Looking Directly at Opabin Pass, with Mount Biddle on the Left and Wenkchemna Peak on the Right
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
North America: Physical Geography by National Geographic, Adapted by Newsela Staff on 09.22.17 Word Count 681 Level 610L
North America: Physical geography By National Geographic, adapted by Newsela staff on 09.22.17 Word Count 681 Level 610L Valley of the Ten Peaks and Moraine Lake, Banff National Park, Canada. Mountains (from left to right) Tonsa (3,057 meters), Mount Perren (3,051 m), Mount Allen (3,310 m), Mount Tuzo (3,246 m), Deltaform Mountain (3,424 m), Neptuak Mountain (3,233 m). North America is the third-largest continent. It includes Canada, the United States, and Mexico. It also includes smaller countries in Central America. Below it sits South America. North America is made up of five main areas. They are the mountainous west, the Great Plains, the Canadian Shield, the eastern region, and the Caribbean. Each area includes different types of biomes. A biome is a type of environment where plants and animals live. North America includes many biomes. It has deserts, grasslands, tundras, coral reefs, and more. Western Region North America's western region is famous for its mountains and deserts. The Rocky Mountains are found there. They are North America's largest mountain chain. The Rockies are part of a system of mountains called the Cordilleras. They include the Sierra Madre Mountains. They stretch from the southwestern United States, through Mexico, and all the This article is available at 5 reading levels at https://newsela.com. way south to Honduras. The mountains include a rare biome called a temperate rainforest. These areas get much rain. This helps them support a large mix of life forms. Black bears are found there. Some trees grow up to 300 feet tall. -
Day Hiking Lake Louise, Castle Junction and Icefields Parkway Areas
CASTLE JUNCTION AREA ICEFIELDS PARKWAY AREA LAKE LOUISE AREA PLAN AHEAD AND PREPARE Remember, you are responsible for your own safety. 1 7 14 Castle Lookout Bow Summit Lookout Wilcox Pass MORAINE LAKE AREA • Get advice from a Parks Canada Visitor Centre. Day Hiking 3.7 km one way; 520 m elevation gain; 3 to 4 hour round trip 2.9 km one way; 245 m elevation gain; 2.5 hour round trip 4 km one way; 335 m elevation gain; 3 to 3.5 hour round trip • Study trail descriptions and maps before starting. Trailhead: 5 km west of Castle Junction on the Bow Valley Parkway Trailhead: Highway 93 North, 40 km north of the Lake Louise junction, Trailhead: Highway 93 North, 47 km north of Saskatchewan Crossing, • Check the weather forecast and current trail conditions. (Highway 1A). at the Peyto Lake parking lot. or 3 km south of the Icefield Centre at the entrance to the Wilcox Creek Trailheads: drive 14 km from Lake Louise along the Moraine Lake Road. • Choose a trail suitable for the least experienced member in Lake Louise, Castle Junction campground in Jasper National Park. Consolation Lake Trailhead: start at the bridge near the Rockpile at your group. In the mid-20th century, Banff erected numerous fire towers From the highest point on the Icefields Parkway (2070 m), Moraine Lake. Pack adequate food, water, clothing, maps and gear. and Icefields Parkway Areas where spotters could detect flames from afar. The Castle Lookout hike beyond the Peyto Lake Viewpoint on the upper self-guided • Rise quickly above treeline to the expansive meadows of this All other trails: begin just beyond the Moraine Lake Lodge Carry a first aid kit and bear spray. -
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 -
Above the Glaciers in the Canadian Rockies
I v» « .1 h •,.- PRIMER 276 fMadsaac MemoriafjFutKf In memory of VERA MAY MACISAAC, BA 1925 Queen's University Libraries The EDITH WLORNE PIERCE COLLECTION of CANADIANA Queens University at Kingston . ^ _....., ,..,. ,. , _._. — TT 1 _ , ; : rT „ ; j:i ^l|l|il||]!iiii!iPI|iii|i|i|!|i!|i|i|ii|!!|||||l||l|l|!|]i|I ; ^ : ms >j#&M Above fhe Glaciers in the 6anadian Rockies I m§^ i «i m '% X — — 1 1 % ; , ^ k Glaciers of the Canadian Rockies DESCRIPTIVE articles of a technical nature are mostly bores, but so many different ideas are entertained by tourists as to the causes of glacial ice, the life of glaciers, etc., it is perhaps necessary to say a few words in explana- tion of these most marvelous of nature's phenomena. The average glacier may best be described as a vast body of ice filling some titanic mountain crev- ice, down which it slowly moves—the outlet of the snows which accumulate in the higher portions of the mountain crevices. In such mountainous local- ities the snows are even and the temperature not rising sufficiently for any considerable proportion to be melted and flow down, fill the spaces between the summits. By the pressure exerted by these vast collections the yielding material is forced through whatever opening is presented for its pas- sage, and the great valleys leading to the base of the mountains are packed full of ice which results from the snow being solidified by pressure, or by its own melting and freezing again. This great river of ice, solid as it appears, is steadily, although almost imperceptibly urged onward until it reaches a region down the valley where the temperature is sufficient- ly high to melt away the fore-foot of the glacier. -
