Evaluating the International Search and Rescue Response to Earthquake Disasters
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New Empirical Relationships Among Magnitude, Rupture Length, Rupture Width, Rupture Area, and Surface Displacement
Bulletin of the Seismological Society of America, Vol. 84, No. 4, pp. 974-1002, August 1994 New Empirical Relationships among Magnitude, Rupture Length, Rupture Width, Rupture Area, and Surface Displacement by Donald L. Wells and Kevin J. Coppersmith Abstract Source parameters for historical earthquakes worldwide are com piled to develop a series of empirical relationships among moment magnitude (M), surface rupture length, subsurface rupture length, downdip rupture width, rupture area, and maximum and average displacement per event. The resulting data base is a significant update of previous compilations and includes the ad ditional source parameters of seismic moment, moment magnitude, subsurface rupture length, downdip rupture width, and average surface displacement. Each source parameter is classified as reliable or unreliable, based on our evaluation of the accuracy of individual values. Only the reliable source parameters are used in the final analyses. In comparing source parameters, we note the fol lowing trends: (1) Generally, the length of rupture at the surface is equal to 75% of the subsurface rupture length; however, the ratio of surface rupture length to subsurface rupture length increases with magnitude; (2) the average surface dis placement per event is about one-half the maximum surface displacement per event; and (3) the average subsurface displacement on the fault plane is less than the maximum surface displacement but more than the average surface dis placement. Thus, for most earthquakes in this data base, slip on the fault plane at seismogenic depths is manifested by similar displacements at the surface. Log-linear regressions between earthquake magnitude and surface rupture length, subsurface rupture length, and rupture area are especially well correlated, show ing standard deviations of 0.25 to 0.35 magnitude units. -
Title: the December 7,1988 Armenia Earthquake Effects on Selected Power, Industrial and Commercial Fa Cilities
XA9952731 Title: The December 7,1988 Armenia earthquake effects on selected power, industrial and commercial fa cilities Contributor: R.D. Campbell Date: June 1995 (preparation date: January 1991) THE DECEMBER 7, 1988 ARMENIA EARTHQUAKE EFFECTS ON SELECTED POWER, INDUSTRIAL, AND COMMERCIAL FACILITIES Prepared for: ELECTRIC POWER RESEARCH INSTITUTE 3412 Hi 11 view Avenue Palo Alto, CA 94303 Prepared by: Michael J. Griffin Leo J. Bragagnoio Peter I. Yanev January 1991 ACKNOWLEDGEMENTS The authors and the Electric Power Research Institute (EPRI) would like to thank the following organizations and individuals for their cooperation and assistance in the investigations of the Armenia Earthquake. Thanks are extended to the U.S. Academy of Sciences and the Soviet Academy of Sciences for their joint sponsorship of the U.S. Investigative Team, with special thanks extended to the following team members: Dr. John Filson, Dr. Armen Der Kiureghian, Dr. Fred Krimgold, Dr. Thomas O'Rourke, and Dr. Robert Sharp. Additional thanks are extended to Dr. N. N. Ambraseys of Imperial College of Science and Technology in London, Mr. Waverly Person of the U.S. Geological Survey, and Dr. Lloyd S. Cluff of Pacific Gas and Electric Company. Thanks are also extended to Mr. Michael G. Melkumian and translator Ms. Susi of the Armenian Scientific Research Institute of Civil Engineering and Architecture in Yerevan, Armenian SSR, USSR, who were instrumental in obtaining information during the second investigative effort. The authors and EPRI would also like to thank Mr. Hevhanisjan Sewada of the Soviet Academy of Sciences, Leninakan, and Mr. Ruslan Martizasian of the Institute of Geophysics, Leninakan, who most graciously accommodated our requests during the second investigative effort. -
Teleseismic Body Wave Analysis of the 1988 Armenian Earthquake
