Canada's Ten Largest Earthquakes
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Seismicity of the Earth 1900–2013 Offshore British Columbia–Southeastern Alaska and Vicinity Compiled by Gavin P
U.S. DEPARTMENT OF THE INTERIOR Open-File Report 2010–1083–O U.S. GEOLOGICAL SURVEY Seismicity of the Earth 1900–2013 Offshore British Columbia–Southeastern Alaska and Vicinity Compiled by Gavin P. Hayes,1 Gregory M. Smoczyk,1 Jonathan G. Ooms,1 Daniel E. McNamara,1 Kevin P. Furlong,2 Harley M. Benz,1 and Antonio Villaseñor3 2014 1U.S. Geological Survey 2Department of Geosciences, Pennsylvania State University, University Park, Pa., 16802 USA Queen Charlotte Fault Graphic 140° 130° 3Institute of Earth Sciences, Consejo Superior de Investigaciones Científicas (CSIC), Lluis Solé i Sabarîs s/n, 08028 Barcelona, Spain This schematic figure shows the tectonic setting of the Pacific–North America plate Delta Junction UNITED boundary (PAC:NAM) in the region of the October 28, 2012, M 7.8 Haida TECTONIC SUMMARY Mackenzie Mountains Deltana Dawson Gwaii earthquake sequence (red circles). Background seismicity Healy from the Centennial and USGS-NEIC catalogs is shown The tectonics of the Pacific margin of North America between Vancouver Island and south-central Alaska are dominated STATES Mayo Alaska Range with gray cubes, in three dimensions. The upper by the northwest motion of the Pacific plate with respect to the North America plate at a velocity of approximately 50 2002 2002 mm/yr. In the south of this mapped region, convergence between the northern extent of the Juan de Fuca plate (also Cantwell Tok panel shows three-dimensional shaded known as the Explorer microplate) and North America plate dominate. North from the Explorer, Pacific, and North relief of GEBCO bathymetry America plate triple junction, Pacific:North America motion is accommodated along the ~650-km-long Queen Charlotte Yukon (GEBCO, 2008). -
West Coast Trail
Hobiton Pacific Rim National Park Reserve Entrance Anchorage Squalicum 60 LEGEND Sachsa TSL TSUNAMI HAZARD ZONE The story behind the trail: Lake Ferry to Lake Port Alberni 14 highway 570 WEST COAST TRAIL 30 60 paved road Sachawil The Huu-ay-aht, Ditidaht and Pacheedaht First Nations However, after the wreck 420 The West Coast Trail (WCT) is one of the three units 30 Self Pt 210 120 30 TSL 30 Lake Aguilar Pt Port Désiré Pachena logging road The Valencia of Pacific Rim National Park Reserve (PRNPR), Helby Is have always lived along Vancouver Island's west coast. of the Valencia in 1906, West Coast Trail forest route Tsusiat IN CASE OF EARTHQUAKE, GO Hobiton administered by Parks Canada. PRNPR protects and km distance in km from Pachena Access TO HIGH GROUND OR INLAND These nations used trails and paddling routes for trade with the loss of 133 lives, 24 300 presents the coastal temperate rainforest, near shore Calamity and travel long before foreign sailing ships reached this the public demanded Cape Beale/Keeha Trail route Creek Mackenzie Bamfield Inlet Lake km waters and cultural heritage of Vancouver Island’s West Coast Bamfield River 2 distance in km from parking lot Anchorage region over 200 the government do River Channel west coast as part of Canada’s national park system. West Coast Trail - beach route outhouse years ago. Over the more to help mariners 120 access century following along this coastline. Trail Map IR 12 Indian Reserve WEST COAST TRAIL POLICY AND PROCEDURES Dianna Brady beach access contact sailors In response the 90 30 The WCT is open from May 1 to September 30. -
Bamfield Official Community Plan Alberni-Clayoquot Regional District
Bamfield Official Community Plan Alberni‐Clayoquot Regional District Table of Contents PART I – BACKGROUND ................................................................................................. 5 1.0 INTRODUCTION .............................................................................................. 5 1.1 Plan Preparation ............................................................................................................................ 5 Map No. 1 Plan Area ............................................................................................................................... 6 1.2 Purpose of the Official Community Plan .................................................................................. 7 1.3 Legislative Authority ..................................................................................................................... 