Hikes in Lake Louise Area
Day hikes in the Lake Louise area Easy trails Descriptions of easy trails For maps, detailed route finding and trail descriptions, visit a Parks Canada Visitor Centre or purchase a hiking guide book and topographical map. Cell service is not reliable. Lake Louise Lakeshore Length: 2 km one way Hiking time: 1 hour Elevation gain: minimal Trailhead: Upper Lake Louise parking area, 4 km from the village of Lake Louise. Description: This accessible stroll allows visitors of all abilities to explore Lake Louise. At the end of the lake you’ll discover the milky creek that gives the lake its magical colour. Fairview Lookout Length: 1 km one way Hiking time: 45 minute round trip Elevation gain: 100 m Trailhead: Upper Lake Louise parking area, 4 km from the village of Lake Louise. Description: Leaving from the boathouse on Lake Louise, this short, uphill hike offers you a unique look at both the lake and the historic Fairmont Chateau Lake Louise. Bow River Loop Length: 7.1 km round trip Hiking time: 2 hour round trip Elevation gain: minimal Trailhead: Parking lot opposite the Lake Louise train station (restaurant) Description: Travel on a pleasant interpretive trail in the rich riparian zone of the Bow River. These waters travel across the prairies to their ultimate destination in Hudson Bay, over 2500 kilometres downstream of Lake Louise. Louise Creek Length: 2.8 km one way Hiking time: 1.5 hour round trip Elevation gain: 195 m Trailhead: From the Samson Mall parking lot, walk along Lake Louise Drive to a bridge crossing the Bow River. -
Banff National Park
Banff National Park Day hikes in the Lake Louise area Along the spine of the North American continent, the Rocky Mountains rise high into the clouds and blue glaciers cling to their slopes. Green forested valleys provide a vital food source for grizzly bears and other species. This is the Lake Louise and Icefields area of Banff National Park, a landscape of wonder which has been dubbed the “hiking capital of Canada”. Use the trail descriptions to choose a hike suitable for everyone in your party. For maps, detailed route finding and trail descriptions, visit a Parks Canada Visitor Centre or purchase a hiking guide book and topographical map. Cell service is not reliable. Easy trails Trail Distance (one way) Time (return) Elevation (m) Lake Louise Lakeshore 2 km 1 hour minimal Fairview Lookout 1 km 45 minutes 100 Bow River Loop 7.1 km (round trip) 2 hours minimal Louise Creek 2.8 km 1.5 hours 195 m Moraine Lake Lakeshore 1.5 km 45 minutes minimal Consolation Lakes 2.9 km 2 hours 65 Descriptions of easy trails Lake Louise Lakeshore Length: 2 km one way Hiking time: 1 hour Elevation gain: minimal Trailhead: Upper Lake Louise parking area, 4 km from the village of Lake Louise. Parking lot is accessible by transit and recommended from June – September. Description: This accessible stroll allows visitors of all abilities to explore Lake Louise. At the end of the lake you’ll discover the milky creek that gives the lake its magical colour. Fairview Lookout Length: 1 km one way Hiking time: 45 minute round trip Elevation gain: 100 m Trailhead: Upper Lake Louise parking area, 4 km from the village of Lake Louise. -
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 .................................................................................................................. -
In the United States Bankruptcy Court for the District of Delaware
IN THE UNITED STATES BANKRUPTCY COURT FOR THE DISTRICT OF DELAWARE In re: ) Chapter 11 ) PACIFIC ENERGY RESOURCES LTD., et al.,' ) Case No. 09-10785 (KJC) ) (Jointly Administered) Liquidating Debtors. ) AFFIDAVIT OF SERVICE STATE OF CALIFORNIA ) ) ss: COUNTY OF LOS ANGELES ) Ann Mason, being duly sworn according to law, deposes and says that she is employed by the law firm of Pachulski Stang Ziehl & Jones LLP, attorneys for the Debtors in the above- captioned action, and that on the 5 th day of October 2012 she caused a copy of the following documents to be served upon the parties on the attached service lists in the manner indicated: Liquidating Debtors’ Notice of Motion for Order Approving Assignment of Assets to Hilcorp Alaska, LLC and Distribution of the Proceeds Thereof ("Notice") Liquidating Debtors’ Motion for Order Approving Assignment of Assets to Hilcorp Alaska, LLC and Distribution of the Proceeds Thereof ("Motion") Because the service list was so large (nearly 9,000 parties), the copies of the Motion that were served on parties in interest other than the core service list did not contain copies of Exhibits A, B or D. However, the service copies of the Motion and the Notice advised parties in interest that they can obtain copies of Exhibits A, B and D by making a request, in writing, to counsel for the Liquidating Debtors at the address listed in the signature block to the Motion. The Liquidating Debtors (and the last four digits of each of their federal tax identification numbers) are: Pacific Energy Resources Ltd. (3442); Pacific Energy Alaska Holdings, LLC (tax I.D. -
