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A Review of Geological Records of Large Tsunamis at Vancouver Island, British Columbia, and Implications for Hazard John J
Quaternary Science Reviews 19 (2000) 849}863 A review of geological records of large tsunamis at Vancouver Island, British Columbia, and implications for hazard John J. Clague! " *, Peter T. Bobrowsky#, Ian Hutchinson$ !Depatment of Earth Sciences and Institute for Quaternary Research, Simon Fraser University, Burnaby, BC, Canada V5A 1S6 "Geological Survey of Canada, 101 - 605 Robson St., Vancouver, BC, Canada V6B 5J3 #Geological Survey Branch, P.O. Box 9320, Stn Prov Govt, Victoria, BC, Canada V8W 9N3 $Department of Geography and Institute for Quaternary Research, Simon Fraser University, Burnaby, Canada BC V5A 1S6 Abstract Large tsunamis strike the British Columbia coast an average of once every several hundred years. Some of the tsunamis, including one from Alaska in 1964, are the result of distant great earthquakes. Most, however, are triggered by earthquakes at the Cascadia subduction zone, which extends along the Paci"c coast from Vancouver Island to northern California. Evidence of these tsunamis has been found in tidal marshes and low-elevation coastal lakes on western Vancouver Island. The tsunamis deposited sheets of sand and gravel now preserved in sequences of peat and mud. These sheets commonly contain marine fossils, and they thin and "ne landward, consistent with deposition by landward surges of water. They occur in low-energy settings where other possible depositional processes, such as stream #ooding and storm surges, can be ruled out. The most recent large tsunami generated by an earthquake at the Cascadia subduction zone has been dated in Washington and Japan to AD 1700. The spatial distribution of the deposits of the 1700 tsunami, together with theoretical numerical modelling, indicate wave run-ups of up to 5 m asl along the outer coast of Vancouver Island and up to 15}20 m asl at the heads of some inlets. -
Individual Artist Fellowships C.O.L.A
INDIVIDUAL ARTIST FELLOWSHIPS C.O.L.A. 2013 C.O.L.A. 2013 INDIVIDUAL ARTIST FELLOWSHIPS Department of Cultural Affairs City of Los Angeles This catalog accompanies an exhibition and performance series sponsored by the City of Los CITY OF Angeles Department of Cultural Affairs featuring LOS ANGELES its C.O.L.A. 2013 Individual Artist Fellowship recipients in the visual and performing arts. 2013 INDIVIDUAL Exhibition: May 19 to July 7, 2013 ARTIST Los Angeles Municipal Art Gallery FELLOWSHIPS Barnsdall Park Opening Reception: May 19, 2013, 2 to 5 p.m. Performances: June 28, 2013 Grand Performances 2 Antonio R. Villaraigosa LOS ANGELES CITY COUNCIL CULTURAL AFFAIRS COMMISSION Department of Cultural Affairs DEPARTMENT OF CULTURAL AffaiRS Mayor City of Los Angeles City of Los Angeles City of Los Angeles Ed P. Reyes, District 1 York Chang Paul Krekorian, District 2 President Olga Garay-English Aileen Adams Dennis P. Zine, District 3 The Department of Cultural Affairs (DCA) generates and supports high-quality Executive Director Deputy Mayor Tom LaBonge, District 4 Josephine Ramirez arts and cultural experiences for Los Angeles’s 4 million residents and 40 million Strategic Partnerships Paul Koretz, District 5 Vice President Senior Staff Tony Cardenas, District 6 annual overnight and day visitors. DCA advances the social and economic impact of the arts and ensures access to diverse and enriching cultural activities through Richard Alarcon, District 7 Maria Bell Matthew Rudnick Bernard C. Parks, District 8 Annie Chu grant making, marketing, public art, community arts programming, arts education, Assistant General Manager Jan Perry, District 9 Charmaine Jefferson and building partnerships with artists and arts and cultural organizations in Herb J. -
California North Coast Offshore Wind Studies