GEOPHYSICALRESEARCH LETTERS, VOL. 16, NO. 12, PAGES1425-1428, DECEMBER1989 TELESEISMICBODY WAVE ANALYSIS OF THE 1988 ARMENIAN EARTHQUAKE J.F. Pachecol,2, C. H. Estabrookl,2, D. W. Simpson2 and J. L. N•b•lek3 Abstract.Long-period and broadband body waves from 14 50 ø digital seismicstations are usedto investigatethe rupture processof the December7, 1988 earthquakenear Spitak, i'......... " ' .--.GC Armenia, USSR. The inversionof thesedata gives the 40 ø followingcentroidal source parameters: strike 299 ø, dip 64ø, rake 151ø, depth6.3 km and seismicmoment 1.5x1019 Nm, .,!-•,".<• -, indicatingthat on averagethe earthquakehad a strike-slip 30 ø mechanismwith a substantialreverse component.The broadband waveforms, however, show significant complexity;they are bestfit with a sourcemodel that includes 20 ø 40 ø 60 ø three sub-events,very similar in size, but with distinctfocal mechanismsand locations. Rupture apparently initiated as a shallowreverse fault at a point of maximumbending on a right-lateralstrike-slip fault, andthen extended bilaterally, 41.0 first towards the southeast and then towards the west. This interpretationagrees with the aftershockdistribution and fault lineationsobserved on LANDSAT images. 40.9 Introduction 40.8 Focal parametersof the devastatingearthquake of December7, 1988near Spitak, Armenia, USSR, reported by 40.7 the National EarthquakeInformation Center (NEIC) are: 43.8 43.9 44.0 44.1 44.2 44.3 44.4 44.5 Ms=6.8, origin time 07h 41m 24.9s, latitude 40.987ø N, Fig. 1. Top figure shows NEIC location of the 1988 longitude44.185 ø E, and 10 km depth.Extensive casualties Armenianearthquake (star). Main plateboundaries and faults anddamage occurred at the townof Spitak,just southof the aredrawn on the map as solidand dashed lines. -
Results and Data from Seismologic and Geologic Studies Following Earthquakes of December 7, 1988, Near Spitak, Armenia S.S.R
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY RESULTS AND DATA FROM SEISMOLOGIC AND GEOLOGIC STUDIES FOLLOWING EARTHQUAKES OF DECEMBER 7, 1988, NEAR SPITAK, ARMENIA S.S.R. edited by Roger D. Borcherdt Volume I OPEN-FILE REPORT 89-163A This report (map) is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards (and stratigraphic nomenclature). Any use of trade names is for descriptive purposes only and does not imply endorsement by the U.S.G.S. Menlo Park, California 1989 TABLE OF CONTENTS VOLUME 1 Page No. PREFACE ........................... iv FOREWORD ......................... v SUMMARY .......................... vi 1. INVESTIGATIONS CONDUCTED BY THE U.S. TEAM FOLLOWING THE EARTHQUAKES OF DECEMBER 7, 1988, NEAR SPITAK, ARMENIA S.S.R. ................. 1 J. Filson 2. INTRODUCTION FOR SEISMOLOGIC AND GEOLOGIC STUDIES CONDUCTED FOLLOWING THE EARTHQUAKES OF DECEMBER 7, 1988, NEAR SPITAK, ARMENIA S.S.R. ...... 9 R. Borcherdi, R. Sharp, D. Simpson, and C. Langer 3. TECTONIC SETTING AND SEISMIC SETTING FOR THE MAIN SHOCK OF DECEMBER 7, 1988 .............. 11 J. Filson 4. SURFACE FAULTING INVESTIGATIONS .............. 21 R. Sharp 5. SEISMOLOGICAL INVESTIGATIONS (OBJECTIVES AND FIELD EXPERIMENTS) ..................... 35 R. Borcherdt, D. Simpson, C, Langer, G. Sembera, C. Dietel, E. Cranswick, C. Mueller, T. Noce, M. Andrews, and G. Glassmoyer 6. INSTRUMENTATION USED FOR SEISMOLOGICAL INVESTIGATIONS ....................... 43 1.) Digital Recording Systems - R. Borcherdt, G. Maxwell, J. Sena, M. Kennedy, G. Jensen, and J. Van Schaack ............. 43 2.) Field Computer and Playback of Digital Data - G. Maxwell and M. Kennedy ......................... 46 3.) Analog Recording Systems - C. Langer and D. Simpson ........ 47 4.) Automated Computer Processing of the Armenian Data Set Recorded by GEOS Portable Autonomous Digital Seismographs (PADS) - E. -
Strong Ground Motion
The Lorna Prieta, California, Earthquake of October 17, 1989-Strong Ground Motion ROGER D. BORCHERDT, Editor STRONG GROUND MOTION AND GROUND FAILURE Thomas L. Holzer, Coordinator U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1551-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Manuscript approved for publication, October 6, 1993 Text and illustrations edited by George A. Havach Library of Congress catalog-card No. 92-32287 For sale by U.S. Geological Survey, Map Distribution Box 25286, MS 306, Federal Center Denver, CO 80225 CONTENTS Page A1 Strong-motion recordings ---................................. 9 By A. Gerald Brady and Anthony F. Shakal Effect of known three-dimensional crustal structure on the strong ground motion and estimated slip history of the earthquake ................................ 39 By Vernon F. Cormier and Wei-Jou Su Simulation of strong ground motion ....................... 53 By Jeffry L. Stevens and Steven M. Day Influence of near-surface geology on the direction of ground motion above a frequency of 1 Hz----------- 61 By John E. Vidale and Ornella Bonamassa Effect of critical reflections from the Moho on the attenuation of strong ground motion ------------------ 67 By Paul G. Somerville, Nancy F. Smith, and Robert W. Graves Influences of local geology on strong and weak ground motions recorded in the San Francisco Bay region and their implications for site-specific provisions ----------------- --------------- 77 By Roger D. -
