BC Geological Survey Assessment Report 37651
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Electoral Area Directors Committee Agenda October 9, 2019; 10:30 AM Pemberton Community Church - Meeting Room 7420 Dogwood Street, Pemberton, BC
Electoral Area Directors Committee Agenda October 9, 2019; 10:30 AM Pemberton Community Church - Meeting Room 7420 Dogwood Street, Pemberton, BC Item Item of Business and Page Number Page 1. Call to Order We would like to recognize that this meeting is being held on the Traditional Territory of the Líl’wat Nation. 2. Approval of Agenda 3. Electoral Area Directors Committee Closed Meeting THAT the Committee close the meeting to the public under the authority of Section 90(1)() of the Community Charter. 4. Rise & Report from the Closed Electoral Area Directors Committee Meeting 5. Consent Agenda (Voting rule on each item may vary; unanimous vote required) Items appearing on the consent agenda which present a conflict of interest for Committee Members must be removed from the Consent Agenda and considered separately. Any items to be debated or voted against must be removed from the Consent Agenda and considered separately. THAT the resolutions set out in the Consent Agenda be approved, and those Consent Agenda items which do not have resolutions related thereto be received. 5.1 Approval and Receipt of Minutes 5.1.1. Electoral Area Directors Committee Meeting Draft 5 - 11 Minutes of September 5, 2019 THAT the Electoral Area Directors Committee Meeting Minutes of September 5, 2019 be approved as circulated. 5.2 Staff Reports & Other Business 5.2.1. September 2019 Select Funds Report 12 - 16 THAT the following resolution of the September 5, 2019 Electoral Area Directors Committee meeting with respect Item Item of Business and Page Number Page -
British Columbia Coastal Range and the Chilkotins
BRITISH COLUMBIA COASTAL RANGE AND THE CHILKOTINS The Coast Mountains of British Columbia are remote with limited accessibility by float plane, helicopter or boating up its deep inlets along the coast and hiking in. The mountains along British Columbia and SE Alaska intermix with the sea in a complex maze of fjords, with thousands of islands. It is a true wilderness where not exploited by logging and salmon farming pens. But there are some areas accessible from roads that can be explored, including west of Lillooet, the Chilcotins, and the Garibaldi Range. The Coast Mountains extend approximately 1,600 kilometres (1,000 mi) long from the southeastern boundaries are surrounded by the Fraser River and the Interior Plateau while its far northwestern edge is delimited by the Kelsall and Tatshenshini Rivers at the north end of the Alaska Panhandle, beyond which are the Saint Elias Mountains. The western mountain slopes are covered by dense temperate rainforest with heavily glaciated peaks and icefields that include Mt Waddington and Mt Silverthrone. Mount Waddington is the highest mountain of the Coast Mountains and the highest that lies entirely within British Columbia, located northeast of the head of Knight Inlet with an elevation of 4,019 metres (13,186 ft). The range along its eastern flanks tapers to the dry Interior Plateau and the boreal forests of the southern Chilkotins north to the Spatsizi Plateau Wilderness Provincial Park. The mountain range's name derives from its proximity to the sea coast, and it is often referred to as the Coast Range. The range includes volcanic and non-volcanic mountains and the extensive ice fields of the Pacific and Boundary Ranges, and the northern end of the volcanic system known as the Cascade Volcanoes. -
COLUMBIA Ministry of Employment and Investment Energy and Minerals Division Geological Survey Branch
