Scottish Coast Range Expedition 2002
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Sunshine Coast Conservation Association
Spring 2013 Issue 24 Sunshine Coast PO Box 1969 Conservation Association Sechelt BC NEWSLETTER V0N 3A0 www.thescca.ca From sand grains to salmon: why Needed: a sound management forage fish are vitally important plan for the future of Howe Sound by Dianne Sanford and Ramona DeGraaf by Ruth Simons You have heard it before: “all things are connected.” Can you Smack in the middle of a panoramic view of Howe Sound, a gi- connect beach sand grains to the food chain of Pacific salmon, ant gravel mine is in the planning stage for McNab Valley. blue herons or killer whales? These are just some of the hun- This is alarming on an immediate level: the impact the mine dreds of predator species that feed on the sea’s “forage fish.” could have on the area is devastating. But the fact that the pro- Herring are the most familiar forage fish, but surf smelt, Pacific posal is even on the table highlights a gap in long-term planning continued on page 3 for the best use of the region’s land and water. If one part of Howe Sound is damaged, the damage ripples out and affects the entire body of water and the sur- rounding communities. Without a common vision among local councils and decision makers, we’re leaving the sound vulnerable. The Future of Howe Sound Society was formed in 2011 by a group of concerned residents in re- sponse to the proposed Burnco mine. The society’s mission is to bring together all levels of govern- ment, First Nations and many stakeholder organiza- tions to come to an official consensus about how to keep Howe Sound strong, economically and envi- ronmentally, with a long-term comprehensive land and water use plan that also recognizes the sound’s social and cultural values. -
CHILCOTIN CENTRAL COAST DESTINATION DEVELOPMENT STRATEGY APE LAKE Photo: Kari Medig
CHILCOTIN CENTRAL COAST DESTINATION DEVELOPMENT STRATEGY APE LAKE Photo: Kari Medig DESTINATION BC Seppe Mommaerts MANAGER, DESTINATION DEVELOPMENT Jody Young SENIOR PROJECT ADVISOR, DESTINATION DEVELOPMENT [email protected] CARIBOO CHILCOTIN COAST TOURISM ASSOCIATION Amy Thacker CEO 250 392 2226 ext. 200 [email protected] Jolene Lammers DESTINATION DEVELOPMENT COORDINATOR 250 392 2226 ext.209 [email protected] MINISTRY OF TOURISM, ARTS AND CULTURE Amber Mattock DIRECTOR, LEGISLATION AND DESTINATION BC GOVERNANCE 250 356 1489 [email protected] INDIGENOUS TOURISM ASSOCIATION OF BC 604 921 1070 [email protected] CHILCOTIN CENTRAL COAST | 2 TABLE OF CONTENTS EXECUTIVE SUMMARY ...........................................................................1 6. A DISTINCTIVE DIRECTION ..........................................................30 a. Distinctive Destination for the Chilcotin Central Coast a. Vision b. Distinctive Direction for the Chilcotin Central Coast b. Goals c. Guiding Principles for Destination Development II. ACRONYMS ...........................................................................................5 d. Motivating Experiences 1. FOREWORD AND ACKNOWLEDGEMENTS..............................7 e. Development Themes 2. INTRODUCING THE STRATEGY .....................................................9 7. STRATEGY AT A GLANCE ................................................................38 a. Program Vision and Goals 8. STRATEGIC PRIORITIES ................................................................. -
2017 SUMMIT of EXCELLENCE AWARD Don Serl
