Cheakamus River Water Use Plan Report of the Consultative Committee
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Varve-Related Publications in Alphabetical Order (Version 15 March 2015) Please Report Additional References, Updates, Errors Etc
Varve-Related Publications in Alphabetical Order (version 15 March 2015) Please report additional references, updates, errors etc. to Arndt Schimmelmann ([email protected]) Abril JM, Brunskill GJ (2014) Evidence that excess 210Pb flux varies with sediment accumulation rate and implications for dating recent sediments. Journal of Paleolimnology 52, 121-137. http://dx.doi.org/10.1007/s10933-014-9782-6; statistical analysis of radiometric dating of 10 annually laminated sediment cores from aquatic systems, constant rate of supply (CRS) model. Abu-Jaber NS, Al-Bataina BA, Jawad Ali A (1997) Radiochemistry of sediments from the southern Dead Sea, Jordan. Environmental Geology 32 (4), 281-284. http://dx.doi.org/10.1007/s002540050218; Dimona, Jordan, gamma spectroscopy, lead-210, no anthropogenic contamination, calculated sedimentation rate agrees with varve record. Addison JA, Finney BP, Jaeger JM, Stoner JS, Norris RN, Hangsterfer A (2012) Examining Gulf of Alaska marine paleoclimate at seasonal to decadal timescales. In: (Besonen MR, ed.) Second Workshop of the PAGES Varves Working Group, Program and Abstracts, 17-19 March 2011, Corpus Christi, Texas, USA, 15-21. http://www.pages.unibe.ch/download/docs/working_groups/vwg/2011_2nd_VWG_workshop_programs_and_abstracts.pdf; ca. 60 cm marine sediment core from Deep Inlet in southeast Alaska, CT scan, XRF scanning, suspected varves, 1972 earthquake and tsunami caused turbidite with scouring and erosion. Addison JA, Finney BP, Jaeger JM, Stoner JS, Norris RD, Hangsterfer A (2013) Integrating satellite observations and modern climate measurements with the recent sedimentary record: An example from Southeast Alaska. Journal of Geophysical Research: Oceans 118 (7), 3444-3461. http://dx.doi.org/10.1002/jgrc.20243; Gulf of Alaska, paleoproductivity, scanning XRF, Pacific Decadal Oscillation PDO, fjord, 137Cs, 210Pb, geochronometry, three-dimensional computed tomography, discontinuous event-based marine varve chronology spans AD ∼1940–1981, Br/Cl ratios reflect changes in marine organic matter accumulation. -
Garibaldi Provincial Park M ASTER LAN P
Garibaldi Provincial Park M ASTER LAN P Prepared by South Coast Region North Vancouver, B.C. Canadian Cataloguing in Publication Data Main entry under title: Garibaldi Provincial Park master plan On cover: Master plan for Garibaldi Provincial Park. Includes bibliographical references. ISBN 0-7726-1208-0 1. Garibaldi Provincial Park (B.C.) 2. Parks – British Columbia – Planning. I. British Columbia. Ministry of Parks. South Coast Region. II Title: Master plan for Garibaldi Provincial Park. FC3815.G37G37 1990 33.78”30971131 C90-092256-7 F1089.G3G37 1990 TABLE OF CONTENTS GARIBALDI PROVINCIAL PARK Page 1.0 PLAN HIGHLIGHTS 1 2.0 INTRODUCTION 2 2.1 Plan Purpose 2 2.2 Background Summary 3 3.0 ROLE OF THE PARK 4 3.1 Regional and Provincial Context 4 3.2 Conservation Role 6 3.3 Recreation Role 6 4.0 ZONING 8 5.0 NATURAL AND CULTURAL RESOURCE MANAGEMENT 11 5.1 Introduction 11 5.2 Natural Resources Management: Objectives/Policies/Actions 11 5.2.1 Land Management 11 5.2.2 Vegetation Management 15 5.2.3 Water Management 15 5.2.4 Visual Resource Management 16 5.2.5 Wildlife Management 16 5.2.6 Fish Management 17 5.3 Cultural Resources 17 6.0 VISITOR SERVICES 6.1 Introduction 18 6.2 Visitor Opportunities/Facilities 19 6.2.1 Hiking/Backpacking 19 6.2.2 Angling 20 6.2.3 Mountain Biking 20 6.2.4 Winter Recreation 21 6.2.5 Recreational Services 21 6.2.6 Outdoor Education 22 TABLE OF CONTENTS VISITOR SERVICES (Continued) Page 6.2.7 Other Activities 22 6.3 Management Services 22 6.3.1 Headquarters and Service Yards 22 6.3.2 Site and Facility Design Standards -
Copyrighted Material
