Fernie & Elk Valley
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Highway 3: Transportation Mitigation for Wildlife and Connectivity in the Crown of the Continent Ecosystem
Highway 3: Transportation Mitigation for Wildlife and Connectivity May 2010 Prepared with the: support of: Galvin Family Fund Kayak Foundation HIGHWAY 3: TRANSPORTATION MITIGATION FOR WILDLIFE AND CONNECTIVITY IN THE CROWN OF THE CONTINENT ECOSYSTEM Final Report May 2010 Prepared by: Anthony Clevenger, PhD Western Transportation Institute, Montana State University Clayton Apps, PhD, Aspen Wildlife Research Tracy Lee, MSc, Miistakis Institute, University of Calgary Mike Quinn, PhD, Miistakis Institute, University of Calgary Dale Paton, Graduate Student, University of Calgary Dave Poulton, LLB, LLM, Yellowstone to Yukon Conservation Initiative Robert Ament, M Sc, Western Transportation Institute, Montana State University TABLE OF CONTENTS List of Tables .....................................................................................................................................................iv List of Figures.....................................................................................................................................................v Executive Summary .........................................................................................................................................vi Introduction........................................................................................................................................................1 Background........................................................................................................................................................3 -
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air Canada (Alberta – VE6/VA6) Association Reference Manual (ARM) Document Reference S87.1 Issue number 2.2 Date of issue 1st August 2016 Participation start date 1st October 2012 Authorised Association Manager Walker McBryde VA6MCB Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged Page 1 of 63 Document S87.1 v2.2 Summits on the Air – ARM for Canada (Alberta – VE6) 1 Change Control ............................................................................................................................. 4 2 Association Reference Data ..................................................................................................... 7 2.1 Programme derivation ..................................................................................................................... 8 2.2 General information .......................................................................................................................... 8 2.3 Rights of way and access issues ..................................................................................................... 9 2.4 Maps and navigation .......................................................................................................................... 9 2.5 Safety considerations .................................................................................................................. -
Intoduction to SNOW PASS - GMC 2003
Intoduction to SNOW PASS - GMC 2003 Welcome to Snow Pass. This is the first GMC to be held at this location, and as far as we can ascertain, you are only the second group to have ever camped amongst this group of lakes. Many GMC’s are situated in valleys; however, this site is unusual as you are on the Continental Divide at an E-W “pass” between the Sullivan and Athabasca rivers, this is the arbitrary division between the Columbia Icefield to the south and the Chaba/Clemenceau Icefields to the north. But, you are also at a N-S pass between the Wales and “Watershed” glaciers, so you are at a “four way intersection” and from Base Camp you can access seven (7) different glacier systems. An intriguing local feature is the snout of the “Watershed” glacier, which