Mountaineering Guidebook Author David P
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Daily Routine Tributes
December 12, 2012 HANSARD 1981 Yukon Legislative Assembly The Old Fire Hall became a satellite venue in 2007 and is Whitehorse, Yukon now a very popular downtown space for a wide range of activi- Wednesday, December 12, 2012 — 1:00 p.m. ties. The Arts Centre has spearheaded some of Yukon’s biggest, Speaker: I will now call the House to order. We will most successful cultural initiatives, including Yukon’s cultural proceed at this time with prayers. component at the 2010 Olympic Winter Games in Vancouver. The Sewing Our Traditions: Dolls of Canada’s North exhibi- Prayers tion, curated by Yukon Arts Centre public gallery staff, is just one example of the exceptional programming that was pro- Withdrawal of motions duced for the Olympics. Speaker: The Chair wishes to inform the House of Sewing Our Traditions is also an example of Yukon Arts some changes that have been made to the Order Paper. Motion Centre’s collaborative spirit and the commitment of its staff to No. 346 and Motion No. 347, standing in the name of the work with local and national partners. Such partnerships and Member for Klondike, have been removed from the Order Pa- activities stem from the determination of the Arts Centre’s per as the actions requested in the motions have been taken. boards, staff and volunteers to develop and foster a creative DAILY ROUTINE economy and to be a cultural, social and economic force in the north. Speaker: We will proceed at this time with the Order 2011-12 attendance figures show that almost 64,000 peo- Paper. -
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. -
Glacier Change in the Cariboo Mountains, British Columbia, Canada (1952–2005)
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | The Cryosphere Discuss., 8, 3367–3411, 2014 www.the-cryosphere-discuss.net/8/3367/2014/ doi:10.5194/tcd-8-3367-2014 TCD © Author(s) 2014. CC Attribution 3.0 License. 8, 3367–3411, 2014 This discussion paper is/has been under review for the journal The Cryosphere (TC). Glacier change in the Please refer to the corresponding final paper in TC if available. Cariboo Mountains, British Columbia, Glacier change in the Cariboo Mountains, Canada (1952–2005) British Columbia, Canada (1952–2005) M. J. Beedle et al. M. J. Beedle, B. Menounos, and R. Wheate Title Page Geography Program, University of Northern British Columbia, Prince George, BC, Canada Abstract Introduction Received: 20 May 2014 – Accepted: 2 June 2014 – Published: 25 June 2014 Conclusions References Correspondence to: M. J. Beedle ([email protected]) Tables Figures Published by Copernicus Publications on behalf of the European Geosciences Union. J I J I Back Close Full Screen / Esc Printer-friendly Version Interactive Discussion 3367 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract TCD We calculated dimensional change for 33 glaciers in the Cariboo Mountains of British Columbia for the latter half of the twentieth century. All glaciers receded during the pe- 8, 3367–3411, 2014 riod 1952–2005; area retreat averaged −0.19 ± 0.05 % a−1. From 1952 to 1985, nine −1 5 glaciers advanced. Following 1985, retreat rates accelerated to −0.41 ± 0.12 % a . Glacier change in the −1 Thinning rates likewise accelerated, from −0.14 ± 0.04 m w.e. a (1952–1985) to Cariboo Mountains, −1 −0.50 ± 0.07 m w.e. -
Tk< Varsity Outdoor Club Journal
Tk< Varsity Outdoor Club Journal VULUMC AAV lyOil ISSN 0524-5613 Tfo Umveuihj of fy&Uk Columbia Vancouver, Canada PRESIDENT STUDLY'S MESSAGE This year I've come across many names of old members of the past sixty years whose exploits in the mountains and elsewhere are well known. This is indicative of the vast history of the club, a history reflected in all aspects of club life, from the traditional trips to the Salty Dog Rag. This is the twenty-fifth year that the club has chosen to put down a part of that history in print and this issue should serve as a reminder to all members of the wealth of experiences inherent in the club. The journal however, as a permanent record of the club, is worthy of far more attention than it receives. This may be due partly to the character istic low profile that it has had with respect to both design and circulation. I hope therefore that the efforts and results of this year's journal committee set a standard to be repeated every year and not just every twenty- f i ve. This year, with almost three hundred members in the club, there has been a growth in popularity in the regular events as well as several exciting new projects. The rock school was a great success, with just under a hundred participants and much snow and ice expertise was passed on in three glacier schools. The highlights of the year though, were two slightly more tangible out lets of expertise and enthusiasm. -