INDEX See also Accommodations and Restaurant indexes, below. AKAL Airport, 79 GENERAL INDEX aby Bedwell Lake, 119 Alder Grove Trail, 68 B Backcountry Tours, 144 Alexander Mackenzie Heri- bbott, Mount, 225 Baden-Powell Trail, 44, 48 A tage Trail (Nuxalk–Carrier Abbott Ridge, 225 Baker, Mount, 60, 214 Grease Trail), 167, 168 Abbott Ridge Trail, Glacier Balancing Rock, 132, 134 Alpha Pool, 180 National Park, 222–225 Bald eagles Alpine Club of Canada, 252 Acadia Beach, 56 Meares Island, 116 American Automobile Asso- Access America, 257 Vancouver Island, 81 ciation (AAA), 14, 254 Accommodations. See also Bald Mountain, 175 American Camp (San Juan Accommodations Index Bandanas, 10 Island), 98–102 best mountain lodges, 4–5 Banff, 248 Amphitrite Lighthouse, 113 Canadian Rockies and the Bare Buns Run, 56 Angel Staircase Falls, 232 Kootenays hikes, Barely Legal Motorsports, Annual Discovery 251–252 144 Package, 13 Cariboo Country, 188–189 Barkerville, gold rush and, Antler Creek, 175 green-friendly, 15 174 Apex Lookout, 201 Okanagan Valley hikes, Barkerville to Summit Rock & Arbutus Trail, 38 216–217 Groundhog Lake, 172–175 Area codes, 254 toll-free numbers and Barkley Sound, 113 Asking Rock, 147 websites, 262 Barred Owl Path, 38 Association of Canadian Vancouver and the Sun- Bate Point, 110 Mountain Guides, 19 shine Coast, 72–75 BC Ferries, 30 Atlin Provincial Park, 180 Vancouver Island, 120–122 BC Orchard Industry Atlin Quest, 180 Whistler area, 149–150 Museum, (Kelowna), 192 ATM networks/cash Admiralty Trail, 54 Beach Access A (West Coast points, -
2010-08-17 Package Council COMPLETE
R EGULAR MEETING OF MUNICIPAL COUNCIL AGENDA TUESDAY, AUGUST 17, 2 0 1 0 , STARTING AT 5:30 PM In the Franz Wilhelmsen Theatre at Maurice Young Millennium Place 4335 Blackcomb Way, Whistler, BC V0N 1B4 APPROVAL OF AGENDA Approval of the Regular Council agenda of August 17, 2010. ADOPTION OF MINUTES Adoption of the Regular Council minutes of August 3, 2010. PUBLIC QUESTION AND ANSWER PERIOD PRESENTATIONS/DELEGATIONS Whistler Half Marathon A presentation by Dave Clark, Race Director, regarding the Whistler Half Marathon for June 2011. RBC GranFondo A presentation by Neil McKinnon, GranFondo Canada co-founder, regarding the RBC Gran Fondo for September 11, 2010. Pay Parking An update regarding pay parking by Bob MacPherson, General Manager of Community Life. BC Transit A presentation by Manuel Achadinha, CEO, Peter Rantucci, Director – Regional Transit Systems, and Johann van Schaik, Regional Transit Manager – South Coast, regarding Key Performance Indicators for BC Transit. MAYOR’S REPORT ADMINISTRATIVE REPORTS RBC GranFondo Whistler That Council endorses the Special Occasion License application of Fraser Boyer for the Special Occasion Liquor RBC GranFondo Whistler to be held on Saturday, September 11, 2010. License Report No. 10-081 File No. 7627.2 Regular Council Meeting Agenda August 17, 2010 Page 2 Whistler Aggregates That Council considers giving first reading to Official Community Plan Amendment Rezoning Bylaw (Material Extraction) No. 1931, 2009; Report No. 10-086 File No. RZ. 1025 That Council considers giving second reading to -
Cheakamus River – Balls to the Wall
Cheakamus River – Balls To The Wall Vitals Locale: Whistler, British Columbia What It's Like: Extension of the Upper Cheak - great class IV-IV+ river running, and a bonus waterfall. Some wood. Class: IV-IV+ Scouting/Portaging: Scouting is ok. Difficult to portage in spots, if you're forced to. Falls is easy to walk. Level: Online gauge: http://wateroffice.ec.gc.ca/report/report_e.html?type=realTime&stn=08GA072 Cheakamus River - this gauge is at the put in. Time: 2-3 hours for a relaxed first trip. When To Go: All season, very pushy at high flows. Reasonable minimum is 2.1. Info From: Many visits. Other Beta: None. Description Gauge info: if you have previous experience on the Cheak, note that the gauge changed sometime before the 2015 season and now reads about 0.1 m lower than it used to. Levels are adjusted appropriately on this page. The Cheakamus River is synonymous with Whistler kayaking, largely because of the ultra-classic Upper Cheak section near Function Junction. Unbeknownst to many and maybe avoided by others because of tales of epic log jams and the Whistler waste water treatment plant, there is an equally fun and perhaps more adventurous stretch that departs from the Upper Cheak take out and ends at the confluence with Callaghan Creek. It's a little bit harder, a little bit more committing, it has a great waterfall for those so inclined and there is a lot more wood in the river. You can run it as a stand-alone section of whitewater if you want something short, but it's best combined with the Upper Cheak to make a great hour or two of river running. -