California North Coast Offshore Wind Studies Overview of Geological Hazards This report was prepared by Mark A. Hemphill-Haley, Eileen Hemphill-Haley, and Wyeth Wunderlich of the Humboldt State University Department of Geology. It is part of the California North Coast Offshore Wind Studies collection, edited by Mark Severy, Zachary Alva, Gregory Chapman, Maia Cheli, Tanya Garcia, Christina Ortega, Nicole Salas, Amin Younes, James Zoellick, & Arne Jacobson, and published by the Schatz Energy Research Center in September 2020. The series is available online at schatzcenter.org/wind/ Schatz Energy Research Center Humboldt State University Arcata, CA 95521 | (707) 826-4345 California North Coast Offshore Wind Studies Disclaimer This study was prepared under contract with Humboldt State University Sponsored Programs Foundation with financial support from the Department of Defense, Office of Economic Adjustment. The content reflects the views of the Humboldt State University Sponsored Programs Foundation and does not necessarily reflect the views of the Department of Defense, Office of Economic Adjustment. This report was created under Grant Agreement Number: OPR19100 About the Schatz Energy Research Center The Schatz Energy Research Center at Humboldt State University advances clean and renewable energy. Our projects aim to reduce climate change and pollution while increasing energy access and resilience. Our work is collaborative and multidisciplinary, and we are grateful to the many partners who together make our efforts possible. Learn more about our work at schatzcenter.org Rights and Permissions The material in this work is subject to copyright. Please cite as follows: Hemphill-Haley, M.A., Hemphill-Haley, E. and Wunderlich, W. (2020). -
Significant Aspects of Geotechnical and Seismic Engineering and Management of Bridges and Structures in the U.S
SIGNIFICANT ASPECTS OF GEOTECHNICAL AND SEISMIC ENGINEERING AND MANAGEMENT OF BRIDGES AND STRUCTURES IN THE U.S. M. Myint Lwin1 Abstract It is important to integrate the knowledge and experience of geotechnical and seismic engineering and management of bridges to make sound decisions to reduce earthquake damages to highways, bridges and structures. Research continues to play important roles in developing modern bridge seismic design criteria, detailing practices and seismic retrofit strategies for reducing structural damages and casualties. Bridge management systems can be used effectively to incorporate seismic assessment data for prioritizing seismic retrofit needs. Introduction Major earthquakes, such as the 1964 Alaska Earthquake, Anchorage, Alaska; the 1989 Loma Prieta Earthquake, California; the 1994 Northridge Earthquake, California; the 1995 Kobe Earthquake, Japan; and so on, have taken thousands of lives, caused billions of dollars in damages, and incurred other indirect costs as a result of damage to bridges and structures, highways, and other public facilities. It is necessary to integrate the knowledge and experience in geotechnical and seismic engineering, and the management of bridges and structures, and other public facilities to mitigate seismic hazards. The important seismic hazards are strong ground shaking, ground failures (such as, liquefaction, lateral spread, differential settlement, landslides), soil-structure interaction, and other indirect effects caused by ground shaking and failures, such as, tsunamis, seiches, floods and fires. The engineers and code writers must take these seismic hazards into account in developing earthquake-resistant design, construction and management. Seismologic and Geologic Aspect of Earthquakes When an earthquake occurs, seismic waves traveled from the source to the earth’s surface through body waves and surface waves. -
Aleutian Island Arc Magma Production Rates and Mechanisms
https://doi.org/10.5194/se-2019-179 Preprint. Discussion started: 4 December 2019 c Author(s) 2019. CC BY 4.0 License. Aleutian island arc magma production rates and mechanisms Yongliang Bai1, Diya Zhang1, Dongdong Dong2, Shiguo Wu3, Zhenjie Wang1 1College of Ocean and Space Information, China University of Petroleum, Qingdao 266580, China 2Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 5 266071, China 3Institute of Deep-sea Science and Engineering, Chinese Academy of Sciences, Sanya 572000, China Correspondence to: Yongliang Bai ([email protected]) Abstract. The variation in island arc magma production rates and their influencing mechanisms are of great significance since island arc magma is considered a main source of continental crust growth. The island arc magma directly originates from the 10 molten mantle wedge, and the mantle melting is driven by fluids or melts from the subducted slab. Slab dehydration flux mainly depends on the slab thermal structures, and subducted slab melting requires a sufficiently high temperature. For the Aleutian subduction system, the subducted Pacific Plate has diverse thermal structures due to the existing fracture zones, ridges and slab window, so it is an ideal region for arc magma production rate research. However, the previous estimations are based on seismic profiles that only provide magma production rates at specific regions of the Aleutian arc, and these results are 15 controversial. Here, we design a magma production rate estimation method based on gravity inversion constrained by deep seismic profiles. The first overview map of magma production rates along the Aleutian arc strike demonstrates that the magma production rates have the same trend as the slab dips, and the peaks correspond to the subduction of the fracture zones and ridges. -