actually divides so that it flows both west to join the Wales Glacier and thus drains to the Pacific and also turns east and feeds to the Arctic, which is why it is called the “Watershed” Glacier. In 2003, it may not be too obvious why in 1919 the Alberta/British Columbia Interprovincial Survey called this location “Snow Pass” but in the 1930’s (and even ? the early 1950’s) your Base Camp was still completely ice covered! There was permanent ice/snow from the “Aqueduct” to the “Watershed” to the “Toronto” Glaciers, an area of snow 5 km E-W and 10km N-S. Thus, in 1919, it really was a “snow pass”. See the appended “deglaciation” map. There is a wonderful photograph taken from the summit of Sundial peak in 1919 in the A/BC Volume, p. -
The Leaders, Volume 11 Construction and Engineering Items Appearing in This Magazine Is Reserved
SHARING YOUR VISION. BUILDING SUCCESS. Humber River Hospital, Toronto ON 2015 Dan Schwalm/HDR Architecture, Inc. We are Canada’s construction leaders. We look beyond your immediate needs to see the bigger picture, provide solutions, and ensure that we exceed your expectations. PCL is the proud builder of Canada’s landmark projects. Watch us build at PCL.com Message from Vince Versace, National Managing Editor, ConstructConnect 4 East and West connected by rail 6 On the road: the Trans-Canada Highway – Canada’s main street 21 Chinese workers integral in building Canada’s first megaproject 24 Canada’s most transformational project, the building The CN Tower: Canada’s iconic tower 53 of the Canadian Pacific Railway. From the ground up: building Canada’s parliamentary precinct 56 CanaData Canada’s Economy on Mend, but Don’t Uncork the Champagne Just Yet 14 Fighting the Fiction that Prospects are Nothing but Rosy in Western Canada 26 In Eastern Canada, Quebec is Winning the Accolades 60 Canada’s Top 50 Leaders in Construction 5 Leaders in Construction – Western Canada 28 Leaders in Construction – Eastern Canada 62 Advertisers’ Index 90 www.constructconnect.com Publishers of Daily Commercial News and Journal of Commerce Construction Record 101-4299 Canada Way 3760 14th Avenue, 6th Floor Burnaby, British Columbia Markham, Ontario L3R 3T7 V5G 1H3 Phone: (905) 752-5408 Phone: (604) 433-8164 Fax: (905) 752-5450 Fax: (604) 433-9549 www.dailycommercialnews.com www.journalofcommerce.com CanaData www.canadata.com Mark Casaletto, President John Richardson, Vice President of Customer Relations Peter Rigakos, Vice President of Sales Marg Edwards, Vice President of Content Alex Carrick, Chief Economist, CanaData Vince Versace, National Managing Editor Mary Kikic, Lead Designer Erich Falkenberg, National Production Manager Kristin Cooper, Manager, Data Operations Copyright © 2017 ConstructConnect™. -
Small Town Charm. Big Mountain Adventure
P.O. Box 1928 542B 2nd Avenue Fernie, BC V0B 1M0 www.tourismfernie.com [email protected] Small Town Charm. Big Mountain Adventure. Fernie offers a real, small-town experience with big Canadian Rocky Mountain adventures, while never losing sight of its enduring history. About Fernie, Facts & Story Ideas Some details to help start a great story about Fernie. Visit tourismfernie.com for details or contact us directly! Fernie Blog – click here What’s New – click here About Fernie From the jagged peaks of the Lizard Range to the unique caricature of Mount Hosmer, the mountains surrounding Fernie offer a sharp contrast to the quaint coal mining and ski town that sits at the base of the Canadian Rocky Mountains. Located in south-eastern British Columbia, Canada. It is the only city in BC completely encircled by the Canadian Rockies. Fernie’s year-round population is approximately 4,300 but sees a surge in population in both the winter and summer months of tourists, seasonal staff and long-term visitors due to the multitude of activities available. Visitors to the area are pleasantly surprised at the many experiences, great restaurants, unique stores and things to do in Fernie given its size. Founded in 1898, Fernie was officially incorporated as a municipality in 1904. The economy was built on extraction of the Elk Valley’s plentiful natural resources - coal and forestry. The Coal Creek mine was officially opened late in 1897, the railway followed in 1898, and Fernie came to life. In 1963, the original ski hill, called Fernie Snow Valley, opened. -
