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High-Resolution Spatial and Temporal Analysis of the Aftershock Sequence of the 23 August 2011 Mw 5.8 Mineral, Virginia, Earthquake
High-Resolution Spatial and Temporal Analysis of the Aftershock Sequence of the 23 August 2011 Mw 5.8 Mineral, Virginia, Earthquake Author: Stephen Glenn Hilfiker Persistent link: http://hdl.handle.net/2345/bc-ir:107179 This work is posted on eScholarship@BC, Boston College University Libraries. Boston College Electronic Thesis or Dissertation, 2016 Copyright is held by the author. This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License (http:// creativecommons.org/licenses/by-nc-nd/4.0). Boston College The Graduate School of Arts and Sciences Department of Earth and Environmental Sciences HIGH-RESOLUTION SPATIAL AND TEMPORAL ANALYSIS OF THE AFTERSHOCK SEQUENCE OF THE 23 AUGUST 2011 Mw 5.8 MINERAL, VIRGINIA, EARTHQUAKE a thesis by STEPHEN GLENN HILFIKER submitted in partial fulfillment of the requirements for the degree of Master of Science August 2016 © copyright by STEPHEN GLENN HILFIKER 2016 High-Resolution Spatial and Temporal Analysis of the Aftershock Sequence of the 23 August 2011 Mw 5.8 Mineral, Virginia, Earthquake Stephen G. Hilfiker John E. Ebel ABSTRACT Studies of aftershock sequences in the Central Virginia Seismic Zone (CVSZ) provide critical details of the subsurface geologic structures responsible for past and (possibly) future earthquakes in an intraplate setting. The 23 August 2011 MW 5.8 Mineral, Virginia, earthquake, the largest magnitude event recorded in the CVSZ, caused widespread damage and generated a lengthy and well-recorded aftershock sequence. Over 1600 aftershocks were recorded using a dense network of seismometers in the four months following the mainshock, offering the unique opportunity to study the fault structure responsible for the post-main event seismicity. -
Canadian Earthquakes - 1985-86
GEOLOGICAL SURVEY OF CANADA PAPER 88-14 CANADIAN EARTHQUAKES - 1985-86 R.J. Wetmiller J. A. Drysdale R.B. Homer M. Lamontagne Energy, Mines and Energie, Mines et ••• Resources Canada Ressources Canada Canada THE ENERGY OF OUR RESOURCES THE POWER OF OUR IDEAS NOTE The format of the annual catalogue of Canadian earthquakes produced by the Geophysics Division and the Cordilleran and Pacific Geoscience Division of the Geological Survey of Canada has been chan ged with this edition. This catalogue covers two years of activity, only lists events with magnitude 4.0 or greater and is also available in a French version. Subsequent editions will be published every other year. More detailed information about Canadian earthquakes is available in the form of quarterly reports prepared by the Geological Survey. Enquiries about Canadian earthquakes, earthquake hazards or seis mological research in Canada should be directed to the Geophysics Division, 1 Observatory Crescent, Ottawa, Ontario, KIA OY3 (613-995-5548) or the Pacific Geoscience Centre, 9860 West Saanich Road, Sidney , B.C., V8L 4B2 (604-356-6500). GEOLOGICAL SURVEY OF CANADA PAPER 88-14 Seismological Series Number 97 CANADIAN EARTHQUAKES - 1985-86 R.J. Wetmiller J. A. Drysdale R.B. Homer M. Lamontagne 1989 © Minister of Supply and Services Canada 1989 Available in Canada through authorized bookstore agents and other bookstores or by mail from Canadian Government Publishing Centre Supply and Services Canada Ottawa, Canada Kl A OS9 and from Geological Survey of Canada offices: 60 l Booth Street Ottawa, Canada Kl A OE8 3303-33rd Street N.W., Calgary, Alberta T2L 2A7 100 West Pender Street Vancouver, B.C. -
A New Analysis of the Magnitude of the February 1663 Earthquake at Charlevoix, Quebec
A new analysis of the magnitude of the February 1663 earthquake at Charlevoix, Quebec Author: J. E. Ebel Persistent link: http://hdl.handle.net/2345/bc-ir:107016 This work is posted on eScholarship@BC, Boston College University Libraries. Published in Bulletin of the Seismological Society of America, vol. 101, no. 3, pp. 1024-1038, 2011 These materials are made available for use in research, teaching and private study, pursuant to U.S. Copyright Law. The user must assume full responsibility for any use of the materials, including but not limited to, infringement of copyright and publication rights of reproduced materials. Any materials used for academic research or otherwise should be fully credited with the source. The publisher or original authors may retain copyright to the materials. Bulletin of the Seismological Society of America This copy is for distribution only by the authors of the article and their institutions in accordance with the Open Access Policy of the Seismological Society of America. For more information see the publications section of the SSA website at www.seismosoc.org THE SEISMOLOGICAL SOCIETY OF AMERICA 400 Evelyn Ave., Suite 201 Albany, CA 94706-1375 (510) 525-5474; FAX (510) 525-7204 www.seismosoc.org Bulletin of the Seismological Society of America, Vol. 101, No. 3, pp. 1024–1038, June 2011, doi: 10.1785/0120100190 A New Analysis of the Magnitude of the February 1663 Earthquake at Charlevoix, Quebec by John E. Ebel Abstract This paper presents a new and comprehensive analysis of the magnitude of the 1663 Charlevoix, Quebec, earthquake. Based on a modified Mercalli intensity scale (MMI) of about VI from reports of damage to chimneys and a masonry wall in Roxbury and Boston, Massachusetts, the best estimate of the moment magnitude of this earthquake is M 7.3 to 7.9 from MMI attenuation relations. -
