The Big Melt British Columbia’S Glaciers Are Receding— There Is No Doubt —But What Does This Mean for the Future of the Province and Its Inhabitants?
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British Columbia Regional Guide Cat
National Marine Weather Guide British Columbia Regional Guide Cat. No. En56-240/3-2015E-PDF 978-1-100-25953-6 Terms of Usage Information contained in this publication or product may be reproduced, in part or in whole, and by any means, for personal or public non-commercial purposes, without charge or further permission, unless otherwise specified. You are asked to: • Exercise due diligence in ensuring the accuracy of the materials reproduced; • Indicate both the complete title of the materials reproduced, as well as the author organization; and • Indicate that the reproduction is a copy of an official work that is published by the Government of Canada and that the reproduction has not been produced in affiliation with or with the endorsement of the Government of Canada. Commercial reproduction and distribution is prohibited except with written permission from the author. For more information, please contact Environment Canada’s Inquiry Centre at 1-800-668-6767 (in Canada only) or 819-997-2800 or email to [email protected]. Disclaimer: Her Majesty is not responsible for the accuracy or completeness of the information contained in the reproduced material. Her Majesty shall at all times be indemnified and held harmless against any and all claims whatsoever arising out of negligence or other fault in the use of the information contained in this publication or product. Photo credits Cover Left: Chris Gibbons Cover Center: Chris Gibbons Cover Right: Ed Goski Page I: Ed Goski Page II: top left - Chris Gibbons, top right - Matt MacDonald, bottom - André Besson Page VI: Chris Gibbons Page 1: Chris Gibbons Page 5: Lisa West Page 8: Matt MacDonald Page 13: André Besson Page 15: Chris Gibbons Page 42: Lisa West Page 49: Chris Gibbons Page 119: Lisa West Page 138: Matt MacDonald Page 142: Matt MacDonald Acknowledgments Without the works of Owen Lange, this chapter would not have been possible. -
The Selkirk Mountains : a Guide for Mountain Climbers and Pilgrims
J Presentee) to ^be Xibrar^ of tbe xaniversit^ of Toronto bs Her"bert B. Sampson, K,C, Digitized by the Internet Archive in 2011 with funding from University of Toronto http://www.archive.org/details/selkirkmountainsOOwhee THE Selkirk Mountains A Guide for Mountain Climbers and Pilgrims Information by A. O. WHEELER, F.R.G.S., A.C.C., A.C., A.A.C. vo A- Stovel Company, Engravers, Lithographers and Printers, Winnipeg, Man. Arthur O. Wheeler, First President of Alpine Club — CONTENTS Foreword—A. 0. Wlieeler Page 1 One Word More—Elizabeth Parker 2 The Snowy Selkirks—Elizabeth Parker 3-5 CHAPTER I. The Rocky Mountain System—The Selkirks—Early Explorers Later Histor}'—The Railway—Discovery of Rogers Pass—An Alpine Club—Members of British Association Visit the Selkirks, (1884) —Result of Completion of Railway—Government Surveys (1886) —First Scientific Observations of Illecillewaet Glacier Topographical Survey by William Spotswood Green—The Alpine Club, England, and the Swiss Alpine Club—The Appalachian Mountain Club—Triangulation of Railway Belt—Subsequent Mountaineering Pages 6-32 CHAPTER n. Peaks, Passes and Valleys Reached from Glacier—Glacier Park Swiss Guides—Glacier House—Outfits and Ponies—Places and Peaks of Interest Alphabetically Arranged 33-104 CHAPTER m. The Caves of Cheops (Xakimu Caves) —the Valley of the Caves The Approach to the Caves—Formation and Structure—Descrip- tion of Caves—The Mill Bridge Series—The Gorge Series—The Judgment Hall 106-117 CHAPTER IV. •Golden and the Country of the Upper Columbia—Along the Columbia River between Golden and Beavermouth are Several Points of Interest—the Upper Columbia—Travel by Waterway on the Upper Columbia 119-135 CHAPTER V. -
Glacier and Mount Revelstoke National Parks Souvenir Guidebook
