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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. -
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). -
Multi-Proxy Record of Holocene Glacial History of the Spearhead and Fitzsimmons Ranges, Southern Coast Mountains, British Columbia
ARTICLE IN PRESS Quaternary Science Reviews 26 (2007) 479–493 Multi-proxy record of Holocene glacial history of the Spearhead and Fitzsimmons ranges, southern Coast Mountains, British Columbia Gerald Osborna,Ã, Brian Menounosb, Johannes Kochc, John J. Claguec, Vanessa Vallisd aDepartment of Geology and Geophysics, University of Calgary, Calgary, Alta, Canada T2N 1N4 bGeography Program, University of Northern British Columbia, Prince George, BC, CanadaV2N 4Z9 cDepartment of Earth Sciences, Simon Fraser University, Burnaby, BC, Canada V5A 1S6 dGolder Associates Ltd., #1000, 940–6th Avenue, Calgary, Alta, Canada T2P 3T1 Received 9 February 2006; received in revised form 10 July 2006; accepted 10 September 2006 Abstract Evidence from glacier forefields and lakes is used to reconstruct Holocene glacier fluctuations in the Spearhead and Fitzsimmons ranges in southwest British Columbia. Radiocarbon ages on detrital wood and trees killed by advancing ice and changes in sediment delivery to downstream proglacial lakes indicate that glaciers expanded from minimum extents in the early Holocene to their maximum extents about two to three centuries ago during the Little Ice Age. The data indicate that glaciers advanced 8630–8020, 6950–6750, 3580–2990, and probably 4530–4090 cal yr BP, and repeatedly during the past millennium. Little Ice Age moraines dated using dendrochronology and lichenometry date to early in the 18th century and in the 1830s and 1890s. Limitations inherent in lacustrine and terrestrial-based methods of documenting Holocene glacier fluctuations are minimized by using the two records together. r 2006 Published by Elsevier Ltd. 1. Introduction is commonly interpreted to reflect enhanced sediment production beneath an expanded body of ice. -
Federation of Mountain Clubs of BC
Federation of Mountain Clubs of BC Accessing the backcountry one step at a time PO Box 19673 Vancouver, BC V5T 4E7 [email protected] www.mountainclubs.org Tel: 604.873.6096 March 14, 2011 By E-mail: [email protected] Chris Platz, Area Supervisor BC Parks P.O. Box 220 Brackendale, B.C. V0N 1H0 Dear Mr. Platz: Re: Renewal of Whistler Heli-ski Ltd. Park Use Permit in Garibaldi Provincial Park The Federation of Mountain Clubs of British Columbia (FMCBC) is an umbrella organization of approximately 20 outdoor recreation clubs, with about 3500 individual members in total, dispersed throughout the province. For almost four decades, the FMCBC has represented the interests of self- propelled/non-motorized backcountry recreationists by maintaining and improving backcountry and wilderness experiences for our members and the public. We understand the Whistler Heli-ski Ltd. (WHSL) park use permit in Garibaldi Provincial Park is up for renewal in 2011. The Spearhead Range has become a very popular recreation area for backcountry skiers. The growth in numbers of backcountry skiers, combined with better gear and fitness, which allow backcountry skiers to go further into the Spearhead Range on day trips, has increased the competition for skiable terrain within Garibaldi Provincial Park. This has led to greater conflicts with heli-skiers. Furthermore, as a result of the government’s inability and unwillingness to enforce designated non- motorized recreation areas within the Sea-to-Sky corridor, snowmobilers are eroding the few safe areas available for backcountry skiing and snowshoeing outside parks, and even sometimes in Garibaldi Park (Brohm Ridge – Mt. -
HOLOCENE GLACIER FI-UCTUATIONS in GARIBALDI PROVINCIAL PARK, Sotjthern COAST MOUNTAINS, BRITISH COLUMBIA
