An Introduction to Technical Issues in the Evaluation of Seismic Hazards for Earthquake-Resistant Design by WALTER W
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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. -
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. -
Preliminary 2021 National Seismic Hazard Model for Hawaii
Preliminary 2021 National Seismic Hazard Model for Hawaii M. Petersen, A. Shumway, P. Powers, M. Moschetti, A. Llenos, A. Michael, C. Mueller, D. McNamara, A. Frankel, P. Okubo, Y. Zeng, S. Rezaeian, K. Jaiswal, J. Altekruse, S. Ahdi, and K. Rukstales USGS Update of the Hawaii Seismic Hazard Model Workshop #2 Virtual Workshop (Microsoft Teams) – November 18, 2020 U.S. Department of the Interior These data are preliminary or provisional and are subject to revision. They are being provided to meet the need for U.S. Geological Survey timely best science. The data have not received final approval by the U.S. Geological Survey (USGS) and are provided Geologic Hazard Science Center (Golden, CO) on the condition that neither the USGS nor the U.S. Government shall be held liable for any damages resulting from the authorized or unauthorized use of the data ■ USGS https://earthquake.usgs.gov/hazards/ sciencefor a changingworld Microsoft Teams Control Bar • When not speaking, please mute your microphone (or please do not be offended if the moderator does it for you!) • When not speaking, please turn off your camera. This also helps save bandwidth, which can help with picture and audio quality issues. • If you have a question, please "raise your hand" or type your question or comment into the meeting chat. Click on the hand when you are done to "unraise your hand". ■ • Troubleshooting: Try leaving and re-entering the meeting. Share your screen Web App Desktop App 00 - co L.....J8 r;ni_,J ••• ■ ◄ ~I [_+Jt ,_ leave v See participants ~USGS USGS Update -
Engineering Geology in Washington, Volume I Washington Diviaion of Geology and Euth Resources Bulletin 78
ENGINEERING GEOLOGY IN WASHINGTON Volume I RICHARD W. GALSTER, Chairman Centennial Volume Committee Washington State Section, Association of Engineering Geologists WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES BULLETIN 78 1989 Prepared in cooperation with the Washington State Section of the A~ociation or Engineering Geologists ''WNatural ASHINGTON STATE Resources DEPARTMENT OF Brian Boyle • Commlssloner 01 Public Lands Ari Stearns - Sup,,rvuor Division of Geology and Earth Resources Raymond LcumanJs. Slate Geologist The use of brand or trade names in this publication is for pur poses of identification only and does not constitute endorsement by the Washington Division of Geology and Earth Resources or the Association of Engineering Geologists. This report is for sale (as the set of two volumes only) by: Publications Washington Department of Natural Resources Division of Geology and Earth Resources Mail Stop PY-12 Olympia, WA 98504 Price $ 27.83 Tax 2.17 Total $ 30.00 Mail orders must be prepaid; please add $1.00 to each order for postage and handling. Make checks or money orders payable to the Department of Natural Resources. This publication is printed on acid-free paper. Printed in the United States of America. ii VOLUME I DEDICATION . ................ .. .. ...... ............ .......................... X FOREWORD ........... .. ............ ................... ..... ................. xii LIST OF AUTHORS ............................................................. xiv INTRODUCTION Engineering Geology in Washington: Introduction Richard W. Galster, Howard A. Coombs, and Howard H. Waldron ................... 3 PART I: ENGINEERING GEOLOGY AND ITS PRACTICE IN WASHINGTON Geologic Factors Affecting Engineered Facilities Richard W. Galster, Chapter Editor Geologic Factors Affecting Engineered Facilities: Introduction Richard W. Galster ................. ... ...................................... 17 Geotechnical Properties of Geologic Materials Jon W. Koloski, Sigmund D. Schwarz, and Donald W. -
The Field Act and Its Effectiveness in Reducing Earthquake Damage
