Southern California Earthquake Center

Total Page:16

File Type:pdf, Size:1020Kb

Southern California Earthquake Center Southern California Earthquake Center Final Technical Report USGS Cooperative Agreement 02HQAG0008 I. Introduction The Southern California Earthquake Center (SCEC) is a regionally focused organization with a tripartite mission to • gather new information about earthquakes in Southern California, • integrate this information into a comprehensive and predictive understanding of earthquake phenomena, and • communicate this understanding to end-users and the general public in order to increase earthquake awareness and reduce earthquake risk. SCEC was founded in 1991 as a Science and Technology Center (STC) of the National Science Foundation (NSF), receiving primary funding from NSF’s Earth Science Division and the United States Geological Survey (USGS). SCEC graduated from the STC Program after a full 11-year run (SCEC1). It was reauthorized as a free-standing center on February 1, 2002 (SCEC2) with base funding from NSF and USGS. In addition, the Center was awarded major grants from NSF’s Information Technology Research (ITR) Program and its National Science, Technology, Engineering, and Mathematics Digital Library (NSDL) program. This report highlights the Center’s research activities during the five-year period (2002- 2007), with emphasis on the fifth and final year of SCEC2. The report is organized into the following sections: I. Introduction II. Planning, Organization, and Management of the Center III. Research Accomplishments IV. Communication, Education, and Outreach Activities V. Director’s Management Report VI. Advisory Council Report VII. Financial Report VIII. Report on Subawards and Monitoring IX. Demographics of SCEC Participants X. Report on International Contacts and Visits XI. Publications II. Planning, Organization, and Management of the Center The transition from SCEC1 to SCEC2 involved considerable planning and restructuring. A five-year planning document, The SCEC Strategic Plan 2002-2007, was submitted to the sponsoring agencies in October, 2001. This plan articulated the Center’s long-term research goals. The organization chart of the Center is shown on the next page. SCEC is an institution-based center, governed by a Board of Directors who represent its members. The SCEC membership now comprises 16 core institutions and 40 participating institutions. Board of Directors Under the SCEC2 by-laws, each core institution appoints one board member, and two at- large members are elected by the Board from the participating institutions. The 18 members of the Board are listed in Table II.1. Table II.1. SCEC Board of Directors Institutional and At-Large Representatives Thomas H Jordan* (Chair) University of Southern California Gregory C. Beroza* (Vice-Chair) Stanford University Peter Bird University of California, Los Angeles Emily Brodsky University of California Santa Cruz James N. Brune University of Nevada Reno Douglas Burbank* University of California Santa Barbara Steven M. Day San Diego State University James Dieterich University of California, Riverside Bill Ellsworth USGS-Menlo Park Lisa Grant (At-Large) University of California Irvine Thomas Heaton California Institute of Technology Thomas A. Herring Massachusetts Institute of Technology Lucile Jones* USGS-Pasadena J. Bernard Minster* University of California San Diego James Rice Harvard University Bruce Shaw Columbia University Terry Tullis (At-Large) Brown University Robert Wesson USGS-Golden Ex-Officio Members Ralph Archuleta (Deputy Director), John McRaney* (Executive Secretary), Mark Benthien (Associate Director, CEO), Phil Maechling (IT Architect) * Executive Committee members Ex officio members include the SCEC Deputy Director, Ralph Archuleta; the Associate Director for Administration, John McRaney, who also serves as Executive Secretary to the Board; the Associate Director for Communication, Education and Outreach, Mark Benthien, and the SCEC IT Architect, Phil Maechling. External Advisory Council SCEC’s Advisory Council (AC) is an external group charged with developing an overview of SCEC operations and giving advice to the Director and the Board. Sean Solomon of the Carnegie Institution of Washington continued as Chair of the AC in 2006. The Advisory