Oberti Resort Design Case Study
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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 -
Municipal Development Plan
Municipality of Crowsnest Pass MUNICIPAL DEVELOPMENT PLAN BYLAW NO. 1059, 2020 © 2021 Oldman River Regional Services Commission Prepared for the Municipality of Crowsnest Pass This document is protected by Copyright and Trademark and may not be reproduced or modified in any manner, or for any purpose, except by written permission of the Oldman River Regional Services Commission. This document has been prepared for the sole use of the Municipality addressed and the Oldman River Regional Services Commission. This disclaimer is attached to and forms part of the document. ii MUNICIPALITY OF CROWSNEST PASS BYLAW NO. 1059, 2020 MUNICIPAL DEVELOPMENT PLAN BYLAW BEING a bylaw of the Municipality of Crowsnest Pass, in the Province of Alberta, to adopt a new Municipal Development Plan for the municipality. AND WHEREAS section 632 of the Municipal Government Act requires all municipalities in the provinceto adopt a municipaldevelopment plan by bylaw; AND WHEREAS the purpose of the proposed Bylaw No. 1059, 2020 is to provide a comprehensive, long-range land use plan and development framework pursuant to the provisions outlined in the Act; AND WHEREAS the municipal council has requested the preparation of a long-range plan to fulfill the requirementsof the Act and provide for its consideration at a public hearing; NOW THEREFORE, under the authority and subject to the provisions of the Municipal Government Act, Revised Statutes of Alberta 2000, Chapter M-26, as amended, the Council of the Municipality of Crowsnest Pass in the province of Alberta duly assembled does hereby enact the following: 1. Bylaw No. 1059, 2020, being the new Municipal Development Plan Bylaw is hereby adopted. -
AGENDA November 14, 2017 5:30 P.M
DISTRICT OF ELKFORD COMMITTEE OF THE WHOLE AGENDA November 14, 2017 5:30 P.M. Council Chambers Elkford's Mission - Through innovative leadership we provide opportunities for responsible growth, in harmony with industry and the environment. We take advantage of opportunities that enhance affordable community living and sustain the quality of life citizens, businesses and visitors expect. Page 1 APPROVAL OF AGENDA (a) Approval of November 14, 2017 Agenda 2 ADOPTION OF MINUTES 3 - 4 (a) Adoption of August 28, 2017 Minutes 3 DELEGATIONS 5 - 134 (a) Draft Community Wildfire Protection Plan • Presenter: Tove Pashkowski, B.A. Blackwell & Associates Ltd. 4 ADJOURNMENT (a) Move to Adjourn Page 1 of 134 Page 2 of 134 DISTRICT OF ELKFORD COMMITTEE OF THE WHOLE Minutes August 28, 2017 Present: Mayor McKerracher, Chair Councillor McGregor Councillor Fairbairn Councillor Wildeman Councillor Bertrand Councillor Zarowny Absent: Councillor Robinson Staff Present: Curtis Helgesen, Chief Administrative Officer Scott Beeching, Director, Planning and Development Services Garity Stanley, Director, Leisure Services Duane Allen, Superintendent, Public Works Marilyn Rookes, Director, Financial Services Corey Kortmeyer, Director, Fire Rescue and Emergency Services Curtis Nyuli, Deputy Director, Fire Rescue and Emergency Services Dorothy Szawlowski, Deputy Director, Corporate Services, Recorder There being a quorum of Council, Mayor McKerracher called the meeting to order at 5:37 pm. APPROVAL OF AGENDA (a) Approval of August 28, 2017 Agenda Moved, Seconded AND RESOLVED THAT the agenda for the August 28, 2017 Committee of the Whole Meeting be approved as circulated. CARRIED ADOPTION OF MINUTES (a) Adoption of August 14, 2017 Minutes Moved, Seconded AND RESOLVED THAT the minutes from the August 14, 2017 Committee of the Whole Meeting be adopted as circulated. -
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 .................................................................................................................. -