Source Zones, Recurrence Rates, and Time Histories for Earthquakes Affecting Kentucky (KTC-96-4)
Commonwealth of Kentucky fred N. Mudge Transportation Cabinet Paul E. Patton Secretary of Transportation Frankfort, Kentucky 40622 Governor August 14, 1996 Mr. Paul Toussaint Division Administrator Federal Highway Administration 330 West Broadway Frankfort, KY 40602 Dear Mr. Toussaint: Subject: IMPLEMENTATION STATEMENT KYHPR 94-155, Evaluation and Analysis of Innovative Concepts for Bridge Seismic Retrofit This report is the first of three reports for the above referenced study. The objective of this study was to develop earthquake time histories for use in the design of transportation facilities throughout the commonwealth. In order to achieve this objective, the following tasks were defined: 1. definition and evaluation of earthquakes in seismic zones that have the potential to generate damaging ground motions in Kentucky, 2. specification of the source characteristics, accounting for the spreading and attenuation of the ground motions to the top-of-the-bedrock at sites in Kentucky, and 3. determination of seismic zoning maps for the commonwealth based on peak particle accelerations, response spectra, and time histories. These tasks have been addressed in the report entitled Source Zones, Recurrence Rates, and Time Histories for Earthquakes Affecting Kentucky (KTC-96-4). Seismic input data (time histories, response spectra, and surface accelerations) were generated for all counties in KENTUCKY TRANSPORTATION CABINET "PROVlDE A SAFE, EFFICIENT, ENVIRONMENTALLY SOUND, AND FISCALLY RESPONSIBLE TRANSPORTATION SYSTEM WHICH PROMOTES ECONOMIC GROWTH AND ENHANCES THE QUAUTY OF LIFE IN KENTUCKY:' "AN EQUAL OPPORTUNITY EMPLOYER M/F/D" Kentucky and have been included in this report. It should be noted that the seismic data is generated at the county seat and not at the county centroid. -
Data for Quaternary Faults, Liquefaction Features, and Possible Tectonic Features in the Central and Eastern United States, East of the Rocky Mountain Front
U.S. Department of the Interior U.S. Geological Survey Data for Quaternary faults, liquefaction features, and possible tectonic features in the Central and Eastern United States, east of the Rocky Mountain front By Anthony J. Crone and Russell L. Wheeler Open-File Report 00-260 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards nor with the North American Stratigraphic Code. Any use of trade names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. 2000 Contents Abstract........................................................................................................................................1 Introduction..................................................................................................................................2 Strategy for Quaternary fault map and database .......................................................................10 Synopsis of Quaternary faulting and liquefaction features in the Central and Eastern United States..........................................................................................................................................14 Overview of Quaternary faults and liquefaction features.......................................................14 Discussion...............................................................................................................................15 Summary.................................................................................................................................18 -
1 1 2 3 4 5 the MAGIC Experiment: a Combined Seismic And
1 2 3 4 5 6 The MAGIC experiment: A combined seismic and magnetotelluric deployment to 7 investigate the structure, dynamics, and evolution of the central Appalachians 8 9 Maureen D. Long1*, Margaret H. Benoit2, Rob L. Evans3, John C. Aragon1,4, James Elsenbeck3,5 10 11 12 1Department of Geology and Geophysics, Yale University, PO Box 208109, New Haven, CT, 13 06520, USA. 14 2National Science Foundation, 2415 Eisenhower Ave., Alexandria, VA, 22314, USA. 15 3Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Clark 263, 16 MS 22, Woods Hole, MA, 02543, USA. 17 4Now at: Earthquake Science Center, U.S. Geological Survey, 345 Middlefield Rd., MS 977, 18 Menlo Park, CA, 94025, USA. 19 5Now at: Lincoln Laboratories, Massachusetts Institute of Technology, 244 Wood St., Lexington, 20 MA, 02421, USA. 21 22 23 Revised manuscript submitted to the Data Mine section of Seismological Research Letters 24 25 26 27 28 29 *Corresponding author. Email: [email protected] 30 31 32 33 34 35 36 37 38 1 39 ABSTRACT 40 The eastern margin of North America has undergone multiple episodes of orogenesis and 41 rifting, yielding the surface geology and topography visible today. It is poorly known how the crust 42 and mantle lithosphere have responded to these tectonic forces, and how geologic units preserved 43 at the surface relate to deeper structures. The eastern North American margin has undergone 44 significant post-rift evolution since the breakup of Pangea, as evidenced by the presence of young 45 (Eocene) volcanic rocks in western Virginia and eastern West Virginia and by the apparently recent 46 rejuvenation of Appalachian topography. -
