Risk Assessment
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Optimizing Multi-Station Template Matching to Identify and Characterize Induced Seismicity in and Around Ohio
Optimizing Multi-Station Template Matching to Identify and Characterize Induced Seismicity in and Around Ohio Final Technical Report for USGS NEHRP Award No. G15AP00089 PI: Michael R. Brudzinskia 1 Co-PI: Brian S. Curriea 2 Grad Student Supported: Robert J. Skoumala 3 aDepartment of Geology and Environmental Earth Science, Miami University, Oxford, OH, [email protected], 001-513-529-3216 [email protected], 001-513-529-3216 [email protected], 001-515-401-8271 Project dates: June 1, 2015 to May 31, 2016. Key Results 1. Multistation template matching finds swarms that help discern induced seismicity 2. 2 swarms were correlated with wastewater disposal, 3 with hydraulic fracturing 3. 17 other cataloged earthquakes between 2010-2014 were non-swarmy, likely natural Abstract This study investigated the utility of multistation waveform cross correlation to help discern induced seismicity. Template matching was applied to all Ohio earthquakes cataloged since the arrival of nearby EarthScope TA stations in late 2010. Earthquakes that were within 5 km of fluid injection activities in regions that lacked previously documented seismicity were found to be swarmy. Moreover, the larger number of events produced by template matching for these swarmy sequences made it easier to establish more detailed temporal and spatial relationships between the seismicity and fluid injection activities, which is typically required for an earthquake to be considered induced. Study results detected three previously documented induced sequences (Youngstown, Poland Township, and Harrison County) and provided evidence that suggests two additional cases of induced seismicity (Belmont/Guernsey County and Washington County). Evidence for these cases suggested that unusual swarm-like behaviors in regions that lack previously documented seismicity can be used to help distinguish induced seismicity, complementing the traditional identification of an anthropogenic source spatially and temporally correlated with the seismicity. -
PEER 2014/17 OCTOBER 2014 Disclaimer
PACIFIC EARTHQUAKE ENGINEERING RESEARCH CENTER PEER NGA-East Database Christine A. Goulet Tadahiro Kishida Pacific Earthquake Engineering Research Center Timothy D. Ancheta Risk Management Solutions, Newark, California Chris H. Cramer Center for Earthquake Research and Information University of Memphis Robert B. Darragh Walter J. Silva Pacific Engineering and Analysis, Inc. El Cerrito, California Youssef M. A. Hashash Joseph Harmon University of Illinois, Urbana-Champaign Jonathan P. Stewart University of California, Los Angeles Katie E. Wooddell Pacific Gas & Electric Company Robert R. Youngs AMEC Environment and Infrastructure Oakland, California PEER 2014/17 OCTOBER 2014 Disclaimer The opinions, findings, and conclusions or recommendations expressed in this publication are those of the author(s) and do not necessarily reflect the views of the study sponsor(s) or the Pacific Earthquake Engineering Research Center. PEER NGA-East Database Christine A. Goulet Tadahiro Kishida Pacific Earthquake Engineering Research Center Timothy D. Ancheta Risk Management Solutions, Newark, California Chris H. Cramer Center for Earthquake Research and Information University of Memphis Robert B. Darragh Walter J. Silva Pacific Engineering and Analysis, Inc. El Cerrito, California Youssef M. A. Hashash Joseph Harmon University of Illinois, Urbana-Champaign Jonathan P. Stewart University of California, Los Angeles Katie E. Wooddell Pacific Gas & Electric Company Robert R. Youngs AMEC Environment and Infrastructure Oakland, California PEER Report 2014/17 Pacific Earthquake Engineering Research Center Headquarters at the University of California, Berkeley October 2014 ii ABSTRACT This report serves as a documentation of the ground motion database development for the NGA- East Project. The ground motion database includes the two- and three-component ground-motion recordings from numerous selected events (M > 2.5, distances up to 1500 km) recorded in the Central and Eastern North America (CENA) region since 1988. -
The University of Alabama College of Engineering Bureau of Engineering Research
THE UNIVERSITY OF ALABAMA COLLEGE OF ENGINEERING BUREAU OF ENGINEERING RESEARCH U,"lmade available under NASA sPonrsl q-0n the interesid ie dis- ,.4N FINAL REPORT Somination of Ladh fesources Survey au Program informa,"on 'j.jioo ut liability So VOLUME THREE r ony use made thereot." m of Contract NAS5-21876 PD INVESTIGATIONS USING DATA N o ALABAMA FROM ERTS-A Q) U 14 p .Principal Investigator " P-"DR. HAROLD R. HENRY Submitted to -O ...4 Goddard Space Flight Center 0M ( National Aeronautics and Space Administration S 0 Greenbelt, Maryland H Po August,, 1974 0 *C4 o l4 BER Report No. 179-122 -U N I V E R 8IT Y, ALABA M A 35486 44. INVESTIGATIONS USING DATA IN ALABAMA FROM ERTS-A FINAL REPORT VOLUME THREE Contract NAS5-21876 GSFC Proposal No. 271 Principal Investigator DR. HAROLD R. HENRY GSFC ID UN604 Submitted to Goddard Space Flight Center National Aeronautics and Space Administration Greenbelt, Maryland Submitted by Bureau,.of Engineering Research The University of Alabama. University, Alabama August, 19i4 GEOLOGICAL SURVEY OF ALABAMA STUDIES James A. Drahovzal SECTION TWELVE of VOLUME THREE INVESTIGATIONS USING DATA IN ALABAMA FROM ERTS-A CONTENTS SECTION TWELVE INTRODUCTION ...................................................... 