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Early Vancouver Volume Four
Early Vancouver Volume Four By: Major J.S. Matthews, V.D. 2011 Edition (Originally Published 1944) Narrative of Pioneers of Vancouver, BC Collected During 1935-1939. Supplemental to Volumes One, Two and Three collected in 1931-1934. About the 2011 Edition The 2011 edition is a transcription of the original work collected and published by Major Matthews. Handwritten marginalia and corrections Matthews made to his text over the years have been incorporated and some typographical errors have been corrected, but no other editorial work has been undertaken. The edition and its online presentation was produced by the City of Vancouver Archives to celebrate the 125th anniversary of the City's founding. The project was made possible by funding from the Vancouver Historical Society. Copyright Statement © 2011 City of Vancouver. Any or all of Early Vancouver may be used without restriction as to the nature or purpose of the use, even if that use is for commercial purposes. You may copy, distribute, adapt and transmit the work. It is required that a link or attribution be made to the City of Vancouver. Reproductions High resolution versions of any graphic items in Early Vancouver are available. A fee may apply. Citing Information When referencing the 2011 edition of Early Vancouver, please cite the page number that appears at the bottom of the page in the PDF version only, not the page number indicated by your PDF reader. Here are samples of how to cite this source: Footnote or Endnote Reference: Major James Skitt Matthews, Early Vancouver, Vol. 4 (Vancouver: City of Vancouver, 2011), 33. -
CANADA's MOUNTAIN Rocky Mountain Goats
CANADA'S MOUNTAIN Rocky Mountain Goats CANADA'S MOUNTAIN PLAYGROUNDS BANFF • JASPER • WATERTON LAKES • YOHO KOOTENAY ° GLACIER • MOUNT REVELSTOKE The National Parks of Canada ANADA'S NATIONAL PARKS are areas The National Parks of Canada may, for C of outstanding beauty and interest that purposes of description, be grouped in three have been set apart by the Federal Govern main divisions—the scenic and recreational ment for public use. They were established parks in the mountains of Western Canada; the to maintain the primitive beauty of the land scenic, recreational, wild animals, and historic scape, to conserve the native wildlife of the parks of the Prairie Provinces; and the scenic, country, and to preserve sites of national his recreational, and historic parks of Eastern Can toric interest. As recreational areas they pro ada. In these pages will be found descriptions vide ideal surroundings for the enjoyment of of the national parks in the first group—areas outdoor life, and now rank among Canada's which lie within the great mountain regions outstanding tourist attractions. of Alberta and British Columbia. Canada's National Park system teas estab * * * lished in 1SS5, when a small area surrounding mineral hot springs at Banff in the Rocky This publication is compiled in co-operation Mountains was reserved as a public posses with the National Parks Branch, Department sion. From this beginning has been developed of Northern Affairs and National Resources. the great chain of national playgrounds note Additional information concerning these parks stretching across Canada from the Selkirk may be obtained from the Park Superintend Mountains in British Columbia to the Atlantic ents, or from the Canadian Government Travel Coast of Nova Scotia. -
Modelling the Transfer of Supraglacial Meltwater to the Bed of Leverett Glacier, Southwest Greenland
The Cryosphere, 9, 123–138, 2015 www.the-cryosphere.net/9/123/2015/ doi:10.5194/tc-9-123-2015 © Author(s) 2015. CC Attribution 3.0 License. Modelling the transfer of supraglacial meltwater to the bed of Leverett Glacier, Southwest Greenland C. C. Clason1, D. W. F. Mair2, P. W. Nienow3, I. D. Bartholomew3, A. Sole4, S. Palmer5, and W. Schwanghart6 1Department of Physical Geography and Quaternary Geology, Stockholm University, 106 91 Stockholm, Sweden 2Geography and Environment, University of Aberdeen, Aberdeen, AB24 3UF, UK 3School of Geosciences, University of Edinburgh, Edinburgh, EH8 9XP, UK 4Department of Geography, University of Sheffield, Sheffield, S10 