Council’s second report is reproduced verbatim in Section VI. Organization of Research A central organization within SCEC is the Science Planning Committee (PC), which is chaired by the Deputy Director and Table II.2. Leadership of the SCEC Working has the responsibility for formulating Groups the Center’s science plan, conducting Disciplinary Committees proposal reviews, and recommending Seismology: John Vidale (chair)* projects to the Board for SCEC Peter Shearer (co-chair) funding Geodesy: Duncan Agnew (chair)* The PC membership includes the Mark Simons (co-chair) chairs of the major SCEC working Geology: Mike Oskin (chair)* groups. There are three types of Tom Rockwell (co-chair) working groups—disciplinary Fault & Rock Mechanics: Terry Tullis (chair)* Judi Chester (co-chair) committees, focus groups, and special project groups. The Center is Focus Groups fortunate that some of its most Structural Representation: John Shaw (leader)* energetic and accomplished Jeroen Tromp (co-leader) colleagues participate as group Fault Systems: Brad Hager (leader)* leaders (Table II.2). Jim Dieterich (co-leader) The Center sustains disciplinary Sally McGill (co-leader) science through standing committees Earthquake Source Physics: Ruth Harris (leader)* in seismology, geodesy, geology, and David Oglesby (co- leader) fault and rock mechanics. These Ground Motions: Paul Davis (leader)* committees are responsible for Robert Graves (co-leader) planning and coordinating Seismic Hazard Analysis: Ned Field (leader)* disciplinary activities relevant to the David Jackson (co-leader) SCEC science plan, and they make recommendations to the Science Special Project Groups Planning Committee regarding the Implementation Interface: Paul Somerville (leader)* support of disciplinary infrastructure. Rob Wesson (co-leader) Interdisciplinary research is SCEC/ITR Project: Bernard Minster (liaison)* organized into five science focus Borderland Working Group: Craig Nicholson (chair)* areas: structural representation, fault * Science Planning Committee members systems, earthquake source physics, ground motion, and seismic hazard analysis. The focus groups are the crucibles for the interdisciplinary synthesis that lies at the core of SCEC’s mission. In addition to the disciplinary committees and focus groups, SCEC manages several special research projects, including the Southern California Integrated GPS Network (SCIGN), the Western InSAR Consortium (WInSAR), the Borderland Working Group, and the SCEC Information Technology Research (SCEC/ITR) Project. Each of these groups is represented on the Science Planning Committee by its chair, with the exception of the SCEC/ITR Project, which is represented by Bernard Minster, a Co-P.I. of the project (the P.I. is the Center Director, Tom Jordan). In June, 2005, the SCEC board voted to disband the SCIGN group as a standing committee of SCEC. SCIGN had completed its mission and the future mainteance of continuous GPS site in southern California will be handled by PBO/UNAVCO, the USGS, and the county surveyors. This action was approved by NSF and the USGS. The transition to PBO maintenance will be completed in March, 2008 The Borderland Working Group represents SCEC researchers interested in coordinating studies of the offshore tectonic activity and seismic hazards in California Borderland. This group will be disbanded at the end of SCEC2. The goal of the SCEC/ITR Project is to develop an advanced information infrastructure for system-level earthquake science in Southern California. Partners in this SCEC-led collaboration include the San Diego Supercomputer Center (SDSC), the Information Sciences Institute (ISI), the Incorporated Research Institutions for Seismology (IRIS), and the USGS. In many respects, the SCEC/ITR Project presents a microcosm of the IT infrastructures now being contemplated in the context of EarthScope and other large-scale science initiatives, so the opportunities and pitfalls in this area need to be carefully assessed. The SCEC/ITR annual report has been submitted as a separate document to NSF. A proposal to fund SCEC3 for the period from 2007-2012 was submitted to NSF and USGS in March, 2005. The proposal was approved in 2006 and SCEC continues as SCEC3 under funding for 2007-2012. Communication, Education, and Outreach SCEC