Subject Index
Subject index Page references to UN agencies and international, regional, B Bangladesh 2, 6, 8, 46, 82, 88, 135, 160, 171, 177, 182, national and specialized organisations are not listed in this 183, 186, 188, 193, 240, 305, 307, 308, 310, 327, 328, index. Instead, they appear in annex 2 (international, regional, 329, 349, 350, 354, 365, 377, 380 national and specialized organisations) and annex 3 (UN Bangladesh Coastal Greenbelt Project 305 agencies). Bangladesh Urban Disaster Mitigation Project 183 community-based approach to reduce the vulnerability of flood-prone communities in the Tongi and Gaibandha A adaptation municipalities 182, 183 see climate, change 2000-2002 comprehensive disaster management afforestation /reforestation 19, 28, 181, 182, 279, 300, 301, programme 82 306, 394 Climate Forecasting Applications 377 Afghanistan 51, 307, (annex 3, 83) Cyclone Preparedness Programme (CPP) 365 Africa 31, 98, 149, 200, 349 Flood Action Plan 6, 88, 310 Agenda 21: 139, 301, 302, 309, (annex 4, 97, 102, 106) Natural Disaster Management Plan 88 agriculture (and farming) 14, 19, 26, 31, 51, 55, 58, 62, 83, 95, Standing Orders on Disaster 88 106, 123, 146, 150, 166, 278, 305, 311, 351, 376, 391, 395 2001: State of the Environment 305, 310 Agricultural Markets Information System 228 Barbados 358, (annex 3, 89) see United States 1994: Barbados Global Conference on the Sustainable Honduran National Network for the Promotion of Ecological Development of Small Island Developing States 358 Agriculture (ANAFAE) 278 Barbados Plan of Action (annex -
Glasnost in Jeopardy Glasnost in Jeopardy
GLASNOST IN JEOPARDY Human Rights in the USSR April 1991 A Helsinki Watch Report 485 Fifth Avenue 1522 K Street, NW, #910 New York, NY 10017 Washington, DC 20005 Tel (212) 972-8400 Tel (202) 371-6592 Fax (212) 972-0905 Fax (202) 371-0124 Copyright 8 March 1991 by Human Rights Watch All Rights Reserved. Printed in the United States of America. ISBN 0-929692-89-6 Library of Congress Catalogue Card Number 91-71495 Cover Design by Deborah Thomas The Helsinki Watch Committee Helsinki Watch was formed in 1978 to monitor and promote observance of domestic and international compliance with the human rights provisions of the 1975 Helsinki Accords. The Chairman is Robert L. Bernstein; Vice Chairs, Jonathan Fanton and Alice Henkin; Executive Director, Jeri Laber; Deputy Director, Lois Whitman; Washington Representative, Catherine Cosman; Staff Counsel, Holly Cartner and Theodore Zang, Jr.; Staff Consultant, Ivana Nizich; Orville Schell Intern, Robert Kushen; Intern, Jemima Stratford; Associates, Sarai Brachman, Mia Nitchun, and Elisabeth Socolow. Helsinki Watch is affiliated with the International Helsinki Federation for Human Rights, which is based in Vienna. Human Rights Watch Helsinki Watch is a component of Human Rights Watch, which includes Americas Watch, Asia Watch, Africa Watch, and Middle East Watch. The Chairman is Robert L. Bernstein and the Vice Chairman is Adrian W. DeWind. Aryeh Neier is Executive Director; Kenneth Roth, Deputy Director; Holly J. Burkhalter, Washington Director; Susan Osnos, Press Director. Executive Directors Africa Watch, Rakiya Omaar; Americas Watch, Juan Mendez; Asia Watch, Sidney R. Jones; Helsinki Watch, Jeri Laber; Middle East Watch, Andrew Whitley. -
Paradoxical South Caucasus: Nations, Conflicts and Alliances A