The Mountain Life of Glen Boles Alpine Artistry the Mountain Life of Glen Boles
Alpine Artistry The Mountain Life of Glen Boles Alpine Artistry The Mountain Life of Glen Boles From anApisi test ratur aut quia que veriaectam volupta eperrum doluptat rem etur, sitatus enimi, el id quos imolor sit omnihiciae velliquas erovitius nossi rehendi cuptates niant lab intias moluptatessi ut est quunt, simi, conemoluptae voluptatiis dem dicietur? Nis sunt modit, occae sunt aliciis itatemperia quatiam facea consequid quam repudam ut lat. On pe volupta sanducid expe nesti blaborpore et, aute perovid ullaborit, quis eatibus tinctur? Tem quo omnim quo maion conesci atureriaeria nes es a susande pliquodipsum simporpora as et plabo. Namet reprendit eius evellat iasperr oriatur alignient.Ectaspis esercimus perum quod que cus autatusantur si dolupide il eosam, solupti dolorehende essi di repe conet aut anda int fugia voluptatium cullamus. Ut fuga. Nem nonsed ut odit dento etur, te omnihicae. Evenis estibus ducideris resto voluptatem cusae labores For further information regarding the Summit Series of mountaineering biographies, please contact the National Office of the Alpine Club of Canada. www.alpineclubofcanada.ca Nineteenth in the SUMMIT SERIES Biographies of people who have made a difference in Canadian mountaineering by Lynn Martel Alpine Artistry The Mountain Life of Glen Boles by Lynn Martel CANADIAN CATALOGUING IN PUBLICATIONS DATA Martel, Lynn. Alpine Artistry: The Mountain Life of Glen Boles Design by Suzan Chamney, Glacier Lily Productions. ISBN: 978-0-920330-53-1 © 2014, The Alpine Club of Canada All rights reserved. No portion of this book may be copied or reproduced without the permission of the author or the subject. The Alpine Club of Canada P.O. -
R O C K Y M O U N T a I
KOOTENAY 115° 114°W Map Key What Is Geotourism All About? NATIONAL According to National Geographic, geotourism “sustains or enhances Community PARK the geographical character of a place—its environment, culture, Museum aesthetics, heritage, and the well-being of its residents.” Geotravelers, To Natural or scenic area then, are people who like that idea, who enjoy authentic sense of Calgary place and care about maintaining it. They find that relaxing and Other point of interest E having fun gets better—provides a richer experience—when they get E Black Diamond Outdoor experience involved in the place and learn about what goes on there. BOB CREEK WILDLAND, AB ALBERTA PARKS Turner Geotravelers soak up local culture, hire local guides, buy local Valley World Heritage site C Radium l foods, protect the environment, and take pride in discovering and EHot Springs os Scenic route ed observing local customs. Travel-spending choices can help or hurt, so i n 22 National Wild and Scenic River geotravelers patronize establishments that care about conservation, BARING CREEK IN GLACIER NATIONAL PARK, MT CHUCKHANEY.COM wi nt er Urban area preservation, beautification, and benefits to local people. 543 Learn more at crownofthecontinent.natgeotourism.com. Columbia High River E 23 Protected Areas Wetlands Indian or First Nation reserve Geotraveler Tips: Buy Local 93 541 National forest or reserve High C w Patronize businesses that support the community and its conservation O Frank 40 oo KMt. Joffre N d Longview Lake National park and preservation efforts. Seek out local products, foods, services, and T E 11250 ft I E ELK N 3429 m E Longview Jerky Shop shops. -
Conodont Biofacies in a Ramp to Basin Setting (Latest Devonian and Earliest Carboniferous) in the Rocky Mountains of Southernmost Canada and Northern Montana