is committed to applying the basic research in earthquake science to the practical problems of reducing earthquake losses. To accomplish this aspect of its mission, SCEC maintains a vigorous Communication, Education, and Outreach (CEO) Program that receives 10% of its base funding plus other funds from special projects, such as the Electronic Encyclopedia of Earthquakes. CEO activities are managed by the Associate Director for CEO, Mark Benthien. The programmatic elements include structured activities in education and public outreach and two new structures: an Implementation Interface, designed to foster two-way communication and knowledge transfer between between SCEC scientists and partners from other communities—in particular, earthquake engineering, risk analysis, and emergency management, and a Diversity Task Force, responsible for furthering the goal of gender and ethnic diversity in earthquake science. A report on the third-year CEO activities is given in Section IV. III. Director’s Summary of SCEC2 and Plans for SCEC3 1. Introduction The
Recommended publications
  • Report of Geotechnical Investigation Proposed Improvements
    REPORT OF GEOTECHNICAL INVESTIGATION PROPOSED IMPROVEMENTS PROPOSED RIO HONDO SATELLITE CAMPUS EL RANCHO ADULT SCHOOL 9515 HANEY STREET PICO RIVERA, CALIFORNIA Prepared for: RIO HONDO PROGRAM MANAGEMENT TEAM Whittier, California January 20, 2016 Project 4953-15-0302 January 20, 2016 Mr Luis Rojas Rio Hondo Program Management Team c/o Rio Hondo College 3600 Workman Mill Road Whittier, California 90601-1699 Subject: LETTER OF TRANSMITTAL Report of Geotechnical Investigation Proposed Improvements Proposed Rio Hondo Satellite Campus El Rancho Adult School 9515 Haney Street Pico Rivera, California, 90660 Amec Foster Wheeler Project 4953-15-0302 Dear Mr. Rojas: We are pleased to submit the results of our geotechnical investigation for the proposed improvements as part of the proposed Rio Hondo Satellite Campus at the El Rancho Adult School in Pico Rivera, California. This investigation was performed in general accordance with our proposal dated November 24, 2015, which was authorized by e-mail on December 15, 2015. The scope of our services was planned with Mr. Manuel Jaramillo of DelTerra. We have been furnished with a site plan and a general description of the proposed improvements. The results of our investigation and design recommendations are presented in this report. Please note that you or your representative should submit copies of this report to the appropriate governmental agencies for their review and approval prior to obtaining a permit. Correspondence: Amec Foster Wheeler 6001 Rickenbacker Road Los Angeles, California 90040 USA
    [Show full text]
  • An Elusive Blind-Thrust Fault Beneath Metropolitan Los Angeles
    R EPORTS 5 The intercept of the line with the abscissa yields Di/D 1/4, which is an extreme case, differs only by 36. N. A. Sulpice and R. J. D’Arcy, J. Phys. E 3, 477 (1970). 7% as compared with D 5 0. DV. This geometry-independent constant is i 37. Electrical charging due to the electron beam cannot 31. Microscopy was performed with a Philips CM30 200- account for the effect, because the charge found to characteristic for the specific nanotube under kV high-resolution TEM. reside on the nanotubes is positive rather than neg- investigation and is typically on the order of 32. The ripple mode may be a precursor to buckling, but ative. Furthermore, the amplitude of vibration at several volts. Similarly, attaching nanoscopic it should not be confused with bucking. Buckling (in resonance does not change with electron dose, as it contrast to rippling) is characterized as an instability would if electron beam charging were important. conducting particles to the nanotubes facilitates giving rise to a nonlinear response. It occurs in highly 38. M. Gurgoze, J. Sound Vib. 190, 149 (1996). measurements of their work functions. stressed nanotubes (and beams) and manifests as 39. We thank U. Landman, R. L. Whetten, L. Forro, and A. The methods developed here are also well one or several kinks with very small radii of curvature Zangwill for fruitful discussion and R. Nitsche for his suited to measure masses in the picogram-to- (about 1 to 10 nm). It is accompanied by abrupt analysis of the static bent nanotube.