2TN, UK 5Geography, College of Life and Environmental Sciences, University of Exeter, Exeter, EX4 4RJ, UK 6Institute of Earth and Environmental Science, University of Potsdam, 14476 Potsdam-Golm, Germany Correspondence to: C. C. Clason ([email protected]) Received: 23 June 2014 – Published in The Cryosphere Discuss.: 29 July 2014 Revised: 12 December 2014 – Accepted: 24 December 2014 – Published: 22 January 2015 Abstract. Meltwater delivered to the bed of the Greenland melt to the bed matches the observed delay between the peak Ice Sheet is a driver of variable ice-motion through changes air temperatures and subsequent velocity speed-ups, while in effective pressure and enhanced basal lubrication. Ice sur- the instantaneous transfer of melt to the bed in a control sim- face velocities have been shown to respond rapidly both ulation does not. Although both moulins and lake drainages to meltwater production at the surface and to drainage of are predicted to increase in number for future warmer climate supraglacial lakes, suggesting efficient transfer of meltwa- scenarios, the lake drainages play an increasingly important ter from the supraglacial to subglacial hydrological systems. -
3,549 Mw Yt 0.810 Mw
Canada Wind Farms As of October 2010 Current Installed Capacity: 3,549 MW YT 0.810 MW NL 54.7 MW BC 656 MW 103.5 MW AB 104 MW SK MB 171.2 MW ON 663 MW 1,298 MW QC PE 164 MW NB 195 MW NS Courtesy of 138 MW Alberta COMPLETED WIND FARMS Installed Capacity Project Project Power Turbine # Project Name (in MW) Developer Owner Purchaser Manufacturer Year Online 1 Cardston Municipal District Magrath 30 Suncor, Enbridge, EHN Suncor, Enbridge, EHN Suncor, Enbridge, EHN GE Wind 2004 McBride Lake 75.24 Enmax, TransAlta Wind Enmax, TransAlta Wind Enmax, TransAlta Wind Vestas 2007 McBride Lake East 0.6 TransAlta Wind TransAlta Wind TransAlta Wind Vestas 2001 Soderglen Wind Farm 70.5 Nexen/Canadian Hydro Nexen/Canadian Hydro Nexen/Canadian Hydro GE 2006 Developers, Inc. Developers, Inc. Developers, Inc. Waterton Wind Turbines 3.78 TransAlta Wind TransAlta Wind TransAlta Wind Vestas 1998 2 Pincher Municipal District Castle River Wind Farm 0.6 TransAlta Wind TransAlta Wind TransAlta Wind Vestas 1997 Castle River Wind Farm 9.9 TransAlta Wind TransAlta Wind TransAlta Wind Vestas 2000 Castle River Wind Farm 29.04 TransAlta Wind TransAlta Wind TransAlta Wind Vestas 2001 Cowley Ridge 21.4 Canadian Hydro Canadian Hydro Canadian Hydro Kenetech 1993/1994 Developers, Inc. Developers, Inc. Developers, Inc. Cowley Ridge North Wind Farm 19.5 Canadian Hydro Canadian Hydro Canadian Hydro Nordex 2001 Developers, Inc. Developers, Inc. Developers, Inc. Lundbreck 0.6 Lundbreck Developments Lundbreck Developments Lundbreck Developments Enercon 2001 Joint Venture A Joint Venture A Joint Venture A Kettles Hill Phase I 9 Enmax Enmax Enmax Vestas 2006 Kettles Hill Phase II 54 Enmax Enmax Enmax Vestas 2007 Old Man River Project 3.6 Alberta Wind Energy Corp. -
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The Glaciers of the Torngat Mountains of Northern Labrador By © Robert Way A Thesis submitted to the School of Graduate Studies in partial fulfillment of the requirements for the degree of Master of Science Department of Geography Memorial University of Newfoundland September 2013 St. John 's Newfoundland and Labrador Abstract The glaciers of the Tomgat Mountains of northem Labrador are the southemmost m the eastern Canadian Arctic and the most eastem glaciers in continental North America. This thesis presents the first complete inventory of the glaciers of the Tomgat Mountains and also the first comprehensive change assessment for Tomgat glaciers over any time period. In total, 195 ice masses are mapped with 105 of these showing clear signs of active glacier flow. Analysis of glaciers and ice masses reveal strong influences of local topographic setting on their preservation at low elevations; often well below the regional glaciation level. Coastal proximity and latitude are found to exert the strongest control on the distribution of glaciers in the Tomgat Mountains. Historical glacier changes are investigated using paleomargins demarking fanner ice positions during the Little Ice Age. Glacier area for 165 Torngat glaciers at the Little Ice Age is mapped using prominent moraines identified in the forelands of most glaciers. Overall glacier change of 53% since the Little Ice Age is dete1mined by comparing fanner ice margins to 2005 ice margins across the entire Torngat Mountains. Field verification and dating of Little Ice Age ice positions uses lichenometry with Rhizocarpon section lichens as the target subgenus. The relative timing of Little Ice Age maximum extent is calculated using lichens measured on moraine surfaces in combination with a locally established lichen growth curve from direct measurements of lichen growth over a - 30 year period. -
