Prepared by Participants in October 1987 This Report Is Preliminary And
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The Race to Seismic Safety Protecting California’S Transportation System
THE RACE TO SEISMIC SAFETY PROTECTING CALIFORNIA’S TRANSPORTATION SYSTEM Submitted to the Director, California Department of Transportation by the Caltrans Seismic Advisory Board Joseph Penzien, Chairman December 2003 The Board of Inquiry has identified three essential challenges that must be addressed by the citizens of California, if they expect a future adequately safe from earthquakes: 1. Ensure that earthquake risks posed by new construction are acceptable. 2. Identify and correct unacceptable seismic safety conditions in existing structures. 3. Develop and implement actions that foster the rapid, effective, and economic response to and recovery from damaging earthquakes. Competing Against Time Governor’s Board of Inquiry on the 1989 Loma Prieta Earthquake It is the policy of the State of California that seismic safety shall be given priority consideration in the allo- cation of resources for transportation construction projects, and in the design and construction of all state structures, including transportation structures and public buildings. Governor George Deukmejian Executive Order D-86-90, June 2, 1990 The safety of every Californian, as well as the economy of our state, dictates that our highway system be seismically sound. That is why I have assigned top priority to seismic retrofit projects ahead of all other highway spending. Governor Pete Wilson Remarks on opening of the repaired Santa Monica Freeway damaged in the 1994 Northridge earthquake, April 11, 1994 The Seismic Advisory Board believes that the issues of seismic safety and performance of the state’s bridges require Legislative direction that is not subject to administrative change. The risk is not in doubt. Engineering, common sense, and knowledge from prior earthquakes tells us that the consequences of the 1989 and 1994 earthquakes, as devastating as they were, were small when compared to what is likely when a large earthquake strikes directly under an urban area, not at its periphery. -
Recent Movements of the Juan De Fuca Plate System
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 89, NO. B8, PAGES 6980-6994, AUGUST 10, 1984 Recent Movements of the Juan de Fuca Plate System ROBIN RIDDIHOUGH! Earth PhysicsBranch, Pacific GeoscienceCentre, Departmentof Energy, Mines and Resources Sidney,British Columbia Analysis of the magnetic anomalies of the Juan de Fuca plate system allows instantaneouspoles of rotation relative to the Pacific plate to be calculatedfrom 7 Ma to the present.By combiningthese with global solutions for Pacific/America and "absolute" (relative to hot spot) motions, a plate motion sequencecan be constructed.This sequenceshows that both absolute motions and motions relative to America are characterizedby slower velocitieswhere younger and more buoyant material enters the convergencezone: "pivoting subduction."The resistanceprovided by the youngestportion of the Juan de Fuca plate apparently resulted in its detachmentat 4 Ma as the independentExplorer plate. In relation to the hot spot framework, this plate almost immediately began to rotate clockwisearound a pole close to itself such that its translational movement into the mantle virtually ceased.After 4 Ma the remainder of the Juan de Fuca plate adjusted its motion in responseto the fact that the youngest material entering the subductionzone was now to the south. Differencesin seismicityand recent uplift betweennorthern and southernVancouver Island may reflect a distinction in tectonicstyle betweenthe "normal" subductionof the Juan de Fuca plate to the south and a complex "underplating"occurring as the Explorer plate is overriddenby the continent.The history of the Explorer plate may exemplifythe conditionsunder which the self-drivingforces of small subductingplates are overcomeby the influenceof larger, adjacent plates. The recent rapid migration of the absolutepole of rotation of the Juan de Fuca plate toward the plate suggeststhat it, too, may be nearingthis condition. -
Seismicity Remotely Triggered by the Magnitude 7.3 Landers, California, Earthquake Author(S): D