BRITISH COLUMBIA Ministry of Employment and Investment Energy and Minerals Division Geological Survey Branch GEOLOGY AND MINERAL OCCURRENCES OF THE TASEKO - BRIDGE RIVER AREA By P. Schiarizzs, P.Geo., R.G. Gaba, P.Geo., J.K. Glover, P.Geo., J.I. Garver and P.J. Umhoefer Contributions by D.A. Archibald, T.P. Poulton,H.W. Tipper, F. Cordey, M.J. Orchard, J.A. Jeletzky, J.W. Haggart, J.F. Basinger, A.R. Sweet and R.M. Friedman BULLETIN 100 Canadian Catalominp,.. in Publication Data r Main entry under title: Geology and mineral Occurrences of the Taseko - Bridge River area (Bulletin ; 100) Issued by Geological Survey Branch. Includes bibliographical references: p. ISBN 0-7726-3044-5 1. Geology -British Columbia - Taseko River Region. 2. Geology, kconamic - British Columbia - Taseko River Region. 3. Mines and mineral resources - British Columbia VICTORIA - Taseko River Region. 1. Schiarizza, P. 11. British BRITISH COLUMBIA Columbia. Minisy of Employment and Investment. 111. CANADA British Columbia. Geological Survey Branch. 1V. Title. V. Series: Bulletin (British Columbia. Minisq of Employment and Invescment ) ; 1W. FEBRUARY 1997 QE187.G46 1997 557.11'31 C96-960332-0 The Taseko -Bridge River map area covers about 3200 rocks, formerly includedin the Noel Formation,that are here square kilometresof mountainous terrain centred200 kilo- assignedtotheinformalGunLakeandDowntonLakeunits. metres northof Vancouver. It lies between latitudesSO"45' These rocks are included withinthe Cayoosh assemblage,a and 5l'lS'north and longitudes 122"OO'and 123"3O'west, thick coherent succession of clastic metasedimenlary rocks and covers NTS map areas 920/2 and 920/3 and portions that conformably overlies the BridgeRiver Comp1,:x to the of map areas920/1,92J/14,92J/IS and 92J/16. -
Assessment of Fish Habitat and Production in Downton Lake
TABLE OF CONTENTS Page ABSTRACT ................... ......................... , i ACKNOWLEGEMENTS ..... ... .... iv TABLE OF CONTENTS ......... ............................ v LIST OF TABLES . " Vll LIST OF FIGURES . ....... ... ......................... Vlll LIST OF APPENDICES .... .... .......................... Xl 1.0 INTRODUCTION............ ..... .................... 1 2.0 BACKGROUND........................................ 3 2.1 Study Area ................ ...................... 3 2.2 Hydroelectric Development ............................. , 5 2.3 Other Development ............. .................... 7 2.4 Fish Resources ........ ............................ 9 3.0 METHODS .. .. .................. ....... .... .... 10 3.1 Description and Evaluation of Stream Habitat ................ " 10 3.2 Fish Sampling in Streams. .. 11 3.3 Estimation and Evaluation of Standing Stock Capability in Streams .................................. 12 3.4 Fish Sampling in the Reservoir ...... ..... ........... 13 3.5 Lirnnological Monitoring . .. 14 4.0 RESULTS........................................... 15 4.1 Weather and Streamflow Conditions During the October ". Field Investigations . .. 15 4.2 Turbidity and the Influence of Glacial Meltwater. .. 16 4.3 .Description and Evaluation of Fish Habitat in Streams .... ....... 17 4.3.1 BridgeRivermainstem ......................... 17 4.3.2 Bridge River side channels and associated tributaries . .. 22 4.3.3 McParlon Creek . .. 30 4.3.4 Smaller tributaries to the reservoir . 30 4.4 Distribution and Abundance of -
BC Hydro-Party Response
BC Hydro—Party Response A14/SEM/97-001/05/RSP DISTRIBUTION: General ORIGINAL: English EXECUTIVE SUMMARY On April 2, 1997, the Sierra Legal Defence Fund and the Sierra Club Legal Defense Fund (the "submitters") made a submission under Article 14 of the North American Agreement on Environmental Cooperation (NAAEC) alleging that the Government of Canada is failing to enforce its environmental law effectively. Specifically, the submission asserts that Canada fails to enforce s.35(1) of the Fisheries Act and fails to utilize its powers pursuant to s.119.06 of the National Energy Board Act to protect fish and fish habitat from damage caused by hydroelectric power generation in British Columbia by BC Hydro (BCH), a provincial Crown corporation. CANADA'S POSITION Canada supports the NAAEC process for submissions on enforcement matters, and considers Articles 14 and 15 to be among the most important provisions of the