Inventory of Wildlife, Ecological and Landscape Coonectivity Values
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Two Wheel Drive: Mountain Biking British Columbia's Coast Range
Registration 1/5/16, 12:00 PM Ritt Kellogg Memorial Fund Registration Registration No. 9XSX-4HC1Z Submitted Jan 4, 2016 1:19pm by Erica Evans Registration Sep 1, 2015- Ritt Kellogg Memorial Fund Waiting for Aug 31 RKMF Expedition Grant 2015/2016/Group Application Approval This is the group application for a RKMF Expedition Grant. In this application you will be asked to provide important details concerning your expedition. Participant Erica Evans Colorado College Student Planned Graduation: Block 8 2016 CC ID Number: 121491 [email protected] [email protected] (435) 760-6923 (Cell/Text) Date of Birth: Nov 29, 1993 Emergency Contacts james evans (Father) (435) 752-3578 (436) 760-6923 (Alternate) Medical History Allergies (food, drug, materials, insects, etc.) 1. Fish, Pollen (Epi-Pen) Moderate throat reaction usually solved by Benadryl. Emergency prescription for Epi-Pen for fish allergy 2. Wear glasses or contacts Medical Details: I wear glasses and contacts. Additional Questions Medications No current medications Special Dietary Needs No fish https://apps.ideal-logic.com/worker/report/28CD7-DX6C/H9P3-DFPWP_d9376ed23a3a456e/p1a4adc8c/a5a109177b335/registration.html Page 1 of 12 Registration 1/5/16, 12:00 PM Last Doctor's Visit Date: Dec 14, 2015 Results: Healthy Insurance Covered by Insurance Yes Insurance Details Carrier: Blue Cross/ Blue Shield Name of Insured: Susanne Janecke Relationship to Erica: Mother Group Number: 1005283 Policy Number: ZHL950050123 Consent Erica Evans Ritt Kellogg Memorial Fund Consent Form (Jul 15, 2013) Backcountry Level II Recorded (Jan 4, 2016, EE) Erica Evans USE THIS WAIVER (Nov 5, 2013) Backcountry Level II Recorded (Jan 4, 2016, EE) I. -
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 -
Glacier Fluctuations in Garibaldi Provincial Park, Coast Mountains, British Columbia, Canada Johannes Koch,1* Gerald D
The Holocene 17,8 (2007) pp. 1069–1078 Pre-‘Little Ice Age’ glacier fluctuations in Garibaldi Provincial Park, Coast Mountains, British Columbia, Canada Johannes Koch,1* Gerald D. Osborn2 and John J. Clague1 ( 1Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia V5A 1S6, Canada; 2Department of Geology and Geophysics, University of Calgary, Calgary, Alberta T2N 1N4, Canada) Received 21 July 2006; revised manuscript accepted 10 June 2007 Abstract: Holocene glacier fluctuations prior to the ‘Little Ice Age’ in Garibaldi Provincial Park in the British Columbia Coast Mountains were reconstructed from geomorphic mapping and radiocarbon ages on 37 samples of growth-position and detrital wood from glacier forefields. Glaciers in Garibaldi Park were smaller than at present in the early Holocene, although some evidence exists for minor, short-lived advances at this time. The first well-documented advance dates to 7700–7300 14C yr BP. Subsequent advances date to 6400–5100, 4300, 4100–2900 and 1600–1100 14C yr BP. Some glaciers approached their maximum Holocene limits several times during the past 10 000 years. Periods of advance in Garibaldi Park are broadly synchronous with advances else- where in the Canadian Cordillera, suggesting a common climatic cause. The Garibaldi Park glacier record is also broadly synchronous with the record of Holocene sunspot numbers, supporting previous research that sug- gests solar activity may be an important climate forcing mechanism. Key words: Glacier advances, dendroglaciology, Holocene, solar forcing, Garibaldi Park, Coast Mountains, British Columbia. Introduction The most direct evidence of pre-‘Little Ice Age’ glacier activ- ity is found in glacier forefields and includes in situ tree stumps Recent studies point to significant and rapid fluctuations of climate (Ryder and Thomson, 1986; Luckman et al., 1993; Wiles et al., throughout the Holocene (Bond et al., 2001; Mayewski et al., 1999; Wood and Smith, 2004), detrital logs and branches (Ryder 2004). -