    [Show full text]
  • UC Santa Cruz UC Santa Cruz Electronic Theses and Dissertations
    UC Santa Cruz UC Santa Cruz Electronic Theses and Dissertations Title Investigations of fault zone behavior during earthquake cycles using hydrology and geodesy Permalink https://escholarship.org/uc/item/90p323z6 Author Xue, Lian Publication Date 2015 Peer reviewed|Thesis/dissertation eScholarship.org Powered by the California Digital Library University of California UNIVERSITY OF CALIFORNIA SANTA CRUZ Investigations of fault zone behavior during earthquake cycles using hydrology and geodesy A dissertation submitted in partial satisfaction of the requirements of the degree of DOCTOR OF PHILOSOPHY in EARTH SCIENCES with an emphasis in GEOPHYSICS by Lian Xue September 2015 The Dissertation of Lian Xue is approved: _________________________________ Professor Emily Brodsky, Chair _________________________________ Professor Susan Schwartz _________________________________ Professor Thorne Lay _________________________________ Professor Andrew Fisher _________________________________ Tyrus Miller Vice Provost and Dean of Graduate Studies Copyright © by Lian Xue All rights reserved Table of Contents List of figures ............................................................................................................. VI Abstract ................................................................................................................... VIII Acknowledgments ...................................................................................................... X Introduction ................................................................................................................
    [Show full text]
  • 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
    [Show full text]
  • The L.A. Earthquake Sourcebook
    THE L.A. EARTHQUAKE SOURCEBOOK Produced by Richard Koshalek and Mariana Amatullo 2/3 Copyright © 2008 Designmatters at Southern California earthquake maps reprinted Art Center College of Design. courtesy of the U. S. Geological Survey. Excerpt from All rights reserved. ISBN 978-0-9618705-0-8 “Los Angeles Days” reprinted with the permission of Simon and Schuster Adult Publishing Group from Design: Sagmeister Inc., NYC After Henry by Joan Didion. Copyright © 1992 by Managing Editor: Gloria Gerace Joan Didion. All rights reserved. Pp. 97–100 from Ask Editor: Alex Carswell The Dust by John Fante. Copyright © 1980 by John Printer: Capital Offset Co. Fante. Reprinted by permission of HarperCollins Publishers. Excerpt from As I Remember by Arnold Genthe. Copyright © 1936 by Reynal & Hitchcock. Reprinted by permission of Ayer Company Publishers. “When Mother Nature Visits Southern California” by David Hernandez, 1998, used by permission of the author. Excerpt from “Assembling California” from Annals of the Former World by John McPhee. Copyright © 1998 by John McPhee. Reprinted by permission of Farrar, Straus and Giroux, LLC. Excerpt from “Folklore of Earthquakes” from Fool’s Paradise: The Carey McWilliams Reader. Reprinted by permission of Harold Ober Associates Incorporated. Copyright © 1933 by Carey McWilliams. First published in American Mercury. “When Living on the Edge Becomes Stark–Naked Reality” originally appeared in the Los Angeles Times. Copyright © 1987 Carolyn See. Used by permission of the author. Excerpt from “The L.A. Quake” © 1994 Lawrence S C C Weschler. Used by permission of the author. The full E essay appeared in the Threepenny Review and is part an NSF+USGS center of Vermeer in Bosnia: Cultural Comedies and Political Tragedies, Pantheon, 2004.