7 1.4 Jurisdiction ..................................................................................................................................... 9 1.5 The Plan ....................................................................................................................................... 10 1.7 Definitions ................................................................................................................................... 13 PART II – VISION & GENERAL GOALS, OBJECTIVES AND POLICIES .................................. 16 2.0 VISION ......................................................................................................... -
Species at Risk Assessment—Pacific Rim National Park Reserve Of
Species at Risk Assessment—Pacific Rim National Park Reserve of Canada Prepared for Parks Canada Agency by Conan Webb 3rd May 2005 2 Contents 0.1 Acknowledgments . 10 1 Introduction 11 1.1 Background Information . 11 1.2 Objective . 16 1.3 Methods . 17 2 Species Reports 20 2.1 Sample Species Report . 21 2.2 Amhibia (Amphibians) . 23 2.2.1 Bufo boreas (Western toad) . 23 2.2.2 Rana aurora (Red-legged frog) . 29 2.3 Aves (Birds) . 37 2.3.1 Accipiter gentilis laingi (Queen Charlotte goshawk) . 37 2.3.2 Ardea herodias fannini (Pacific Great Blue heron) . 43 2.3.3 Asio flammeus (Short-eared owl) . 49 2.3.4 Brachyramphus marmoratus (Marbled murrelet) . 51 2.3.5 Columba fasciata (Band-tailed pigeon) . 59 2.3.6 Falco peregrinus (Peregrine falcon) . 61 2.3.7 Fratercula cirrhata (Tufted puffin) . 65 2.3.8 Glaucidium gnoma swarthi (Northern pygmy-owl, swarthi subspecies ) . 67 2.3.9 Megascops kennicottii kennicottii (Western screech-owl, kennicottii subspecies) . 69 2.3.10 Phalacrocorax penicillatus (Brandt’s cormorant) . 73 2.3.11 Ptychoramphus aleuticus (Cassin’s auklet) . 77 2.3.12 Synthliboramphus antiquus (Ancient murrelet) . 79 2.3.13 Uria aalge (Common murre) . 83 2.4 Bivalvia (Oysters; clams; scallops; mussels) . 87 2.4.1 Ostrea conchaphila (Olympia oyster) . 87 2.5 Gastropoda (Snails; slugs) . 91 2.5.1 Haliotis kamtschatkana (Northern abalone) . 91 2.5.2 Hemphillia dromedarius (Dromedary jumping-slug) . 95 2.6 Mammalia (Mammals) . 99 2.6.1 Cervus elaphus roosevelti (Roosevelt elk) . 99 2.6.2 Enhydra lutris (Sea otter) . -
Only a Matter of Time: the Impacts of the Cascadia Subduction Zone And
Running head: ONLY A MATTER OF TIME Only a Matter of Time: The Impacts of the Cascadia Subduction Zone and Colonialism on Indigenous Communities in Vancouver Island Sydney M. Dyck Mount Royal University ONLY A MATTER OF TIME Abstract The Cascadia Subduction Zone is a fault line that runs seven hundred miles off of the coast of the Pacific Northwest, where two borders of tectonic plates meet and have been subducting for centuries (Schulz, 2015). This fault line poses the threat of an impending earthquake and tsunami, as the subduction zone will eventually give way to the enormous amounts of pressure on the undersea plates, triggering what Schulz calls a “seven-hundred-mile liquid wall that will reach the Northwest coast, on average, fifteen minutes after the earthquake begins” (2015). The devastation this earthquake and tsunami duo will unleash upon coastal British Columbia and the Pacific Northwest will inevitably be catastrophic, with approximately 7,000,000 people being at risk of exposure to this disaster and an estimated 71,000 people living directly in the inundation zone (Schulz, 2015). Kenneth Murphy, who directs the Federal Emergency Management Agency’s Region X, the division responsible for Oregon, Washington, Idaho, and Alaska, stated, “Our operating assumption is that everything west of Interstate 5 will be toast;” under this premise it is of utmost importance for us to consider those who are most vulnerable to the risks associated with a disaster of this size (Schulz, 2015). In this paper, I will be focusing on the potential effects that a natural disaster triggered by the Cascadia Subduction Zone could have on those living on Vancouver Island, specifically the Indigenous peoples who have populated the area for centuries. -
Earthquakes Back Olympic Penin