treaty. Canada submits that it is enforcing its environmental laws, and is in full compliance with its obligations under the NAAEC. Therefore, Canada submits that, in this instance, the development of a factual record is unwarranted as: · the assertions concerning the enforcement of the Fisheries Act are the subject of pending judicial or administrative proceedings within the meaning of Article 14(3)(a); · Canada is fully enforcing the environmental provisions of the Fisheries Act, and the National Energy Board (NEB) has properly exercised its power under the National Energy Board Act; · the provisions of the NAAEC cannot be applied retroactively to assertions of a failure to effectively enforce environmental laws prior to the coming into force of the NAAEC on January 1, 1994. -
BC Geologcal Survey Assessment Report 38364
Assessment Report on the Mike Property Lillooet Mining Division Southern British Columbia, Canada Mineral Claims: 1063762, 1063763, 1063764, 1063765, 1063766, 1063767, 1063768, 1063769, 1063770, 1063771, 1063772, 1063773, 1063774 NTS Map Sheet 92J/13E, 14W Latitude 55°55’N / Longitude 123°25’W Prepared for Cresval Capital Corp. By Christopher Basil Coast Mountain Geological Ltd June, 2019 Contents Page Summary / Introduction….…………………………………………………………………………………………………………1 Property Description, Location and Access……….…………………………………….…………………………………1 Climate, Local Resources, Infrastructure and Physiography……………………..………………………………..3 History……………………………………………………………………………………………………………………………………….5 Regional Geology……………………………………………………………………………………………………………………….5 Property Geology……………………………………………………………………………………………………………………….6 Mineralization …………………………………………………………………………………………………………………………..7 2019 Ground Magnetics Survey……………………………………………………………………………………………….12 Conclusions…………………………………..…………………………………………………………………………………………15 References……………………………………………………………………………………………………………………………….16 Figure 1 – Location Plan…………………………………………………………………………………………………………….2 Figure 2 – Tenure Map………………………….…………………………………………………………………………………..4 Figure 3 – Regional Geology………………….…………………………………………………………………………………..9 Figure 4 – Local Geology……………………………………………………………………………………………………….…11 Figure 5 – Ground Magnetics Survey Location……………………………………………………..…….……………13 Figure 6 – Ground Magnetic Survey Plan ……………………………………………………………………..…………14 Table 1 – Tenure Details………………………………………………………………………………………………………….…3 -
Preserving British Columbia's Coast
PRESERVING BRITISH COLUMBIA’S COAST: A REGULATORY REVIEW Background Report by West Coast Environmental Law for the BC Near Shore Habitat Loss Work Group Puget Sound/Georgia Basin International Task Force Linda Nowlan, Barrister & Solicitor West Coast Environmental Law 1001 – 207 West Hastings Street Vancouver, BC V6B 1H7 (604) 601-2509 [email protected] Acknowledgements This report is the result of a contract from the BC Habitat Loss Work Group, a sub- group of the Puget Sound-Georgia Basin International Task Force. The report was funded by the BC Ministry of Environment, Lands and Parks and Department of Fisheries and Oceans. The Members of the Task Group are: Ted Pobran, Ministry of Environment, Lands and Parks; Karen Wipond, Ministry of Environment, Lands and Parks; Don Howes, Land Use Coordination Office; Mark Zacharias, Land Use Coordination Office; Erik Karlsen, Ministry of Municipal Affairs; Les Bogdan, Ducks Unlimited; Michael Dunn, Canadian Wildlife Service; and Karen Calla, Department of Fisheries and Oceans. The author wishes to thank the members of the Task Group for their assistance and comments on this report. Special thanks go to Michael Dunn, Karen Wipond, and Mark Zacharias for their detailed comments. The author would also like to thank the staff of West Coast Environmental Law Research Foundation for their assistance in producing this report. Karen Campbell commented on a draft, Alexandra Melnyk did word processing, Catherine Ludgate did project coordination, Christopher Heald was responsible for desktop publishing, -