Seismicity Remotely Triggered by the Magnitude 7.3 Landers, California, Earthquake Author(s): D. P. Hill, P. A. Reasenberg, A. Michael, W. J. Arabaz, G. Beroza, D. Brumbaugh, J. N. Brune, R. Castro, S. Davis, D. dePolo, W. L. Ellsworth, J. Gomberg, S. Harmsen, L. House, S. M. Jackson, M. J. S. Johnston, L. Jones, R. Keller, S. Malone, L. Munguia, S. Nava, J. C. Pechmann, A. Sanford, R. W. Simpson, R. B. Smith, M. Stark, M. Stickney, A. Vidal, S. Walter, V. Wong and J. Zollweg Source: Science, New Series, Vol. 260, No. 5114 (Jun. 11, 1993), pp. 1617-1623 Published by: American Association for the Advancement of Science Stable URL: http://www.jstor.org/stable/2881709 . Accessed: 28/10/2013 21:58 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. American Association for the Advancement of Science is collaborating with JSTOR to digitize, preserve and extend access to Science. http://www.jstor.org This content downloaded from 128.95.104.66 on Mon, 28 Oct 2013 21:58:06 PM All use subject to JSTOR Terms and Conditions ............................................---.----..;- Rv'>'E S5'5.' EA ; a ar"T I_Cl E few tens of kilometersor less of the induc- Seismicity Remotely Triggered by ing source (4). -
Seismic Resilience Report Is Located on the Seismic Resilience Sharepoint Site
REPORT SEISMIC RESILIENCE FIRST BIENNIAL REPORT The Metropolitan Water District of Southern California 700 N. Alameda Street, Los Angeles, California 90012 Report No. 1551 February 2018 The Metropolitan Water District of Southern California Seismic Resilience First Biennial Report SEISMIC RESILIENCE FIRST BIENNIAL REPORT Prepared By: The Metropolitan Water District of Southern California 700 North Alameda Street Los Angeles, California 90012 Report Number 1551 February 2018 Report No. 1551 – February 2018 iii The Metropolitan Water District of Southern California Seismic Resilience First Biennial Report Copyright © 2018 by The Metropolitan Water District of Southern California. The information provided herein is for the convenience and use of employees of The Metropolitan Water District of Southern California (MWD) and its member agencies. All publication and reproduction rights are reserved. No part of this publication may be reproduced or used in any form or by any means without written permission from The Metropolitan Water District of Southern California. Any use of the information by any entity other than Metropolitan is at such entity's own risk, and Metropolitan assumes no liability for such use. Prepared under the direction of: Gordon Johnson Chief Engineer Prepared by: Robb Bell Engineering Services Don Bentley Water Resource Management Winston Chai Engineering Services David Clark Engineering Services Greg de Lamare Engineering Services Ray DeWinter Administrative Services Edgar Fandialan Water Resource Management Ricardo Hernandez -
United States Department of the Interior Geological Survey
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY NATIONAL EARTHQUAKE HAZARDS REDUCTION PROGRAM, SUMMARIES OF TECHNICAL REPORTS VOLUME XXIII Prepared by Participants in NATIONAL EARTHQUAKE HAZARDS REDUCTION PROGRAM October 1986 OPEN-FILE REPORT 87-63 This report is preliminary and has not been reviewed for conformity with U.S.Geological Survey editorial standards Any use of trade name is for descriptive purposes only and does not imply endorsement by the USGS. Menlo Park, California 1986 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY NATIONAL EARTHQUAKE HAZARDS REDUCTION PROGRAM, SUMMARIES OF TECHNICAL REPORTS VOLUME XXIII Prepared by Participants in NATIONAL EARTHQUAKE HAZARDS REDUCTION PROGRAM Compiled by Muriel L. Jacobson Thelma R. Rodriguez The research results described in the following summaries were submitted by the investigators on May 16, 1986 and cover the 6-months period from May 1, 1986 through October 31, 1986. These reports include both work performed under contracts administered by the Geological Survey and work by members of the Geological Survey. The report summaries are grouped into the three major elements of the National Earthquake Hazards Reduction Program. Open File Report No. 87-63 This report has not been reviewed for conformity with USGS editorial standards and stratigraphic nomenclature. Parts of it were prepared under contract to the U.S. Geological Survey and the opinions and conclusions expressed herein do not necessarily represent those of the USGS. Any use of trade names is for descriptive purposes only and does not imply endorsement by the USGS. The data and interpretations in these progress reports may be reevaluated by the investigators upon completion of the research. -