ZUZANA DRIEDIGER Contributors Designer – Kathryn Whiteside Print and Interactive Design Parks Canada Design Team – Vérèna Blasy, Rob Buchanan, Heather Caverhill, Zuzana Driediger, Megan Long, Rick Reynolds parkscanada.gc.ca Cover Art and Glacier 125 Commemorative Posters – Rob Buchanan – Parks Canada Call our toll-free Contributing Artists – Vérèna Blasy, Rob Buchanan, Zuzana information line Driediger, Friends of Mount Revelstoke and Glacier, Ryan Gill, Diny Harrison, Greg Hill, Jason Keerak, Mas Matsushita, Dan McCarthy, 1-888-773-8888 Jackie Pendergast, Rick Reynolds, Shelley L. Ross, Chili Thom, Alice Mount Revelstoke Weber, Kathryn Whiteside, Kip Wiley, John Woods and Glacier National Parks reception Many thanks to the following institutions for permission to reproduce historic images: Canada Post Corporation, Canada 250-837-7500 Science and Technology Museum, Canadian Pacific Archives, Library www.pc.gc.ca/glacier and Archives Canada, National Herbarium of Canada, Revelstoke Museum and Archives, Smithsonian Institution Archives, Whyte www.pc.gc.ca/revelstoke Museum of the Canadian Rockies Printed by: Hemlock Printers $2.00 Souvenir Guide Book 2 Welcome to Glacier and Mount Revelstoke National Parks and Rogers Pass National Historic Site We hope that you enjoy your visit to these very special Canadian places. Glacier, Mount Revelstoke and Rogers Pass are part of an exciting and historic cultural landscape that stretches from Kicking Horse Pass on the British Columbia/Alberta boundary to the site of the Canadian Pacific Railway’s Last Spike at Craigellachie. Close connection with nature has always been a hallmark of the human experience here in the Columbia Mountains. First Nations people have lived and travelled along the mighty Columbia River for millennia. -
Community Wildfire Protection Plan
Coombs-Hilliers COMMUNITY WILDFIRE PROTECTION PLAN SFC Prepared by: Strathcona Forestry Consulting GIS mapping: Madrone Environmental Services Ltd. August 2011 Community Wildfire Protection Plan: Coombs Hilliers Coombs Hilliers Community Wildfire Protection Plan Prepared for: Coombs-Hilliers Fire Protection Area Submitted by: Strathcona Forestry Consulting GIS Mapping by: Madrone Environmental Consulting Ltd. August 2011 This Community Wildfire Protection Plan was developed in association with: BC Ministry of Forests and Range Union of British Columbia and Municipalities Wildfire Management Branch Regional District of Nanaimo Coombs-Hilliers Volunteer Fire Department Administration Preparation: RPF Name (Printed) RPF Signature Date: ___________________ RPF No: _________ 2011 Page 2 Community Wildfire Protection Plan: Coombs Hilliers TABLE OF CONTENTS 1.0 INTRODUCTION 1.1 COOMBS-HILLIERS 3 1.2 COMMUNITY WILDFIRE PROTECTION PLAN PROGRAM 9 1.3 COOMBS-HILLIERS CWPP 11 2.0 THE SETTING 2.1 COMMUNITY PROFILES 12 2.2 TRANSPORTATION, COMMUNITY INFRASTRUCTURE 26 3.0 GOVERNMENT INFRASTRUCTURE 3.1 COMMUNITY VALUES 31 3.2 TOOLS AVAILABLE TO LOCAL GOVERNMENT 31 3.3 PUBLIC EDUCATION AND COMMUNICATION 32 3.4 PREVENTATIVE MEASURES 32 3.5 POLICE PROTECTION 35 3.6 FIRE PROTECTION 35 4.0 BIOGEOCLIMATIC 4.1 CLIMATE 40 4.2 PHYSIOGRAPHIC FEATURES 41 4.3 VEGETATION 42 4.4 NATURAL DISTURBANCE HISTORY 44 4.5 RECENT FIRE HISTORY 45 5.0 PREPARATION OF THE COMMUNITY WILDFIRE PROTECTION PLAN 47 6.0 ASSESSMENT 6.1 CANADIAN FOREST FIRE DANGER RATING SYSTEM 49 6.2 INTERFACE COMMUNITY FIRE HAZARD ASSESSMENT 61 6.3 HIRV MODELING 62 6.4 INTERFACE WILDFIRE THREAT RATING 62 7.0 ASSESSMENT RESULTS 66 8.0 INTERFACE WILDFIRE THREAT RATING INTERFACE FIRE HAZARD MAP 71 9.0 DISCUSSION 72 10.0 COMMUNITY ACTION PLAN 74 79 11.0 IMPLEMENTATION 12.0 REFERENCES 80 APPENDIX 1. -
Glacier and Mx Revelstoke
MOUNT REVELSTOKE NATIONAL PARK HOW TO REACH THE PARK TRAILS GENERAL INFORMATION There are more than 40 miles of improved trails in the 3 British Columbia Mount Revelstoke National Park is accessible by both railway and motor road. A scenic highway has been built park. Perhaps the most popular of these is the trail leading PARKS ADMINISTRATION < GLACIER AND from the main through highway near the town of Revelstoke from the Lookout at the Summit to Millar and Eva Lakes, and Location and Description to the summit of Mount Revelstoke on which the park is Lake of Jade. This trail crosses alpine meadows, popularly The administration of Glacier and Mount Revelstoke situated. In a distance of 18 miles this road rises 4,850 feet known as the "wild flower garden", and skirting the Columbia National Parks is carried out by a superintendent whose office Valley winds through rocky hollows to crystal pools of pale is located at Field in Yoho National Park, British Columbia. to an altitude of 6,350 feet above sea-level, yet it has no The superintendent is assisted by wardens stationed in the 1 Mount Revelstoke National Park is situated on the summit MX REVELSTOKE mental hazards for the average driver. The ascent is gradual green water that reflects the surrounding trees, rocks and parks. Information, maps, and literature concerning the parks of Mount Revelstoke. It has an area of 100 square miles and and is made by a number of switchbacks with sweeping mountains. Millar Lake is 4 miles from the Lookout, and Eva may be obtained from the Superintendent's office and from NATIONAL PARKS occupies a broad undulating plateau at a general elevation curves, with plenty of room for cars to pass. -
