Two Wheel Drive: Mountain Biking British Columbia's Coast Range
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Community Risk Assessment
COMMUNITY RISK ASSESSMENT Squamish-Lillooet Regional District Abstract This Community Risk Assessment is a component of the SLRD Comprehensive Emergency Management Plan. A Community Risk Assessment is the foundation for any local authority emergency management program. It informs risk reduction strategies, emergency response and recovery plans, and other elements of the SLRD emergency program. Evaluating risks is a requirement mandated by the Local Authority Emergency Management Regulation. Section 2(1) of this regulation requires local authorities to prepare emergency plans that reflects their assessment of the relative risk of occurrence, and the potential impact, of emergencies or disasters on people and property. SLRD Emergency Program [email protected] Version: 1.0 Published: January, 2021 SLRD Community Risk Assessment SLRD Emergency Management Program Executive Summary This Community Risk Assessment (CRA) is a component of the Squamish-Lillooet Regional District (SLRD) Comprehensive Emergency Management Plan and presents a survey and analysis of known hazards, risks and related community vulnerabilities in the SLRD. The purpose of a CRA is to: • Consider all known hazards that may trigger a risk event and impact communities of the SLRD; • Identify what would trigger a risk event to occur; and • Determine what the potential impact would be if the risk event did occur. The results of the CRA inform risk reduction strategies, emergency response and recovery plans, and other elements of the SLRD emergency program. Evaluating risks is a requirement mandated by the Local Authority Emergency Management Regulation. Section 2(1) of this regulation requires local authorities to prepare emergency plans that reflect their assessment of the relative risk of occurrence, and the potential impact, of emergencies or disasters on people and property. -
British Columbia Geological Survey Geological Fieldwork 1987
GEOLOGY OF THE NOAXE CREEK MAP AREA* (920/02) By J. K. Glover, P. Schiarizza and J. I. Garver KEYWORDS: Regional geology, Noaxe Creek, Warner Pass, The '&aughton 'kough: Marine sedimentary strata of he BridgeRiver terrane, Cadwallader terrane, Tyaughton Middle Jurassic to Lower Cretaceous Relay Mountain GrrNugl trough. Yalakom fault, Shulaps ultramafic complex, wrench and the mid-Cretaceous Taqlor Creek and Jackass Mountain faults. groups (Jeletzky and Tipper, 1968). An Upper Cretaceous succession, which comprises her- INTRODUCTION ally discontinuous, nonmarine basinal deposits that grade up into continental volcanicarcrelated rocks, overlies theo13e: The Noaxe Creek map area lies 200 kilometres north of marine strata of the the Tyaughton trough with local pro- Vancouver on the eastern margin of the Coast Mountains, nounced angular unconformity (Glover and Schiarizra, and covers an area of 1000 squarekilometres within the 1987). Chilcotin Range. The topography and vegetation vary from The BridgeRiver terraneand Tyaughton trough are alpine tosubalpine in thewest, southeast and northeast, thought to have been offset from their correlatives to thc: where elevations range up to 2850 metres, to rolling tree- south, the tiozameen Group andMethow basin, by at leas170 covered ridges with intervening broad river valleys in the kilometres of right-lateral strike-slip movement along the central part of the area. north-trending Fraser - Straight Creek fanlt system during Approximately 70 per cent of the area, mostly north of Late Cretaceous (?) and Early Tertiary time (Monger, 19U). Tyaughton and Noaxe creeks, was mapped at ascale of Earlier, post-Albian fragmentation of the Tyaughton-Methow 120 000 by a four-person field crew duringthe 1987 season. -
Tyax Lodge Tyax Whirlpool
