Puget Sound Tsunami Sources—2002 Workshop Report
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Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information
Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information Index Abancay Deflection, 201, 204–206, 223 Allmendinger, R. W., 206 Abant, Turkey, earthquake of 1957 Ms 7.0, 286 allochthonous terranes, 26 Abdrakhmatov, K. Y., 381, 383 Alpine fault, New Zealand, 482, 486, 489–490, 493 Abercrombie, R. E., 461, 464 Alps, 245, 249 Abers, G. A., 475–477 Alquist-Priolo Act, California, 75 Abidin, H. Z., 464 Altay Range, 384–387 Abiz, Iran, fault, 318 Alteriis, G., 251 Acambay graben, Mexico, 182 Altiplano Plateau, 190, 191, 200, 204, 205, 222 Acambay, Mexico, earthquake of 1912 Ms 6.7, 181 Altunel, E., 305, 322 Accra, Ghana, earthquake of 1939 M 6.4, 235 Altyn Tagh fault, 336, 355, 358, 360, 362, 364–366, accreted terrane, 3 378 Acocella, V., 234 Alvarado, P., 210, 214 active fault front, 408 Álvarez-Marrón, J. M., 219 Adamek, S., 170 Amaziahu, Dead Sea, fault, 297 Adams, J., 52, 66, 71–73, 87, 494 Ambraseys, N. N., 226, 229–231, 234, 259, 264, 275, Adria, 249, 250 277, 286, 288–290, 292, 296, 300, 301, 311, 321, Afar Triangle and triple junction, 226, 227, 231–233, 328, 334, 339, 341, 352, 353 237 Ammon, C. J., 464 Afghan (Helmand) block, 318 Amuri, New Zealand, earthquake of 1888 Mw 7–7.3, 486 Agadir, Morocco, earthquake of 1960 Ms 5.9, 243 Amurian Plate, 389, 399 Age of Enlightenment, 239 Anatolia Plate, 263, 268, 292, 293 Agua Blanca fault, Baja California, 107 Ancash, Peru, earthquake of 1946 M 6.3 to 6.9, 201 Aguilera, J., vii, 79, 138, 189 Ancón fault, Venezuela, 166 Airy, G. -
2021 WSTC Tolling Report and Tacoma Narrows Bridge Loan Update
2021 WSTC TOLLING REPORT & TACOMA NARROWS BRIDGE LOAN UPDATE January 2021 2021 WSTC TOLLING REPORT & TACOMA NARROWS BRIDGE LOAN UPDATE TABLE OF CONTENTS Introduction 4 SR 16 Tacoma Narrows Bridge 7 2020 Commission Action 7 2021 Anticipated Commission Action 7 SR 99 Tunnel 8 2020 Commission Action 8 2021 Anticipated Commission Action 8 SR 520 Bridge 9 2020 Commission Action 9 2021 Anticipated Commission Action 9 I-405 Express Toll Lanes & SR 167 HOT Lanes 10 2020 Commission Action 10 2021 Anticipated Commission Action 11 I-405 Express Toll Lanes & SR 167 HOT Lanes Low Income Tolling Program Study 11 Toll Policy & Planning 12 Toll Policy Consistency 12 Planning for Future Performance & Operations 12 Looking Forward To Future Tolled Facilities 13 2021 Tolling Recommendations 14 Summary of Current Toll Rates and Revenues by Facility 16 2021 Tacoma Narrows Bridge Loan Update 17 2019-21 Biennium Loan Estimates 17 2021-23 Biennium Loan Estimates 18 Comparison of Total Loan Estimates: FY 2019 – FY 2030 18 TNB Loan Repayment Estimates 19 2021 Loan Update: Details & Assumptions 20 Factors Contributing to Loan Estimate Analysis 20 Financial Model Assumptions 21 P age 3 2021 WSTC TOLLING REPORT & TACOMA NARROWS BRIDGE LOAN UPDATE INTRODUCTION As the State Tolling Authority, the Washington State Transportation Commission (Commission) sets toll rates and polices for all tolled facilities statewide, which currently include: the SR 520 Bridge, the SR 16 Tacoma Narrows Bridge, the I-405 express toll lanes (ETLs), the SR 167 HOT lanes, and the SR 99 Tunnel. -
Executive Summary San Juan Islands Scenic Byway Corridor Management Plan
execuTive SuMMary San Juan iSlandS Scenic byway corridor ManaGeMenT Plan whaT iS a corridor Purpose of Developing the ManaGeMenT Plan? Corridor Management Plan Citizens from communities on San Juan Island and Orcas Island, along with agency partners at the local, regional, state, and federal level, have joined A corridor management together to develop this corridor management plan (CMP), which charts a course for the future of the San Juan Islands Scenic Byway. The CMP includes plan presents a clear recommendations for expanding stewardship and enhancing visitors’ experiences along the byway, while at the same time preserving the sensitive vision of what the scenic scenic, natural, archaeological, historic, cultural, and recreational resources of the islands and the quality of life enjoyed by islanders. CMP recommendations