #ooding and storm surges, can be ruled out. The most recent large tsunami generated by an earthquake at the Cascadia subduction zone has been dated in Washington and Japan to AD 1700. The spatial distribution of the deposits of the 1700 tsunami, together with theoretical numerical modelling, indicate wave run-ups of up to 5 m asl along the outer coast of Vancouver Island and up to 15}20 m asl at the heads of some inlets. -
Earthquake Weather: Where Grief and Memory Collide
EARTHQUAKE WEATHER: WHERE GRIEF AND MEMORY COLLIDE ELLA H. This work explores the relationship between grief and memory in my own life. In my research, I looked into earthquakes and compared the geological change that they cause to personal change in my life as a result of loss. To me, earthquakes feel like an appropriate metaphor for loss because, while they are destructive, they shape our world. Their unpredictability also mirrors the unpredictability of loss. As a San Franciscan, I’ve been taught to be prepared for disaster, even though we don’t know exactly when it will strike. During my sophomore year of high-school, my best friend died after a year and a half long battle with cancer. Within the last month of her life, I knew that she was close to death, although I didn’t know when it would happen. In my art, I aimed to create a piece to represent some of my memories of her, while also expressing the instability of not knowing when loss would occur. My art focuses on a specific memory that took place in my best friend’s old backyard. I recently returned there and sat on her rope-swing from our childhood. Although the yard was empty, I could clearly picture younger versions of ourselves, as well as other various memories associated with the place. I recreated the swing to physically recreate my present perspective; I intend for the swing to create a sense of instability for the viewer. I painted clouds in oil on a large-scale canvas and collaged charcoal drawings that represent memories from the backyard onto it. -
Engineering Geology and Seismology for Public Schools and Hospitals in California
The Resources Agency California Geological Survey Michael Chrisman, Secretary for Resources Dr. John G. Parrish, State Geologist Engineering Geology and Seismology for Public Schools and Hospitals in California to accompany California Geological Survey Note 48 Checklist by Robert H. Sydnor, Senior Engineering Geologist California Geological Survey www.conservation.ca.gov/cgs July 1, 2005 316 pages Engineering Geology and Seismology performance–based analysis, diligent subsurface for Public Schools and Hospitals sampling, careful reading of the extensive geologic in California literature, thorough knowledge of the California Building Code, combined with competent professional geological work. by Robert H. Sydnor Engineering geology aspects of hospital and public California Geological Survey school sites include: regional geology, regional fault July 1, 2005 316 pages maps, site-specific geologic mapping, geologic cross- sections, active faulting, official zones of investigation Abstract for liquefaction and landslides, geotechnical laboratory The 446+ hospitals, 1,400+ skilled nursing facilities testing of samples, expansive soils, soluble sulfate ±9,221 public schools, and 109 community college evaluation for Type II or V Portland-cement selection, campuses in California are regulated under California and flooding. Code of Regulations, Title 24, California Building Code. Seismology aspects include: evaluation of historic These facilities are plan–checked by senior–level seismicity, probabilistic seismic hazard analysis of Registered Structural Engineers within the Office of earthquake ground–motion, use of proper code terms Statewide Health Planning and Development (OSHPD) (Upper–Bound Earthquake ground–motion and Design– for hospitals and skilled nursing facilities, and the Basis ground–motion), classification of the geologic Division of the State Architect (DSA) for public schools, subgrade by shear–wave velocity to select the correct community colleges, and essential services buildings. -
Canada's Earthquakes
Document generated on 09/26/2021 12:45 p.m. Geoscience Canada Canada’s Earthquakes: ‘The Good, the Bad, and the Ugly’ J. F. Cassidy, G. C. Rogers, M. Lamontagne, S. Halchuk and J. Adams Volume 37, Number 1, January 2010 Article abstract Much of Canada is ‘earthquake country’. Tiny earthquakes (that can only be URI: https://id.erudit.org/iderudit/geocan37_1art01 recorded by seismographs) happen every day. On average, earthquakes large enough to be felt occur every week in Canada, damaging earthquakes are years See table of contents to decades apart, and some of the world’s largest earthquakes are typically separated by intervals of centuries. In this article, we provide details on the most significant earthquakes that have been recorded in, or near, Canada, Publisher(s) including where and when they occurred, how they were felt, and the effects of those earthquakes. We also provide a brief review of how earthquakes are The Geological Association of Canada monitored across Canada and some recent earthquake hazard research. It is the results of this monitoring and research, which provide knowledge on ISSN earthquake hazard, that are incorporated into the National Building Code of Canada. This, in turn, will contribute to reduced property losses from future 0315-0941 (print) earthquakes across Canada. 1911-4850 (digital) Explore this journal Cite this article Cassidy, J. F., Rogers, G. C., Lamontagne, M., Halchuk, S. & Adams, J. (2010). Canada’s Earthquakes:: ‘The Good, the Bad, and the Ugly’. Geoscience Canada, 37(1), 1–16. All rights reserved © The Geological Association of Canada, 2010 This document is protected by copyright law. -
California North Coast Offshore Wind Studies