North Thompson Official Community Plan
Schedule “A” to Bylaw 2700 North Thompson Official Community Plan Foreword and Acknowledgements The North Thompson Official Community Plan is the outcome of over two years of research, public participation and planning. The Regional District is grateful to all those residents and groups who provided interest, passion, and support from all corners of the Plan area culminating in the Plan development. In particular, we wish to recognize the following people for the exceptional amount of time and energy they dedicated to the planning process. OCP Advisory Committee Director Carol Schaffer, Electoral Area “A” Director Stephen Quinn, Electoral Area “B” Director Bill Kershaw, Electoral Area “O” Tom Eustache – Simpcw First Nation Rick Dee Harley Wright Willow Macdonald (past member) Meetings, Conversations and Information Providers Anna Kay Eldridge – Simpcw First Nation Ashley Dyck – Planning Services Celia Nord – Little Shuswap Indian Band Chris Ortner Dan Winiski Doris Laner – North Thompson Arts Council James Demens and Brandon Gustafsen – Ministry of Transportation and Infrastructure Jenny Green and Clare Audet – Interior Health Authority Kelly Funk – Kelly Funk Photography Laura Ryser – Research Manager, Rural and Small Town Studies Program, UNBC Leanne Nystoruk Mike Scarff, TNRD GIS Services PIBC and the Planners from the local Interior Chapter Sarah Cooke and Mike Cloet – Ministry of Mines, Energy and Petroleum Resources Staff and students at Clearwater and Barriere Secondary Schools Staff from the Agricultural Land Commission Staff -
Kootenay National Park Visitor Guide
Visitor Guide 2021 – 2022 Paint Pots Trail Également offert en français Z. Lynch / Parks Canada 1 Welcome Welcome 2 Plan your adventure 3 Be a responsible visitor 4 Radium Hot Springs area Kootenay 6 Kootenay National Park map National Park 8 Make the most of your visit 10 Camping On April 21, 1920, the Government of Canada agreed to build a road connecting the Bow and Columbia 10 Interpretive programs and activities valleys. As part of the agreement, eight kilometres of land on either side of the road was set aside for a 11 Stay safe national park. 12 Conservation stories The first cars to travel along the new highway bounced over bumps and chugged up steep hills, 13 National park regulations but according to a 1924 guidebook, “every mile is a surprise and an enchantment.” A century later, Kootenay National Park continues to surprise and enchant. Visitors can relax in the soothing mineral pools at Radium Hot Springs, stroll through canyons, picnic beside glacial-blue rivers or backpack along one of the Rockies’ most scenic hiking trails. The park’s diverse ecosystems support a variety of wildlife, and newly unearthed Burgess Shale fossils reveal exquisite details about life half a Did you know? billion years ago. Kootenay National Park lies within the traditional lands of the Ktunaxa and Shuswap. Vermilion Crossing Z. LynchIconic / Parks 55 Canada km backcountry route: Z. Lynch / Parks Canada Rockwall Trail Z. Lynch / Parks Canada Ktunaxa Nation Shuswap Indian Band Columbia Valley Métis Association A place of global importance The Ktunaxa (k-too-nah-ha), also known as The Kenpesq’t (ken-pesk-t) community, currently Kootenay National Park is an important place for The United Nations Educational, Scientific, and Kootenay, have occupied the lands adjacent to the known as the Shuswap Indian Band, is part of the British Columbia Métis based on a history of trade Cultural Organization (UNESCO) recognizes four Kootenay and Columbia Rivers and the Arrow Lakes Secwépemc (seck-wep-em) Nation occupying relationships and expeditions. -