    [Show full text]
  • Abstract the Hazus Challenge
    2016 USEIT: Loss Analysis of Earthquake Sequences Sophia Belvoir1, Vianca Severino2, Jenepher Zamora1, Jadson Silva4, Luis Gomez5, Jozi Pearson6, Mark Benthien6, Thomas Jordan6 1Pasadena City College, 2University of Puerto Rico, Mayagüez, 4University of Brazilia, 5Chaffey College, 6University of Southern California ABSTRACT The 2016 Undergraduate Studies in Earthquake Information Technology (USE-IT) intern research program challenged the Hazard and Risk Visualization Team to illustrate threatening and probable multi-event earthquake scenarios in California using ShakeMaps and risk analysis maps. The interns are implementing FEMA’s Hazards United States (HAZUS) software to estimate and visualize the potential losses including physical damage of infrastructure, economic loss, and social impacts of these mul- ti-earthquake sequences. This is the first time multiple events will be analyzed with HAZUS. As a team based project, USEIT interns depend on collaboration with other working groups within the intern program to identify potential earthquake sequences. The Rate-State earthQuake Simulator (RSQSim) was run on a high performance computer (HPC) to generate catalogs of events. Rupture sequences were then selected to be visualized in SCEC-VDO. Earthquake sequences that were seen as most threatening had ShakeMap files created utilizing seismic hazard analysis (OpenSHA) software. Multiple events were combined as single ShakeMaps and imported into HAZUS for analysis. Ground motion values were combined and calculated in two differ- ent ways for multi-event ShakeMaps: 1) by using the greatest value and 2) sum of the squares, where the maps overlap. The greatest value method proves more appropriate for events that are further apart geographically. The sum of the squares method is ideal for events that are closer together.
    [Show full text]
  • Do Faults Preserve a Record of Seismic Slip: a Second Opinion
    Journal of Structural Geology 78 (2015) 1e26 Contents lists available at ScienceDirect Journal of Structural Geology journal homepage: www.elsevier.com/locate/jsg Review article Do faults preserve a record of seismic slip: A second opinion * Christie D. Rowe a, , W. Ashley Griffith b a Department of Earth & Planetary Sciences, McGill University, 3450 University St., Montreal, QC H3A 0E8, Canada b Department of Earth and Environmental Sciences, University of Texas at Arlington, Box 19049, Arlington, TX 76019, USA article info abstract Article history: Exhumed fault zones offer insights into deformation processes associated with earthquakes in unpar- Received 31 January 2015 alleled spatial resolution; however it can be difficult to differentiate seismic slip from slow or aseismic Received in revised form slip based on evidence in the rock record. Fifteen years ago, Cowan (1999) defined the attributes of 5 June 2015 earthquake slip that might be preserved in the rock record, and he identified pseudotachylyte as the only Accepted 9 June 2015 reliable indicator of past earthquakes found in ancient faults. This assertion was based on models of Available online 12 June 2015 frictional heat production (Sibson, 1975, 1986) providing evidence for fast slip. Significant progress in fault rock studies has revealed a range of reaction products which can be used to detect frictional heating Keywords: Fault rocks at peak temperatures less than the melt temperature of the rock. In addition, features formed under Paleoseismology extreme transient stress conditions associated with the propagating tip of an earthquake rupture can Pseudotachylyte now be recognized in the rock record, and are also uniquely seismic.
    [Show full text]
  • In Memory of Keiiti Aki, 1930–2005
    Ó Birkha¨user Verlag, Basel, 2006 Pure appl. geophys. 163 (2006) 617–618 0033–4553/06/030617–3 Pure and Applied Geophysics DOI 10.1007/s00024-005-0028-4 In Memory of Keiiti Aki, 1930–2005 While editing this volume in honor of Kei Aki, we were greatly saddened to receive the news that he passed away on May 17, 2005, in La Re´union, a French Island in the Indian Ocean. According to Thomas Staudacher, the Director of the Observatoire volcanologique du Piton de la Fournaise, Aki fell in the street coming home from a grocery store on May 13. The next day, he was disoriented and X-rays revealed bleeding in the brain. Aki was sent to the hospital where doctors performed two surgeries to stop the bleeding without success. He fell into a coma, died on May 17, and was buried in the cemetery of the town of Le Tampon on May 18. Keiiti Aki was born on March 3, 1930, in Yokohama, Japan to a family of engineers with a 100-year tradition of education and openness to the west. Various aspects of his family history, upbringing and scientific influences on his career, described by Kei to one of us, are given in the introduction to the 2003 Pageoph Aki Volume. Here we provide complementary details that shed additional light on his life and career. When Aki was 19 years old, he was among the 12 students admitted to the Department of Geophysics of the University of Tokyo. It was a very exciting place with world class professors in both Solid and Fluid Earth, including Chuji Tsuboi, Takeshi Nagata, Takeo Matuzawa, and Koji Hidaka.