2017 SUMMIT OF EXCELLENCE AWARD Don Serl The Banff Mountain Film and Book Festival is proud to announce Don Serl as the 2017 recipient of the Summit of Excellence Award, which recognizes an individual who has made a significant contribution to mountain life in Canada. Regarded as one of Canada’s most accomplished and prolific mountaineers, Serl has about 200 first ascents to his name. “With the Summit of Excellence Award now being presented to deserving recipients outside of the Canadian Rockies, Don Serl was an obvious and easy choice,” said Nancy Hansen, Summit of Excellence selection committee member. “Over several decades, Don has made significant contributions to Canadian mountain climbing and culture and is humble about his achievements, preferring to discuss new ideas and what others have done. He is a wealth of information about climbing on the West Coast and enjoys sharing his knowledge.” Born in Victoria and raised in Kamloops, Serl discovered a love for the mountains at the age of 25. while working as a chemist in Vancouver. In 1974, Serl trained in the Federation of Mountain Clubs of British Columbia (FMCBC) basic mountaineering course where he said his “energies and imagination were unleashed” and by 1975 he completed his initial first ascent on the north face of Mt Cheam in British Columbia. Since then “he has reigned as the preeminent Coast climber” according to author and climbing peer Chic Scott. Heavily influenced by Canadian climber Dick Culbert, Serl’s horizons opened after an Alpine Club of Canada trip into the multi-summitted Waddington Range, followed by numerous expeditionary trips into remote corners of the Coast Mountains in British Columbia. -
Uvic Thesis Template
Dendroclimatological and dendroglaciological investigations at Confederation and Franklin glaciers, central Coast Mountains, British Columbia, Canada. by Bethany L. Coulthard B.A., Mount Allison University, 2007 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE in the Department of Geography © Bethany Coulthard, 2009 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 Dendroclimatological and dendroglaciological investigations at Confederation and Franklin glaciers, central Coast Mountains, British Columbia, Canada. by Bethany L. Coulthard B.A., Mount Alison University, 2007 Supervisory Committee Dr. Dan J. Smith, (Department of Geography) Supervisor Dr. J. Gardner, (Department of Geography) Departmental Member Dr. T. Lacourse, (Department of Geography) Departmental Member iii Abstract Supervisory Committee Dr. Dan J. Smith, (Department of Geography) Supervisor Dr. J. Gardner, (Department of Geography) Departmental Member Dr. T. Lacourse, (Department of Geography) Departmental Member It has become increasingly clear that climate fluctuations during the Holocene interval were unusually frequent and rapid, and that our current understanding of the temporal and spatial distribution of these oscillations is incomplete. Little paleoenvironmental research has been undertaken on the windward side of the central Coast Mountains of British Columbia, Canada. Very high annual orographic precipitation totals, moderate annual temperatures regulated by the Pacific Ocean, and extreme topographic features result in a complex suite of microclimate conditions in this largely unstudied area. Dendroclimatological investigations conducted on a steep south-facing slope near Confederation and Franklin glaciers suggest that both mountain hemlock (Tsuga mertensiana) and subalpine fir (Abies lasiocarpa) trees at the site are limited by previous year mean and maximum summer temperatures. -
Author's Personal Copy
Author's personal copy Geomorphology 121 (2010) 197–205 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Dendrogeomorphic reconstruction of Little Ice Age paraglacial activity in the vicinity of the Homathko Icefield, British Columbia Coast Mountains, Canada Sarah J. Hart a, John J. Clague b, Dan J. Smith a,⁎ a University of Victoria Tree-Ring Laboratory, Department of Geography, University of Victoria, Victoria, British Columbia, Canada V8W 3R4 b Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia, Canada V5A 1S6 article info abstract Article history: Moraine and glacier dams bordering the Homathko Icefield in the southern British Columbia Coast Received 10 August 2009 Mountains failed in the 1980s and 1990s, causing catastrophic downstream