State of California Alfred E. Alquist Seismic Safety Commission The Field Act and its Relative Effectiveness in Reducing Earthquake Damage in California Public Schools Appendices October 2009 1755 Creekside Oaks Drive, #100 Sacramento, California 95833 (916) 263-5506 www.seismic.ca.gov CSSC 09-02 i Table of Contents Page Appendix A: Synopsis of Research Methodology 1 Appendix B: Major 20th Century California Earthquakes 4 Appendix C: Counties that were Affected by California Earthquakes 5 Appendix D: School Sites that Experienced MMI VII or Greater Ground Shaking 6 Appendix E: Mapping of School Sites on Google Earth and Google Maps 18 Appendix F: History of Significant Building Code Changes 21 Appendix G: Comparison of Administrative Requirements of the Uniform 34 Building Code and the Field Act Appendix H: Performance of Field Act Structures as Compared to Non-Field 35 Act Structures in Significant California Earthquakes Since 1933 Appendix I: Description of the Modified Mercalli Intensity (MMI) Scale 45 Appendix J: ATC-20 Building Rating System 47 Appendix K: Significant U.S. Earthquakes Since 1933 Outside California 48 Appendix L: American Red Cross Designated Shelters in 23 California Counties 53 Appendix M: Bibliography of Literature Related to the Field Act 54 References 55 ii Appendix A: Synopsis of Research Methodology The objective of this study was to determine if the Field Act has been effective in reducing structural damage in public school buildings, including community colleges, as compared to comparable buildings constructed to non-Field Act standards. This effort was based on literature that has already been published; no primary data collection was intended to be part of this study. -
Database of Potential Sources for Earthquakes Larger Than Magnitude 6 in Northern California
U. S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY DATABASE OF POTENTIAL SOURCES FOR EARTHQUAKES LARGER THAN MAGNITUDE 6 IN NORTHERN CALIFORNIA By The Working Group on Northern California Earthquake Potential Open-File Report 96-705 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American stratigraphic code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1996 Working Group on Northern California Earthquake Potential William Bakun U.S. Geological Survey Edward Bortugno California Office of Emergency Services William Bryant California Division of Mines & Geology Gary Carver Humboldt State University Kevin Coppersmith Geomatrix N. T. Hall Geomatrix James Hengesh Dames & Moore Angela Jayko U.S. Geological Survey Keith Kelson William Lettis Associates Kenneth Lajoie U.S. Geological Survey William R. Lettis William Lettis Associates James Lienkaemper* U.S. Geological Survey Michael Lisowski Hawaiian Volcano Observatory Patricia McCrory U.S. Geological Survey Mark Murray Stanford University David Oppenheimer U.S. Geological Survey William D. Page Pacific Gas & Electric Co. Mark Petersen California Division of Mines & Geology Carol S. Prentice U.S. Geological Survey William Prescott U.S. Geological Survey Thomas Sawyer William Lettis Associates David P. Schwartz* U.S. Geological Survey Jeff Unruh William Lettis Associates Dave Wagner California Division of Mines & Geology -
Seismic Intensities of Earthquakes of Conterminous United States Their Prediction and Interpretation
Seismic Intensities of Earthquakes of Conterminous United States Their Prediction and InterpretationJL Seismic Intensities of Earthquakes of Conterminous United States Their Prediction and Interpretation By J. F. EVERNDEN, W. M. KOHLER, and G. D. CLOW GEOLOGICAL SURVEY PROFESSIONAL PAPER 1223 Description of a model for computing intensity patterns for earthquakes. Demonstration and explanation of systematic variations of attenuation and earthquake parameters throughout the conterminous United States UNITED STATES GOVERNMENT PRINTING OFFICE, WASH INGTON: 1981 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Doyle G. Frederick, Acting Director Library of Congress catalog-card No. 81-600089 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract ___________________________ ___ 1 Examples of observed predicted intensities Con. Introduction __ ____________________ 1 Seattle earthquake of April 13, 1949 ____________ 23 Rossi-Forel intensities versus Modified Mercalli intensities __ 2 Lompoc earthquake of November 4, 1927 __________ 27 Presently available models for predicting seismic intensities __ 3 Earthquakes of Eastern United States _ _______ _ 36 California ___________________________ 3 Fault length versus moment, magnitude, and energy release Conterminous United States _______________ 4 versus k region._______________________ 36 Examples of observed versus predicted intensities____ ___ 7 Crustal calibration as function of region __ -
Building for the Earthquakes of Tomorrow Complying with Executive Order 12699 IS-8.A / February 2006