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 -
Carnivores and Corridors in the Crowsnest Pass
Carnivores and Corridors in the Crowsnest Pass Alberta Species at Risk Report No. 50 Carnivores and Corridors in the Crowsnest Pass Prepared by: Cheryl-Lesley Chetkiewicz and Mark S. Boyce, Principal Investigator Department of Biological Sciences University of Alberta Prepared for: Alberta Sustainable Resource Development Fish and Wildlife Division Alberta Species at Risk Report No. 50 December 2002 Publication No. I/071 ISBN: 0-7785-2182-6 (Printed Edition) ISBN: 0-7785-2183-4 (On-line Edition) ISSN: 1496-7219 (Printed Edition) ISSN: 1496-7146 (On-line Edition) Illustration by: Brian Huffman For copies of this report, contact: Information Centre- Publications Alberta Environment/ Alberta Sustainable Resource Development Main Floor, Great West Life Building 9920- 108 Street Edmonton, Alberta, Canada T5K 2M4 Telephone: (780) 422-2079 OR Information Service Alberta Environment/ Alberta Sustainable Resource Development #100, 3115- 12 Street NE Calgary, Alberta, Canada T2E 7J2 Telephone: (403) 297- 3362 OR Visit our web site at: http://www3.gov.ab.ca/srd/fw/riskspecies/ This publication may be cited as: Chetkiewicz, C. 2002. Carnivores and corridors in the Crowsnest Pass. Alberta Sustainable Resource Development, Fish and Wildlife Division, Alberta Species at Risk Report No. 50. Edmonton, AB. DISCLAIMER The views and opinions expressed are those of the authors and do not necessarily represent the policies or positions of the Department or of the Alberta Government. EXECUTIVE SUMMARY Habitat loss, fragmentation and subsequent isolation of habitat patches due to human activities are major factors contributing to species endangerment. Large carnivores such as grizzly bears and cougars are particularly susceptible to fragmentation because they are wide-ranging and exist at relatively low population densities. -
Dr. Robert D. Lawrence the Thesis Area Is Located in the Western Foothills of the North Three Major Rock Units Are Present and T
AN ABSTRACT OF THE THESIS OF David Allen Jenne for the degree of Master of Science in Geology presented on March 15,1978 Title:STRUCTURAL GEOLOGY AND METAMORPHIC PETROLOGY OF THE GOLD MOUNTAIN AREA SNOHOMISH COUNTY WASHINGTON d' Abstract approved: Signature redacted for privacy. Dr. Robert D. Lawrence The thesis area is located in the western foothills of the North Cascade Mountains immediately east of Darrington, Washington. Three major rock units are present and these include, from west to east, the Darrington Phyllite, a sedimentary m1ange unit, and the Shuksan Schist.Each of these units is bounded by major faults.In the present thesis only the Darrington Phyllite and the melange unit were studied in detail. The Darrington Phyllite consists of phyllitic metapelites with very local interbedded graywacke, conglomerate, and greenschist. The phyllites contain alternating layers of quartz-albite and musco- vite-graphite.In some rocks, this compositional layering is equiva- lent to sedimentary bedding.However, in most locations,it has resulted from metamorphic processes involving the transposition of bedding and metamorphic differentiation during mimetic recrystal- lization. Greenschist is present as tectonically emplaced blocks and as very local interbeds in the phyllite.Along the western margin of the thesis area, greenschist and meta-igneous rocks have been faulted into place.These rocks probably are part of the Jumbo Mountain Complex. The interbedded greenschists contain lawsonite that has been altered to chlorite.This suggests that blueschist.-facies meta- morphism was followed by a temperature increase and greenschist- facies metamorphism. The mlange unit consists of blocks of sedimentary, meta- igneous, and metamorphic rocks in tectonic contact with a sheared pelitic matrix. -
Castle Designated Summer Trails