floods. The largest of the floods Received in revised form 11 April 2010 occurred in August 1997 and was caused by overtopping and rapid breaching of the moraine dam that Accepted 19 April 2010 impounds Queen Bess Lake. The floodwaters from Queen Bess Lake eroded Holocene-age sedimentary Available online 29 April 2010 deposits along the west fork of Nostetuko River and caused a steep rise in the hydrograph of Homathko River at the head of Bute Inlet, ∼115 km downstream. A field investigation of the eroded valley fill in 2008, Keywords: fi Dendrogeomorphology revealed multiple paraglacial valley- ll units, many of which are capped by in situ stumps and woody Homathko Icefield detritus. Dendrogeomorphological field techniques were employed to develop a chronology for the buried Coast Mountains forests. A regional tree-ring chronology spanning the interval CE 1572–2007 was constructed from living Paraglacial subalpine fir(Abies lasiocarpa) trees at seven sites in the southern Coast Mountains. -
Scale Site SS Region SS District Site Name SS Location Phone
Scale SS SS Site Region District Site Name SS Location Phone 001 RCB DQU MISC SITES SIFR 01B RWC DQC ABFAM TEMP SITE SAME AS 1BB 2505574201 1001 ROM DPG BKB CEDAR Road past 4G3 on the old Lamming Ce 2505690096 1002 ROM DPG JOHN DUNCAN RESIDENCE 7750 Lower Mud river Road. 1003 RWC DCR PROBYN LOG LTD. Located at WFP Menzies#1 Scale Site 1004 RWC DCR MATCHLEE LTD PARTNERSHIP Tsowwin River estuary Tahsis Inlet 2502872120 1005 RSK DND TOMPKINS POST AND RAIL Across the street from old corwood 1006 RWC DNI CANADIAN OVERSEAS FOG CREEK - North side of King Isla 6046820425 1007 RKB DSE DYNAMIC WOOD PRODUCTS 1839 Brilliant Road Castlegar BC 2503653669 1008 RWC DCR ROBERT (ANDY) ANDERSEN Mobile Scale Site for use in marine 1009 ROM DPG DUNKLEY- LEASE OF SITE 411 BEAR LAKE Winton Bear lake site- Current Leas 2509984421 101 RWC DNI WESTERN FOREST PRODUCTS INC. MAHATTA RIVER (Quatsino Sound) - Lo 2502863767 1010 RWC DCR WESTERN FOREST PRODUCTS INC. STAFFORD Stafford Lake , end of Loughborough 2502863767 1011 RWC DSI LADYSMITH WFP VIRTUAL WEIGH SCALE Latitude 48 59' 57.79"N 2507204200 1012 RWC DNI BELLA COOLA RESOURCE SOCIETY (Bella Coola Community Forest) VIRT 2509822515 1013 RWC DSI L AND Y CUTTING EDGE MILL The old Duncan Valley Timber site o 2507151678 1014 RWC DNI INTERNATIONAL FOREST PRODUCTS LTD Sandal Bay - Water Scale. 2 out of 2502861881 1015 RWC DCR BRUCE EDWARD REYNOLDS Mobile Scale Site for use in marine 1016 RWC DSI MUD BAY COASTLAND VIRTUAL W/S Ladysmith virtual site 2507541962 1017 RWC DSI MUD BAY COASTLAND VIRTUAL W/S Coastland Virtual Weigh Scale at Mu 2507541962 1018 RTO DOS NORTH ENDERBY TIMBER Malakwa Scales 2508389668 1019 RWC DSI HAULBACK MILLYARD GALIANO 200 Haulback Road, DL 14 Galiano Is 102 RWC DNI PORT MCNEILL PORT MCNEILL 2502863767 1020 RWC DSI KURUCZ ROVING Roving, Port Alberni area 1021 RWC DNI INTERNATIONAL FOREST PRODUCTS LTD-DEAN 1 Dean Channel Heli Water Scale. -
Climate Change and Hazardous Processes in High Mountains
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2012 Climate change and hazardous processes in high mountains Clague, John J ; Huggel, Christian ; Korup, Oliver ; McGuire, Bill Abstract: The recent and continuing reduction in glacier ice cover in high mountains and thaw of alpine permafrost may have an impact on many potentially hazardous processes. As glaciers thin and retreat, existing ice- and moraine-dammed lakes can catastrophically empty, generating large and destructive downstream floods and debris flows. New ice-dammed lakes will form higher in mountain catchments, posing additional hazards in the future. The magnitude or frequency of shallow landslides and debris flows in some areas will increase because of the greater availability of unconsolidated sediment innew deglaciated terrain. Continued permafrost degradation and glacier retreat probably will decrease the stability of rock