Valemount Visitor's Guide
Valemount Visitor’s Guide Summer 2020 Winter 2020/21 ACTIVITIES • ACCOMMODATIONS • DINING 60 North Highway 5, Valemount, BC | www.swiftcreekresort.com River front camping with glacier view www.bbcanada.com/summitriver FREE FREE Valemount’s Best Kept Secret Located 20 kms south of town Contact Us at: 250-566-9933 email: summitriverlodge@ hotmail.com Valemount Summer 2020 Valemount Summer 2020 Yearly Events Mount Robson Marathon JUNE Valemountain Days Table of Contents June 12–14, 2020 Yearly Events 4 Valemount Farmer’s Market Welcome to Valemount, B C 5 Welcome to Valemount, B.C. June 18–September 24, 2020 Exciting Adventures 7 every Thursday Kinbasket Lake 8 Valemount—a friendly stop on Yellowhead Highway 5—offers a surprising variety Valemount Visitor Information of hotels and restaurants in a typical rural mountain community setting. Valemount Centre Dunster Ice Cream Social Hiking Trails 10 is surrounded by the Rocky, the Cariboo and Monashee Mountains. July 4, 2020 Cranberry Marsh 12 Make the Valemount Visitor Information Centre Valemount is your gateway to many natural wonders. Mount Robson Provincial your first stop for great local and provincial in- JULY Salmon Viewing–George Hicks Park 13 Park, a 20-minute drive from the Village, is home to black bears, grizzlies, moose formation. Our friendly staff will provide you with Canada Day Celebrations Mount Robson Provincial Park 15 and elk. In August, you can experience the phenomenal Chinook salmon spawning great local and provincial information. We offer July 1, 2020 in Swift Creek at George Hicks Regional Park. Enjoy the wide-open mountain views a range of services including local adventure Backcountry Cabins 16 along the dikes or boardwalk section of the Cranberry Marsh—1.9 km south from activity bookings and accommodation bookings Canoe Mountain Rodeo Museum 18 the Visitor Centre—observe the local and migratory wildlife. -
Glaciers of North America— GLACIERS of CANADA
Glaciers of North America— GLACIERS OF CANADA HISTORY OF GLACIER INVESTIGATIONS IN CANADA By C. SIMON L. OMMANNEY SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–1 The earliest recorded description of a Canadian glacier was in 1861. Since that time, various glaciological investigations have been conducted in the several glacierized regions of Canada (for example, Coast Mountains, Interior Ranges, Rocky Mountains, and Arctic Islands), including mass balance, modeling, dendrochronology, climatology, ice chemistry and physics, ice-core analyses, glacier-surge mechanics, and airborne and satellite remote sensing CONTENTS Page Abstract ------------------------------------------------------------------------------ J27 Occurrence of Glaciers----------------------------------------------------------- 27 FIGURE 1. Index map of the glaciers of western Canada -------------------- 29 2. Index map of the glaciers of arctic and eastern Canada---------- 34 TABLE 1. Summary of historical information on glaciers of western Canada --------------------------------------------------------- 30 2. Summary of historical information on glaciers of arctic and eastern Canada ------------------------------------------------- 32 3. The glacierized areas of Canada --------------------------------- 35 Observation of Glaciers ---------------------------------------------------------- 35 Historic (Prior to World War II) ------------------------------------------ -
Location Mappremier Rangecariboo Mountains, British Columbia
British Alberta Columbia 50 kilometres to to Prince Prince George George 16 McBride to Edmonton 16 16 Jasper Valemount Fraser River 98 16 Premier Range 5 N to Banff to Kamloops 16 93 H 83 E 53°N 93 A 83 D k to Jasper e e r C R a k w e a i re u K C s te h e T Premier R i Range Valemount v e r Canoe Kinbasket River Lake N N o 5 rt h T ho m p so n R 120°W iver to Kamloops 10 kilometres Glaciated Area Location Map 16 Highway River/Creek Premier Range Lake Cariboo Mountains, British Columbia RHW, September 2004 120°W British Alberta to Columbia 50 kilometres to Location Map Prince Prince Mts. Quanstrom George George 16 McBride McBride to and Pierrway Edmonton Mts. Quanstrom Wells Gray Group and Pierrway 16 Cariboo Mountains 16 British Columbia Jasper Valemount 98 Premier Range 5 N to Banff to ek Fraser River Kamloops 10 kilometres e Cr 16 le st a C to Jasper 16 93 H 83 E 53°N Mt. Quanstrom 93 A 83 D N R a ek u re s C h a r R a i Valemount g v a e i Mt. Pierrway r N e i v R r e t a Premier 5 w r Range a e l C to Kamloops RHW, September 2004 to Prince George to Jasper r 16 16 Fraser Rive 100 km k e e Tete Jaune r 10 kilometres C Cache a iw K k e e N r C e 5 et Raush River T “Northwest” “Northeast” Valemount (helicopter base) 7 3 2 5 1 Glacier “Central” 4 6 Kinbasket r Canoe Rive Lake “South Central” Previous base camps CMH’s 5 “Popular” bivouac sites Cariboo Lodge Major peaks “South” to Kamloops 1 Mt. -