\ Building for the Earthquakes of Tomorrow Complying with Executive Order 12699 IS-8.A / February 2006 Table of Contents Copyright Permissions ............................................................................................................... iii Background ................................................................................................................................... v Course Goals and Objectives.................................................................................................... vii Unit 1: Course Introduction ....................................................................................................... 1-1 Unit 2: Executive Order 12699 .................................................................................................. 2-1 Unit 3: Earthquake Causes and Characteristics ......................................................................... 3-1 Unit 4: Earthquake Effects ......................................................................................................... 4-1 Unit 5: Protecting Your Community.......................................................................................... 5-1 Unit 6: Evaluating Your Community’s Safety........................................................................... 6-1 Unit 7: Conclusions.................................................................................................................... 7-1 Appendix A: Major Earthquakes in the United States, Mexico, and Canada, 1700-2004 ....... A-1 Appendix B: -
Significant Earthquakes Experienced in Washington Since 1872 Note: Top 6 Earthquakes with Greatest Impacts Are Preceded by ** and Underlined
Significant Earthquakes Experienced in Washington Since 1872 Note: Top 6 earthquakes with greatest impacts are preceded by ** and underlined 1800s **December 14, 1872 Washington State Earthquake The earthquake is the largest historical earthquake in eastern Washington, and the most widely felt earthquake in the state. The magnitude of the shallow earthquake, centered around Lake Chelan, WA, is debated. It was an estimated M 6.5 to M 7.5, with a moment intensity (MI) of 6.8. The maximum modified Mercalli intensity was IX. It was felt over 390,000 mi2. Landslides and groundwater disturbances occurred near the lake and along the Columbia River, and a fissure split in the ground south of Seattle. Damages included chimney cracks and shattered windows. People were knocked off their feet at Snoqualmie Pass, and trees toppled. The failed Spencer Canyon fault was discovered long after the earthquake. Sources: https://assets.pnsn.org/HIST_CAT/SSA01274.pdf https://web.archive.org/web/20160101023203/https://www.seattletimes.com/seattle- news/scientists-may-be-cracking-mystery-of-big-1872-earthquake/ http://www.burkemuseum.org/static/earthquakes/cur-history.html December 12, 1880 Earthquake The earthquake originating near Kent, WA has no recorded magnitude, but was felt from Victoria to Portland. It had a maximum modified Mercalli intensity of VII. Shaking caused ringing of bells, chimney damage. Source: https://assets.pnsn.org/CASCAT2006/Index_152_216.html April 30, 1882 Earthquake Originating in the Puget Sound - Salish Sea area, the deep earthquake was estimated to be M 5.75 to M 6.2. Modified Mercalli intensity reported in Olympia was VI. -
Normalized Earthquake Damage and Fatalities in the United States: 1900–2005
Normalized Earthquake Damage and Fatalities in the United States: 1900–2005 Kevin Vranes1 and Roger Pielke Jr.2 Abstract: Damage estimates from 80 U.S. earthquakes since 1900 are “normalized” to 2005 dollars by adjusting for inflation, increases in wealth, and changes in population. Factors accounting for mitigation at 1 and 2% loss reduction per year are also considered. The earthquake damage record is incomplete, perhaps by up to 25% of total events that cause damage, but all of the most damaging events are accounted for. For events with damage estimates, cumulative normalized losses since 1900 total $453 billion, or $235 billion and $143 billion when 1 and 2% mitigation is factored, respectively. The 1906 San Francisco earthquake and fire adjusts to $39–$328 billion depending on assumptions and mitigation factors used, likely the most costly natural disaster in U.S. history in normalized 2005 values. Since 1900, 13 events would have caused $1 billion or more in losses had they occurred in 2005; five events adjust to more than $10 billion in damages. Annual average losses range from $1.3 billion to $5.7 billion with an average across data sets and calculation methods of $2.5 billion, below catastrophe model estimates and estimates of average annual losses from hurricanes. Fatalities are adjusted for population increase and mitigation, with five events causing over 100 fatalities when mitigation is not considered, four ͑three͒ events when 1% ͑2%͒ mitigation is considered. Fatalities in the 1906 San Francisco event adjusts from 3,000 to over 24,000, or 8,900 ͑3,300͒ if 1% ͑2%͒ mitigation is considered. -