HOLOCENE GLACIER FI-UCTUATIONS IN GARIBALDI PROVINCIAL PARK, SOtJTHERN COAST MOUNTAINS, BRITISH COLUMBIA Johannes Koch M.Sc. (Geography, Geology, Mineralogy), University Freiburg, 2001 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY In the Department of Earth Sciences 0Joharmes Koch 2006 SIMON FkISER UNIVERSITY Spring 2006 All rights reserved. This work may not be reproduced in wh'ole or in part, by photocopy or other means, without permission of the author. APPROVAL Name: Johannes Koch Degree: Doctor of Philosophy Title of Thesis: Holocene glacier fluctuations in Garibaldi Provincial Park, southern Coast Mountains, British Columbia Examining Committee: Dr. Peter Mustard Chair Dr. John Clague Senior Supervisor Dr. Gerald Osborn Comrriittee Member Dr. Dan Smith Comrriittee Member Dr. Rolf Mathewes Committee Member Dr. Lionel Jackson Internal Examiner Dr. Brian Luckman External Examiner University of Western Ontario Date Approved: .fl,gIICNL+IC z JO~ SIMON FRASER &8Cl? "N~~mlibrary DECLARATION OF PARTIAL COPYRIGHT LICENCE The author, whose copyright is declared on the title page of this work, has granted to Simon Fraser University the right to lend this thesis, project or extended essay to users of the Simon Fraser University Library, and to make partial or single copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users. The author has further granted permission to Simon Fraser University to keep or make a digital copy for use in its circulating collection, and, without changing the content, to translate the thesislproject or extended essays, if technically possible, to any medium or format for the purpose of preservation of the digital work. -
Veeocee Mountain (Right Centre) and Ubyssey Glacier (Left), in the Mcbride Range of Garibaldi Park Photo by Alaistair Macdonald Th« Varsity Outdoor Quh Journal
Veeocee Mountain (right centre) and Ubyssey Glacier (left), in the McBride Range of Garibaldi Park photo by Alaistair Macdonald Th« Varsity Outdoor Quh Journal VOLUME Vm - 1965 7he VnivetMj of 3tiflih CoiumHa. Vancouver 8, B.C. i FRONTISPIECE PICTURE: Veeocee Mountain (ca. 7750') lies in the McBride Range of Garibaldi Park. Referring to the map drawn by Bert Port in the VOC Journal Vol. VII, the mountain lies three miles south-east of Mt. Cheakamus—just off the map. When the pioneers of mountaineering in northern Garibaldi Park, the Carters, Mrs. P. Munday and the Hooleys, met with the mem bers of the 1964 VOC Fitzsimmons Horseshoe Expedition to discuss new-name proposals for the area's unnamed features, it was commonly acknowledged that the VOC had, in the last twenty years, accomplished many outstanding mountaineering and ski-touring activities in Garibaldi Park. It was also agreed that these activities should be commemorated in the form of permanent geographic names for some of the park features. Proposed names were to be applied to prominent features and difficulty of ascent was to have no bearing on the selection. Glacier-clad Veeocee Mtn. is located on the outer extremity of a ridge trending first south, then west and finally northwest from Mt. Sir Richard. North and below the mountain in a valley bottom lies Ubyssey Glacier. To the north of this icy highway is a high jagged ridge with four chisel-like prominences, now officially known as The Lectures Cutters (ca. 8100'-8400'). This ridge is a portion of the colossal Sir Richard massif» VOC is greatly honoured that the Canadian Permanent Committee for Geographic Names and especially Messrs. -
British Columbia – VE7)
Summits on the Air Canada (British Columbia – VE7) Association Reference Manual Document Reference S61.1 Issue number 1.6 Date of issue 01-Apr-2018 Participation start date 01-Nov-2010 Authorised Date: 01-Apr-2018 obo SOTA Management Team Association Manager Nathon Hall VE7ETS Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Summits on the Air – ARM for Canada (British Columbia – VE7) Table of Contents 1 ASSOCIATION REFERENCE DATA................................................................................. 6 1.1 PROGRAM DERIVATION ..................................................................................................................... 8 1.2 GENERAL INFORMATION ................................................................................................................... 8 1.3 FINAL ASCENT AND ACTIVATION ZONE ............................................ ERROR! BOOKMARK NOT DEFINED. 1.4 RIGHTS OF WAY AND ACCESS ISSUES ................................................................................................ 9 1.5 MAPS AND NAVIGATION .................................................................................................................... 9 1.6 SAFETY CONSIDERATIONS .............................................................................................................. 10 1.7 -