The Cariboo and Monashee Ranges of British Columbia: an Alpinist’S Guide
1 THE CARIBOO AND MONASHEE RANGES OF BRITISH COLUMBIA: AN ALPINIST’S GUIDE by EARLE R. WHIPPLE Even today, British Columbia is still a wilderness of mountains, valleys, glaciers, forest and plateau. The Columbia Mountains (Interior Ranges; which include the Cariboo and Monashee Ranges) lie within British Columbia, west of the Canadian Rockies and the southern Alberta-British Columbia border. This guide describes the access and mountaineering in these two ranges. Aside from parts of the Coast Range and the northern Rockies, the Cariboo and Monashee Ranges are the most isolated in B.C. However, if one listens to the helicopters from the lodges in these ranges, when camped there, one may question this. Large, active glaciers (now in retreat) with spectacular icefalls exist in the mountains of the western part of the Halvorson Group, the northern Wells Gray Group, the Premier Ranges, the Dominion Group and northern Scrip Range; there is climbing on rock, snow and ice, and routes for those climbers wishing easy, relaxing climbing in beautiful scenery. Good rock climbing on gneiss is in the southern Gold Range and Mt. Begbie in the north. There are also locales offering fine hiking on trails or alpine meadows (Halvorson Group, southern Wells Gray Group, southern Scrip Range, and the Shuswap Group), and backpacking traverses have been worked out through the Halvorson and Dominion Groups, the Scrip Range and the Gold Range. Beautiful lake districts exist in the northern Cariboos, and the Monashees. The area covered by this book starts northwest of the town of McBride, on Highway 16, southeast of Prince George, and extends south to near the border with the U.S.A., staying within the great bend of the Fraser River, and then west of Canoe Reach (lake; formerly Canoe River) and just west of the lower Columbia River south of its great bend. -
Natural History Feeding
BRITISH COLUMBIA VANCOUVER ISLAND GEOLOGY The Creation of the Johnstone Strait Over a span of thousands of years and a combination of processes such as tectonics, volcanism, erosion and glaciation the 110km Johnstone Strait off of Vancouver Island was formed. Formally known as Wrangellia, a land mass that collided with North America causing it to fold and buckle forming the many of the mountains and ranges we associate with British Columbia today. The formation of the narrow channels that make up Northeastern Vancouver Island dates back to the ice ages when glacial ice sheets settled in the area. During the Pleistocene Epoch Ice Age ice sheets carved their way through the igneous rock or the channel creating what is now known as Johnstone Strait, Queen Charlotte strait, and the Discovery Passage. Glacial carving transpires through the slow movement of the ice sheet. Due to their sheer size and weight combined with gravity ice sheets move slowly down mountain valleys, and across plains. As glaciers move they sculpt the land via erosion and deposition. While they gradually move across the landscape the ice erodes the surface beneath it, creating fjords, glacial valleys, and horns. During this erosion the ice actually picks up and retains sediment and particles depositing them along the way. This process of deposition, depositing of material as the glacier retreats and melts away, forms moraines which are narrow ridges that show where the ice used to be. Robson Bight Ecological Reserve ceremonial purposes. Ubiquitous to the area are manmade geological features known as clam beds. For the First Nations’ people clams were a staple not only for their food source but for their economy as Ecological Reserves were formed in Canada in 1971 as a way to encourage the preservation of natural well for they used them in trade with other tribes. -