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. -
Final Report Filed by Wayne Mccrory, Rpbio, to Federal Review Panel On
McCRORY WILDLIFE SERVICES LTD. RESPONSE TO 2011 TERRESTRIAL-WILDLIFE COMPONENT OF THE ENVIRONMENTAL IMPACT STATEMENT (EIS) & ASSOCIATED DOCUMENTS REGARDING THE PROPOSED NEW PROSPERITY GOLD-COPPER MINE PROJECT AT TEZTAN BINY (FISH LAKE) WITH SPECIFIC REFERENCE TO THE GRIZZLY BEAR [With added comments on Northwestern Toad & Wild Horses] Report for Friends of Nemaiah Valley (FONV) for submission to the CEAA Panel CEAR reference number 782 August 14, 2013 version Wayne P. McCrory, RPBio McCrory Wildlife Services 208 Laktin Road, New Denver, British Columbia, V0G 1S1 Phone (250) 358-7796 email:[email protected] 2 PROFESSIONAL BACKGROUND AND QUALIFICATIONS & DISCLAIMER INFORMATION Professional background & relevant qualifications This report was prepared by me, bear biologist Wayne McCrory, for Friends of Nemaiah Valley (FONV) for submission to the federal CEAA Panel reviewing the New Prosperity mine proposal in the BC Chilcotin. I am a registered professional bear biologist in the province of British Columbia. I have an Honours Zoology degree from the University of British Columbia (1966) and have more than 40 years professional experience. My wildlife and extensive bear work has been published in ten proceedings, peer-reviewed journals, and government publications. I have produced 80 professional reports, some peer-reviewed, many involving environmental impacts, and bear habitat and bear hazard assessments. I served for four years on the BC government’s Grizzly Bear Scientific Advisory Committee (GBSAC). Qualifications relevant to my review of the New Prosperity 2011 EIS include the following. I have had extensive experience in environmental impact assessment involving a diverse array of developments, including impacts of logging on grizzly bears, caribou surveys in the Yukon related to the Gas Arctic Pipeline, impacts of the Mackenzie Valley Pipeline road, impacts of the Syncrude Tar Sands development on waterfowl and other wildlife, and others. -
PRELIMINARY CONSERVATION ASSESSMENT of the RAINSHADOW WILD HORSE ECOSYSTEM, Brittany Triangle, Chilcotin, British Columbia, Canada
PRELIMINARY CONSERVATION ASSESSMENT of the RAINSHADOW WILD HORSE ECOSYSTEM, Brittany Triangle, Chilcotin, British Columbia, Canada. A review of GRIZZLY AND BLACK BEARS, OTHER WILDLIFE, FERAL HORSES & WILD SALMON March, 2002 By Wayne McCrory, RPBio. Submitted to McCrory Wildlife Services Ltd. Friends of the Nemaiah Valley PO Box 479, New Denver, BC, V0G 1S0, Canada 1010 Foul Bay Road Victoria, BC V8S 4J1 Ph: 250-358-7796; E-mail: [email protected] 250 592-1088 www.fonv.ca [email protected] i With thanks to the Xeni Gwet’in First Nation for welcoming us on to their traditional territory to carry out this research Xeni Gwet’in Chief Roger William on trail in Brittany Triangle in September, 2001 Suggested Citation: McCrory, W.P. 2002. Preliminary conservation assessment of the Rainshadow Wild Horse Ecosystem, Brittany Triangle, Chilcotin, British Columbia, Canada. A review of grizzly and black bears, other wildlife, wild horses, and wild salmon. Report for Friends of Nemaiah Valley (FONV), 1010 Foul Bay Road, Victoria, B.C. V8S 4J1. [Copies available from FONV at cost. For more information see: http://www.fonv.ca. Copying and distribution of this report are encouraged. Readers are welcome to cite this report but are requested that citations and references be acknowledged and placed in context]. ii One of two wild horse herds studied in Nuntsi Provincial Park in 2001. Hundreds of these small and large meadows are scattered throughout the pine forests of the Brittany Triangle, providing important habitats for wild horses, grizzly and black bears, and other wildlife from spring to fall. Over the long Chilcotin winter, the horses survive on grasses and sedges in these meadow areas as well as pine grass in the adjacent forests. -