Tyax Lodge Tyax whirlpool TYAX LODGE Activity Level: 1 September 30, 2021 – 6 Days A Fall Foliage Tour in the South Chilcotin 12 Meals Included: 5 breakfasts, 4 lunches, 3 dinners Escape to Tyax Lodge, a peaceful retreat Fares per person: $1,945 double/twin; $2,665 single; $1,825 triple on the shore of Tyaughton Lake with a fine Please add 5% GST. view of snowy peaks. The lodge is one of Early Bookers: the largest log buildings in western Canada $60 discount on first 15 seats; $30 on next 10 and you are sure to admire its fine crafts- Experience Points: manship, especially the cathedral lobby Earn 29 points on this tour. Redeem 29 points if you book by August 12, 2021. with a soaring stone chimney. It was built in 1986 and totally renovated in 2010. We Mowson Pond near Tyax stay here for three nights. Nearby is Bralorne, once one of British Columbia’s greatest gold mines. The fabulous Pioneer Mine produced $140 million of gold between 1914 and 1960. A local historian accompanies us to explain the fascinating story of Bralorne, Bradian, Gold Bridge, the Haylmore Historic Site, and Gun Lake. Another highlight of this valley is the fall foliage which usually peaks in early October. ITINERARY Day 1: Thursday, September 30 the Lajoie Dam to lovely Gun Lake. The fall foli- Transportation is provided to Victoria airport. We age is usually outstanding during today’s drive. fly to Kelowna and stay overnight at the Best Meals included: Breakfast, Lunch, Dinner Western Hotel. Accommodation: Tyax Lodge Day 2: Friday, October 1 Day 4: Sunday, October 3 We have lunch at historic Ashcroft Manor. -
Layouttry Copy
Every Second Strait of Georgia Thursday & Online ‘24/7’ at islandtides.com Uniting The Salish Sea ~ From Coast To Coast to Coast Canadian Publications Mail Product Sales Agreement Nº 40020421 Volume 21 Number 12 June 18-July 1, 2009 $1 at Selected Retailers Tide tables 2 Earth hiring 2 Letters 4 Saturna 6 Grade 8 9 Bulletin board 11 Talking about the ocean The Institute of Ocean Sciences (IOS) has joined with the communities of the Saanich Peninsula for Ocean Discovery Days, by offering a series of free science talks and demonstrations at its North Saanich location on June 22 and 23. For the two days, the public is invited to hear a host of experts talk about their special interests—from tsunamis, to sponge reefs, to underwater observatories, to climate change. The two-day event will be a showcase for the multidisciplinary research centre on West Saanich Road, which boasts extensive resources and world-leading scientists employing cutting-edge technology in search of a better Photo: Ayla McKean understanding of the ocean. On Monday at 10am, William Environmental planning student Nadia Nowak (right) is going on a cycle journey to Ottawa this summer with Crawford presents a talk on the effects of her sister Martina to raise awareness and gather comments about the climate crisis from youngsters they the Pacific Ocean on BC’s marine meet. They will present their findings to the federal government as it gets ready to participate in the United resources. He is followed at 11am by Sophie Johannessen speaking on Nations Climate Conference in Copenhagen this December. -
Aerial Overview 2012.Pmd
Resource Practices Branch Pest Management Report Number 15 Library and Archives Canada Cataloguing in Publication Data Main entry under title: Summary of forest health conditions in British Columbia. - - 2001 - Annual. Vols. for 2012- issued in Pest management report series. Also issued on the Internet. ISSN 1715-0167 = Summary of forest health conditions in British Columbia. 1. Forest health - British Columbia - Evaluation - Periodicals. 2. Trees - Diseases and pests - British Columbia - Periodicals. 3. Forest surveys - British Columbia - Periodicals. I. British Columbia. Forest Practices Branch. II. Series: Pest management report. SB764.C3S95 634.9’6’09711 C2005-960057-8 Front cover photo by Joan Westfall: Western hemlock looper defoliation on Quesnel Lake 2012 SUMMARY OF FOREST HEALTH CONDITIONS IN BRITISH COLUMBIA Joan Westfall1 and Tim Ebata2 Contact Information 1 Forest Health Forester, EntoPath Management Ltd., 1654 Hornby Avenue, Kamloops, BC, V2B 7R2. Email: [email protected] 2 Forest Health Officer, Resource Practices Branch, Ministry of Forests, Lands and Natural Resource Operations, PO Box 9513 Stn Prov Govt, Victoria, BC, V8W 9C2. Email: [email protected] TABLE OF CONTENTS Summary ............................................................................................................................................. i Introduction ......................................................................................................................................... 1 Methods ............................................................................................................................................. -