And Induced Seismicity
UNITED STATES DEPARTMENT OF THE INTERIOR " GEOLOGICAL SURVEY SUMMARIES OF TECHNICAL REPORTS, VOLUME XIII Prepared by Participants in NATIONAL EARTHQUAKE HAZARDS REDUCTION PROGRAM Compiled by Barbara B. Charonnat External Research Program Thelma R. Rodriguez Earthquake Prediction Wanda H. Seiders Earthquake Hazards and Risk Assessment Global Seismology and Induced Seismicity The research results described in the following summaries were submitted by the investigators on November 30, 1981 and cover the 6-month period from April 1, 1981 through October 31, 1981. These reports include both work performed under contracts administered by the Geological Survey and work by members of the Geological Survey. The report summaries are grouped into the four major elements of the National Earthquake Hazards Reduction Program: Earthquake Hazards and Risk Assessment (H) Robert D. Brown, Jr., Coordinator U.S. Geological Survey 345 Middlefield Road, MS-77 Menlo Park, California 94025 Earthquake Prediction (P) James H. Dieterich, Coordinator U.S. Geological Survey 345 Middlefield Road, MS-77 Menlo Park, California 94025 Global Seismology (G) Eric R. Engdahl, Coordinator U.S. Geological Survey Denver Federal Center, MS-967 Denver, Colorado 80225 Induced Seismicity (IS) Mark D. Zoback, Coordinator U.S. Geological Survey 345 Middlefield Road, MS-77 Menlo Park, California 94025 Open File Report No. 82-6£ This report has not been reviewed for conformity with USGS editorial standards and stratigraphic nomenclature. Parts of it were prepared under contract to the U.S. Geological Survey and the opinions and conclusions expressed herein do not necessarily represent those of the USGS. Any use of trade names is for descriptive purposes only and does not imply endorsement by the USGS. -
Explanatory Text to Accompany the Fault Activity Map of California
An Explanatory Text to Accompany the Fault Activity Map of California Scale 1:750,000 ARNOLD SCHWARZENEGGER, Governor LESTER A. SNOW, Secretary BRIDGETT LUTHER, Director JOHN G. PARRISH, Ph.D., State Geologist STATE OF CALIFORNIA THE NATURAL RESOURCES AGENCY DEPARTMENT OF CONSERVATION CALIFORNIA GEOLOGICAL SURVEY CALIFORNIA GEOLOGICAL SURVEY JOHN G. PARRISH, Ph.D. STATE GEOLOGIST Copyright © 2010 by the California Department of Conservation, California Geological Survey. All rights reserved. No part of this publication may be reproduced without written consent of the California Geological Survey. The Department of Conservation makes no warranties as to the suitability of this product for any given purpose. An Explanatory Text to Accompany the Fault Activity Map of California Scale 1:750,000 Compilation and Interpretation by CHARLES W. JENNINGS and WILLIAM A. BRYANT Digital Preparation by Milind Patel, Ellen Sander, Jim Thompson, Barbra Wanish, and Milton Fonseca 2010 Suggested citation: Jennings, C.W., and Bryant, W.A., 2010, Fault activity map of California: California Geological Survey Geologic Data Map No. 6, map scale 1:750,000. ARNOLD SCHWARZENEGGER, Governor LESTER A. SNOW, Secretary BRIDGETT LUTHER, Director JOHN G. PARRISH, Ph.D., State Geologist STATE OF CALIFORNIA THE NATURAL RESOURCES AGENCY DEPARTMENT OF CONSERVATION CALIFORNIA GEOLOGICAL SURVEY An Explanatory Text to Accompany the Fault Activity Map of California INTRODUCTION data for states adjacent to California (http://earthquake.usgs.gov/hazards/qfaults/). The The 2010 edition of the FAULT ACTIVTY MAP aligned seismicity and locations of Quaternary OF CALIFORNIA was prepared in recognition of the th volcanoes are not shown on the 2010 Fault Activity 150 Anniversary of the California Geological Map. -
Survey of Strong Motion Earthquake Effects on Thermal Power Plants in California with Emphasis on Piping Systems Main Report