1 LINEAMENTS ......................................................... 24 A COMPARISON OF LINEAMENTS AND FRACTURE TRACES TO JOINTING IN THE APPALACHIAN PLATEAU OF ALABAMA -- DORA-SYLVAN SPRINGS AREA .... 146 LINEAMENT ANALYSIS OF ERTS-1 IMAGERY OF THE ALABAMA PIEDMONT ...... 181 LINEAMENT ANALYSIS IN THE CROOKED CREEK AREA, CLAY AND RANDOLPH COUNTIES, ALABAMA ......................................... 209 GEOCHEMICAL EVALUATION OF LINEAMENTS ............................... 226 HYDROLOGIC EVALUATION AND APPLICATION OF ERTS DATA ................ 404 A COMPARISON OF SINKHOLE, CAVE, JOINT AND LINEAMENT ORIENTATIONS . -
Mineral, Virginia, Earthquake Illustrates Seismicity of a Passive
GEOPHYSICAL RESEARCH LETTERS, VOL. 39, L02305, doi:10.1029/2011GL050310, 2012 Mineral, Virginia, earthquake illustrates seismicity of a passive-aggressive margin Emily Wolin,1 Seth Stein,1 Frank Pazzaglia,2 Anne Meltzer,2 Alan Kafka,3 and Claudio Berti2 Received 9 November 2011; revised 22 December 2011; accepted 23 December 2011; published 24 January 2012. [1] The August 2011 M 5.8 Mineral, Virginia, earthquake North America is a “passive” continental margin, along that shook much of the northeastern U.S. dramatically which the continent and seafloor are part of the same plate. demonstrated that passive continental margins sometimes The fundamental tenet of plate tectonics, articulated by have large earthquakes. We illustrate some general aspects Wilson [1965, p. 344], is that “plates are not readily of such earthquakes and outline some of the many unresolved deformed except at their edges.” Hence if plates were the questions about them. They occur both offshore and onshore, ideal rigid entities assumed in many applications, such as reaching magnitude 7, and are thought to reflect reactivation calculating plate motions, passive continental margins of favorably-oriented, generally margin-parallel, faults cre- should be seismically passive. ated during one or more Wilson cycles by the modern stress [3] In reality, however, large and damaging earthquakes field. They pose both tsunami and shaking hazards. How- occur along passive margins worldwide [Stein et al., 1979, ever, their specific geologic setting and causes are unclear 1989; Schulte and Mooney, 2005] (Figure 1). These earth- because large magnitude events occur infrequently, micro- quakes release a disproportionate share, about 25%, of the seismicity is not well recorded, and there is little, if any, net seismic moment release in nominally-stable continental surface expression of repeated ruptures. -
Earthquake Safety Guidelines for Educational Facilities
Earthquake Safety Guidelines for require an increased earthquake awareness Educational Facilities for parents, educators, school boards and students. Such an increase in awareness has By Rob Jackson, P. E. been a focus of the Earthquake Engineering Research Institute’s (EERI) Seismic Safety Every child has the right to attend school in of Schools Committee (EERI, 2012). safe buildings. The United States has been relatively lucky so far regarding school children and the occurrence of earthquakes. However, the United States cannot rely on such continued good fortune in the future. Governmental and educational leaders must fulfill their responsibilities for the safety of school children by implementing school safety programs that include the design and construction of seismically safe buildings. Such programs must emphasize seismic resistance and overall earthquake hazard resilience. Earthquake hazard mitigation is A typical unreinforced masonry high school in most readily accomplished through the the United States. (Wang, Y., EERI, 2012a) improved seismic design and construction of Similar advocacy efforts have impacted buildings, since “earthquakes don’t kill people, unsafe buildings do.” Earthquake policy across the United States. In California, hazard mitigation requires an increase in the positive steps have been taken to increase the prioritization and perceived value of seismic seismic safety of schools. The 1933 Long design within the project delivery systems of Beach earthquake resulted in passage of the the owners, construction managers, architects Field and Riley Acts. In California, no school and engineers who operate, design and child has been killed or seriously injured construct educational facilities in the United since 1933. However, no major California States. -
Effectiveness of the National Earthquake Hazards Reduction