    [Show full text]
  • Tectonic Geomorphology of the Santa Ana Mountains
    Final Technical Report ACTIVE DEFORMATION AND EARTHQUAKE POTENTIAL OF THE SOUTHERN LOS ANGELES BASIN, ORANGE COUNTY, CALIFORNIA Award Number: 01HQGR0117 Recipient’s name: University of California - Irvine Sponsored Projects Administration 160 Administration Building, Univ. of CA - Irvine Irvine, CA 92697-1875 Principal investigator: Lisa B. Grant, Ph.D. Department of Environmental Analysis & Design 262 Social Ecology 1 University of California Irvine, CA 92697-7070 Program element: Research on earthquake occurrence and effects Research supported by the U.S. Geological Survey (USGS), Department of the Interior, under USGS award number 01HQGR0117. The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government. p. 1 Award number: 01HQGR0117 ACTIVE DEFORMATION AND EARTHQUAKE POTENTIAL OF THE SOUTHERN LOS ANGELES BASIN, ORANGE COUNTY, CALIFORNIA Eldon M. Gath, University of California, Irvine, 143 Social Ecology I, Irvine, CA, 92697-7070; tel: 949-824-5382, fax: 949-824-2056, email: [email protected] Eric E. Runnerstrom, University of California, Irvine, 143 Social Ecology I, Irvine, CA, 92697- 7070; tel: 949-824-5382, fax: 949-824-2056, email: [email protected] Lisa B. Grant (P.I.), University of California, Irvine, 262 Social Ecology I, Irvine, CA, 92697- 7070; tel: 949-824-5491, fax: 949-824-2056, email: [email protected] TECHNICAL ABSTRACT The Santa Ana Mountains (SAM) are a 1.7 km high mountain range that form the southeastern boundary of the Los Angeles basin between Orange and Riverside counties in southern California. The SAM have three well developed erosional surfaces preserved on them, as well as a suite of four fluvial fill terraces preserved in Santiago Creek, which is a drainage trapped between the uplifting SAM and a parallel Loma Ridge.
    [Show full text]
  • Stress Triggering in Thrust and Subduction Earthquakes and Stress
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 109, B02303, doi:10.1029/2003JB002607, 2004 Stress triggering in thrust and subduction earthquakes and stress interaction between the southern San Andreas and nearby thrust and strike-slip faults Jian Lin Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA Ross S. Stein U.S. Geological Survey, Menlo Park, California, USA Received 30 May 2003; revised 24 October 2003; accepted 20 November 2003; published 3 February 2004. [1] We argue that key features of thrust earthquake triggering, inhibition, and clustering can be explained by Coulomb stress changes, which we illustrate by a suite of representative models and by detailed examples. Whereas slip on surface-cutting thrust faults drops the stress in most of the adjacent crust, slip on blind thrust faults increases the stress on some nearby zones, particularly above the source fault. Blind thrusts can thus trigger slip on secondary faults at shallow depth and typically produce broadly distributed aftershocks. Short thrust ruptures are particularly efficient at triggering earthquakes of similar size on adjacent thrust faults. We calculate that during a progressive thrust sequence in central California the 1983 Mw = 6.7 Coalinga earthquake brought the subsequent 1983 Mw = 6.0 Nun˜ez and 1985 Mw = 6.0 Kettleman Hills ruptures 10 bars and 1 bar closer to Coulomb failure. The idealized stress change calculations also reconcile the distribution of seismicity accompanying large subduction events, in agreement with findings of prior investigations. Subduction zone ruptures are calculated to promote normal faulting events in the outer rise and to promote thrust-faulting events on the periphery of the seismic rupture and its downdip extension.