Proposed Program and Budget Estimates
Official Documents of the Pan American Health Organization No. 40 PROPOSED PROGRAM AND BUDGET ESTIMATES PAN AMERICAN HEALTH ORGANIZATION, 1963 WORLD HEALTH ORGANIZATION, REGION OF THE AMERICAS, 1964 PAN AMERICAN HEALTH ORGANIZATION, PROVISIONAL DRAFT, 1964 PAN AMERICAN HEALTH ORGANIZATION Pan American Sanitary Bureau, Regional Office of the WORLD HEALTH ORGANIZATION Washington, D. C. July 1962 Official Documents of the 152 74 Pan American Health Organization No. 40 '70o3 030 PROPOSED PROGRAM AND BUDGET ESTIMATES PAN AMERICAN HEALTH ORGANIZATION, 1963 WORLD HEALTH ORGANIZATION, REGION OF THE AMERICAS, 1964 PAN AMERICAN HEALTH ORGANIZATION, PROVISIONAL DRAFT, 1964 PAN AMERICAN HEALTH ORGANIZATION Pan American Sanitary Bureau, Regional Office of the WORLD HEALTH ORGANIZATION 1501 New Hampshire Ave., N.W. Washington 6, D. C., U. S. A. ii ABBREVIATIONS AID Agency for International Development AIDIS Asociación Interamericana de Ingenieria Sanitaria AMRO The Americas Regional Office (Regional symbol for Intercountry and Interzone Projects) BCG Bacillus Calmette-Cuerin DDT Dichlorodiphenyltrichloroethane FAO Food and Agriculture Organization IADB Inter-American Development Bank ILO International Labor Organization INCAP Institute of Nutrition of Central America and Panama MCH Maternal and Child Health OAS Organization of American-States PAHD Pan American Health Organization PASB Pan American Sanitary Bureau SCISP Servicio Cooperativo Interamericano de Salud Pública TPO Tripartite Plan of Operationa UCWI University College of the West Indies UN United Nations UNESCO United Nations Educational, Scientific and Cultural Organization Ung Ungraded UNICEF United Nations Children's Fund USA United States of America USPHS United States Public Health Service WHO World Health Organization WDO/TA World Health Organization/Technical Assistance r iii ¶TABLE OF CO NTE N T S TEext Details Text Details age Page Page Page Letter of Transmittal ix PART III Introduction 1 PAN AMERICAN HEALTH ORGANIZATION - FIELD AND OTHER PROGRAMS Method of Preparation 5 SECTION 1. -
What Happens When Plates Collide? Assessment
Name __________________________ Investigation 6: What Happens When Plates Collide? Assessment Answer the questions below in complete sentences. Part 1: Subduction Zones 1. How deep is the trench in the Aleutian subduction zone? The trench in the Aleutian subduction zone is approximately 7,000 m below sea level. The deepest point on the elevation profile is 6,921 m below sea level. 2. a. What is the height of the volcano along the elevation profile? The highest volcano along the elevation profile is 2,517 meters in elevation (Shishaldin on Unimak Island). The actual height of the volcanoes is 2,857 meters according to the Web GIS data set. Note: When discussing this answer with students, you may point out that the elevation profile line was not drawn through the volcano’s peak. b. On which plate is this volcano located? The Shishaldin volcano is on North American Plate. 3. What is the name of the plate immediately north of the Aleutian Trench? The North American Plate is the plate located immediately north of the Aleutian Trench. 4. What is the name of the plate immediately south of the Aleutian Trench? The Pacific Plate is the plate located immediately south of the Aleutian Trench. 5. What type of plate boundary is located along the eastern section of the Aleutian Trench where most volcanoes are located? The plate boundary is convergent in the eastern section of the Aleutian Trench where most volcanoes are located. 6. What type of plate boundary is located along the western section of the Aleutian Trench where volcanoes are absent? The plate boundary is transform in the western section of the Aleutian Trench where volcanoes are absent. -
How to Survive Earthquakes and Tsunamis in Oregon