In This Issue
VOLUME 26, NO. 3 • FEBRUARY 2008 Jason West walks along the fracture line of an avalanche incident in Silver Fork, Big Cottonwood Canyon, Utah, that occurred November 14, 2006. Jason was completely buried in an avalanche he triggered but was quickly dug out by his partners in time to save his life. Here he returns to the scene the following day to investigate the accident. photo © Bruce Tremper www.brucetremper.com In This Issue Avalanche Data— The avalanche is classified SS-AS-R4-D3-G. regain the ridge and then walk east on the ridge. It appears this From the President. 2 Rough measurements on a topographic map indicate this avalanche deviated from the original plan of sticking to low-angle terrain. Mailbag . 2 was around 2000' wide. It ran 600 vertical feet. The fracture line Perhaps since they successfully skied the run and did not see any depth ranged from 14-36" and averaged around 28". The slope cracking, collapsing, or other avalanches, this influenced their From the Editor . 3 angle ranged from 35-40 degrees in steepness. The aspect ranged decision. Excitement about the new ski season could have also Metamorphism . 4 from northwest to northeast. It released at about 10,000' in elevation. played a role. At least one member of the party had reservations A second avalanche released sympathetic to the original. It was about some of the decisions but did not speak up. Later when the AAA News. 4 around 100' wide, 30" deep, and ran around 500' vertical distance. group discussed the accident, the other two had reservations as What’s New . -
View - Meager and Keyhole Hotsprings Project Update - Visitor Use Monitoring - Update
VILLAGE OF PEMBERTON -COMMITTEE OF THE WHOLE MEETING AGENDA- Agenda for the Committee of the Whole of Council of the Village of Pemberton to be held Tuesday, February 25, 2020, at 1:00 p.m. in Council Chambers, 7400 Prospect Street. This is Meeting No. 202. “This meeting is being recorded on audio tape for minute-taking purposes as authorized by the Village of Pemberton Audio recording of Meetings Policy dated September 14, 2010.” Item of Business Page No. 1. CALL TO ORDER In honour of the Lil’wat7ul, the Village of Pemberton acknowledges that we are meeting within the unceded territory of the Lil’wat Nation. 2. APPROVAL OF AGENDA 1 Recommendation: THAT the Agenda be approved as presented. 3. ADOPTION OF MINUTES 2 a) Committee of the Whole Meeting No. 201, Tuesday, January 28, 2020 Recommendation: THAT the minutes of the Committee of the Whole Meeting No. 201, held Tuesday, January 28, 2020, be adopted as circulated. 4. DELEGATIONS a) BC Parks & Ministry of Forests, Lands, Natural Resource Operations & Rural 6 Development – Updates BC Parks Elyse Curley, Community Liaison Officer – South Coast Jennie Aikman, Regional Director – South Coast Kevin Wagner, Area Supervisor - Pemberton Area Ministry of Forests, Lands, Natural Resource Operations & Rural Development Scott Shaw-MacLaren, Resource Manager, Regional Operations Division – Coast Area Susie Dain-Owens, Land and Resource Specialist, Regional Operations Division – Coast Area Presentation Topics: - Introduction to Visitor Use Management Approach - Joffre Lakes Park 2019 Update and 2020 Next Steps - Introduction to Visitor Use Management Approach - Sea to Sky Visitor Use Management Projects – Brief Overview - Meager and Keyhole Hotsprings Project Update - Visitor Use Monitoring - Update 5. -
Spearhead Traverse. This Description Was Culled From
1. From top of Showcase T-bar on Blackcomb, cross Blackcomb Glacier to the Blackcomb-Spearhead col 2. Climb over Decker mountain. You can go right over the top to the Trorey-Decker col, or drop down a steep slope from the east ridge of Decker to a lower part of the Trorey Glacier. 3. Traverse around the North side of Mt. Trorey on the Trorey Glacier. 4. Ski around the south side of Mt. Pattison. 5. Climb to the col between Tremor and Shudder. 6. Traverse the Platform, Ripsaw and Naden Glaciers to the Macbeth Glacier. 7. Follow a ridge off the Macbeth Glacier to the Iago Glacier (steep) and climb the Iago Glacier. 8. Descend off Mt. Iago to the Diavolo Glacier (steep). 9. Climb over Mt. Benvolio and then do a spiralling descent around the N side of Overlord (crevasses). 