Field Collection and Geochemical Characterization of Potential Mesozoic Source Rocks on Northern Vancouver Island and the Queen Charlotte Islands
Field Collection and Geochemical Characterization of Potential Mesozoic Source Rocks on Northern Vancouver Island and the Queen Charlotte Islands Report prepared for University of Victoria (UVic) – Ministry of Energy and Mines (MEM) Partnership Program Dr. Torge Schuemann School of Earth and Ocean Sciences University of Victoria 2005 1 Introduction The Tertiary Queen Charlotte Basin (QCB) is located immediately inboard of the Pacific - North American plate boundary and comprises Dixon Entrance, Hecate Strait, and Queen Charlotte Sound from north to south (Figure 3). A network of fault-bound sub-basins in Hecate Strait and Queen Charlotte Sound contain up to 5 km of sandstones, siltstones and conglomerates with some coals, which are known as the Skonun Formation (Figure 1). Based on reflection seismic and well data the Skonun Formation has been divided into syn-rift and post-rift successions. Fossils indicate Miocene and Pliocene ages. At many locations, the basal sediments either interfinger or overly extensional basaltic rocks of the Masset Formation (Hickson, 1992; Hyndman & Hamilton, 1993). Masset rocks on Graham Island have yielded ages of 35-12 Ma; most fall between 25-20 Ma (Figure 1). Unfortunately no reliable dates are available from basalts drilled in the wells. Upper Triassic / Lower Jurassic potential source rocks, mainly in the Peril, Sandilands and Ghost Creek formations from the Kunga and Maude groups as well as Cretaceous formations, are exposed on the Queen Charlotte Islands (QCI). Both the Sandilands and Ghost Creek formations comprise significant organic-rich petroleum source rocks in the region, which reach up to 600m in thickness with Total Organic Carbon (TOC) up to 6.1%, comprising oil-prone Type I and oil and gas-prone Type II kerogens with Hydrogen Index (HI) values ranging up to 589 mg HC/g Corg (Bustin & Mastalerz, 1995; Macauley, 1983; Snowdon etal., 2002, see also Figure 2). -
Table of Contents
BACKGROUND EPORT R March 2005 for Big Creek Provincial Park Spruce Lake Protected Area Ministry of Water, Land and Air Protection Parks Division Table of Contents INTRODUCTION ....................................................................................................................................................... 9 PLANNING AND MANAGEMENT HISTORY ................................................................................................................ 10 PARK ESTABLISHMENT AND LEGISLATION .............................................................................................................. 13 MANAGEMENT DIRECTION FROM LAND USE PLANS ................................................................................................ 13 NATURAL VALUES ................................................................................................................................................ 16 CLIMATE .................................................................................................................................................................. 16 PHYSIOGRAPHY ....................................................................................................................................................... 17 GEOLOGY ................................................................................................................................................................ 18 SOILS ...................................................................................................................................................................... -