Living on Shaky Ground How to survive earthquakes and tsunamis in Oregon Copyright 2018, Oregon Office of Emergency Management with help from the Oregon Department of Geology and Mineral Industries. Originally adapted from Humboldt Earthquake Education Center at Humboldt State University. Reproduction by permission only. Disclaimer: This document is intended to promote earthquake and tsunami readiness. It is based on the best currently available scientific, engineering, and sociological research. Following its suggestions, however, does not guarantee the safety of an individual or of a structure. Contributors • Michael Murphy, Coos County • Patence Winningham, City of Eugene • Justin Ross, Multnomah County • Cynthia Valdivia, Washington County • Bonny Cushman, City of Portland • Barbara Ayers, Hood River County • Curtis Peetz, American Red Cross • John Bowles, Morrow County • Virginia Demaris, Lincoln County • Terri Eubanks, City of Ashland • Althea Rizzo, Oregon Office of Emergency Management • Paula Negele, Oregon Office of Emergency Management ii Oregon Office of Emergency Management Introduction You can prepare for the What do I do? next quake or tsunami an earthquake you should: During Some people think it is not worth preparing for • If you are indoors, DROP and take COVER an earthquake or a tsunami because whether you under a sturdy table or other furniture. HOLD survive or not is up to chance. NOT SO! ON to it and stay put until the shaking stops. Most Oregon buildings will survive even a large • Stay clear of items that can fall and injure you, earthquake, and so will you, especially if you such as windows, fireplaces and heavy furniture. follow the simple guidelines in this handbook • Stay inside. -
The 1964 Prince William Sound Earthquake Subduction Zone Steven C
Adv. Geophys. ms. Last saved: 2/12/2003 6:lO:OO PM 1 Crustal Deformation in Southcentral Alaska: The 1964 Prince William Sound Earthquake Subduction Zone Steven C. Cohen Geodynamics Branch, Goddard Space Flight Center, Greenbelt, MD 2077 1 email: Steven.C.Cohen @ .nasa.gov; phone: 301-6 14-6466 Jeffrey T. Freymueller Geophysical Institute, University of Alaska, Fairbanks, AK 99775 Outline: 1. Introduction 2. Tectonic, Geologic, and Seismologic Setting 3. Observed Crustal Motion 3.1 Coseismic Crustal Motion 3.2 Preseismic and Interseismic (pre-1964) Crustal Motion 3.3 Postseismic and Interseismic (post-1964) Crustal Motion 4. Models of Southcentral Alaska Preseismic and Postseismic Crustal Deformation 5. Conclusions 6. References Adv. Geophys. ms. Last saved: a1 a2003 6:lO:OO PM 2 1. Introduction The M, = 9.2 Prince William Sound (PWS) that struck southcentral Alaska on March 28, 1964, is one of the important earthquakes in history. The importance of this Great Alaska Earthquake lies more in its scientific than societal impact. While the human losses in the PWS earthquake were certainly tragic, the sociological impact of the earthquake was less than that of is earthquakes that have struck heavily populated locales. By contrast Earth science, particularly tectonophysics, seismology, and geodesy, has benefited enormously from studies of this massive earthquake. The early 1960s was a particularly important time for both seismology and tectonophysics. Seismic instrumentation and analysis techniques were undergoing considerable modernization. For example, the VELA UNIFORM program for nuclear test detection resulted in the deployment of the World Wide Standard Seismographic Network in the late 1950s and early 1960s (Lay and Wallace, 1995). -
Dating the 1700 Cascadia Earthquake: Great Coastal Earthquakes in Native Stories
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/252069651 Dating the 1700 Cascadia Earthquake: Great Coastal Earthquakes in Native Stories Article in Seismological Research Letters · March 2005 DOI: 10.1785/gssrl.76.2.140 CITATIONS READS 52 1,359 10 authors, including: R. S. Ludwin Deborah Carver University of Washington Seattle University of Alaska Anchorage 18 PUBLICATIONS 188 CITATIONS 2 PUBLICATIONS 62 CITATIONS SEE PROFILE SEE PROFILE Robert J. Losey John J. Clague University of Alberta Simon Fraser University 86 PUBLICATIONS 648 CITATIONS 458 PUBLICATIONS 11,366 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Sedimentological and Paleomagnetic Study of Glacial Lake Missoula Lacustrine and Flood Sediment View project PALEOECOLOGY OF HAIDA GWAII View project All content following this page was uploaded by Robert J. Losey on 03 June 2014. The