byway organization also include expanding multi-modal transportation options to reduce environmental impacts, enhance community livability, and improve visitor access. intends to accomplish. Telling Our Stories With specific strategies The CMP includes recommendations for telling the many interesting for managing tourism stories of the byway through interpretation, education, promotion, and hands-on stewardship activities. Through various projects and programs, and protecting unique visitors will become inspired as they learn and understand how islanders: natural and cultural • Live in this unique environment • Conserve energy and water; with a strong commitment to • Promote and enhance visitors’ resources, the plan sustainability and stewardship; experiences in the islands by • Protect natural resources such offering abundant recreation should reflect community as endangered wildlife, marine opportunities; life, and unique habitats; goals and respect local • Create and display diverse • Preserve and restore cultural works of art and architecture lifestyles and cultures. -
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. -
Earthquake Hazard
SUB-SECTION 4G.2 PUYALLUP TRIBE ALL HAZARD MITIGATION PLAN EARTHQUAKE HAZARD Table of Contents TABLE OF CONTENTS ............................................................................................... 1 IDENTIFICATION DESCRIPTION ................................................................................ 2 DEFINITION ............................................................................................................. 2 TYPES .................................................................................................................... 2 SECONDARY HAZARDS: ................................................................................................ 3 PROFILE ................................................................................................................... 5 LOCATION AND EXTENT ............................................................................................... 5 VULNERABILITY ....................................................................................................... 15 IMPACTS ............................................................................................................... 16 RESOURCE DIRECTORY .......................................................................................... 24 REGIONAL ............................................................................................................. 24 NATIONAL ............................................................................................................. 24 ENDNOTES ............................................................................................................ -
SR 16 Tacoma Narrows Bridge to SR 3 Congestion Study – December 2018
SR 16, Tacoma Narrows Bridge to SR 3, Congestion Study FINAL December 28, 2018 Olympic Region Planning P. O. Box 47440 Olympia, WA 98504-7440 SR 16 Tacoma Narrows Bridge to SR 3 Congestion Study – December 2018 This page intentionally left blank. SR 16 Tacoma Narrows Bridge to SR 3 Congestion Study – December 2018 Washington State Department of Transportation Olympic Region Tumwater, Washington SR 16 Tacoma Narrows Bridge to SR 3 Congestion Study Project Limits: SR 16 MP 8.0 to 29.1 SR 3 MP 30.4 to 38.9 SR 304 MP 0.0 to 1.6 December 2018 John Wynands, P.E. Regional Administrator Dennis Engel, P.E. Olympic Region Multimodal Planning Manager SR 16 Tacoma Narrows Bridge to SR 3 Congestion Study – December 2018 This page intentionally left blank. SR 16 Tacoma Narrows Bridge to SR 3 Congestion Study – December 2018 Title VI Notice to Public It is the Washington State Department of Transportation’s (WSDOT) policy to assure that no person shall, on the grounds of race, color, national origin or sex, as provided by Title VI of the Civil Rights Act of 1964, be excluded from participation in, be denied the benefits of, or be otherwise discriminated against under any of its federally funded programs and activities. Any person who believes his/her Title VI protection has been violated, may file a complaint with WSDOT’s Office of Equal Opportunity (OEO). For additional information regarding Title VI complaint procedures and/or information regarding our non- discrimination obligations, please contact OEO’s Title VI Coordinator at (360) 705-7082. -