Midcretaceous Thrusting in the Southern Coast Belt, British
TECTONICS, VOL. 15, NO. 2, PAGES, 545-565, JUNE 1996 Mid-Cretaceous thrusting in the southern Coast Belt, British Columbia and Washington, after strike-slip fault reconstruction Paul J. Umhoefer Departmentof Geology,Northern Arizona University, Flagstaff Robert B. Miller Departmentof Geology, San JoseState University, San Jose,California Abstract. A major thrust systemof mid-Cretaceousage Introduction is presentalong much of the Coast Belt of northwestern. The Coast Belt in the northwestern Cordillera of North North America. Thrusting was concurrent,and spatially America containsthe roots of the largest Mesozoic mag- coincided,with emplacementof a great volume of arc intrusives and minor local strike-slip faulting. In the maticarc in North America, which is cut by a mid-Creta- southernCoast Belt (52ø to 47øN), thrusting was followed ceous,synmagmatic thrust system over muchof its length by major dextral-slipfaulting, which resultedin significant (Figure 1) [Rubin et al., 1990]. This thrust systemis translationalshuffling of the thrust system. In this paper, especiallywell definedin SE Alaska [Brew et al., 1989; Rubin et al., 1990; Gehrels et al., 1992; Haeussler, 1992; we restorethe displacementson major dextral-slipfaults of the southernCoast Belt and then analyze the mid-Creta- McClelland et al., 1992; Rubin and Saleeby,1992] and the southern Coast Belt of SW British Columbia and NW ceousthrust system. Two reconstructionswere madethat usedextral faulting on the Yalakom fault (115 km), Castle Washington(Figure 1)[Crickmay, 1930; Misch, 1966; Davis et al., 1978; Brown, 1987; Rusrnore aad Pass and Ross Lake faults (10 km), and Fraser fault (100 Woodsworth, 199 la, 1994; Miller and Paterson, 1992; km). The reconstructionsdiffer in the amount of dextral offset on the Straight Creek fault (160 and 100 km) and Journeayand Friedman, 1993; Schiarizza et al. -
Fisheries Presentation to the CEAA Panel on the Prosperity Project April 27, 2010
Fisheries Presentation to The CEAA Panel On the Prosperity Project April 27, 2010 20+20=20+20= 4040 By: Richard Holmes MSc. RPBio. QEP WildWild SalmonSalmon PolicyPolicy (Photo by Peter Essick) ConservationConservation UnitsUnits sockeye-lake 218 sockeye-river 24 chinook 68† coho 43 chum 38† pink-even 13 pink-odd 19 Sub-total 423 FishFish SpeciesSpecies KnownKnown toto InhabitInhabit TasekoTaseko RiverRiver ¾ BullBull TroutTrout ¾ DollyDolly VardenVarden ¾ LongnoseLongnose SuckerSucker ¾ MountainMountain WhitefishWhitefish ¾ RainbowRainbow TroutTrout ¾ SockeyeSockeye SalmonSalmon ¾ ChinookChinook SalmonSalmon ¾ SteelheadSteelhead ¾ WhitefishWhitefish (General)(General) TasekoTaseko RiverRiver SockeyeSockeye EscapementEscapement 19491949--20092009 ¾¾ EscapementEscapement == thosethose returningreturning toto spawnspawn ¾¾ 19631963 == 31,66731,667 ¾¾ 19881988 == 11,13811,138 ¾¾ 2009=2009= 4040 ¾¾ Sorry,Sorry, butbut II’’mm notnot convincedconvinced whatsoeverwhatsoever thatthat thingsthings areare simplysimply goinggoing toto bebe okok inin thethe TasekoTaseko RiverRiver watershedwatershed shouldshould thisthis minemine bebe grantedgranted approvalapproval toto proceedproceed Lake Sockeye CUs in Pacific/Yukon 218 CUs • notable diversity: NC CC, NVI, SFj Diversity = Production Lake Sockeye CUs in Pacific/Yukon 218 CUs • notable diversity: NC CC, NVI, SFj Diversity = Production Year Population Peak of Spawn Total Males Females Jacks 1948 Taseko Lake 0000 1949 Taseko Lake 100 62 38 0 1950 Taseko Lake 500 250 250 0 1951 Taseko Lake 500 250 -
Inventory of Wildlife, Ecological and Landscape Coonectivity Values