    [Show full text]
  • The Earthquake
    DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY PROCEEDINGS OF THE NATIONAL EARTHQUAKE PREDICTION EVALUATION COUNCIL JUNE 11-12, 1991 ALTA, UTAH by Virgil A. Frizzell, Jr. Open-File Report 92-249 This report is preliminary and has not been edited or reviewed for conformity with U.S.G.S. publication standards. 1992 REPRODUCED FKOK OUST A * » " * * TABLE OF CONTENTS Page Preface v Current Membership of National Earthquake Prediction Evaluation Council vii Proceedings of the meeting 1 References cited 33 Appendices 35 PREFACE The National Earthquake Prediction Evaluation Council (NEPEC) was established in 1979 pursuant to the Earthquake Hazards Reduction Act of 1977 to advise the Director of the United States Geological Survey (USGS) about issuing any formal predictions or other information pertinent to the potential for the occurrence of a significant earthquake. The Director of the USGS is responsible for deciding whether and/or when to issue predictions or other information pertinent to a prediction. A prediction is defined as a statement on the time of occurrence, location, and magnitude of a future significant earthquake including an analysis of the uncertainty of those factors. NEPEC advises the Director concerning the completeness and scientific validity of the available data and on related matters. Duties include the evaluation of predictions made by other scientists, from within or outside of government, rather than issuance of predictions based on data gathered by NEPEC itself. According to its charter, NEPEC, also referred to in this document as the Council, is comprised of a Chairman, Vice Chairman and from 8 to 12 other members appointed by the Director of the USGS.
    [Show full text]
  • Seismic Triggering of Eruptions in the Far Field: Volcanoes and Geysers
    ANRV273-EA34-09 ARI 26 April 2006 20:33 Seismic Triggering of Eruptions in the Far Field: Volcanoes and Geysers Michael Manga1 and Emily Brodsky2 1Department of Earth and Planetary Science, University of California, Berkeley, California 94720-4767; email: [email protected] 2Department of Earth Sciences, University of California, Santa Cruz, California 95060 Annu. Rev. Earth Planet. Sci Key Words 2006. 34:263–91 First published online as a rectified diffusion, advective overpressure, magma chamber Review in Advance on convection, liquefaction, mud volcanoes, triggered seismicity January 16, 2006 Abstract The Annual Review of Earth and Planetary Science Approximately 0.4% of explosive volcanic eruptions occur within a few days of large, is online at earth.annualreviews.org distant earthquakes. This many “triggered” eruptions is much greater than expected by chance. Several mechanisms have been proposed to explain triggering through doi: 10.1146/ annurev.earth.34.031405.125125 changes in magma overpressure, including the growth of bubbles, the advection of large pressures by rising bubbles, and overturn of magma chambers. Alternatively, Copyright c 2006 by Annual Reviews. All rights triggered eruptions may occur through failure of rocks surrounding stored magma. by University of California - Berkeley on 05/02/06. For personal use only. reserved All these mechanisms require a process that enhances small static stress changes 0084-6597/06/0530- caused by earthquakes or that can convert (the larger) transient, dynamic strains into 0263$20.00 permanent changes in pressure. All proposed processes, in addition to viscoelastic Annu. Rev. Earth. Planet. Sci. 2006.34:263-291. Downloaded from arjournals.annualreviews.org relaxation of stresses, can result in delayed triggering of eruptions, although quanti- fying the connection between earthquakes and delayed, triggered eruptions is much more challenging.
    [Show full text]