Seismicity Rates from GPS and other Deformation Rate Estimates in Washington State Roy Hyndman, Lucinda Leonard & Stephane Mazzotti Geological Survey of Canada, Pacific Geoscience Centre, Sidney, B.C.; SEOS, University of Victoria; Univ. Montpellier, France Forearc crustal earthquakes Back Olympic Penin. Puget Sound arc x x x x x xx x x x x x xx Subduction thrust earthquakes x x Benioff-Wadati x slab earthquakes PGC R.D. Hyndman Pacific Geoscience Centre Geological Survey of Canada Catalogue Seismicity Rates Large event rates based on smaller event rates 10 Are there large events without Puget-Georgia Basin corresponding smaller magnitude 1 ) 1 - seismicity? r M 6 y ( ~50 yrs i.e., "characteristic . q e 0.1 earthquakes"? r f M 7 e v i ~400 yrs Cascadia t a l megathrust u 0.01 m & central Van. Is. m u Mx=7.5 two M7 with little C other seismicity 0.001 7.7 b~0.77 7.3 0.0001 3 4 5 6 7 8 R.D. Hyndman Magnitude PGC Pacific Geoscience Centre Geological Survey of Canada Long-term Crustal Seismicity Rate in Pacific Northwest --Can we estimate the earthquake rate from that required to accommodate deformation rate assuming all seismic? (GPS, paleoseismic fault displacement rates, tectonic models, etc.) (1) Puget Sound, (2) Olympic Penin., (3) E. Washington --Problem of short duration of catalogue seismicity; possibility of large infrequent earthquakes where few smaller ones, i.e., Cascadia megathrust, M7 central Van. Is. events, etc. "characteristic earthquakes"? --also issue of large crustal events in Puget Sound after megathrust as predicted by deformation data PGC R.D. -
Earthquakes in Southwestern British Columbia
Earthquakes in southwestern British Columbia Southwestern British Columbia is one of the most seismically active regions in Canada. Approximately 400 earthquakes occur each year in the region extending from the north end of Vancouver Island to Seattle, Washington U.S. seen on the map below. About a dozen of these earthquakes are felt by people, but many of the larger earthquakes occur offshore. Earthquakes capable of causing structural damage happen every decade or so. What Causes Earthquakes? The surface or crust of the Earth is always moving. Large segments of this crust, called tectonic plates, continually shift against each other, causing stress to build-up. When the stress becomes too great, a sudden rupture or earthquake occurs along a zone of weakness called a fault, generating seismic waves. Earthquakes occur most Maintaining the frequently where tectonic plates interact - such as the Cascadia antennae that receive Subduction Zone of southwestern British Columbia. earthquake data from 15 Years of Earthquakes remote stations. 15 Years of Earthquakes 15 Years of Earthquakes 15 Years of Earthquakes The Cascadia Subduction Zone (CSZ) 50˚ 50˚ Southwestern British Columbia is located above the boundary between the oceanic Juan de Fuca Plate and the continental 50˚ Vancouver North American Plate. This boundary, the Cascadia Subduction Vancouver Zone, spans 1000 km from northern Vancouver Island to northern Vancouver California. The Juan de Fuca Plate is descending or subducting Victoria 48˚ Victoria Seattle 48˚ beneath the North American Plate at roughly the same rate as Seattle fingernails grow – about four centimetres per year. Victoria 48˚ Seattle 46˚ 46˚ 128˚ 128˚ 126˚126˚ 124124˚ ˚ 122˚122˚ 120˚ 120˚ 46˚ 128˚ 126˚ 124˚ 122˚ 120˚ Juan de de de Fuca Fuca Fuca Plate Plate Plate earthquakes North America America American Plate Plate Plate earthquakes Juan de Fuca Plate Earthquakes occur in three regions of southwestern British North America Plate Columbia. -
Carnivores in Human Use Areas of Pacific Rim
Noninvasive Approaches to Reduce Human-Cougar Conflict in Protected Areas on the West Coast of Vancouver Island by Danielle M. Thompson B.Sc. (Wildlife Management), University of Northern British Columbia, 2001 A Thesis Submitted in Partial Fulfilment of the Requirements for the Degree of MASTER OF SCIENCE In the Department of Biology © Danielle M. Thompson, 2010 University of Victoria All rights reserved. This thesis may not be reproduced in whole or in part, by photocopy or other means, without permission by the author ii Supervisory Committee Noninvasive Approaches to Reduce Human-Cougar Conflict in Protected Areas on the West Coast of Vancouver Island By Danielle M. Thompson B.Sc. (Wildlife Management), University of Northern British Columbia, 2001 Supervisory Committee Dr. Don Eastman, (Department of Biology) Co-Supervisor Dr. Patrick Gregory (Department of Biology) Co-Supervisor Dr. Peter Keller (Department of Geography) Outside Member Dr. Alton Harestad (Simon Fraser University) Additional