Livingstone South Peak BC AB 3 Coleman Island Lake Provincial Castle Provincial Park & Recreation 3 Bluff Mountain Area Wildland Provincial Park Crowsnest Island Loop CROWSNEST Blairmore 510 Peak Ridge 22 Sentry Designated Summer Robertson Peak Mountain ek PASS Frank re C r Oldman Dam a t S Provincial Talon Peak Trails 2018 ek Recreation Area Trail Hill re Lundbreck 5 C rk o Y 3 Chinook Peak th Mount McLaren or Bellevue N Lundbreck 510 Falls Provincial Turtle Mountain Mount Parrish Recreation Area 3 Map Legend 6 7 Hillcrest Mines Willoughby Peak Andy Good Peak Cowley eek Cr ork Tent 5 Y Castle Provincial Park Towns and Villages Mountain Mount 3 Coulthard Mount Ptolemy Castle Wildland Provincial Park Mountain Adanac Hillcrest Road Mountain Other Provincial Parks Pass 3 BC AB Hearts Peak 507 k n Cree Sartoris Byro Ecological Reserve Lakes Road Ptolemy SE5 Castle Wildland Campground Rivers / Streams Byron Hill Provincial Park Spades Peak Mount McGladrey Backcountry Campground Roads - Paved J a Mount Pengelly c Tapay Road 3 k s Poker Peak o n 9 C Creek oat re G e Group Use Campground Roads - Gravel Clubs Peak k AB Ginger Hill Day Use Area Alberta - British Columbia Border 507 L Maverick Hill BC y n x C Pincher Creek to Hwy 6 8 re ek Equestrian Hiking Trail Mount Darrah 507 Fishing Hiking / Biking / Equestrian Trail 3 Beaver Mines 6 Lynx Creek nda ver Staging / Parking Multi-Use Trail / Off-Highway Vehicle (OHV) Trail bo le Ri Campground Car k 775 e 774 re Castle Gladstone 1 C 12 L Trailhead Designated Camping Areas t o s s Valley Road o t -
Geology of the Canadian Rockies and Columbia Mountains Summary by Ben Gadd
Geology of the Canadian Rockies and Columbia Mountains Summary by Ben Gadd 1. Basic geological history of western Canada The evidence reposes in four great layers, each thousands of metres thick. These four great layers (I call them the ancient sediments, the old clastics, the middle carbonates and the young clastics) show two main phases in the geological history of western Canada. First came a long period of sediment deposition, followed by a shorter period of mountain-building. Throughout this time—1.7 billion years altogether—the movement of the world’s crustal plates played a key role. • See last page for the currently accepted geological time scale, with period names and dates. First phase: deposition of most of the rock. About 1.7 billion years ago, part of what is now North America was imbedded in a supercontinent (amalgamation of continents) called Columbia (no relation to the Columbia Mountains). The oldest sedimentary rock in the Rockies was deposited about this time in an inland sea on Columbia. This rock is mostly argillite—very hard mud—and it is now found at the northern end of the Rockies. It is not found in ranges west of the Rockies. The supercontinent of Columbia broke up about 200 million years later. While North America was drifting free some 1.5 billion years ago, a second batch of ancient argillite, with additional limestone and dolostone—more on dolostone in a minute—was deposited in another inland sea, this time at the southern end of the Canadian Rockies in the Waterton area, and to the west in what are now the Purcell Mountains, one of the ranges in the Columbia Mountains (Purcells, Selkirks, Monashees and Cariboos). -
The Amateur Mountain Photography of Ken Betts, 1929-1936
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies Legacy Theses 2001 "Down to the valley and up to right": the amateur mountain photography of Ken Betts, 1929-1936 Bryan, Dawn Margaret Bryan, D. M. (2001). "Down to the valley and up to right": the amateur mountain photography of Ken Betts, 1929-1936 (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/20621 http://hdl.handle.net/1880/41259 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca The author of this thesis has granted the University of Calgary a non-exclusive license to reproduce and distribute copies of this thesis to users of the University of Calgary Archives. Copyright remains with the author. Theses and dissertations available in the University of Calgary Institutional Repository are solely for the purpose of private study and research. They may not be copied or reproduced, except as permitted by copyright laws, without written authority of the copyright owner. Any commercial use or publication is strictly prohibited. The original Partial Copyright License attesting to these terms and signed by the author of this thesis may be found in the original print version of the thesis, held by the University of Calgary Archives. -