• Banff • Jasper • Kootenay • Yoho • Mount Revelstoke • Glacier • Waterton Lakes • National Parks • Fort St
• BANFF • JASPER • KOOTENAY • YOHO • MOUNT REVELSTOKE • GLACIER • WATERTON LAKES • NATIONAL PARKS • FORT ST. JAMES • BANFF PARK MUSEUM • CAVE AND BASIN • ROCKY MOUNTAIN HOUSE • BAR U RANCH • NATIONAL HISTORIC SITES Celebrating 100 years of this land and its stories e Ye f Jef 2007/2008 Également offert en français MAPS INSIDE! Welcome You are Visiting a National Treasure anadian national parks and Cnational historic sites are a country-wide system of significant natural areas, places, persons and events. These special locales are gateways to nature, adventure, discovery and to our past. They celebrate the beauty and infinite variety of our country and bear witness to our nation’s defining moments. Each national park is a sanctuary in And world heritage sites too! which nature is allowed to evolve in anff, Jasper, Kootenay and Yoho national parks, together its own way. Each national historic Bwith the provincial parks of Hamber, Mount Robson site tells a unique story, contributing and Mount Assiniboine, are recognized internationally as a a sense of time, identity, and place UNESCO World Heritage Site. The Canadian Rocky Mountain to our understanding of Canada as Parks World Heritage Site encompasses 20 585 km2–one of the a whole. largest protected areas in the world. Protected and preserved for all Waterton-Glacier International Peace Park, spanning the Canadians and for the world, Canada-U.S.A. boundary between Montana and Alberta, was Canada’s national parks and designated as a World Heritage Site because of its superlative national historic sites provide a mountain scenery, high topographic relief, glacial landforms, haven for plants and animals and and abundant diversity of wildlife and wildflowers. -
Long-Toed Salamander (Ambystoma Macrodactylum) Monitoring Study in Alberta: Summary Report 1998-2001
Long-toed Salamander (Ambystoma macrodactylum) Monitoring Study in Alberta: Summary Report 1998-2001 Alberta Species at Risk Report No. 36 Long-toed Salamander (Ambystoma macrodactylum) Monitoring Study in Alberta: Summary Report 1998-2001 Mai-Linh Huynh Lisa Takats and Lisa Wilkinson Alberta Species at Risk Report No. 36 January 2002 Project Partners: Publication No.: I/053 ISBN: 0-7785-2002-1 (Printed Edition) ISBN: 0-7785-2003-X (On-line Edition) ISSN: 1496-7219 (Printed Edition) ISSN: 1496-7146 (On-line Edition) Illustration: 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: Huynh, M., L. Takats and L. Wilkinson. 2002. Long-toed salamander (Ambystoma macrodactylum) monitoring study in Alberta: summary report 1998-2001. Alberta Sustainable Resource Development, Fish and Wildlife Division, Alberta Species at Risk Report No. 36. Edmonton, AB. TABLE OF CONTENTS ACKNOWLEDGEMENTS ............................................................................................. v EXECUTIVE SUMMARY ............................................................................................ -
Management Plan for Bighorn Sheep in Alberta
Management Plan for Bighorn Sheep in Alberta Wildlife Management Series Number Wildlife Management Branch June 25, 2015 Pub. No. ISBN No. XXXXXXXXX (Printed Edition) ISBN No. XXXXXXXXX (On-line Edition) Copies of this report are available from: Information Centre Alberta Environment and Parks Main Floor, Great West Life Building 9920-108 Street Edmonton, Alberta T5K 2M4 (780) 422-2079 OR The Alberta Environment and Parks Web Site: aep.alberta.ca Preface This plan represents the Department’s goals, objectives and management strategies for the management of bighorn sheep in Alberta. It will periodically be reviewed and updated as necessary. Implementation will be subject to priorities established during the budgeting process. This plan includes historical information up to the winter of 2012-2013. Note: for the purposes of this publication, information is presented in a format that corresponds to fiscal years. Data for the year 2010, for example, corresponds to April 1, 2010 to March 31, 2011. Jun 25, 2015 Management Plan for Bighorn Sheep in Alberta Page 2 of 137 © 2015 Government of Alberta Table of Contents Acknowledgements ........................................................................................................................ 9 Executive Summary ..................................................................................................................... 10 1.0 Introduction ..................................................................................................................... 12 2.0 Background .................................................................................................................... -
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