Determining Annual Cryosphere Storage Contributions to Streamflow Using Historical Hydrometric Records
Determining annual cryosphere storage contributions to streamflow using historical hydrometric records Brahney, Janicea*, Menounos, Brianb, Wei, Adama, Curtis, Paul Jeffersona a Department of Earth and Environmental Sciences, University of British Columbia, Okanagan. Kelowna, BC V1V 1V7, Canada, [email protected], [email protected], [email protected] b Geography Program and Natural Resources and Environmental Studies Institute, University of Northern British Columbia, Prince George, BC V6T 1Z9, Canada. [email protected] *Corresponding Author, [email protected], 435-797-4479 Current Address: Department of Watershed Sciences, Utah State University, Logan UT, 84322, USA 1 Abstract Alpine glaciers and perennial snow fields are important hydrologic elements in many mountain environments providing runoff during the late summer and during periods of drought. Because relatively long records of glacier mass-balance data are absent from many glacierized catchments, it remains unclear to what extent shrinking perennial snow and glaciers have affected runoff trends from these watersheds. Here we employ a hydrograph separation technique that uses a double mass curve in an attempt to isolate changes in runoff due to glacier retreat and disappearance of perennial snow. The method is tested using hydrometric data from 20 glacierized and 16 non-glacierized catchments in the Columbia Basin of Canada. The resulting estimates on cryosphere storage contribution to streamflow were well correlated to other regional estimates based on measurements as well as empirical and mechanistic models. Annual cryosphere runoff changed from +19 to -55% during the period 1975-2012, with an average decline of 26%. For August runoff, these changes ranged from +17 to -66%, with an average decrease of 24%. -
Late Pleistocene Palaeoenvironments, Archaeology, and Indicators of a Glacial Refugium on Northern Vancouver Island, Canada
Late Pleistocene palaeoenvironments, archaeology, and indicators of a glacial refugium on northern Vancouver Island, Canada by Christopher Franklin George Hebda B.A., University of Victoria, 2014 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF ARTS in the Department of Anthropology © Christopher Franklin George Hebda, 2019 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. We acknowledge with respect the Lekwungen peoples on whose territory the university stands and the Songhees, Esquimalt and W̱ SÁNEĆ peoples whose historical relationships with the land continue to this day. ii Supervisory Committee Late Pleistocene palaeoenvironments, archaeology, and indicators of a glacial refugium on northern Vancouver Island, Canada by Christopher Franklin George Hebda B.A., University of Victoria, 2014 Supervisory Committee Dr. Quentin Mackie, Department of Anthropology Co-Supervisor Dr. Duncan McLaren, Department of Anthropology Co-Supervisor iii Abstract Recent research has revealed human settlement on the Pacific coast of Canada extending back nearly 14,000 years, but much of the late Pleistocene record is unknown due to shifting sea levels, poor understanding of Cordilleran ice extent, and limited research on the biota of the coast during this time. This study, undertaken in Quatsino First Nation and ‘Namgis First Nation territories as part of the Northern Vancouver Island Archaeology and Palaeoecology Project, employs modern multi-proxy analysis of lake sediment cores from two sites on northern Vancouver Island to reconstruct palaeoenvironments during and immediately following the Fraser Glaciation in coastal British Columbia. -
Hiking in Glacier National Park