USGS Geologic Investigation Series I-2592, Pamphlet
GEOLOGIC MAP OF THE SAUK RIVER 30- BY 60-MINUTE QUADRANGLE, WASHINGTON By R.W. Tabor, D.B. Booth, J.A. Vance, and A.B. Ford But lower, in every dip and valley, the forest is dense, of trees crowded and hugely grown, impassable with undergrowth as toughly woven as a fisherman’s net. Here and there, unnoticed until you stumble across them, are crags and bouldered screes of rock thickly clothed with thorn and creeper, invisible and deadly as a wolf trap.1 The Hollow Hills by Mary Stewart, 1973 INTRODUCTION AND Ortenburger for office and laboratory services. R.W. Tabor ACKNOWLEDGMENTS prepared the digital version of this map with considerable help from Kris Alvarez, Kathleen Duggan, Tracy Felger, Eric When Russell (1900) visited Cascade Pass in 1898, he Lehmer, Paddy McCarthy, Geoffry Phelps, Kea Umstadt, Carl began a geologic exploration which would blossom only after Wentworth, and Karen Wheeler. three-quarters of a century of growing geologic theory. The Paleontologists who helped immensely by identifying region encompassed by the Sauk River quadrangle is so struc- deformed, commonly recrystallized, and usually uninspiring turally complex that when Misch (1952) and his students fossils are Charles Blome, William Elder, Anita Harris, David began their monumental studies of the North Cascades in L. Jones, Jack W. Miller, and Kate Schindler. Chuck Blome 1948, the available geologic tools and theories were barely has been particularly helpful (see table 1). adequate to start deciphering the history. Subsequently, Bryant We thank John Whetten, Bob Zartman, and John Stacey (1955), Danner (1957), Jones (1959), Vance (1957a), Ford and his staff for unpublished U-Pb isotopic analyses (cited (1959), and Tabor (1961) sketched the fundamental outlines of in table 2). -
Snohomish County Hiking Guide
2015- 2016 TO OUTDOOR ADVENTURE! 30 GREAT HIKES • DRIVING DIRECTIONS MAPS • ACCOMMODATIONS • LOCAL RESOURCES photo by Scott Morris PB | www.snohomish.org www.snohomish.org | 1 SCTB Print - Hiking Guide Cover 5.5” x 8.5” - Full Color 5-2015 HIKE NAME 1 Hike subtitle ROUNDTRIP m ile ELEVATION GAIN m ile HIKING SEASON m ile MAP m ile NOTES m ile DRIVING DIRECTIONS m ile CONTACT INFO m ile Hard to imagine, but one of the finest beaches River Delta. A fairly large lagoon has developed on in all of Snohomish County is just minutes from the island where you can watch for sandpipers, downtown Everett! And this two mile long sandy osprey, kingfishers, herons, finches, ducks, and expanse was created by man, not nature. Beginning more. in the 1890s, the Army Corp of Engineers built a You won’t be able to walk around the island as the jetty just north of Port Gardiner—then commenced channel side contains no beach. But the beach to dredge a channel. The spoils along with silt and on Possession Sound is wide and smooth and you sedimentation from the Snohomish River eventually can easily walk 4 to 5 miles going from tip to tip. created an island. Sand accumulated from tidal Soak up views of the Olympic Mountains; Whidbey, influences, birds arrived and nested, and plants Camano, and Gedney Islands; and downtown Everett soon colonized the island. against a backdrop of Cascades Mountains. In the 1980s the Everett Parks and Recreation Department began providing passenger ferry service to the island. Over 50,000 folks visit this sandy gem each year.