CHEAKAMUS RIVER Coho Salmon Production from Constructed Off-Channel Habitat, 2001
LOWER MAINLAND BCH HABITAT RESTORATION 2000-2001 CHEAKAMUS RIVER Coho Salmon Production From Constructed Off-Channel Habitat, 2001 M. Foy, Biologist; H. Beardmore, Engineer; S. Gidora, Bio-technician Resource Restoration Group, Habitat and Enhancement Branch Lower Fraser Area, Pacific Region, Fisheries and Oceans Canada August, 2002 1 TABLE OF CONTENTS EXECUTIVE SUMMARY……………………………………………….……………...3 1. INTRODUCTION……………………………………………………………………..3 2. STUDYAREA………………………………………………………….………………3 3. METHODS…………………………………………………………………………….4 3.1. Coho population estimate, off-channel habitat……………………4 3.1.1. Downstream weir counts………………………………………….4 3.1.2. Minnow trap mark-recapture estimate…………………………..5 3.1.3. Total coho production from constructed habitat………………..5 3.2. Coho population estimate, Cheakamus watershed………….…………….5 3.2.1. Marked population………………………………………………..5 3.2.2. Recovery of marked fish………………………………………….6 3.2.3. Coho production estimate, Cheakamus watershed……………..6 4. RESULTS……………………………………………………………….……………..6 4.1. Coho population estimate, off-channel habitat……………………6 4.1.1. Downstream weir counts………………………………………….6 4.1.2. Minnow trapping mark-recapture estimate……………………..7 4.1.3. Total coho production from constructed habitat………………..7 4.2. Coho population estimate, Cheakamus watershed………….…………….7 4.2.1. Marked population………………………………………………..7 4.2.2 Recovery of marked fish…………………………………………..7 4.2.3. Coho production, Cheakamus watershed……………………….7 5. DISCUSSION………………………………………………………………………….8 6. CONCLUSIONS………………………………………………………………………9 7. ACKNOWLEDGEMENTS…………………………………………………………..9 -
The Mamquam River Floodplain Restoration Project
Background Information: The Mamquam River Floodplain Restoration Project The Mamquam River Floodplain Restoration project is being undertaken in The partnership with the Squamish River Watershed Society, Fisheries and Oceans Mamquam Canada, District of Squamish, and Squamish Nation. Funding support has been River is received from the Pacific Salmon Commission, B.C. Ministry of Transportation, important Pacific Salmon Foundation, Canadian Hydro Development Corporation. The coho and Squamish River Watershed Society and the local community are working closely Chinook to provide future working plans for conservation of these important floodplain salmon lands. habitat. 2005 The Mamquam River is an important coho, pink, chum and Chinook salmon producing tributary within the Squamish River watershed. The Squamish River estuary, lying at the head of Howe Sound, was formed at the confluences of the Mamquam and Squamish Rivers and historically supported a large complex wetland with interconnected tidally influenced sloughs and channels. These diverse habitats provided exceptional quality habitat for many salmonid species particularly coho, pink, chum and Chinook salmon. Dyking in the early twentieth century confined the Mamquam River and Squamish Rivers to relatively narrow corridors isolated from most of their historic floodplain The building lands. Internal drainages remain in some of the undeveloped portions of these of dykes on isolated floodplain areas but suffer from reduced flows and poor connections to the viable salmon populations in adjacent habitats. One such drainage is Loggers Lane Mamquam & Creek. Loggers Lane Creek was originally a river channel of the Mamquam River Squamish but was isolated following a giant storm in 1921 after which the dyke was built. -
Cheakamus River Watershed Action Plan