Paradoxical South Caucasus: Nations, Conflicts and Alliances A thesis presented to the faculty of the College of Arts and Sciences of Ohio University In partial fulfillment of the requirements for the degree Master of Arts Gevorg Melikyan August 2010 © 2010 Gevorg Melikyan. All Rights Reserved. 2 This thesis titled Paradoxical South Caucasus: Nations, Conflicts and Alliances by GEVORG MELIKYAN has been approved for the Department of Political Science and the College of Arts and Sciences by Patricia A. Weitsman Professor of Political Science Benjamin M. Ogles Dean, College of Arts and Sciences 3 ABSTRACT MELIKYAN, GEVORG, M.A., August 2010, Political Science Paradoxical South Caucasus: Nations, Conflicts and Alliances (172 pp.) Director of Thesis: Patricia A. Weitsman On one hand, the collapse of the Soviet Union was the end of a number of insolvable issues; on the other, it created new, no less challenging ones with which states that emerged from the ashes of the Red Empire had to deal. Ancient hatreds, hostilities and violence became an inseparable part of the South Caucasus where confrontations closed ways to cooperation and peace. How did the Soviet Union generate these hatreds and conflicts? Why these threats and bloody armed conflicts? Where do they come from? How does each state react to those threats? The newly independent states even had to fight each other by forming, inter alia, powerful military alliances. What are the dynamics and implications of the alliance formation in the South Caucasus? How do these states choose their strategic-military allies? To what extent do heterogeneous military alliances between Armenia and Russia or Azerbaijan and Turkey, along with Georgia’s effort to join NATO at any price despite negative messages from Russia, stabilize or destabilize the overall status-quo in the region? What drives those newly independent states in choosing their partners? Are those alliances cohesive? If so, how so? These questions are at the core of this research and are discussed and explored along with other important issues and conundrums. -
SOVIET DECISIONMAKING for CHERNOBYL : an ANALYSIS of SYSTEM PERFORMANCE and POLICY CHANG E By
NATIONAL COUNCIL FOR SOVIET AND EAST EUROPEAN RESEARC H TITLE : SOVIET DECISION_MAKING FOR CHERNOBYL : An Analysis of System Performance an d Policy Chang e AUTHOR : William C. Potte r CONTRACTOR : University of California, Los Angele s PRINCIPAL INVESTIGATOR : William C . Potte r COUNCIL CONTRACT NUMBER : 802-1 2 DATE : March, 199 0 The work leading to this report was supported by funds provided by the National Council for Soviet and East European Research . Th e analysis and interpretations contained in the report are those o f the author . EXECUTIVE SUMMARY SOVIET DECISIONMAKING FOR CHERNOBYL : AN ANALYSIS OF SYSTEM PERFORMANCE AND POLICY CHANG E by William C . Potte r This report analyzes the systemic (as opposed to technical ) factors which contributed to the April 26, 1986 Chernobyl nuclea r accident, assesses the performance of the major organizationa l actors at Chernobyl, analyzes the impact of the accident on polic y change with respect to nuclear safety, and discerns lessons fro m the performance of Soviet organizations at Chernobyl that may b e applicable to other crisis situations . Its major conclusions may be summarized as follows : * Chernobyl was only the latest and most catastrophic in a lon g series of sometimes fatal accidents at Soviet nuclear powe r facilities ; * The Chernobyl accident should not have been totall y unanticipated, especially when viewed against the prior record o f accidents at Soviet nuclear facilities ; * Gorbachev may have been the patron of one of the few pre - Chernobyl nuclear safety critics -
The 2002 Denali Fault and 2001 Kunlun Fault Earthquakes: Complex Rupture Processes of Two Large Strike-Slip Events by A
Bulletin of the Seismological Society of America, Vol. 94, No. 6B, pp. S278–S292, December 2004 The 2002 Denali Fault and 2001 Kunlun Fault Earthquakes: Complex Rupture Processes of Two Large Strike-Slip Events by A. Arda Ozacar and Susan L. Beck Abstract We studied the source processes of two large continental earthquakes, the 3 November 2002 Denali fault earthquake and the 14 November 2001 Kunlun fault earthquake, associated with strike-slip faulting along ancient sutures. We in- verted teleseismic P waveforms using a pulse-stripping method for multiple time windows with different focal mechanisms and derived composite source models. According to our results, the 2002 Denali fault earthquake began with initial thrusting (Mw 7.3) along a 40-km-long segment of the north-northwest-dipping Susitna Glacier fault and later ruptured a 300-km-long