In the Supreme Court of British Columbia
No. 90 0913 Victoria Registry IN THE SUPREME COURT OF BRITISH COLUMBIA BETWEEN: ROGER WILLIAM, on his own behalf and on behalf of all other members of the Xeni Gwet’in First Nations Government and on behalf of all other members of the Tsilhqot’in Nation PLAINTIFF AND: HER MAJESTY THE QUEEN IN RIGHT OF THE PROVINCE OF BRITISH COLUMBIA, THE REGIONAL MANAGER OF THE CARIBOO FOREST REGION and THE ATTORNEY GENERAL OF CANADA DEFENDANTS PLAINTIFF’ S REPLY APPENDIX 1B PLAINTIFF’S RESPONSE TO THE DEFENDANTS’ SUBMISSIONS ON DEFINITE TRACTS OF LAND WOODWARD & ATTORNEY GENERAL DEPARTMENT OF COMPANY OF BRITISH COLUMBIA JUSTICE, CANADA Barristers and Solicitors Civil Litigation Section Aboriginal Law Section 844 Courtney Street, 2nd Floor 3RD Floor, 1405 Douglas Street 900 – 840 Howe Street Victoria, BC V8W 1C4 Victoria, BC V8W 9J5 Vancouver, B.C. V6Z 2S9 Solicitors for the Plaintiff Solicitor for the Defendants, Her Solicitor for the Defendant, Majesty the Queen in the Right of The Attorney General of Canada the Province of British Columbia and the Manager of the Cariboo Forest Region ROSENBERG & BORDEN LADNER ROSENBERG GERVAIS LLP Barristers & Solicitors Barristers & Solicitors 671D Market Hill Road 1200 Waterfront Centre, 200 Vancouver, BC V5Z 4B5 Burrard Street Solicitors for the Plaintiff Vancouver, BC V7X 1T2 Solicitor for the Defendants, Her Majesty the Queen in the Right of the Province of British Columbia and the Manager of the Cariboo Forest Region Exhibit 43 Photograph 38 Plaintiff’s Reply Appendix 1B Plaintiff’s Response to the Defendants’ Submissions on Definite Tracts of Land A. Southeast Tsilhqox Biny (Chilko Lake): west Ts’il?os (Mount Tatlow) and Relevant Portions of the Tl’echid Gunaz (Long Valley), Yuhitah (Yohetta Valley), Ts’i Talhl?ad (Rainbow Creek), Tsi Tese?an (Tchaikazan Valley) and Tsilhqox Tu Tl’az (Edmonds River) Watersheds .................................................................................................................................... -
1 CURRICULUM VITAE Wayne P. Mccrory, Registered Professional
1 CURRICULUM VITAE Wayne P. McCrory, Registered Professional Biologist (R.P.Bio.) President, McCrory Wildlife Services Ltd. <personal information removed> August 3, 2012 (Last up-date) EDUCATION B.Sc. Honours Zoology, University of British Columbia, 1966. Course emphasis: Wildlife management. Honors thesis on sub-speciation of mountain goats (published), thesis advisor was Dr. Ian McTaggart-Cowan. PROFESSIONAL LICENCE Registered Professional Biologist (R.P.Bio.), British Columbia. Member #168 EXPERTISE Primarily a specialist in black bear and grizzly bear ecology, conservation, safety, bear risk assessments, bear-people conflict prevention plans, design and management of bear-viewing tourism programs, bear safety and bear aversion training, bear problem analysis and other aspects. However, a broad range of experience in wildlife research involving numerous birds and mammals including design of GIS habitat map projects, conservation area design, travel corridors/connectivity and environmental impacts/cumulative effects assessments. Teaches bear safety and bear safety courses. PROFESSIONAL SOCIETIES Member, College of Applied Biology (Registered Professional Biologist (R.P.Bio.) Member and certified guide and trainer with the BC Commercial Bear Viewing Association (CBVA) Member of, and contributor to, the International Association for Bear Research and Management, also known as the International Bear Association (IBA). With members from some 50 countries, the organization supports the scientific management of bears through research and