U. S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY Conodont biofacies in a ramp to basin setting (latest Devonian and earliest Carboniferous) in the Rocky Mountains of southernmost Canada and northern Montana by Lauret E. Savoy1 and Anita G. Harris 2 Open-File Report 93-184 This report is preliminary and has not been reviewed for conformity with Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. \ Department of Geology and Geography, Mount Holyoke College, South Hadley, MA 01075 2 U.S. Geological Survey, Reston, VA 22092 1993 TABLE OF CONTENTS ABSTRACT 1 INTRODUCTION 2 LITHOSTRATIGRAPHY AND DEPOSITIONAL SETTING 2 CONODONT BIOSTRATIGRAPHY AND BIOFACIES 8 Palliser Formation 8 Exshaw Formation 13 Banff Formation 13 Correlative units in the Lussier syncline 15 PALEOGEOGRAPfflC SETTING 17 CONCLUSION 23 ACKNOWLEDGMENTS 23 REFERENCES CITED 24 APPENDIX 1 38 FIGURES 1. Index map of sections examined and major structural features of the thrust and fold belt 3 2. Correlation chart of Upper Devonian and Lower Mississippian stratigraphic units. 4 3. Selected microfacies of the Palliser Formation. 5 4. Type section of Exshaw Formation, Jura Creek. 6 5. Lower part of Banff Formation, North Lost Creek. 7 6. Conodont distribution in Palliser and Exshaw formations, Inverted Ridge. 9 7. Conodont distribution in upper Palliser and lower Banff formations, Crowsnest Pass. 11 8. Conodont distribution in upper Palliser, Exshaw, and lower Banff formations, composite Jura Creek - Mount Buller section. 12 9. -
Glaciers of the Canadian Rockies
Glaciers of North America— GLACIERS OF CANADA GLACIERS OF THE CANADIAN ROCKIES 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 Rocky Mountains of Canada include four distinct ranges from the U.S. border to northern British Columbia: Border, Continental, Hart, and Muskwa Ranges. They cover about 170,000 km2, are about 150 km wide, and have an estimated glacierized area of 38,613 km2. Mount Robson, at 3,954 m, is the highest peak. Glaciers range in size from ice fields, with major outlet glaciers, to glacierets. Small mountain-type glaciers in cirques, niches, and ice aprons are scattered throughout the ranges. Ice-cored moraines and rock glaciers are also common CONTENTS Page Abstract ---------------------------------------------------------------------------- J199 Introduction----------------------------------------------------------------------- 199 FIGURE 1. Mountain ranges of the southern Rocky Mountains------------ 201 2. Mountain ranges of the northern Rocky Mountains ------------ 202 3. Oblique aerial photograph of Mount Assiniboine, Banff National Park, Rocky Mountains----------------------------- 203 4. Sketch map showing glaciers of the Canadian Rocky Mountains -------------------------------------------- 204 5. Photograph of the Victoria Glacier, Rocky Mountains, Alberta, in August 1973 -------------------------------------- 209 TABLE 1. Named glaciers of the Rocky Mountains cited in the chapter -
The Letters F and T Refer to Figures Or Tables Respectively
INDEX The letters f and t refer to figures or tables respectively "A" Marker, 312f, 313f Amherstberg Formation, 664f, 728f, 733,736f, Ashville Formation, 368f, 397, 400f, 412, 416, Abitibi River, 680,683, 706 741f, 765, 796 685 Acadian Orogeny, 686, 725, 727, 727f, 728, Amica-Bear Rock Formation, 544 Asiak Thrust Belt, 60, 82f 767, 771, 807 Amisk lowlands, 604 Askin Group, 259f Active Formation, 128f, 132f, 133, 139, 140f, ammolite see aragonite Assiniboia valley system, 393 145 Amsden Group, 244 Assiniboine Member, 412, 418 Adam Creek, Ont., 693,705f Amundsen Basin, 60, 69, 70f Assiniboine River, 44, 609, 637 Adam Till, 690f, 691, 6911,693 Amundsen Gulf, 476, 477, 478 Athabasca, Alta., 17,18,20f, 387,442,551,552 Adanac Mines, 339 ancestral North America miogeocline, 259f Athabasca Basin, 70f, 494 Adel Mountains, 415 Ancient Innuitian Margin, 51 Athabasca mobile zone