slopes. Cambio Climático y peligros naturales en altas montañas. La reciente y continua reducción de la cobertura glaciaria en alta montaña y el deshielo del permafrost pueden tener un impacto negativo en muchos procesos potencialmente peligrosos. A medida que los glaciares reducen su espesor y retroceden, los lagos formados por diques de hielo o morenas pueden vaciarse catastróficamente, resul- tando en grandes y destructivas inundaciones o flujos detríticos río abajo. Nuevos diques de hielo vana formarse en zonas más altas de las cuencas montañosas, generando peligros adicionales en el futuro. La magnitud o frecuencia de movimientos en masa superficiales y flujos detríticos va a aumentar en algunas áreas debido a la mayor disponibilidad de materiales no consolidados en nuevos terrenos desglasados. -
Homathko River & Mosley Creek Watersheds
Homathko River & Mosley Creek Watersheds Level 2 Fish Habitat & Riparian Assessment Procedure & Restoration Prescriptions Final Report G3 Consulting Ltd. Innovation & Excellence in Environmental Science Homathko River & Mosley Creek Watersheds LEVEL 2 FISH HABITAT & RIPARIAN ASSESSMENT PROCEDURE & RESTORATION PRESCRIPTIONS Final Report Prepared for: Tatlayoko Woodlot Association. Tatlayoko Lake, B.C. Submitted by: G3 Consulting Ltd. 1A-12880 Bathgate Way Richmond, BC V6V 1Z4 October 1999 Tatlayoko Woodlot Association Homathko/Mosley Level 2 FHAP & RAPP Final Report CONTENTS 1.0 INTRODUCTION ________________________________________________ 1 1.1 Project Scope __________________________________________________________ 1 Target Species _________________________________________________________ 1 1.2 Study Area Description ___________________________________________________ 2 1.3 Land Use______________________________________________________________ 2 2.0 METHODOLOGY ______________________________________________ 3 2.1 Site Identification, Selection & Confirmation___________________________________ 3 2.2 Site Classification _______________________________________________________ 3 2.3 Restoration & Rehabilitation Options ________________________________________ 3 Stream Bank Stabilization ________________________________________________ 4 Restoration of Primary Fish Habitat _________________________________________ 4 Restoration of Secondary & Tertiary Fish Habitat ______________________________ 4 Restoration of Riparian Habitat ____________________________________________ -
River Valley, Southern Coast Mountains, British Columbia Fluvial
Geological Society, London, Special Publications Fluvial response to Holocene glacier fluctuations in the Nostetuko River valley, southern Coast Mountains, British Columbia Kenna Wilkie and John J. Clague Geological Society, London, Special Publications 2009; v. 320; p. 199-218 doi:10.1144/SP320.13 Email alerting click here to receive free email alerts when new articles cite this service article Permission click here to seek permission to re-use all or part of this article request Subscribe click here to subscribe to Geological Society, London, Special Publications or the Lyell Collection Notes Downloaded by University of Alberta on 28 August 2009 © 2009 Geological Society of London Fluvial response to Holocene glacier fluctuations in the Nostetuko River valley, southern Coast Mountains, British Columbia KENNA WILKIE & JOHN J. CLAGUE* Department of Earth Sciences, Simon Fraser University, 8888 University Drive, Burnaby, British Columbia, Canada V5A 1S6 *Corresponding author (e-mail: [email protected]) Abstract: Mountain rivers, like alpine glaciers, are sensitive indicators of climate change. Some rivers may provide a more complete record of Holocene climate change than the glaciers in their headwaters. We illustrate these points by examining the record preserved in the upper part of the alluvial fill in the Nostetuko River valley in the southern Coast Mountains, British Columbia (Canada). Glacier advances in the upper part of the watershed triggered valley-wide aggradation and complex changes in river planform. Periods when glaciers were restricted in extent coincide with periods of incision of the valley fill and floodplain stability. As many as 10 overbank aggradation units are separated by peat layers containing tree roots and stems in growth position. -