Recent Changes in Area and Thickness of Torngat Mountain Glaciers (Northern Labrador, Canada)
The Cryosphere, 11, 157–168, 2017 www.the-cryosphere.net/11/157/2017/ doi:10.5194/tc-11-157-2017 © Author(s) 2017. CC Attribution 3.0 License. Recent changes in area and thickness of Torngat Mountain glaciers (northern Labrador, Canada) Nicholas E. Barrand1, Robert G. Way2, Trevor Bell3, and Martin J. Sharp4 1School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham, UK 2Department of Geography, University of Ottawa, Ottawa, Canada 3Department of Geography, Memorial University of Newfoundland, St. John’s, Canada 4Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Canada Correspondence to: Nicholas E. Barrand ([email protected]) Received: 6 July 2016 – Published in The Cryosphere Discuss.: 5 September 2016 Revised: 22 December 2016 – Accepted: 22 December 2016 – Published: 24 January 2017 Abstract. The Torngat Mountains National Park, northern 1 Introduction Labrador, Canada, contains more than 120 small glaciers: the only remaining glaciers in continental northeast North The glaciers of the Torngat Mountains, northern Labrador, America. These small cirque glaciers exist in a unique topo- Canada, occupy a unique physiographic and climatic setting climatic setting, experiencing temperate maritime summer at the southern limit of the eastern Canadian Arctic. Their conditions yet very cold and dry winters, and may pro- proximity to the Labrador Current provides temperate, mar- vide insights into the deglaciation dynamics of similar small itime summer conditions yet very cold and dry winters. Ex- glaciers in temperate mountain settings. Due to their size and amination of Torngat glacier change may provide insights remote location, very little information exists regarding the into the deglaciation dynamics of other similarly situated health of these glaciers. -
Supraglacial Rivers on the Northwest Greenland Ice Sheet, Devon Ice Cap, and Barnes Ice Cap Mapped Using Sentinel-2 Imagery
This is a repository copy of Supraglacial rivers on the northwest Greenland Ice Sheet, Devon Ice Cap, and Barnes Ice Cap mapped using Sentinel-2 imagery. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/141238/ Version: Accepted Version Article: Yang, K., Smith, L., Sole, A. et al. (4 more authors) (2019) Supraglacial rivers on the northwest Greenland Ice Sheet, Devon Ice Cap, and Barnes Ice Cap mapped using Sentinel-2 imagery. International Journal of Applied Earth Observation and Geoinformation, 78. pp. 1-13. ISSN 0303-2434 https://doi.org/10.1016/j.jag.2019.01.008 Article available under the terms of the CC-BY-NC-ND licence (https://creativecommons.org/licenses/by-nc-nd/4.0/). Reuse This article is distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs (CC BY-NC-ND) licence. This licence only allows you to download this work and share it with others as long as you credit the authors, but you can’t change the article in any way or use it commercially. More information and the full terms of the licence here: https://creativecommons.org/licenses/ Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ 1 Supraglacial rivers on the northwest Greenland Ice Sheet, Devon Ice Cap, and 2 Barnes Ice Cap mapped using Sentinel-2 imagery 3 Kang Yang1,2,3, Laurence C. -
Bow & Kananaskis Valleys Trail
Old Fort Creek 1300 Stone Creek To Cochrane 1650 To Calgary BOW CORRIDOR & To Banff Bow Valley 0 40 20 3 Yamnuska 0 4 2 0 Tibits 3 N Ridge 6 Quarry 0 KANANASKIS VALLEY 0 0 3 NW NE Montane 1 Wildland 8 0 0 8 1A 2 Traverse 2000 W E Bow 1 0 Ridge 0 6 0 2 Yamnuska River Mount Traverse SW SE Harvie 1 Mount John Laurie 2 0 0 4 Stoneworks 2 Lady MacDonald Provincial 1 (aka Yamnuska) 4 Mount Heights Creek 0 2 0 2 S 1 6 0 0 2,606 m 0 2 1 8 0 Rundle 1 2,240 m Meander ROAD CLOSURES: 2,949 m ParkEExxplpl rree Montane HIGHWAY #40: Traverse Mount Lady Cougar Bow Valley st Bow Valley 1 MacDonald Creek Closed December 1 to Wildland th Wildlife Corridor Wildland June 14 inclusive from Johnny’s Management Area Stoney Provincial 1500 Nakoda Kananaskis Lakes Trail to 1X Resort & Chiniki Canmore Lake Park Cougar Provincial Brewster’s Casino the Highwood House Junction. Goat Kananaskis Nordic