see Athabasca Adel Mountains Volcanics, 455 Ancient Wall Complex, 184 polymetamorphic terrane Adirondack Dome, 714, 765 Anderdon Formation, 736f Athabasca oil sands see also oil and gas fields, Adirondack Inlier, 711 Anderdon Member, 664f 19, 21, 22, 386, 392, 507, 553, 606, 607 Adirondack Mountains, 719, 729,743 Anderson Basin, 50f, 52f, 359f, 360, 374, 381, Athabasca Plain, 617f Aftonian Interglacial, 773 382, 398, 399, 400, 401, 417, 477f, 478 Athabasca polymetamorphic terrane, 70f, Aguathuna Formation, 735f, 738f, 743 Anderson Member, 765 71-72,73 Aida Formation, 84,104, 614 Anderson Plain, 38, 106, 116, 122, 146, 325, Athabasca River, 15, 20f, 35, 43, 273f, 287f, Aklak -
Fernie & Elk Valley
Fernie & Elk Valley Cultural Guide SPRING 2017 Photo: Raven Eye Photography Eye Raven Photo: TOURISMFERNIE.COM SPRING 2017 The Communities of the Elk Valley In the heart of the majestic Canadian SPARWOOD lies in the middle of Rocky Mountains, the Elk Valley is a the valley and is the first community hidden oasis of verdant landscapes, reached on entering from Alberta. The charming towns and abundant town’s name is derived from the local recreation. For over 100 years, trees that were used for manufacturing pioneers have travelled to the region, spars for ocean vessels. The town was first in search of valuable minerals, and founded as a new home for the residents now seeking a sanctuary focused on of the temporary communities of A CULTURAL GUIDE TO FERNIE AND THE ELK VALLEY family, community and the beautiful Michel and Natal. Several art murals ARTS, CULTURE & HERITAGE outdoors. Mining still forms the base can be seen here, depicting the strong of a thriving economy that has now connection to coal mining, with some by Canada 150 in Fernie 4 diversified and welcomes a variety of Michelle Loughery who was born in the The Fernie Museum and Downtown Visitor Centre 6 artisans, small businesses, and an active area and went on to become a world- Cultural Attractions in the Elk Valley 8 year-round recreational and cultural renowned muralist. Heritage Walking Tour of Fernie 10 tourism industry. Patio Season 15 Pop: 3,784 | Founded 1966 The Balmer North Mine Disaster 16 FERNIE is the largest and oldest of the 3 main communities in the Elk Valley. -
Fernie Sections 3-2-1-1A
CROSS SECTION 1 WEST STRUCTURAL CROSS SECTION ACROSS EAST WESTERN FRONT RANGES, NORTH PART OF ELK RIVER VALLEY, AND HIGHROCK RANGE based on geological mapping by Douglas (1958), Leach LEGEND WEST EAST CROSS SECTION 1a (1979), Mott (1989), and Grieve (1993) CROSS SECTIONS 1, 1a and 3 NORCEN ELK STRUCTURAL 0123 a - 64 - E / 82 - J - 7 kilometre Ku Upper Cretaceous, Blackstone, Cardium, Wapiabi and Belly CROSS SECTION SHELL FORSYTH River (br) Formations 0123 ALEXANDER THROUGH d - 25 - A / 82 - J - 6 B.C. ALBERTA WESTERN FRONT RANGES ELK B.C. ALBERTA kilometre CREEK OVERTURNED (no vertical exaggeration) SYNCLINE OF ROCKY MOUNTAINS RIVER Kl Lower Cretaceous, Blairmore Group SYNCLINE IN VALLEY Jurassic-Lower Cretaceous Morrissey, Mist Mountain, and HIGHROCK RANGE JK Kl NORTHERN PART ALEXANDER 2 PP 2 Elk Formations sea level CREEK M OF ELK RIVER PP SYNCLINE M 1 1 kilometre kilometre JK JT Triassic Spray River Group and Jurassic Fernie Formation VALLEY 2 KL 2 0 Bourgeau Thrust 0 sea level M based on JT Ku (br) JT JK JT PP Pennsylvanian - Permian, Rocky Mountain Supergroup geological mapping 1 1 PP D 1 1 M PP Ku by Grieve (1993) Thrust JK JK M 0 JT 0 JT JT Mississippian Banff, Livingstone, Mount Head and 2 2 JT JT M Bourgeau Kl JT Etherington Formations kilometre kilometre 1 PP PP JT 1 PP JK M M D M JT 2 M PP 2 Devonian Yahatinda Formation, Fairholme Group, Alexo, M D C S Sassenach and Palliser Formations 3 JT D M 3 D PP Cambrian and PP C CD 4 4 CS Cambrian to Silurian Devonian only M C Cambrian undivided Lewis Thrust CROSS SECTION 2 STRUCTURAL CROSS SECTION ACROSS CENTRAL PART OF ELK RIVER VALLEY AND HIGH ROCK RANGE SHOWING SUB-LEWIS DUPLEXES EAST OF FORDING MTN.