Objective Preliminary Assessment of Outburst Flood Hazard from Moraine-Dammed Lakes in Southwestern British Columbia
OBJECTIVE PRELIMINARY ASSESSMENT OF OUTBURST FLOOD HAZARD FROM MORAINE-DAMMED LAKES IN SOUTHWESTERN BRITISH COLUMBIA Robin James McKillop B.Sc., University of British Columbia, 2001 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE In the Department of Earth Sciences O Robin James McKillop 2005 SIMON FRASER UNIVERSITY Fall 2005 All rights reserved. This work may not be reproduced in whole or in part, by photocopy or other means, without permission of the author. APPROVAL Name: Robin James McKillop Degree: Master of Science Title of Thesis: Objective preliminary assessment of outburst flood hazard from moraine-dammed lakes in southwestern British Columbia Examining Committee: Chair: Dr. Peter Mustard Associate Professor, Department of Earth Sciences Dr. John Clague Senior Supervisor Professor, Department of Earth Sciences Dr. Tracy Brennand Supervisor Associate Professor, Department of Georgraphy Dr. Matthias Jakob Supervisor BGC Engineering Inc. Dr. Jim O'Connor External Examiner U.S. Geological Survey Date Defended: SIMON FRASER 0~~~~~~dibrary 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. -
REGION 3 - Thompson-Nicola
REGION 3 - Thompson-Nicola CONTACT INFORMATION Fish and Wildlife Regional Office Salmon Information: (250) 371-6200 1259 Dalhousie Dr Fisheries and Oceans Canada Kamloops BC V2C 5Z5 District Offices (DFO) Conservation Officer Service Kamloops: (250) 851-4950 Please call 1-877-952-7277 for recorded Lillooet: (250) 256-2650 information or to make an appointment at Salmon Arm: (250) 804-7000 any of the following Field Offices: Clearwater, Kamloops, Lillooet and Merritt R.A.P.P. Report All Poachers and Polluters Conservation Officer 24 Hour Hotline 1-877-952-RAPP (7277) STAY UP TO DATE: Cellular Dial #7277 Check website for in-season changes or Please refer to page 78 for more information closure dates for the 2021-2023 season rapp.bc.ca at: www.gov.bc.ca/FishingRegulations 7-1 7-4 5-15 WARNING Due to aeration projects, DANGEROUS THIN ICE & OPEN WATER may 5-13 3-46 exist on Bleeker, Horseshoe, Lodgepole, 7-2 Logan, Rose, Stake, Tulip & Walloper Lakes. 3-44 3-43 4-40 3-45 5-14 3-40 5-2 3-39 5-1 3-42 5-4 3-41 4-38 5-3 4 3-38 3-31 3-36 4-39 3-30 3-35 3-37 3-32 3-29 3-28 3-34 3-27 3-33 3-26 3-17 8-24 2-11 3-18 8-26 3-16 3-19 3-20 2-6 8-21 8-25 8-22 8-23 3-14 3-13 3-12 8-11 2-7 2-9 2-10 3-15 8-10 8-6 8-8 2-18 2-8 2-17 8-5 8-9 The Management Unit boundaries indicated on the2-19 map above are shown only as a reference8-7 to help anglers locate waters in the region. -
Chapteir 5 Tectonic Implications"
Ministry of Employment and In vestment CHAPTEIR 5 TECTONIC IMPLICATIONS"- REGIONALCORRELATION AND which extends continuously along the southwestside ofthe SIGNIFICANCE OF MAIN Yalakom fault for 80 kilometres to Chilko Lake (Figure 39). At the southeast end of thisbelt, within theTaseko . Bridge LITHOTECTONIC ASSEMBLAGES River map area, this clastic succession is inferred to have BRIDGE RIVER TERRANE been deposited abovethe Bridge River Complex($e? Chap- ter 2). The Tyaughton basin beltis also bounded onits north- The Bridge River Terrane is represented the West side by sparse exposures ofthe BridgeRiver Complex BridgeRiver Complex, which includes Mississippianto (Riddell eT 1993a,b), indicating that the Bridge River Middle Jurassic chert, pillowed and massive greenstone, Complex probably underlies, in the subsurface, th3 entire limestone, clastic rocks and blueschist. The Taseko - Bridge belt of clastic sedimentary Theexposures at th north- River map area encompasses the northwestern end Of the west end of the belt, east of Chilko Lake, are bounded to the mainoutcrop beltoftheBridgeRiverComplex~A1ougstrike north by fault-bounded panels OfCadwaIlader and p/Iethow to thenorthwest is the main exposure beltJura-Creta-of terranes, and are the exposures of tl,e ceous clastic sedimentary rocksof the Tyaughton basin, Bridge River complex. Figure 39.Map showing the distributionof major tectonostratigraphic elementsof the southeastern Coast Beltin the Pemhrton, Taseko Lakes and Mount Waddington map sheets. BRC=narrow lens of Bridge River Complex east of Chilko Lake. Map is basec on the compilations of Schiarizza et ai. (1994) and Monger and Joumeay (1994). The Bridge River Terranealso includes local exposures cludes Permian limestone containing Tethyan fusilin :ds of clastic sedimentary rocks assignedto the Gun Lake and (Brandon et 41. -