Glaciers of North America— GLACIERS of CANADA
Glaciers of North America— GLACIERS OF CANADA MAPPING CANADA’S GLACIERS By C. SIMON L. OMMANNEY With a section on MAPPING GLACIERS IN THE INTERIOR RANGES AND ROCKY MOUNTAINS WITH LANDSAT DATA By ROGER D. WHEATE, ROBERT W. SIDJAK, and GARNET T. WHYTE SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–1 Between the mid-1940’s and the mid-1990’s, seven 1:1,000,000-scale, forty-eight 1:500,000-scale (Glacier Atlas of Canada), and more than 110 miscellaneous scale (1:2,500- to 1:125,000-scale) maps of selected glaciers of Canada were completed by governmental and academic institutions; the types of maps include sketch, topographic, and stereo-orthophoto maps. Satellite images of glaciers and digital elevation models can be combined to produce maps (planimetric and topographic) and three-dimensional perspectives CONTENTS Page Abstract ------------------------------------------------------------------------------ J83 Introduction------------------------------------------------------------------------- 83 Glacier Maps of Canada (1:1,000,000 Scale)--------------------------------- 83 TABLE 1. Glacier maps of Canada (1:1,000,000 scale) ---------------------- 84 Glacier Atlas of Canada (1:500,000 Scale) ----------------------------------- 84 FIGURE 1. Part of Glacier Atlas of Canada map of the White and Thompson Glaciers, Axel Heiberg Island, Nunavut ------------ 87 TABLE 2. Glacier Atlas of Canada (1:500,000-scale Glacier Inventory maps)----------------------------------------------------------- 85 Water Survey of Canada---------------------------------------------------------- 88 TABLE 3. Water Survey of Canada Glacier Map Series --------------------- 88 Salmon Glacier --------------------------------------------------------------------- 90 TABLE 4. Miscellaneous glacier maps of Canada--------------------------- 90 Glacier Maps of the High Arctic ------------------------------------------------ 93 FIGURE 2. -
Remote Sensing of Glaciers in the Canadian Cordillera, Western Canada
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2014 Remote sensing of glaciers in the Canadian Cordillera, western Canada Wheate, Roger D ; Berthier, Etienne ; Bolch, Tobias ; Menounos, Brian P ; Shea, Joseph M ; Clague, John J ; Schiefer, Erik DOI: https://doi.org/10.1007/978-3-540-79818-7_14 Posted at the Zurich Open Repository and Archive, University of Zurich ZORA URL: https://doi.org/10.5167/uzh-102086 Book Section Published Version Originally published at: Wheate, Roger D; Berthier, Etienne; Bolch, Tobias; Menounos, Brian P; Shea, Joseph M; Clague, John J; Schiefer, Erik (2014). Remote sensing of glaciers in the Canadian Cordillera, western Canada. In: Kargel, Jeffrey S; Leonard, Gregory J; Bishop, Michael P; Kääb, Andreas; Raup, Bruce H. GlobalLand Ice Measurements from Space. Berlin: Springer, 333-352. DOI: https://doi.org/10.1007/978-3-540-79818-7_14 CHAPTER 14 Remote sensing of glaciers in the Canadian Cordillera, western Canada Roger D. Wheate, Etienne Berthier, Tobias Bolch, Brian P. Menounos, Joseph M. Shea, John J. Clague, and Erik Schiefer ABSTRACT of 1:20,000 in the 1980s. In both cases, technicians employed photogrammetric methods to extract We review the use of spaceborne imagery and glacier outlines from black-and-white aerial photos. digital elevation models (DEMs) to evaluate glacier Canada’s contribution to the International Hydro- thinning and retreat in the Canadian Cordillera, an logical Decade (1965–1974) included repeat map- area that includes the provinces of British Columbia ping of selected glaciers along an east–west (BC), Alberta, and Yukon Territory. -
Master Plan for a Glacier Tourism Destination Centred on Mt