HIKING IN GLACIER NATIONAL PARK Photo: Danyelle Magnan Photo: Danyelle Magnan Photo: Joey Vosburgh Glacier National Park has a rich natural and cultural of national significance, both historical and natural. history. The park protects unique stands of old-growth The abandoned rail-grade, stone bridges and trestle cedar and hemlock, and a great diversity of wildlife. supports, snow sheds and other structures associated The hiking trails in Glacier National Park will lead you to stunning ridges Created in 1886 following the completion of the with the railway may all be visited on self-guiding trails. and viewpoints that will make the climbs worthwhile. The Columbia Mountains Canadian Pacific Railway’s transcontinental line, the park Trails leading to spectacular glacier viewpoints were laid enticed travellers to its uncharted wilderness and the out by the Swiss guides for their clients a century ago – are steep and the valleys narrow, allowing for only a few easy hikes and a good area became the birthplace of mountaineering in North and are still waiting for you to discover the magic of the number of difficult ones.Use the trail chart below to choose a hike suitable America. Today’s explorers will find heritage resources Selkirks for yourself. for everyone in your party. Photos left to right: Hiking Balu Pass; dwarf dogwood and foam flower; mountain goats Our trails are managed to protect the safety of both bears and people. Plan Ahead and Prepare Safety Type Hiking Trail Estimated Time Distance Elevation Trail Description Remember, you are responsible for your own safety. Emergency (Return) (Return) Gain • Get advice from a Parks Canada Information Centre. -
Eastern Vancouver Island (#196)
EASTERN VANCOUVER ISLAND (#196) The Eastern Vancouver Island ecoregion stretches along the eastern slopes of the Vancouver Island Ranges to the Pacific Ocean. The forests are characterized by Douglas-fir, western hemlock and grand fir, with scattered examples of globally rare Garry oak ecosystem. It supports more biological diversity than anywhere else in the province and contains many of BC’s most ecologically significant estuaries. There are 59 species at risk that have been documented here, and 38 species that are of global conservation concern. Just over 93% of this ecoregion remains in natural cover and 13.8% is within conserved/protected areas. LOCATION The Eastern Vancouver Island ecoregion stretches along the eastern slopes of the Vancouver Island Ranges to the Strait of Georgia between Victoria and Nanaimo. This ecoregion is part of BC’s Coastal Douglas-Fir Biogeoclimatic Zone, and it is the northern extension of the Central Pacific Coastal Forests, a region of coastal temperate rainforests that extends through southern Oregon to the northern tip of Vancouver Island. CLIMATE/GEOLOGY The climate of the Eastern Vancouver Island ecoregion is charac- terized by warm, dry summers and wet, very mild winters. Frosts are common in winter, but snow cover at sea level is rare. The mean annual temperature is approximately 9⁰C, with a summer mean of 14⁰C and a winter mean of 3.5⁰C. Mean annual precip- itation ranges from 800 millimetres at lower elevations to 2,500 millimetres at higher elevations. The ecoregion contains low relief on the coast and in valleys, to high mountain peaks in the Vancouver Island ranges toward the central and northern end of the island. -
Landforms of British Columbia 1976
Landforms of British Columbia A Physiographic Outline bY Bulletin 48 Stuart S. Holland 1976 FOREWORD British Columbia has more variety in its climate and scenery than any other Province of Canada. The mildness and wetness of the southern coast is in sharp contrast with the extreme dryness of the desert areas in the interior and the harshness of subarctic conditions in the northernmost parts. Moreover, in every part, climate and vegetation vary with altitude and to a lesser extent with configuration of the land. Although the Province includes almost a thousand-mile length of one of the world’s greatest mountain chains, that which borders the north Pacitic Ocean, it is not all mountainous but contains a variety of lowlands and intermontane areas. Because of the abundance of mountains, and because of its short history of settlement, a good deal of British Columbia is almost uninhabited and almost unknown. However, the concept of accessibility has changed profoundly in the past 20 years, owing largely to the use of aircraft and particularly the helicopter. There is now complete coverage by air photography, and by far the largest part of the Province has been mapped topographically and geologically. In the same period of time the highways have been very greatly improved, and the secondary roads are much more numerous. The averagecitizen is much more aware of his Province, but, although knowledge has greatly improved with access,many misconceptions remain on the part of the general public as to the precise meaning even of such names as Cascade Mountains, Fraser Plateau, and many others.