CHEAKAMUS RIVER WATERSHED ACTION PLAN FINAL November 14, 2017 Administrative Update July 21, 2020 The Fish & Wildlife Compensation Program is a partnership between BC Hydro, the Province of B.C., Fisheries and Oceans Canada, First Nations and Public Stakeholders to conserve and enhance fish and wildlife impacted by BC Hydro dams. The Fish & Wildlife Compensation Program is conserving and enhancing fish and wildlife impacted by BC Hydro dam construction in this watershed. Top row from left: Cheakamus Dam and powerhouse. Bottom row from left: Squamish River Powerhouse (Credit BC Hydro). Cover photos: Coho fry (Credit iStock) and Roosevelt Elk (Credit iStock). The Fish & Wildlife Compensation Program (FWCP) is a partnership between BC Hydro, the Province of BC, Fisheries and Oceans Canada, First Nations and Public Stakeholders to conserve and enhance fish and wildlife impacted by BC Hydro dams. The FWCP funds projects within its mandate to conserve and enhance fish and wildlife in 14 watersheds that make up its Coastal Region. Learn more about the Fish & Wildlife Compensation Program, projects underway now, and how you can apply for a grant at fwcp.ca. Subscribe to our free email updates and annual newsletter at www.fwcp.ca/subscribe. Contact us anytime at [email protected]. 2 Cheakamus River Action Plan EXECUTIVE SUMMARY: CHEAKAMUS RIVER WATERSHED The Fish & Wildlife Compensation Program is a partnership between BC Hydro, the Province of B.C., Fisheries and Oceans Canada, First Nations and Public Stakeholders to conserve and enhance fish and wildlife impacted by BC Hydro dams. This Action Plan builds on the Fish & Wildlife Compensation Program’s (FWCP’s) strategic objectives, and is an update to the previous FWCP Watershed and Action Plans. -
Department of Recreation and Conservation 1 K
PROVINCE OF BRITISH COLUMBIA DEPARTMENT OF RECREATION AND CONSERVATION 1 K. KIBRNAN, Minister D. B. TURNER, Deputy Mini REPORT OF THE Department of Recreation and Conservation containing the reports of the FISH AND GAME BRANCH, PROVINCIAL PARKS BRANCH, BRITISH COLUMBIA GOVERNMENT TRAVEL BUREAU, PROVINCIAL MUSEUM OF NATURAL HISTORY AND ANTHROPOLOGY, PHOTOGRAPHIC BRANCH, AND COMMERCIAL FISHERIES BRANCH Year Ended December 31 1964 VICTORIA, B.C., January 21, 1965. To Major-General the Honourable GEORGE RANDOLPH PEARKES, V.C., P.C., C.B., D.S.O., M.C., Lieutenant-Governor of the Province of British Columbia. MAY IT PLEASE YOUR HONOUR: Herewith I beg respectfully to submit the Annual Report of the Department of Recreation and Conservation for the year ended December 31, 1964. VICTORIA, B.C., January 21, 1965. SIR,—I have the honour to submit the Annual Report of the Department of Recreation and Conservation for the year ended December 31, 1964. CONTENTS Introduction by the Deputy Minister of Recreation and Conservation Fish and Game Branch Provincial Parks Branch British Columbia Government Travel Bureau Provincial Museum of Natural History and Anthropology— Photographic Branch ___ Commercial Fisheries Branch... r Report of the Department of Recreation and Conservation, 1964 D. B. TURNER, DEPUTY MINISTER AND COMMISSIONER OF FISHERIES INTRODUCTION The Department of Recreation and Conservation was created in 1957 and commenced operation as an entity April 1st of that year. That event was unique, for it was the first time in the history of Province or State in North America that the major elements of outdoor recreation were brought together under a single administration. -
“Salmon on the Rough Edge of Canada and Beyond”
“Salmon on the Rough Edge of Canada and Beyond” A Squamish Thanksgiving By Matt Foy Located in south-western British Columbia, Canada, the Squamish River is a large glacial fed watershed. The brawling mountain river, with its major tributaries such as the Elaho, Cheakamus, Ashlu, and Mamquam Rivers drains from the rugged terrain of the BC Coast mountains into the head of Howe Sound, part of the Salish Sea. Once known for its prolific runs of pink salmon these runs were decimated during the late- twentieth century. This is a story about their remarkable recovery and some of the people who worked hard to see pink salmon return to this beautiful mountain domain. As summer slid into fall, the phenomenal pink salmon run to the Squamish River was just winding down. The run of 2013 had exceeded all expectations, and such an abundance of pink salmon had not been observed in over fifty years, since the memorable return of 1963. For many people, the 2013 return would seem to have come out of nowhere but many other people understood the hard work and dedication that had led to this remarkable recovery. In that season of giving thanks, it seems fitting to reflect back on the path that has led from the last great run of 1963 to the years when pink salmon were almost absent from the Squamish River watershed, to the fall of 2013, one of great abundance to be celebrated and remembered. Upper Howe Sound, Squamish, BC, Canada Photo: Courtesy Ruth Hartnup Boom and Bust The growth decades of the 1950’s through the 1970’s were not kind to pink salmon populations around the Strait of Georgia. -