user has requested enhancement of the downloaded file. Dating the 1700 Cascadia Earthquake: Great Coastal Earthquakes in Native Stories Ruth S. Ludwin1, Robert Dennis2, Deborah Carver3, Alan D. McMillan4, Robert Losey5, John Clague6, Chris Jonientz-Trisler7, Janine Bowechop8, Jacilee Wray9, and Karen James10 INTRODUCTION were killed when their roots were suddenly plunged into salt water. Beneath the surface of these same estuaries, soil cores Although scientific recognition of the earthquake hazard pre- revealed layered deposits showing a repeated cycle of slow sented by the Cascadia subduction zone (CSZ) is relatively uplift and rapid submergence. Preliminary age estimates recent, native peoples have lived on the Cascadia coast for based on radiocarbon dating (Nelson et al., 1995) and tree- thousands of years, transferring knowledge from generation ring studies (Yamaguchi et al., 1989) suggested that the most to generation through storytelling. -
Observed Performance of Dams During Earthquakes Vol. 3
United States Society on Dams Observed Performance of Dams During Earthquakes Volume III February 2014 United States Society on Dams Observed Performance of Dams During Earthquakes Volume III Volume III February 2014 Prepared by the USSD Committee on Earthquakes U.S. Society on Dams Vision To be the nation's leading organization of professionals dedicated to advancing the role of dams for the benefit of society. Mission — USSD is dedicated to: · Advancing the knowledge of dam engineering, construction, planning, operation, performance, rehabilitation, decommissioning, maintenance, security and safety; · Fostering dam technology for socially, environmentally and financially sustainable water resources systems; · Providing public awareness of the role of dams in the management of the nation's water resources; · Enhancing practices to meet current and future challenges on dams; and · Representing the United States as an active member of the International Commission on Large Dams (ICOLD). The information contained in this report regarding commercial products or firms may not be used for advertising or promotional purposes and may not be construed as an endorsement of any product or firm by the United States Society on Dams. USSD accepts no responsibility for the statements made or the opinions expressed in this publication. Copyright © 2014 U. S. Society on Dams Printed in the United States of America ISBN 978-1-884575-65-5 Library of Congress Control Number: 2014932950 U.S. Society on Dams 1616 Seventeenth Street, #483 Denver, CO 80202 Telephone: 303-628-5430 Fax: 303-628-5431 E-mail: [email protected] Internet: www.ussdams.org FOREWORD In July, 1992, the U. S. -
Along-Strike Variation in Lavas of the Aleutian Island Arc: Implications for the Genesis of High Mg# Andesite and the Continental Crust
Along-strike Variation in Lavas of the Aleutian Island Arc: Implications for the Genesis of High Mg# Andesite and the Continental Crust Peter B. Kelemen1, Gene M. Yogodzinski2 and David W. Scholl3 1: Dept. of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543; [email protected] 2: Dept. of Geological Sciences, University of South Carolina, Columbia, SC 29208 3: Dept. of Geophysics, Stanford University, Stanford, CA, 94035; [email protected] submitted to AGU Geophysical Monograph Series, John Eiler, editor 6/01 ABSTRACT Western Aleutian, high Mg# andesite compositions bracket the composition of the continental crust. This is not due to recycling of terrigenous sediments. Is juvenile continental crust being produced in the western Aleutians? If so, how? These questions form the rationale for our paper. Based on a compilation of whole rock geochemistry for approximately 1100 lava samples and 200 plutonic rock samples from the Aleutian island arc, we characterize along-strike variation, including data for the western part of the arc which has recently become available. The composition of primitive magmas (molar Mg# > 0.6) varies systematically along the strike of the arc. Concentrations of SiO2, Na2O and perhaps K2O increase from east to west, while MgO, FeO, CaO decrease from east to west. Thus, primitive magmas in the central and eastern Aleutians (east of 174°W) are mainly basalts, while those in the western Aleutians are mainly andesites. Along-strike variation in Aleutian magma compositions may be related to a westward decrease in sediment input, and/or to the westward decrease in down-dip subduction velocity.