Annual Report for Fiscal Year 2017
This report covers the National Earthquake Hazards Reduction Program (NEHRP or Program) activities during fiscal year (FY) 2017. It is submitted to the Congress by the Interagency Coordinating Committee on Earthquake Hazards Reduction (Interagency Coordinating Committee), as required by the Earthquake Hazards Reduction Act of 1977 (Public Law 95-124, 42 U.S.C. 7701 et. seq.), as amended by the National Earthquake Hazards Reduction Program Reauthorization Act of 2004 (Public Law 108-360). The members of the Interagency Coordinating Committee are as follows: Chair Dr. Walter Copan Under Secretary of Commerce for Standards and Technology and Director National Institute of Standards and Technology U.S. Department of Commerce Mr. Peter Gaynor Acting Administrator Federal Emergency Management Agency U.S. Department of Homeland Security Dr. France A. Córdova Director National Science Foundation Mr. John Michael “Mick” Mulvaney Director Office of Management and Budget Executive Office of the President Dr. Kelvin Droegemeier Assistant to the President for Science and Technology and Director Office of Science and Technology Policy Executive Office of the President Dr. James F. Reilly II Director U.S. Geological Survey U.S. Department of the Interior Disclaimer: Certain trade names or company products may be identified in this document to describe a procedure or concept adequately. Such identification is not intended to imply recommendation or endorsement by any of the agencies represented on the Interagency Coordinating Committee on Earthquake Hazards Reduction, nor does it imply that the trade names or company products are necessarily the best available for the purpose. Table of Contents Executive Summary ..................................................................................................................................... i Section 1 – Introduction ............................................................................................................................. -
88 Annual Meeting of the Eastern Section of the Seismological
88th Annual Meeting of the Eastern Section of the Seismological Society of America October 23-26th, 2016 Reston, VA 88th Annual Meeting of the Eastern Section of the Seismological Society of America Acknowledgements The work of many people made this meeting possible and we are grateful for their contributions. These people include: Field Trip Leaders: J. Wright Horton, Jr., Steven Schindler, Terrence Paret Banquet Guest Speaker: Terrence Paret Abstract Submission and Registration: Bo Orloff, Sissy Stone, Nan Broadbent, SSA main office Budget and planning: Charles Scharnberger from the Eastern Section of SSA Graphic Design and Webmaster: Bo Orloff Jesuit Seismological Society Award Committee. Past meeting organizers, especially Steven Jaume, Chris Cramer, and Maurice Lamontagne. Many thanks to all the session chairs! Thomas Pratt, Oliver Boyd, and Christine Goulet Planning Committee Chairs Many thanks to our generous sponsors: 2 88th Annual Meeting of the Eastern Section of the Seismological Society of America General Information Meeting Theme: The 2016 Eastern Section meeting is titled “From the Mantle to the Surface” and is a joint meeting with the Pacific Earthquake Engineering Research (PEER) Center’s Next Generation Attenuation-East (NGA- East) project. It will include a combination of geophysical studies being carried out using the USArray and other ground-motion data in the eastern United States. Special sessions include crust and mantle studies utilizing USArray, studies of central and eastern U.S. faults, seismicity and ground motions, and the Next Generation Attenuation Project for Central and Eastern North America—NGA-East. NGA-East Special Session (Wednesday 8:30-12:00): The Next Generation Attenuation project for Central and Eastern North America (CENA), NGA-East, is a major multi-disciplinary project coordinated by the PEER. -
Earthquake Hazard Studies in the Northeastern United States