Member iii Abstract Supervisory Committee Dr. Don Eastman, (Department of Biology) Co-Supervisor Dr. Patrick Gregory (Department of Biology) Co-Supervisor Dr. Peter Keller (Department of Geography) Outside Member Dr. Alton Harestad (Simon Fraser University) Additional Member Cougars (Puma concolor) are a growing concern for managers of Pacific Rim National Park Reserve and Clayoquot Sound UNESCO Biosphere Reserve on the west coast of Vancouver Island, British Columbia. Since the mid-1990s, the frequency and intensity of human-cougar interactions have dramatically increased. Concurrently, these areas have become increasingly popular for human activities. The primary goal of my study was to recommend ways to reduce the potential risk of human-cougar interactions to ensure long-term conservation of cougars while minimizing risks to visitor safety. -
1968 Mountaineer Outings
The Mountaineer The Mountaineer 1969 Cover Photo: Mount Shuksan, near north boundary North Cascades National Park-Lee Mann Entered as second-class matter, April 8, 1922, at Post Office, Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during June by The Mountaineers, P.O. Box 122, Seattle, Washington 98111. Clubroom is at 7191h Pike Street, Seattle. Subscription price monthly Bulletin and Annual, $5.00 per year. EDITORIAL STAFF: Alice Thorn, editor; Loretta Slat er, Betty Manning. Material and photographs should be submitted to The Mountaineers, at above address, before Novem ber 1, 1969, for consideration. Photographs should be black and white glossy prints, 5x7, with caption and photographer's name on back. Manuscripts should be typed double-spaced and include writer's name, address and phone number. foreword Since the North Cascades National Park was indubi tably the event of this past year, this issue of The Mountaineer attempts to record aspects of that event. Many other magazines and groups have celebrated by now, of course, but hopefully we have managed to avoid total redundancy. Probably there will be few outward signs of the new management in the park this summer. A great deal of thinking and planning is in progress as the Park Serv ice shapes its policies and plans developments. The North Cross-State highway, while accessible by four wheel vehicle, is by no means fully open to the public yet. So, visitors and hikers are unlikely to "see" the changeover to park status right away. But the first articles in this annual reveal both the thinking and work which led to the park, and the think ing which must now be done about how the park is to be used. -
S51B-2362 Chastity Aiken1, Zhigang Peng1, David R
Tectonic Tremor Triggered along Major Strike-Slip Faults around the World S51B-2362 Chastity Aiken1, Zhigang Peng1, David R. Shelly2, David P. Hill2, Hector Gonzalez-Huizar3, Kevin Chao4, Jessica Zimmerman5, Roby Douilly6, Anne Deschamps7, Jennifer Haase8, and Eric Calais9 1Georgia Institute of Technology; 2 U.S. Geological Survey, Menlo Park; 3 University of Texas, El Paso; 4 University of Tokyo, Earthquake Research Institute; 5 Texas A & M University, Commerce; 6 Purdue University; 7 Université de Nice Sophia Antipolis; 8 Scripps Institute of Oceanography; 9 Ecole Normale Superieure Research Question Triggered Tremor Observations Triggering Potential How does triggered tremor differ on strike-slip faults around the world? Eastern Denali Fault of Yukon Territory, Canada San Andreas Fault of Parkfield, California Figure 7 (LEFT). Theoretical example of triggering Background 20130105 M7.5 Dist: 625.8 km BAZ: 163.2 deg Station: CN.HYT 20121028 M7.7 Dist: 2080.0 km BAZ: 337.7 deg Station: BK.PKD potential as a function of wave amplitude (i.e. stress), Deep tectonic tremor, which generally occurs in the lower crust beneath the 64˚ (a) 6 (a) 0.08 depth (i.e. frequency), and incidence angle on a vertical Mw7.9 North Love American BHT seismogenic zone where earthquakes occur, has been observed at several major Plate HHT 4 strike-slip fault. From Hill and Prejean (2013). CDF 0.04 Yukon Alaska Parkfield plate-bounding faults around the Pacific Rim. In order to investigate the potential 2012 Haida Gwaii 63˚ 2 M 7.5 0 BHR link between tremor and earthquake nucleation, further study of when, where, and Totschunda Fault HHR 2012 Sumatra EDF Pacific 0 Plate M 7.7 how tremor occurs is needed. -
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. -
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