INVENTORY OF WILDLIFE, ECOLOGICAL, AND LANDSCAPE CONNECTIVITY VALUES, TSILHQOT'IN FIRST NATIONS CULTURAL/HERITAGE VALUES, & RESOURCE CONFLICTS IN THE DASIQOX-TASEKO WATERSHED, BC CHILCOTIN FINAL REPORT (Revised) August 4, 2014 For Xeni Gwet’in & Yunesit’in First Nations By Wayne McCrory, RPBio McCrory Wildlife Services Ltd. Phone: 250-358-7796; email: [email protected] and First Nations cultural/heritage research: Linda Smith, MSc, & Alice William GIS mapping by Baden Cross, Applied Conservation GIS Corridor modeling by Dr. Lance Craighead, Craighead Research Institute ii LEGAL COVENANT FROM THE XENI GWET’IN GOVERNMENT When the draft of this report was completed in March 2014, the following legal covenant was included: The Tsilhqot'in have met the test for aboriginal title in the lands described in Tsilhqot’in Nation v. British Columbia 2007 BCSC 1700 (“Tsilhqot’in Nation”). Tsilhqot’in Nation (Vickers J, 2007) also recognized the Tsilhqot’in aboriginal right to hunt and trap birds and animals for the purposes of securing animals for work and transportation, food, clothing, shelter, mats, blankets, and crafts, as well as for spiritual, ceremonial, and cultural uses throughout the Brittany Triangle (Tachelach’ed) and the Xeni Gwet’in Trapline. This right is inclusive of a right to capture and use horses for transportation and work. The Court found that the Tsilhqot’in people also have an aboriginal right to trade in skins and pelts as a means of securing a moderate livelihood. These lands are within the Tsilhqot'in traditional territory, the Xeni Gwet'in First Nation’s caretaking area, and partially in the Yunesit’in Government’s caretaking area. -
Tungsten Deposits of British Columbia
BRITISH COLUMBIA DEPARTMENT OF MINES Hon. E. C. CARSON, Minister . JOHN F. WALKER, Deputy Minister - BULLETIN No. 10 (REVISED)- Tungsten Deposits of British Columbia hl JOHN S. STEVENSON and Staff of Department of Mines 1943 VIDTORIA, 8.0. : PhotpoRset by CHARLESF. BANIIBU). Printer to the Kinn’n Most Excellent Majesty 1948. LIST OF TUNGSTEN OCCURRINCES. 1 . Tungsten and Wolfra- 42 . Brlrtol ........... 106 mite ......................... 51 43 . Ashla0 .- .. 106 2 . Devil's Elbow Mt. -... 52 44. 'Srakum Mf............. 107 3 . Little Pat. Badland and 45. Consolidated Nicola Hasback ......... ~ ....... 52 Coldfields. Ltd......... 107 4 . Lucille No. 1 . 53 46 . Granite .. 116 5 . LOVire end Dot ........ 53 47. Mammoth ............... 116 6. Molly B ..... 54 48. Hedley (Twenty Mile) 7 . Rainier ISilveradd .... 56 Creek.. .. 117 8 . Red Bluff Mt. .. 56 49 . Olslla ........... 117 9 . Erperanra .. 57 50. White Elephant ........ 117 10. Princerr Royal Island .. 57 51 . Elite .-...... 117 11. Bear andCub ........... 58 Other Occurrences ... 118 12. Thornhill Mt............ 58 52. Ole Bull-Orphan Boy- 120 13 . Black Bvll .. 58 53 . Rwal Silver .... 120 14. White Bluffs ~~ ........ ! 58 54. United Victory .... .- . 130 15. Lucky Luke 58 55. Lucky Boy ....... 131 16. Cordillera ................ 58 56. Meteor . ....... 155 17. Emma and I.X.L. -.... 58 57. Scranton 156 18. Ridge . 59 58. Alpine .................... 156 19. Gmtto ..... 59 59. Paorman ....... 155 20. Zona May .- 59 60. Vena090 ~-155 21 . Red Row - ....... 60 61. Royal Canadian 155 22. Black Prince .-.......... 67 62. Nevada .................... 155 23 . Raher Deboule .. 71 63. Acorn Iplaced .......... 155 24. Mohawk ................. 71 64. Spotted Horse ........... 155 25. Higgins 71 65. Pork Rico andEu- 26. Whitwafer -.......... 71 ohrates .................... -
Community Emergency Plan Tyaughton Lake Area
Community Emergency Plan Tyaughton Lake Area Table of Contents Key definitions .............................................................................................................................................. 3 Introduction ................................................................................................................................................. 4 Community Overview ................................................................................................................................... 5 Demographics .......................................................................................................................................... 5 Land Use ................................................................................................................................................... 