Island County Fire Protection District No. 5 (Central Whidbey Island Fire and Rescue)
Financial Statements Audit Report Island County Fire Protection District No. 5 (Central Whidbey Island Fire and Rescue) For the period January 1, 2017 through December 31, 2018 Published May 6, 2019 Report No. 1023772 Office of the Washington State Auditor Pat McCarthy May 6, 2019 Board of Commissioners Central Whidbey Island Fire and Rescue Coupeville, Washington Report on Financial Statements Please find attached our report on Central Whidbey Island Fire and Rescue’s financial statements. We are issuing this report in order to provide information on the District’s financial condition. Sincerely, Pat McCarthy State Auditor Olympia, WA Insurance Building, P.O. Box 40021 Olympia, Washington 98504-0021 (360) 902-0370 [email protected] TABLE OF CONTENTS Independent Auditor's Report on Internal Control Over Financial Reporting and on Compliance and Other Matters Based on an Audit of Financial Statements Performed in Accordance with Government Auditing Standards..................................................................................................... 4 Independent Auditor's Report on Financial Statements .................................................................. 7 Financial Section ........................................................................................................................... 11 About the State Auditor's Office ................................................................................................... 33 Washington State Auditor’s Office Page 3 INDEPENDENT AUDITOR’S REPORT ON INTERNAL -
Constraining the Holocene Extent of the Northwest Meers Fault, Oklahoma Using High-Resolution Topography and Paleoseismic Trenching
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses Summer 9-8-2017 Constraining the Holocene Extent of the Northwest Meers Fault, Oklahoma Using High-Resolution Topography and Paleoseismic Trenching Kristofer Tyler Hornsby Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geology Commons, and the Geomorphology Commons Let us know how access to this document benefits ou.y Recommended Citation Hornsby, Kristofer Tyler, "Constraining the Holocene Extent of the Northwest Meers Fault, Oklahoma Using High-Resolution Topography and Paleoseismic Trenching" (2017). Dissertations and Theses. Paper 3890. https://doi.org/10.15760/etd.5778 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Constraining the Holocene Extent of the Northwest Meers Fault, Oklahoma Using High-Resolution Topography and Paleoseismic Trenching by Kristofer Tyler Hornsby A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science In Geology Thesis Committee: Ashley R. Streig, Chair Scott E.K. Bennett Adam M. Booth Portland State University 2017 ABSTRACT The Meers Fault (Oklahoma) is one of few seismogenic structures with Holocene surface expression in the stable continental region of North America. Only the ~37 km- long southeastern section of the ~55 km long Meers Fault is interpreted to be Holocene- active. The ~17 km-long northwestern section is considered to be Quaternary-active (pre- Holocene); however, its low-relief geomorphic expression and anthropogenic alteration have presented difficulties in evaluating the fault length and style of Holocene deformation. -
2020 Hunting Prospects: District 13