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. -
Monarch Mountain, Southwest Face, and Other Ascents
AAC Publications Monarch Mountain, Southwest Face, and Other Ascents Canada, British Columbia, Coast Mountains ON JULY 28, Micha Rinn from Germany and I flew by helicopter to the col between Monarch Mountain and Page Mountain at the head of the Empire Way Glacier, deep in the Coast Mountains. Our objective was the pronounced spur that runs up the center of the unclimbed 1,250m southwest face of Monarch Mountain (3,555m). It was a line that prompted awe and excitement in equal measure—a veritable Walker Spur leading directly to the summit of the peak. How a Scottish-German climbing team came to know about one of the finest unclimbed features in western Canada requires some explanation. My fascination with Monarch, the second-highest massif in the Coast Mountains, began 20 years ago when Dave Hesleden and I traversed the Serra Group after making the first ascent of the southeast ridge of Asperity Mountain in the Waddington Range. [The route referred to in the AAJ report as the south ridge later came to be called the southeast ridge. It faces more or less south-southeast.]As we tussled with the jagged crest of the Serras, reputedly the most difficult summits in the range, Monarch stood out like a sentinel 70 miles to the north. With a prominence of 2,925m, there is no higher peak until you reach Mt. Fairweather, a thousand miles up the spine of the coastal range. I was smitten by Monarch’s dominance and resolved to climb it. The Coast Mountains had got under my skin, and I made two further trips to the Waddington massif, a couple to the Pantheon Spires, and one to the difficult-to-access Mt. -
Tamed Rivers | a Guide to River Diversion Hydropower in British Columbia Table of Contents
Tamed Rivers A Guide to River Diversion Hydropower in British Columbia Tamed Rivers A Guide to River Diversion Hydropower in British Columbia Watershed Watch Salmon Society – October 2012 Acknowledgements Watershed Watch Salmon Society prepared this document with funding from the Vancouver Foundation, the Orange County Community Foundation, the Liber Ero Foundation and the Gordon and Betty Moore Foundation. It was authored by Tanis Gower, Andrew Rosenberger, Alison Peatt, and Aaron Hill with assistance from Craig Orr. We wish to thank peer reviewers Dr. Jack Stanford (aquatic effects), Dr. Paul Paquet (terrestrial effects) and Dr. Viorel Popescu (cumulative effects). John Kelson provided expertise on eulachon and Dr. Alan Burger provided expertise on marbled murrelet. Dr. Jim Pojar and Patrick Williston provided expertise on rare plants in spray zones. cover photos: Homathko River Valley, Bute Inlet, Damien Gillis; Ashlu River diversion under construction, Damien Gillis; juvenile chinook salmon, Roger Tabor USFWS; inside the penstock tunnel for the Tyson Creek river diversion, Sunshine Coast Conservation Association. report design: Henrich Creative; diagrams on p. 3, and p. 9, Soren Henrich. The recommended citation for this document is as follows: Gower, T., A. Rosenberger, A. Peatt, and A. Hill. 2012. Tamed Rivers: A guide to river diversion hydropower in British Columbia. Prepared for Watershed Watch Salmon Society. 64 pages. Tamed Rivers | A Guide to River Diversion Hydropower in British Columbia Table of Contents Executive Summary . i The Taming of BC’s Rivers . 1 What is river diversion hydropower? . 3 Hydroelectricity in BC . 4 Aquatic impacts of river diversion . .5 Reduced instream flows . 6 Less habitat, and changes to the remaining habitat .