Squamish Whistler Pemberton
dowed a major slide. If history is to be any kind cher, a series of smaller rock slides in the was up to 15 metres deep and covering 100 of the highway in the area of the salt sheds, about etres north of Squamish. work was occurring last Tuesday, more rubble I above. And then on Wednesday morning, ers should expect delays of up to four hours on sday and Thursday this week. About 2 1/2 years etres south of where the current slides are occur- iGEIViXhann, a forest industry consultant, can often be $fl-aversing!. proposed logging CLI t blocks or logging ;,’looking for tension cracks or any other sign of bili ty ‘s!I bann said that he has stood just south of the salt &where. .+ one can see a major fault cutting through ’ . He said the area where the slides are occurring is of unusual faulting. In fact, the Cheakamus The Ministry of Transportation and Highways continues to monitor the area of recent rockslides in the Cheakamus is located where it is because of faults in the area. canyon north of Squamish. Brian Goldstone photo intain that you can identify these faults - the stry has to do this on a daily basis.” clues could not have been picked up on.’’ and Highways. said that after the Cheakamus canyon slide The rocks in the area are metavolcanic rocks that have In the slide 2 1/2 years ago, two defined discontinuities ears ago an in-depth study of the area should been heated up and thus altered, resulting in a random in a wedge quite high ~ipon the slope popped out and n done, in which the entire area would be jointing and fracturing pattern with ”some shear zones resulted in the slide. -
Cayoosh Mountains
Vol.31 No.1 Winter 2012 Published by the Wilderness Committee FREE REPORT BENDOR AND CAYOOSH MOUNTAINS TRIBAL PARK PROTECTION NEEDED NOW! BEAUTIFUL LANDS OF THE ST'ÁT'IMC Joe Foy National Campaign Portage, Shalalth, Samahquam, Skatin which means they have pockets of both proposed tribal parks encompassing Director, and Douglas are strategically located on types of habitat. Unfortunately both the Bendor and Cayoosh mountains. Wilderness Committee trail and canoe routes that are thousands ranges are under threat from proposed This is an important step forward of years old near some of the world's industrial developments including that needs to be taken, and one most productive wild salmon rivers.1 logging and a proposed ski resort. So that is long overdue. Read on to Within St'át'imc territory are some of far the rugged nature of the Bendor and learn how you can help gain tribal here do I go when I want my favourite protected areas, including Cayoosh mountains and the courageous park protection for the Bendor and Wto see some of the wildest, portions of Garibaldi Provincial Park, nature of the St'át'imc people have Cayoosh mountains! most beautiful landscapes in the Stein Valley Nlaka'pamux Heritage been able to fend off the worst of the world? Where do I go when I want to Park and South Chilcotin Mountains industrial projects, which is why these Learn about the experience a place and a culture where Provincial Park. areas are still so wild and beautiful. But St'át'imc people people have lived for centuries upon However, two wilderness mountain for how long? centuries? I go to St'át'imc of course! ranges located in the heart of St'át'imc The St'át'imc have produced a land- and their land Several hundred kilometres to territory that are critical to the region's use plan for the northern portion of at statimc.net the north of Vancouver, BC lies the ecological and cultural well-being are their territory.