Influence of a Large Debris Flow Fan on the Late Holocene Evolution of Squamish River, Southwest British Columbia, Canada
Canadian Journal of Earth Sciences Influence of a large debris flow fan on the late Holocene evolution of Squamish River, southwest British Columbia, Canada Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2017-0150.R2 Manuscript Type: Article Date Submitted by the Author: 02-Jan-2018 Complete List of Authors: Fath, Jared; University of Alberta, Renewable Resources Clague, John J.; Dept of Earth Sciences, Friele, Pierre;Draft Cordilleran Geoscience Is the invited manuscript for consideration in a Special N/A Issue? : Quaternary geology, Alluvial fans, Fan-impounded lakes, Squamish River, Keyword: Cheekye Fan https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 48 Canadian Journal of Earth Sciences 1 Influence of a large debris flow fan on the late Holocene evolution of Squamish River, southwest British Columbia, Canada 1 2 3 4 Jared Fatha,c *, [email protected] Draft 5 John J. Claguea,*, [email protected] 6 Pierre Frieleb, [email protected] 7 8 a Department of Earth Sciences, Simon Fraser University, 8888 University Drive, Burnaby, 9 BC, V5A 1S6 10 b Cordilleran Geoscience, PO Box 612, Squamish, BC, V0N 3G0 11 c Presently at Department of Renewable Resources, University of Alberta, Edmonton 12 *Corresponding author 13 https://mc06.manuscriptcentral.com/cjes-pubs Canadian Journal of Earth Sciences Page 2 of 48 2 1 Abstract 2 Cheekye Fan is a large paraglacial debris flow fan in southwest British Columbia. It owes its 3 origin to the collapse of Mount Garibaldi, a volcano that erupted in contact with glacier ice 4 near the end of the Pleistocene Epoch. The fan extended across Howe Sound, isolating a 5 freshwater lake upstream of the fan from a fjord downstream of it. -
Canada Cheakamus River Habitat Restoration Sue's Channel Project
Cheakamus River Habitat Restoration Sue’s Channel Project (06.CMS.01) Sue’s Channel Bridge March 2007 Canada Government of Canada North Vancouver Fisheries and Oceans Outdoor School Cheakamus River Salmon Habitat Restoration 06.CMS.01 “Sue’s Channel” Final Report This channel, and the educational opportunities that occur along its banks, are a memorial to Sue Emerson, and her dedication to the Bridge Coastal Restoration Program. Submitted by: Squamish River Watershed Society Prepared by: Carl Halvorson North Vancouver Outdoor School, School District #44 and Edith Tobe Squamish River Watershed Society with financial support of the BC Hydro Bridge Coastal Fish and Wildlife Restoration Program Executive Summary This project involved construction of new channel habitats and support structures for salmonid habitat located at North Vancouver Outdoor School (NVOS) (Sue’s Channel) and the restoration of channel habitats that were impacted by the October 2003 flood of record on the Cheakamus River and the August 5, 2005 CN Rail sodium hydroxide spill (Moody’s Channel), located on Squamish First Nation (SFN) I.R. 11. Design and engineering work were undertaken by Fisheries and Oceans Canada (DFO) and NVOS staff during the winter of 2005 - 2006. Construction work started late in 2005 with right of way clearing to facilitate surveys for construction levels, grades and cuts. Initial excavation for the Sue's Channel complex area started in the spring of 2006. These early excavations were funded by the concurrent Mamquam Reunion project. Approx. 1200 m3 of alluvial gravels extracted on-site at NVOS were utilized in that project. Excavation started in earnest in late spring with the start of the "Moody's Channel" phase of the project.