Master Plan for a Glacier Tourism Destination centred on Mt. Arthur Meighen near Valemount, British Columbia Year-Round Skiing and Sightseeing for an International Clientele near Jasper and Banff National Parks © Copyright All Rights Reserved Valemount Glacier Destinations Ltd. and Pheidias Project Management Corporation Valemount Glacier Destination Master Plan Prepared for: Valemount Glacier Destinations Ltd. 1435-1188 West Georgia Street Vancouver, BC V6E 4A2 www.valemountglaciers.com Prepared by: 660-1188 West Georgia Street, Vancouver, BC V6G 2T3 (604) 662-8833 www.obertiresorts.com | www.pheidias.ca August 2, 2016 Valemount Glacier Destination: Master Plan FOREWORD It has been our pleasure to work together with the people of Valemount and the Simpcw First Nation to prepare this Master Plan for what will be an iconic project for the Robson Valley and tourism in British Columbia. The public support for this project has been overwhelming and we are privileged to work on a project of this nature. We have been studying the Premier Range since the 1990s and due to climate, elevations, glaciers, snowfall and snow quality we believe it is one of the most suitable locations for a sightseeing and ski resort in North America. Our experience in ski area planning and master planning dates back to the 1970s, when our company group was founded. Our approach and design philosophy is simple: always seek a better idea and a better solution for each unique project. We allow the natural environment to shape our decisions, rather than shaping the environment to fit. For projects to be truly successful, they must offer a lasting vision that stands the test of time – even when faced with changing markets, trends, technology, and demographics. -
Glacier Change in the Cariboo Mountains, British Columbia, Canada (1952–2005)
The Cryosphere, 9, 65–80, 2015 www.the-cryosphere.net/9/65/2015/ doi:10.5194/tc-9-65-2015 © Author(s) 2015. CC Attribution 3.0 License. Glacier change in the Cariboo Mountains, British Columbia, Canada (1952–2005) M. J. Beedle, B. Menounos, and R. Wheate Geography Program, University of Northern British Columbia, Prince George, BC, Canada Correspondence to: M. J. Beedle ([email protected]) Received: 20 May 2014 – Published in The Cryosphere Discuss.: 25 June 2014 Revised: 3 November 2014 – Accepted: 10 November 2014 – Published: 7 January 2015 Abstract. We applied photogrammetric methods with aerial when glaciers undergo changes in extent and volume. As photography from 11 different years between 1946 and 2005 glaciers and ice caps (GIC; all glaciers outside of the Antarc- to assess changes in area and volume of 33 glaciers in the tic and Greenland ice sheets) lose volume, sea level rises Cariboo Mountains of British Columbia for the latter half of (Radic´ and Hock, 2011). The largest GIC contributions to the 20th century. These are used to identify changes in extent sea level rise include the Canadian Arctic Archipelago and and elevation primarily for the periods 1952–1985, 1985– Gulf of Alaska regions (Gardner et al., 2011; Berthier et al., 2005, and 1952–2005. All glaciers receded during the pe- 2010), but recent work demonstrates that, collectively, small riod 1952–2005; area retreat averaged −0.19 ± 0.05 % a−1. glaciers (< 1 km2/ contribute a significant amount to total From 1952 to 1985, nine glaciers advanced; following GIC volume (Bahr and Radic,´ 2012). -
World Best Landscapes Report
WORLD’S BEST LANDSCAPES PROJECT Dr Andrew Lothian Scenic Solutions 2016 Cover: Top – Grand Canyon, United States Bottom – Torres del Paine, Chile © 2016 Dr Andrew Lothian, Scenic Solutions ABN: 55 275 407 146 [email protected] www.scenicsolutions.com.au World’s Best Landscapes WORLD’S BEST LANDSCAPES ASSESSMENT PROJECT EXECUTIVE SUMMARY Introduction preferences. Strict criteria apply to the photography of the landscape so that the The World’s Best Landscapes rating is of the quality of the scene, not the Assessment project was carried out during quality of the photograph. early 2016. Having measured and mapped landscapes in South Australia and the Photo selection Lake District in the UK, all of which averaged in the range 5 to 7, the question The project commenced in early February arose, what rating does the World’s best and was completed by the end of March, it landscapes achieve? What are the being much quicker than my other projects characteristics of such landscapes? as it did not involve taking original Where are such landscapes located? photography but rather relied on existing photographs from the Internet. The list of Concept of World class landscapes what may be the World’s best landscapes was prepared based on previous work on In examining the concept of World class the World Heritage list which includes landscapes, the scale and definition of landscapes that meet Criterion 7 of landscapes at varying scales, from landscape aesthetics. In addition, two immediate to continental in scale is dozen lists of the World’ Wonders had reviewed. It then examines landscape been previously reviewed and from these quality profiles, i.e.