10. Either descend Overlord Glacier and climb back to Russet Lake, or cross the Fissile-Whirlwind col and descend to Russet Lake. 11. Head West and descend to Singing Pass. 12. Ski out the singing pass trail to Whistler Village or ski up over the summits of Oboe and Flute to reach the Whistler downhill ski area and descend the ski runs to Whistler Village. From the top of the glacier, drop down towards the Decker Glacier, staying low heading S.E. Cross the northern glaciated slopes of Mt Trorey. Good camping can be found here. Mt Pattison can be passed by the northern col or by climbing a short but steep west facing chute south of the peak. -
Joffre Lakes Provincial Park | 2019 Visitor Use Management Action Plan 1 Contents
Joffre Lakes Provincial Park 2019 Visitor Use Management Action Plan Acknowledgments Development of this 2019 Visitor Use Management Action Plan for Joffre Lakes Park has been jointly undertaken by the Lil’wat Nation, N’Quatqua, Ministry of Forests, Lands, Natural Resource Operations and Rural Development (FLNRORD), Ministry of Transportation and Infrastructure (MOTI), and BC Parks. Joffre Lakes Park is in the shared territory of the St’at’imc peoples, which includes the N’Quatqua and Lil’wat Nation. BC Parks staff are grateful for their support and cooperation in developing this Action Plan, and for the shared St’at’imc value of i tmícwsa i ucwalmícwa (the people and the land are one) that has guided this planning process. Joffre Lakes Provincial Park | 2019 Visitor Use Management Action Plan 1 Contents Acknowledgments. 1 Message from the Lil’wat Nation and N’Quatqua . 4 Message from the Assistant Deputy Minister. 5 PART 1: THE FOUNDATION . 6 Background. 6 Action Plan Purpose. 6 Action Plan Planning Process. 7 A Collaborative Approach with First Nations. 7 External Engagement. 7 Relationship with Communities . 7 PART 2: THE PARK . 9 Key Management Issues . 9 Natural Values. 11 Indigenous Values, Culture, and History . 11 Recreational Values . 11 2 Joffre Lakes Provincial Park | 2019 Visitor Use Management Action Plan PART 3: VISION FOR JOFFRE LAKES PARK . 13 PART 4: MANAGEMENT STRATEGIES AND ACTIONS . 14 Goal 1: Address Illegal Parking and Safety Concerns with Park Access . 15 Goal 2: Ensure Park Facilities Support Levels of Use. 16 Goal 3: Effectively Manage Day-Use Visitation . 17 Goal 4: Increase Public Appreciation and Respect for the Park . -
Latest Pleistocene and Holocene Behaviour of Franklin Glacier, Mt
Latest Pleistocene and Holocene behaviour of Franklin Glacier, Mt. Waddington Area, British Columbia Coast Mountains, Canada by Bryan Joel Mood B.Sc., Mount Allison University, 2013 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE in the Department of Geography © Bryan Joel Mood, 2015 University of Victoria All rights reserved. This thesis may not be reproduced in whole or in part, by photocopy or other means, without the permission of the author. ii Supervisory Committee Latest Pleistocene and Holocene behaviour of Franklin Glacier, Mt. Waddington area, British Columbia Coast Mountains, Canada By Bryan Joel Mood B.Sc., Mount Allison University, 2013 Supervisory Committee Dr. Dan J. Smith (Department of Geography) Supervisor Dr. John J. Clague (Department of Geography) Departmental Member iii Supervisory Committee Dr. Dan J. Smith (Department of Geography) Supervisor Dr. John J. Clague (Department of Geography) Departmental Member Abstract Holocene climate variability in the British Columbia Coast Mountains has resulted in repeated intervals of glacier expansion and retreat. Since reaching their late Holocene maximum positions in the late 20th century, glaciers in the region have experienced significant volumetric loss. The subsequent downwasting and frontal retreat has revealed forests buried by glacier advances throughout the Holocene, enabling description of significant intervals of ice expansion using dendroglaciology. This thesis characterizes dendroglaciological evidence as it relates to climate at two scales: (1) at Franklin Glacier in the Mt. Waddington area, and; (2) throughout the Coast Mountains. Dendroglaciological evidence from glacier forefields and lateral moraines in the Coast Mountains provides evidence for at least 11 intervals of glacier activity during the Holocene.