5 Critical infrastructure ............................................................................................................................... 5 Response Capabilities .............................................................................................................................. 6 Hazard, Risk and Evacuation ........................................................................................................................ 8 Evacuation Routes ................................................................................................................................... 8 Interface Fire ......................................................................................................................................... -
Taseko Lake Outfitters
MANAGEMENT PLAN Taseko Lake Outfitters Siegfried Jurgen Reuter Kelly Gayle Reuter October 2012 Taseko Lake Outfitters Management Plan 1 TABLE OF CONTENTS Management Plan 2 Proponents & General Overview of Business 2 Description of Operation & Activities 2 1.1 General Area & Base Operation 2 1.2.1 Purpose & Description of Experience 2 Activities Offered 2 1.2.2 Improvements 2 1.2.3 Detailed list of Activities & Level of Use 2 Table 1 Extensive Use Area 2 1.2.4 Staff 2 1.3 Intensive Use Sites 2 Facilities & Camps 2 Table 3 Details of Intensive Use Sites 2 Overlap with Environmental & Cultural Values 2 2.1 Fish Values 2 2.2 Wildlife Values 2 2.3 Water Values 2 2.4 First Nations 2 Overlap with Existing Use 2 3.1 Mineral tenures 2 Taseko Lake Outfitters Management Plan 2 3.2 Timber Tenures and Public Recreation: 3 3.3 Land Use, Community, Public Health 3 3.4 Hazards and Safety Plan 3 Maps of Taseko Lake Outfitters 3 Taseko Lake Outfitters Management Plan 3 MANAGEMENT PLAN Taseko Lake Outfitters Executive Summary Proponents & General Overview of Business Siegfried & Kelly Reuter wholly owns Taseko Lake Outfitters. It is a subsidiary of North- ern Spruce Log homes & Landscaping Ltd. and was incorporated on January 16, 1991 with British Columbia incorporation #399997. The Taseko Lake Lodge has been on a License of Occupation for Guide Outfitting for over 75 years. The structures are solid log and not merely tent frames. There has been substantial investment and improvement made to BC land over the years by dedicated and hard working pioneers of wilderness tourism, former guide outfitters. -
Record of Large, Late Pleistocene Outburst floods Preserved in Saanich Inlet Sediments, Vancouver Island, Canada A
ARTICLE IN PRESS Quaternary Science Reviews 22 (2003) 2327–2334 Record of large, Late Pleistocene outburst floods preserved in Saanich Inlet sediments, Vancouver Island, Canada A. Blais-Stevensa,*, J.J. Clagueb,c, R.W. Mathewesd, R.J. Hebdae, B.D. Bornholdf a Geological Survey of Canada, 601 Booth Street, Ottawa, Ont., Canada K1A 0E8 b Department of Earth Sciences, Simon Fraser University, Burnaby, Canada BC V5A 1S6 c Geological Survey of Canada, 101-605 Robson Street, Vancouver, Canada BC V6B 5J3 d Department of Biological Sciences, Simon Fraser University, Burnaby, Canada BC V5A 1S6 e Royal British Columbia Museum, P.O. Box 9815 Stn. Prov. Gov., Victoria, Canada BC V8W 9W2 f School of Earth and Ocean Science, University of Victoria, P.O. Box 3055, Stn. CSC, Victoria, Canada BC V8W 3P6 Received 23 December 2002; accepted 27 June 2003 Abstract Two anomalous, gray, silty clay beds are present in ODP cores collected from Saanich Inlet, Vancouver Island, British Columbia, Canada. The beds, which date to about 10,500 14C yr BP (11,000 calendar years BP), contain Tertiary pollen derived from sedimentary rocks found only in the Fraser Lowland, on the mainland of British Columbia and Washington just east of the Strait of Georgia. Abundant illite-muscovite in the sediments supports a Fraser Lowland provenance. The clay beds are probably distal deposits of huge floods that swept through the Fraser Lowland at the end of the Pleistocene. Muddy overflow plumes from these floods crossed the Strait of Georgia and entered Saanich Inlet, where the sediment settled from suspension and blanketed diatom-rich mud on the fiord floor.