California North Coast Offshore Wind Studies Overview of Geological Hazards This report was prepared by Mark A. Hemphill-Haley, Eileen Hemphill-Haley, and Wyeth Wunderlich of the Humboldt State University Department of Geology. It is part of the California North Coast Offshore Wind Studies collection, edited by Mark Severy, Zachary Alva, Gregory Chapman, Maia Cheli, Tanya Garcia, Christina Ortega, Nicole Salas, Amin Younes, James Zoellick, & Arne Jacobson, and published by the Schatz Energy Research Center in September 2020. The series is available online at schatzcenter.org/wind/ Schatz Energy Research Center Humboldt State University Arcata, CA 95521 | (707) 826-4345 California North Coast Offshore Wind Studies Disclaimer This study was prepared under contract with Humboldt State University Sponsored Programs Foundation with financial support from the Department of Defense, Office of Economic Adjustment. The content reflects the views of the Humboldt State University Sponsored Programs Foundation and does not necessarily reflect the views of the Department of Defense, Office of Economic Adjustment. This report was created under Grant Agreement Number: OPR19100 About the Schatz Energy Research Center The Schatz Energy Research Center at Humboldt State University advances clean and renewable energy. Our projects aim to reduce climate change and pollution while increasing energy access and resilience. Our work is collaborative and multidisciplinary, and we are grateful to the many partners who together make our efforts possible. Learn more about our work at schatzcenter.org Rights and Permissions The material in this work is subject to copyright. Please cite as follows: Hemphill-Haley, M.A., Hemphill-Haley, E. and Wunderlich, W. (2020). -
Folklore and Earthquakes: Native American Oral Traditions from Cascadia Compared with Written Traditions from Japan
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/249551808 Folklore and earthquakes: Native American oral traditions from Cascadia compared with written traditions from Japan Article in Geological Society London Special Publications · January 2007 DOI: 10.1144/GSL.SP.2007.273.01.07 CITATIONS READS 20 5,081 12 authors, including: R. S. Ludwin Deborah Carver University of Washington Seattle University of Alaska Anchorage 18 PUBLICATIONS 261 CITATIONS 2 PUBLICATIONS 95 CITATIONS SEE PROFILE SEE PROFILE Robert J. Losey Coll Thrush University of Alberta University of British Columbia - Vancouver 103 PUBLICATIONS 1,174 CITATIONS 20 PUBLICATIONS 137 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Cheekye Fan - Squamish Floodplain Interactions View project Peace River area radiocarbon database View project All content following this page was uploaded by John J. Clague on 07 June 2016. The user has requested enhancement of the downloaded file. Downloaded from http://sp.lyellcollection.org/ at Simon Fraser University on June 6, 2016 Folklore and earthquakes: Native American oral traditions from Cascadia compared with written traditions from Japan RUTH S. LUDWIN 1 & GREGORY J. SMITS 2 IDepartment of Earth and Space Sciences, University of Washington, Box 351310, Seattle, WA 98195-1310, USA (e-mail: [email protected]) 2Department of Histoo' and Program in Religious Studies, 108 Weaver Building, The Pennsylvania State UniversiO', Universio' Park, PA 16802, USA With Contributions from D. CARVER 3, K. JAMES 4, C. JONIENTZ-TRISLER 5, A. D. MCMILLAN 6, R. LOSEY 7, R. -
Earthquake Safety
S P E C I A L E D I T I O N Planning and Preparing for a a publication of the City of Palm Desert Major Earthquake As the staggering magnitude of the Special Edition Gulf Coast hurricane disasters unfold, Palm Desert residents probably Fall 2005 wonder “Will we be prepared if a major disaster happens here?” By reviewing this special issue of the BrightSide, you are taking the What’s Inside first step in being prepared. This information will assist you in getting Planning for an as prepared as possible for a major earthquake and to let you know that Earthquake preparation must be an ongoing photo credit: Arthur Coleman process. The City of Palm Desert, our San Andreas Fault After the Quake neighboring cities, Riverside County, and California be self-sufficient before the big quake strikes and making have spent much time and money preparing for sure your supplies are accessible in the days that Survival Supplies a disaster. follow. However, there are limitations of what can be done Please review the checklists and tips to help you. The best source of help will be yourself. It included in this publication. Be creative and add Business Emergency is extremely important to realize you may need to be your own ideas. If you have not started planning and Planning self-sufficient for one, two, or more days. The only way preparing, please start today. Earthquakes are not like to be truly self-sufficient is hurricanes. They strike without warning and can happen Local Emergency Teams to take two main actions any time of the day or night. -
Fragility Functions of Manufactured Houses Under Earthquake Loads
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Civil and Environmental Engineering Theses, Dissertations, and Student Research Civil and Environmental Engineering 7-2021 Fragility Functions of Manufactured Houses under Earthquake Loads Shuyah Tani Aurore Ouoba University of Nebraska-Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/civilengdiss Part of the Civil Engineering Commons, Other Civil and Environmental Engineering Commons, and the Structural Engineering Commons Ouoba, Shuyah Tani Aurore, "Fragility Functions of Manufactured Houses under Earthquake Loads" (2021). Civil and Environmental Engineering Theses, Dissertations, and Student Research. 170. https://digitalcommons.unl.edu/civilengdiss/170 This Article is brought to you for free and open access by the Civil and Environmental Engineering at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Civil and Environmental Engineering Theses, Dissertations, and Student Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. FRAGILITY FUNCTIONS OF MANUFACTURED HOUSES UNDER EARTHQUAKE LOADS by Shuyah T. A. Ouoba A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For the Degree of Master of Science Major: Civil Engineering Under the Supervision of Professor Christine E. Wittich Lincoln, Nebraska July, 2021 FRAGILITY FUNCTIONS OF MANUFACTURED HOUSES UNDER EARTHQUAKE LOADS Shuyah T. A. Ouoba, M.S University of Nebraska, 2021 Advisor: Christine E. Wittich Manufactured homes are factory-built homes made of wooden structural members, then transported and installed on a given site. Manufactured housing is used in many countries, such as in Australia, and in New Zealand but remain mostly popular in the United States.