Creek Jura Slabs Guest Douglas Montane Creek Ranch 40 Centre Policeman’s Fir Traverse Loder Park 1A 1 Creek Bench Door Jamb Peak P POWDERFACE TRAIL/ROAD: Banff Provincial Mountain 2,088 m Flowing 1,996m Open May 1- Water Closed December 1st to May 14th, P Bow October Long Park Nanny Goat Weekend National Butress Valley Canmore Bow River Montane inclusive south of Dawson. Kananaskis Nordic Centre Grotto Exshaw Mountain Grotto Creek Park Day Lodge Horseshoe 2500 Mountain Willow Stoney Nation Canmore Loop 2,706 m Kid Goat Bow Rock No 142, 143, 144 Butress WhiteshMoraine Valley Reclaimer 1500 Bike ALBERTA East End Grassi Middle Path 2000 Lake Grassi Lakes 2200 Middle (Paved) -
Dinosaur Provincial Park and Area Tourism Development Plan Study
Final Report Dinosaur Provincial Park and Area Tourism Development Plan Study Submitted to: Canadian Badlands Ltd. Alberta Tourism, Parks and Recreation by IBI Group July 2010 Government of Alberta and Canadian Badlands Ltd. DINOSAUR PROVINCIAL PARK AND AREA TOURISM DEVELOPMENT PLAN STUDY REPORT FINAL REPORT JULY 2010 IBI GROUP FINAL REPORT TABLE OF CONTENTS EXECUTIVE SUMMARY .................................................................................................................... 1 1. INTRODUCTION ...................................................................................................................... 7 1.1 Purpose and Scope of the Study ......................................................................................................... 8 1.2 Study Limitations .................................................................................................................................. 9 1.3 Outline of Report ................................................................................................................................... 9 2. CHARACTERIZATION OF THE STUDY AREA .................................................................... 10 2.1 County of Newell ................................................................................................................................. 13 2.2 City of Brooks ...................................................................................................................................... 16 2.3 Special Area No. 2 .............................................................................................................................. -
First Assessment of Mountains on Northwestern Ellesmere Island, Nunavut, As Potential Astronomical Observing Sites
Preprint, November 8, 2018 First Assessment of Mountains on Northwestern Ellesmere Island, Nunavut, as Potential Astronomical Observing Sites Eric Steinbring1, Ray Carlberg2, Bryce Croll2 Greg Fahlman1, Paul Hickson3, Liviu Ivanescu4, Brian Leckie1, Thomas Pfrommer3 & Matthias Schoeck1 ABSTRACT Ellesmere Island, at the most northerly tip of Canada, possesses the highest mountain peaks within 10 degrees of the pole. The highest is 2616 m, with many summits over 1000 m, high enough to place them above a stable low-elevation thermal inversion that persists through winter darkness. Our group has studied four mountains along the northwestern coast which have the additional benefit of smooth onshore airflow from the ice-locked Arctic Ocean. We deployed small robotic site testing stations at three sites, the highest of which is over 1600 m and within 8 degrees of the pole. Basic weather and sky clarity data for over three years beginning in 2006 are presented here, and compared with available nearby sea-level data and one manned mid-elevation site. Our results point to coastal mountain sites experiencing good weather: low median wind speed, high clear-sky fraction and the expectation of excellent seeing. Some practical aspects of access to these remote locations and operation and maintenance of equipment there are also discussed. Subject headings: site testing arXiv:1007.1680v1 [astro-ph.IM] 9 Jul 2010 1. Introduction The cold, dry, dark winter skies of the earth’s polar regions are well suited for astronomy. Smooth airflow is aided by a highly stratified atmosphere with strong, stable low-elevation 1Herzberg Institute of Astrophysics, National Research Council Canada, Victoria, BC V9E 2E7, Canada 2University of Toronto, Dept.