DRAFT (4/27/2012 ACEHR teleconference meeting) Effectiveness of the National Earthquake Hazards Reduction Program A Report from the Advisory Committee on Earthquake Hazards Reduction May 2012 Contents Executive Summary .................................................................................................. 1 Introduction .............................................................................................................. Program Effectiveness and Needs .......................................................................... Management, Coordination, and Implementation of NEHRP ............................... Federal Emergency Management Agency ..................................................................... National Institute of Standards and Technology ........................................................ National Science Foundation .............................................................................................. U.S. Geological Survey ........................................................................................................... Appendix: Trends and Developments in Science and Engineering .................... Social Science ............................................................................................................................ Earth Science ............................................................................................................................. Geotechnical Earthquake Engineering ........................................................................... -
Foreshocks, B Value Map, and Aftershock Triggering for the 2011
Journal of Geophysical Research: Solid Earth RESEARCH ARTICLE Foreshocks, b Value Map, and Aftershock Triggering 10.1029/2017JB015136 for the 2011 Mw 5.7 Virginia Earthquake Key Points: Xiaofeng Meng1,2 , Hongfeng Yang3 , and Zhigang Peng4 • Dynamic triggering explains aftershocks along the rupture plane, 1Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA, 2Now at Southern California Earthquake while static triggering explains the 3 off-fault seismicity Center, University of Southern California, Los Angeles, CA, USA, Earth System Science Programme, The Chinese University of 4 • We find great spatial variability of the Hong Kong, Hong Kong, School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA b values within the aftershock zone, suggesting strong heterogeneity in stress distribution and material Abstract The 2011 Mw 5.7 Virginia earthquake and subsequent dense deployment provide us an • We find no foreshock activity, which unprecedented opportunity to study in detail an earthquake sequence within stable continental United adds to a growing body of fi observations that intraplate States. Here we apply the waveform-based matched lter technique to obtain more complete earthquake earthquakes tend to not have catalogs around the origin time of the Virginia mainshock. With the enhanced earthquake catalogs, we foreshocks conclude that no foreshock activity existed prior to the Virginia mainshock. The b value map shows significant variations across the aftershock zone, suggesting strong heterogeneity in stress distribution or crustal Supporting Information: material in the study region. We also investigate multiple earthquake triggering mechanisms, including static • Supporting Information S1 and dynamic triggering, afterslip, and atmospheric pressure changes. -
FY2014 USGS Budget Justification
The United States BUDGET Department of the Interior JUSTIFICATIONS and Performance Information Fiscal Year 2014 U.S. GEOLOGICAL SURVEY NOTICE: These budget justifications are prepared for the Interior, Environment and Related Agencies Appropriations Subcommittees. Approval for release of the justifications prior to their printing in the public record of the Subcommittee hearings may be obtained through the Office of Budget of the Department of the Interior. U.S. Geological Survey Table of Contents U.S. GEOLOGICAL SURVEY FY 2014 BUDGET JUSTIFICATION References to the 2013 Full Yr. CR signify annualized amounts appropriated in P.L. 112-175, the Continuing Appropriations Act. These amounts are the 2012 enacted numbers annualized through the end of FY 2013 with a 0.612 percent across-the-board increase for discretionary programs. Exceptions to this include Wildland Fire Management, which received an anomaly in the 2013 CR to fund annual operations at $726.5 million. The 2013 Full Yr. CR does not incorporate reductions associated with the Presidential sequestration order issued in accordance with section 251A of the Balanced Budget and Emergency Deficit Control Act, as amended (BBEDCA), 2 U.S.C. 109a. This column is provided for reference only. 2014 Budget Justification i Table of Contents U.S. Geological Survey This page left intentionally blank. ii 2014 Budget Justification U.S. Geological Survey Table of Contents U.S. GEOLOGICAL SURVEY FY 2014 BUDGET JUSTIFICATION TABLE OF CONTENTS Organization Organization Chart .............................................................................................................................. -
William Barnhart – Curriculum Vitae [email protected] Updated May 2014 Education Ph.D