2020 RUTH MILNER, District Wildlife Biologist MATT HAMER, Assistant District Wildlife Biologist Photo by Doug Harms 2020 DISTRICT 13 HUNTING PROSPECTS Snohomish, San Juan, and Island counties; Skagit County Islands TABLE OF CONTENTS DISTRICT 13 GENERAL OVERVIEW ...................................................................................................................... 1 Snohomish County ................................................................................................................................................ 2 San Juan and Island counties ................................................................................................................................ 3 ELK ............................................................................................................................................................................... 4 DEER ............................................................................................................................................................................. 6 Black-tailed Deer GMU 448 ................................................................................................................................. 6 Black-tailed Deer Island Units .............................................................................................................................. 7 GMUs 410-419 ..................................................................................................................................................... 8 GMU 420 -
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). -
Chapter 13 -- Puget Sound, Washington
514 Puget Sound, Washington Volume 7 WK50/2011 123° 122°30' 18428 SKAGIT BAY STRAIT OF JUAN DE FUCA S A R A T O 18423 G A D A M DUNGENESS BAY I P 18464 R A A L S T S Y A G Port Townsend I E N L E T 18443 SEQUIM BAY 18473 DISCOVERY BAY 48° 48° 18471 D Everett N U O S 18444 N O I S S E S S O P 18458 18446 Y 18477 A 18447 B B L O A B K A Seattle W E D W A S H I N ELLIOTT BAY G 18445 T O L Bremerton Port Orchard N A N 18450 A 18452 C 47° 47° 30' 18449 30' D O O E A H S 18476 T P 18474 A S S A G E T E L N 18453 I E S C COMMENCEMENT BAY A A C R R I N L E Shelton T Tacoma 18457 Puyallup BUDD INLET Olympia 47° 18456 47° General Index of Chart Coverage in Chapter 13 (see catalog for complete coverage) 123° 122°30' WK50/2011 Chapter 13 Puget Sound, Washington 515 Puget Sound, Washington (1) This chapter describes Puget Sound and its nu- (6) Other services offered by the Marine Exchange in- merous inlets, bays, and passages, and the waters of clude a daily newsletter about future marine traffic in Hood Canal, Lake Union, and Lake Washington. Also the Puget Sound area, communication services, and a discussed are the ports of Seattle, Tacoma, Everett, and variety of coordinative and statistical information. -
"Seismites" (Seilacher 1969; Vittori, Sylos-Labini & Serva 1988), Which Include Faults, Sandblows, Folds and Fissures
Radiocarbon Dating of Paleoseismicity Along an Earthquake Fault in Southern Italy Item Type Article; text Authors Calderoni, Gilberto; Petrone, Vincenzo Citation Calderoni, G., & Petrone, V. (1993). Radiocarbon dating of paleoseismicity along an earthquake fault in southern Italy. Radiocarbon, 35(2), 287-293. DOI 10.1017/S0033822200064961 Publisher Department of Geosciences, The University of Arizona Journal Radiocarbon Rights Copyright © by the Arizona Board of Regents on behalf of the University of Arizona. All rights reserved. Download date 27/09/2021 12:51:50 Item License http://rightsstatements.org/vocab/InC/1.0/ Version Final published version Link to Item http://hdl.handle.net/10150/653403 [RADIOCARBON, VOL. 35, No. 2, 1993, P. 287-293] RADIOCARBON DATING OF PALEOSEISMICITY ALONG AN EARTHQUAKE FAULT IN SOUTHERN ITALY GILBERTO CALDERONI and VINCENZO FETRONE Department of Earth Sciences, University of Rome I "La Sapienza" Piazzale Aldo Moro, 5, 00100 Rome Italy ABSTRACT. On 23 November 1980, a major earthquake (M, = 6.9) struck a large area of the southern Apennines (Campania and Lucania regions, southern Italy). This seismic event, the largest in Italy over the last 80 years, almost completely destroyed 15 villages and caused extensive damage to other towns, including Naples. The quake produced the first well-documented example in Italy of surface dislocation, represented by a fault scarp 38 km long. We undertook a study that included 14C dating of organic materials from layers displaced by paleoseismic events to assess the seismologic hazard for the area. We collected peat and charred wood samples from the walls of two trenches excavated across the 1980 fault at Piano di Pecore di Colliano, Salerno, where the sedimentary suite is faulted and warped by five quakes (including that of 1980).