segment along the Denali and Totschunda faults with a right-lateral strike-slip mechanism (Mw 7.7). In contrast, the 2001 Kun- lun fault earthquake nucleated near an extensional step-over with a subevent pair consisting of 30-km-long strike-slip (Mw 6.9) event and 40-km-long normal (Mw 6.8) faulting event and later ruptured a 350-km-long segment along the Kunlun fault with a left-lateral strike-slip mechanism (Mw 7.7). Both earthquakes propagated primarily unilaterally to the east and released most of their energy along slip patches (asperities) far from the hypocenter locations. We find that both the Denali fault and Kunlun fault earthquakes had high-average rupture velocities of 3.2 km/sec and 3.4 km/sec, respectively. -
Industry and Society in Baku, Azerbaijan, 1870- Present
OIL CAPITAL: INDUSTRY AND SOCIETY IN BAKU, AZERBAIJAN, 1870- PRESENT by REBECCA LINDSAY HASTINGS A DISSERTATION Presented to the Department of History and the Graduate School of the University of Oregon in partial fulfillment of the requirements for the degree of Doctor of Philosophy June 2020 DISSERTATION APPROVAL PAGE Student: Rebecca Lindsay Hastings Title: Oil Capital: Industry and Society in Baku, Azerbaijan, 1870-Present This dissertation has been accepted and approved in partial fulfillment of the requirements for the Doctor of Philosophy degree in the Department of History by: Julie Hessler Chairperson, Advisor Julie Weise Core Member Ryan Jones Core Member Alexander Murphy Institutional Representative and Kate Mondloch Interim Vice Provost and Dean of the Graduate School Original approval signatures are on file with the University of Oregon Graduate School Degree awarded June 2020 ii © 2020 Rebecca Lindsay Hastings iii DISSERTATION ABSTRACT Rebecca Lindsay Hastings Doctor of Philosophy Department of History June 2020 Title: Oil Capital: Industry and Society in Baku, Azerbaijan, 1870-Present This dissertation is a historical study of the city of Baku, Azerbaijan, and its oil industry from the 1870s to the present, covering the tsarist Russian, Soviet, and post- Soviet eras. The history of the Baku oil industry offers a clear, focused example of the social and physical effects of the imposition of external parties’ financial and commodity demands on an urban-industrial setting. Baku as an urban environment, comprising not just the physical elements of the city but also its sociocultural communities, has embodied priorities imposed on the oil industry that have shifted as the global importance of oil and natural gas has grown, as those commodities’ uses have changed over time, and according to successive regimes’ respective political and economic ideologies. -
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Arm enia General Inform ation Armenia is a country with an approximate area of 30 thousand sq. km. (UNO, 2001). Its population is 3.052 million, and the sex ratio (men per hundred women) is 94 (UNO, 2004). The proportion of population under the age of 15 years is 19% (UNO, 2004), and the proportion of population above the age of 60 years is 13% (WHO, 2004). The literacy rate is 99.7% for men and 99.2% for women (UNESCO/MoH, 2004). The country is a lower middle income group country (based on World Bank 2004 criteria). The proportion of health budget to GDP is 7.8% . The per capita total expenditure on health is 273 international $, and the per capita government expenditure on health is 112 international $ (WHO, 2004). The main language(s) used in the country is (are) Armenian and Russian. The largest ethnic group(s) is (are) Armenian. The largest religious group(s) is (are) Armenian Apostolic Christian. The life expectancy at birth is 67 years for males and 73 years for females (WHO, 2004). The healthy life expectancy at birth is 59 years for males and 63 years for females (WHO, 2004). Epidem iology Recent data (2000-2002) obtained on a representative sample (n=395) by means of a specially elaborated unified questionnaire and properly adapted and standardized Symptom Checklist (SCL-90R), Beck Depression Inventory (BDI) and Hospital Anxiety and Depression Scale (HADS) suggested high levels of emotional disorders in comparison to that reported in Western Europe and Russia. Anxiety and depression were significantly higher in those areas reporting an inability to access medical aid due to financial reasons.