Earthquakes in Hawaii: What You Need to Know
Earthquakes in Hawaii: What you need to know U.S. Department of the Interior Prepared by: Janet L. Babb U.S. Geological Survey Hawaiian Volcano Observatory The State of Hawaii experiences thousands of earthquakes every year. Most of these earthquakes are closely related to volcanic processes in Hawaii, and are so small they can be detected only by seismometers. 03-06 00:00 12:00 More than 500 earthquakes were recorded by a nearby seismometer during the Kamoamoa fissure eruption Hawaii Standard Time along Kīlauea’s East Rift Zone on March 6, 2011. 23:30 0 + Minutes 30 Many earthquakes are strong enough to be felt on one or more islands. Locations of the 481 magnitude-3.0 and stronger earthquakes that were recorded during 2005–2015. Color and size of dots reflect earthquake magnitude: 3 4 5 6 7 M a g n i t u d e Source: USGS Hawaiian Volcano Observatory Some earthquakes are large enough to cause damage and impact residents across the State of Hawaii. Since 1868, more than 30 magnitude-6.0 or greater earthquakes have rattled the islands. Source: USGS Fact Sheet 2011-3013 (http://pubs.usgs.gov/fs/2011/3013) Two ways to measure or describe earthquakes: Magnitude and Intensity Magnitude Measures the amount of seismic energy released during an earthquake. A unit increase in magnitude corresponds to a ~ 30-fold increase in released energy. Compared to a M-3.0 earthquake… • a M-4.0 earthquake releases ~ 30 times more energy! • a M-5.0 earthquake releases ~ 1,000 times more energy!! • a M-6.0 earthquake releases ~ 30,000 times more energy!!! • a M-7.0 earthquake releases ~ 1,000,000 times more energy!!!! Intensity Describes what people experience during an earthquake— the effects of shaking on structures and the extent of damage. -
EERI / SEAOH / UH Compilation of Reports on the October 15, 2006
Compilation of Observations of the October 15, 2006 Kiholo Bay (Mw 6. 7) and Mahukona (Mw 6.0) Earthquakes, Hawai‘i December 31, 2006 Kalahikiola Church in Hawi, North Kohala, Island of Hawai‘i Contributors Gary Chock (Contributor and Editor) Troy Kindred Ian Robertson Gen Iinuma Peter Nicholson Ernest Lau Horst Brandes Afaq Sarwar Edward Medley John Dal Pino Paul Okubo William Holmes Barry Hirshorn Structural Engineers Association of Hawaii Jiro Sumada Hawaii State Earthquake Advisory Committee Acknowledgements This report was compiled by EERI member Gary Chock of Martin & Chock, Inc., Honolulu, Hawai`i for the Earthquake Engineering Research Institute and the Structural Engineers Association of Hawaii as part of the initial reconnaissance after the earthquake. He drew on his own observations as well as information from, and materials prepared by a number of other professionals: Ian Robertson, Peter Nicholson, and Horst Brandes, of the University of Hawai`i at Manoa; Edward Medley, the Geo-Engineering Earthquake Reconnaissance Association; Paul Okubo, the Hawaiian Volcano Observatory; Barry Hirshorn, the Pacific Tsunami Warning Center; Jiro Sumada, the County of Hawaii Department of Public Works; Troy Kindred, Hawaii County Civil Defense Agency; Gen IInuma, Maui County Civil Defense Agency, Ernest Lau, State of Hawaii Department of Accounting and General Services; Afaq Sarwar, Sarwar Structural Engineering, John Dal Pino, Albert Chen, William Grogan, Lisbeth Blaisdell, Degenkolb Engineers; and William Holmes, Rutherford & Chekene and EERI Learning from Earthquakes Program Committee chair. A number or organizations were also involved in the post-earthquake reconnaissance: ATC-20 building safety engineers from the Structural Engineers Association of Hawaii – Bennett Fung, Clifford Lau, Kylie Yamatsuka, Ron Iwamoto, Gary Suzuki, Glenn Miyasato, Ian Robertson, Jeffrey Hanyu, James Walifish, Lee Takushi, Michael Kasamoto, Steven Heywood, Timothy Waite, Myles Shimokawa, and Randy Chu; the Hawaii State Earthquake Advisory Committee of State Civil Defense; and the U.S.