THE LAMONT COOPERATIVE SEISMIC NETWORK AND THE ADVANCED NATIONAL SEISMIC SYSTEM: EARTHQUAKE HAZARD STUDIES IN THE NORTHEASTERN UNITED STATES. Annual Project Summary October 01, 2003 - September 30, 2004 External Grant Award Number: 04HQAG-0115 Won-Young Kim Lamont-Doherty Earth Observatory of Columbia University Palisades, NY 10964, USA Tel: 845-365-8387, Fax: 845-365-8150 E-mail: [email protected] URL: <http://www.ldeo.columbia.edu/LCSN> Program Element: Element II. Research on Earthquake Occurrence and Effects Key Words: Wave Propagation, Regional Seismic Hazards and Real-time earthquake information Investigations undertaken The operation of the Lamont-Doherty Cooperative Seismographic Network (LCSN) to mon- itor earthquakes in the northeastern United States is supported under this award. The goal of the project is to compile a complete earthquake catalog for this region to assess the earthquake haz- ards, and to study the causes of the earthquakes in the region. The LCSN now operates 40 seis- mographic stations in seven states: Connecticut, Delaware, Maryland, New Jersey, New York, Pennsylvania and Vermont. During October 2003 through September 2004, scientists and staff at the Lamont-Doherty Earth Observatory of Columbia University (LDEO) satisfactorily carried out three main objectives of the project: 1) continued seismic monitoring for improved delineation and evaluation of hazards associated with earthquakes in the Northeastern United States, 2) im- proved real-time data exchange between regional networks and the USNSN for development of an Advanced National Seismic System (ANSS) and expanded earthquake reporting capabilities, and 3) promoted effective dissemination of earthquake data and information. A significant amount of associated research effort was related to determining seismic mo- ment tensor and focal depth of small to moderate-sized earthquakes in the eastern United States by using three-component, broadband seismic waveform data. -
Earthquake Hazard and Emergency Management Session 3
Session 3: Distribution of Earthquakes Session No. 3 Course Title: Earthquake Hazard and Emergency Management Session 3: Distribution of Earthquakes Author: James R. Martin, II Time: 90 minutes Objectives: 3.1 Identify the three primary “belts” where most earthquakes occur worldwide. 3.2 Identify regions of the United States where earthquakes tend to occur and explain the primary fault systems/mechanisms for earthquakes in each region. 3.3 Recognize the national seismic hazard maps, identify where they can be obtained, and explain what information is presented on these maps. Scope: During this session, the instructor will present the major plate boundary systems, and discuss the locations of earthquakes worldwide. The instructor will then focus on specific regions of the U.S. where earthquakes are prone to occur. The instructor should present and discuss the national seismic hazard maps and tie in the fact that the hazard maps reflect in scientific terms the information presented in the first part of the lecture. The instructor should explain the maps in general terms and discuss how they were developed, but the technical details of how the maps were developed and how the various maps are specifically used in engineering design is beyond the scope of this class. A suggested student exercise involves an in-class discussion (about 10 -15 minutes) on the concepts of probability and risk and the U.S. seismic hazard maps. This information is important to cover in this class because the basis of seismic hazard assessment in the U.S., including all building codes, is based on the government’s probabilistic seismic hazard assessments displayed on these maps. -
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. -
SEISMOLOGICAL SOCIETY of AMERICA 94Th ANNUAL MEETING
SEISMOLOGICAL SOCIETY OF AMERICA 94th ANNUAL MEETING May 3-5, 1998 (Monday-Wednesday) Northwest Rooms, Seattle Center Seattle, Washington, USA For Current Information: WWW: http://www.geophys.washington.edu/SEIS/SSA99/ Email: [email protected] Important Dates Program/Abstracts on WWW: March 15, 1999 Hotel Reservation Cutoff: March 31, 1999 Preregistration Deadline: April 16, 1999 MEETING CHAIRMAN MEETING INFORMATION Steve Malone Meeting Committee University of Washington Ken Creager, Bob Crosson, Ruth Ludwin, Tony Qamar, Bill Geophysics Program, Box 351650 Steele Seattle, WA 98195-1650 Email for general business and info: ssa99@geophys. Telephone: (206) 685-3811 washington.edu Fax: (206) 543-0489 Email: [email protected] Registration Information The registration form is in this issue of SRL on page 194 and EXHIBITS is available via the WWW at http://mail.seismosoc.org/ ssa99_Reg.html. Ruch Ludwin, telephone: (206) 543-4292 Fax: (206) 543-0489 Meeting Location Email: [email protected] The meeting will be held in the Northwest Rooms at Seattle Center, adjacent to the Key Arena and a shorr walk from the PROGRAM COMMITTEE Space Needle and monorail terminal. The icebreaker on Sunday evening will be held at the Best Western Executive Bob Crosson, telephone: (206) 543-6505 Inn. The luncheon, at the Space Needle, will be held on Email: [email protected] Tuesday, May 4. Ken Creager, telephone: (206) 685-2803 PLANNED SCHEDULE Email: [email protected] Sunday, May 2 Registration: 4:30-7:00 PM, Best