RECEIVED NUREG/CR-6239 DEC 1 4 1995 ORNL/Sub/94-SD427/2/Vl O S TI VoL ! Survey of Strong Motion Earthquake Effects on Thermal Power Plants in California with Emphasis on Piping Systems Main Report Prepared by J. D. Stevenson Oak Ridge National Laboratory Prepared for U.S. Nuclear Regulatory Commission r ' , \ la DISTRIBUTION OF THIS DOCUMENT IS UNLIMITED AVAILABILITY NOTICE Availability of Reference Matenals Cited in NRC Publications Most documents cited In NRC publications will be available from one of the following sources: 1. The NRC Public Document Room, 2120 L Street, NW , Lower Level. Washington, DC 20555-0001 2. The Superintendent of Documents, U. S Government Printing Office, P. O. Box 37082, Washington, DC 20402-9328 3. The National Technical Information Service, Springfield, VA 22161-0002 Although the listing that follows represents the majority of documents cited in NRC publications, it is not in• tended to be exhaustive. Referenced documents available for inspection and copying for a fee from the NRC Public Document Room include NRC correspondence and internal NRC memoranda, NRC bulletins, circulars, information notices, in• spection and investigation notices, licensee event reports, vendor reports and correspondence; Commission papers; and applicant and licensee documents and correspondence The following documents in the NUREG series are available for purchase from the Government Printing Office: formal NRC staff and contractor reports, NRC-sponsored conference proceedings, international agreement reports, grantee reports, -
San Andreas Fault and Coastal Geology from Half Moon Bay to Fort Funston: Crustal Motion, Climate Change, and Human Activity David W
Field SanTrip Andreas4 Fault and Coastal Geology from Half Moon Bay to Fort Funston: Crustal Motion, Climate Change, and Human Activity San Andreas Fault and Coastal Geology from Half Moon Bay to Fort Funston: Crustal Motion, Climate Change, and Human Activity David W. Andersen Department of Geology, San José State University, Calif. Andrei M. Sarna-Wojcicki U.S. Geological Survey, Menlo Park, Calif. Richard L. Sedlock Department of Geology, San José State University, Calif. Introduction The geology of the San Francisco Peninsula reflects many processes operating at time scales ranging from hundreds of millions of years to a fraction of a human lifetime. We can attribute today’s landscape in the San Francisco Bay area to three major processes, each operating at its own pace, but each interacting with the others and with subsidiary processes: (1) the slow, long-term motion of the North American tectonic plate as it moves relative to the northwest-moving Pacific Plate, and the smaller but important component of crustal compression between the two plates; (2) the more rapid changes in global climate during the last few million years, which have controlled the rise and fall of sea level and the succession of flora and fauna on land and along the coast; and (3) the very recent, explosive growth of human population and its related activity, as expressed in pervasive ecological impact and urbanization. The oldest rocks in the region formed nearly 170 Ma (million years ago) under conditions very different from those in the San Francisco Bay area today, and rocks that were formed far apart have been juxtaposed during their later history. -
FEMA P-530, Earthquake Safety at Home (March 2020)
Earthquake Safety at Home FEMA P-530 / March 2020 This page intentionally left blank. Earthquake Safety at Home FEMA P-530 Earthquake Safety at Home Prepared by APPLIED TECHNOLOGY COUNCIL 201 Redwood Shores Parkway, Suite 240 Redwood City, California 94065 www.ATCouncil.org Prepared for FEDERAL EMERGENCY MANAGEMENT AGENCY Michael Mahoney, Project Officer Andrew Herseth, Project Manager Washington, D.C. ATC MANAGEMENT AND OVERSIGHT Jon A. Heintz, Program Executive, Program Manager Ayse Hortacsu, Project Manager Veronica Cedillos, Project Manager Zahraa Saiyed, Project Management Consultant Project Technical Committee Colin Blaney (Project Technical Director) Michael Griffin Buehler Structural Engineers, Inc. CCS Group, Inc. Kelly E. Cobeen Lucy Jones Wiss Janney Elstner Associates, Inc. Dr. Lucy Jones Center for Science and Society Project Review Panel Mark Benthien Fred Turner Southern California Earthquake Center Alfred E. Alquist Seismic Safety Commission Graphics Consultants Christopher Mills Christina Zagara Christopher Mills Illustration Creative Engagement Solutions, LLC Carol Singer Carol Singer Design Earthquake Safety at Home FEMA P-530 ACKNOWLEDGEMENTS FEMA 530 was originally developed and published by the California Seismic Safety Commission. This document also benefited greatly from the USGS publication, Putting Down Roots in Earthquake Country, originally written by Lucy Jones and Mark Benthien. NOTICE Any opinions, findings, conclusions, or recommendations expressed in this publication do not necessarily reflect the views of the Applied Technology Council (ATC), the Department of Homeland Security (DHS), or the Federal Emergency Management Agency (FEMA). Additionally, neither ATC, DHS, FEMA, nor any of their employees, makes any warranty, expressed or implied, nor assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, product, or process included in this publication. -