William Barnhart – Curriculum Vitae [email protected] updated May 2014 Education Ph.D. Geophysics, Cornell University (May 2013) Advisor: Dr. Rowena Lohman B.S. Geology, Washington and Lee University (June 2008) Advisor: Dr. Jeffrey Rahl Appointments Jan. 2015 Assistant Professor, The University of Iowa, Iowa City, IA 2013-2014 USGS Mendenhall Postdoctoral Fellow, NEIC, Golden CO 2009-2012 NASA Graduate Research Fellow, Cornell University 2010 Adjunct Lecturer, Washington and Lee University Publications Barnhart, W.D., G.P. Hayes, R.W. Briggs, R.D. Gold, R. Bilham, Ball-and-socket tectonic rotations during the 2013 Mw7.7 Balochistan earthquake, EPSL, in revision Hayes et al., Mind the Gap – the northern Chile Subduction Zone and the 2014 Earthquake Sequence, Nature, in revision Barnhart, W.D., Benz, H., Hayes, G.P., Rubinstein, J., Bergman, E., Seismological and geodetic constraints on the 2011 Mw5.3 Trinidad, Colorado earthquake and deformation in the Raton Basin, JGR, in review Witter, R.C., Briggs, R.W., Engelhart, S.E., Gelfenbaum, G., Koehler, R.D., Barnhart, W.D., Little late Holocene strain accumulation and release on the Aleutian megathrust below the Shumagin Islands, Alaska, Geophysical Research Letters Barnhart, W.D., G.P. Hayes, S.V. Samsonov, E.J. Fielding, L.E. Seidman, (2014) Breaking the Oceanic Lithosphere in Subduction Zones: The 2013 Khash, Iran Earthquake, Geophysical Research Letters, doi: 10.1002/2013GL058096 Godt, J.W., Coe, J.A., Kean, J.W., Baum, R.L., Jones, E.S., Harp, E.L., Staley, D.M., Barnhart, W.D., (2014) Landslides in the Northern Colorado Front Range Caused by Rainfall, September 11-13, 2013, USGS Publications, Fact Sheet 2013-3114. -
2013 Annual Report
2013 Annual Report WSSPC U.S. states ranked by national number of annual earthquakes. Western States Seismic Policy Council 801 K Street, Suite 1236, Sacramento, CA 95814 916-444-6816 [email protected] DISCLAIMER The views and conclusions contained in this report are those of the authors and should not be interpreted as representing the opinions or policies of the U.S. Government. Mention of trade names or commercial products does not constitute their endorsement by the U.S. Government; by the Western States Seismic Policy Council (WSSPC), or by WSSPC members, agencies and affiliates. Cover image: Map of the United States ranking states by number of earthquakes. States that fall within the WSSPC region are colored green (Canada and U.S. Territories were not included in the original map). Cover map presented as modified from the United States Geological Survey map located at: http://earthquake.usgs.gov/earthquakes/states/top_states.php 2013 WSSPC ANNUAL REPORT TABLE OF CONTENTS Page Section A: WSSPC Organization Mission and Goals .................................................................................................................. A-1 WSSPC Board and Staff ......................................................................................................... A-2 WSSPC Members, Earthquake/Tsunami Program Managers, & State Hazard Mitigation Officers ................................................................................... A-3 WSSPC Members’ Agencies .................................................................................................. -
The Mw 5.8 Virginia Earthquake of August 23, 2011 EERI, GEER, And
EERI Special Earthquake Report — December 2011 Learning from Earthquakes The Mw 5.8 Virginia Earthquake of August 23, 2011 After the Mw 5.8 earthquake of social disruptions up and down the The epicenter of the August 23 August 23, 2011, EERI assembled East Coast that lasted from several quake was 8 km from Mineral, a team of East Coast EERI mem- hours to some months. The quake Virginia, 61 km from Richmond, bers to document various aspects caused widespread interruptions to and 135 km from Washington, of the event. Co-leaders were communications and transportation D.C. (Figure 1). A network of James Beavers, a consulting struc- systems, numerous school closings in seismographs installed following tural engineer from Knoxville, Ten- the epicentral area of Louisa County, the August 23rd main shock has nessee, and William Anderson, a other closures in the greater Wash- enabled accurate location of many sociologist and an EERI Board ington, D.C., area, and an automatic aftershocks. The aftershocks define member from Washington, D.C. shutdown of the North Anna Nuclear a 10-km-long, N28°E striking, Other team members included Power Plant. The earthquake is a 45°ESE dipping fault at between Matthew Eatherton, Virginia Tech; noteworthy reminder that communi- 2.5 and 8 km depth, in good agree- Ramon Gilsanz, Gilsanz Murray ties on the East Coast are not pre- ment with the focal mechanism of Steficek Inc; Frederick Krimgold, pared to cope with a major earth- the main shock. The locations of Virginia Tech; Ying-Cheng Lin, quake, and that steps could be taken aftershocks do not correspond to a Lehigh University; Claudia Marin, to improve their readiness and in- previously identified fault; previous, Howard University; Justin Marshall, crease loss reduction efforts. -