Stratigraphic and Diagenetic Comparisons of the Monterey Formation, Point Reyes and Monterey Areas, California
STRATIGRAPHIC AND DIAGENETIC COMPARISONS OF THE MONTEREY FORMATION, POINT REYES AND MONTEREY AREAS, CALIFORNIA A Thesis submitted to the faculty of San Francisco State University In partial fulfillment of The requirements for The Degree AS m Master of Science C,E0L In . ^ 5 Geosciences by Burcin Kelez San Francisco, California May 2016 Copyright by Burcin Kelez 2016 CERTIFICATION OF APPROVAL I certify that I have read Stratigraphic and diagenetic comparisons o f the Monterey Formation, Point Reyes and Monterey Areas, California by Burcin Kelez, and that in my opinion this work meets the criteria for approving a thesis submitted in partial fulfillment of the requirements for the degree: Master of Science in Geosciences at San Francisco State University. u X aaA i ; Lisa White, Ph.D. Adjunct Professor Thomas MacKinnon, Ph.D. Geologist, retired Chevron STRATIGRAPHIC AND DIAGENETIC COMPARISONS OF THE MONTEREY FORMATION, POINT REYES AND MONTEREY AREAS, CALIFORNIA Burcin Kelez San Francisco, California 2016 The Miocene Monterey Formation is a deep marine deposit characterized by a high content of biogenic silica and organic matter. The biogenic silica is derived mainly from diatoms. Rock types include diatomaceous rocks and their diagenetic equivalents- chert, porcelanite and siliceous mudstone. The Monterey Formation is the source and reservoir rock for most of the oil and gas resources in California. Although the Monterey Formation in many other places in California is composed of three distinctive members, calcareous, phosphatic, and siliceous, the younger siliceous part is the most extensive facies and is the only member well exposed at Point Reyes and the Monterey area. I have examined the stratigraphic and diagenetic features of the sub-members of the siliceous part of the Monterey Formation at two locations: Pt Reyes and the Monterey area. -
Explanitory Text to Accompany the Fault Activity Map of California
An Explanatory Text to Accompany the Fault Activity Map of California Scale 1:750,000 ARNOLD SCHWARZENEGGER, Governor LESTER A. SNOW, Secretary BRIDGETT LUTHER, Director JOHN G. PARRISH, Ph.D., State Geologist STATE OF CALIFORNIA THE NATURAL RESOURCES AGENCY DEPARTMENT OF CONSERVATION CALIFORNIA GEOLOGICAL SURVEY CALIFORNIA GEOLOGICAL SURVEY JOHN G. PARRISH, Ph.D. STATE GEOLOGIST Copyright © 2010 by the California Department of Conservation, California Geological Survey. All rights reserved. No part of this publication may be reproduced without written consent of the California Geological Survey. The Department of Conservation makes no warranties as to the suitability of this product for any given purpose. An Explanatory Text to Accompany the Fault Activity Map of California Scale 1:750,000 Compilation and Interpretation by CHARLES W. JENNINGS and WILLIAM A. BRYANT Digital Preparation by Milind Patel, Ellen Sander, Jim Thompson, Barbra Wanish, and Milton Fonseca 2010 Suggested citation: Jennings, C.W., and Bryant, W.A., 2010, Fault activity map of California: California Geological Survey Geologic Data Map No. 6, map scale 1:750,000. ARNOLD SCHWARZENEGGER, Governor LESTER A. SNOW, Secretary BRIDGETT LUTHER, Director JOHN G. PARRISH, Ph.D., State Geologist STATE OF CALIFORNIA THE NATURAL RESOURCES AGENCY DEPARTMENT OF CONSERVATION CALIFORNIA GEOLOGICAL SURVEY An Explanatory Text to Accompany the Fault Activity Map of California INTRODUCTION data for states adjacent to California (http://earthquake.usgs.gov/hazards/qfaults/). The The 2010 edition of the FAULT ACTIVTY MAP aligned seismicity and locations of Quaternary OF CALIFORNIA was prepared in recognition of the th volcanoes are not shown on the 2010 Fault Activity 150 Anniversary of the California Geological Map.