DOCSLIB.ORG

Yoho National Park of Canada Spring 2005

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Yoho National Park of Canada Spring 2005 Yoho National Park of Canada Spring 2005 Yoho Location Yoho and Glacier National Park were both declared Vegetation National Park of Canada Canada's second national parks on the same day. Three distinct vegetation zones exist in this Yoho was established in 1886. Located in mountainous region, largely because of the southeastern British Columbia on the Alberta border, inherent changes in elevation. The montane Climate Yoho is part of the world-famous Rocky Mountains. 2 zone is the lowest of the three, and is The 1 313 km park is about 8 km west of Lake Louise, Dramatic variations in Yoho's climate are characterized by grassy meadows, and forests Alberta, and represents the Rocky Mountain Natural caused by a combination of elevation, rain of Douglas fir, white spruce, trembling aspen, Region, part of the Central Rockies ecosystem. Yoho shadow effects, and latitude. Generally, and lodgepole pine. The eastern limit of is part of the Montane Cordillera Ecozone. winters are long and summers cool and interior western hemlock forest is found in short, with only occasional hot spells. the park. The subalpine zone of the slopes Average January highs are -7oC, while July supports a largely closed coniferous forest of averages to 22oC. These temperatures Engelmann spruce, subalpine fir, and apply to valley bottoms. At higher lodgepole pine. Some open meadowland in elevations temperatures are about 5 to 7oC upper regions can also be found. During the cooler. Annual precipitation ranges from summer, these meadows are covered with a thick carpet of wildflowers. The highest of the less than 380 mm at lower elevations to Banff over 1 250 mm at higher elevations. National three zones, the alpine region, cannot Activities R Park support trees. Vegetation is sparse, with some alpine meadows, and as one goes O Visitors to Yoho can enjoy a multitude of Geology higher up still, one enters the exclusive activities, including camping at one of five C domain of hardy lichens that cling to the bare campgrounds, hiking along backcountry The Western and Eastern Main Ranges of the Rocky Mountains are found in Yoho, K rock. trails, canoeing on the park's larger lakes and ponds, and driving the scenic and are composed of limestone, Y Y o roadways. The park, which attracts visitors h sandstone, and shale. The mountains A o m i s k from all over the world each year, offers occasionally show folded layers of these w i R iv Wildlife fishing, mountain climbing, cycling, sedimentary bedrocks that are among the e r horseback riding, and cross-country skiing. oldest in the whole mountain chain. It is M R Emerald iv Yoho, like all of the Rocky Mountain Parks, is e Commercial services offer ski rentals, dog r Lake believed that the Rockies have seen at least O er famous for its wildlife. Some 60 mammal Riv sledding, and mountain guiding. four ice ages. Yoho is a region of waterfalls, U species are found here, including moose, elk, rock walls, and igneous formations, which Field P N white-tailed deer, mule deer, cougars, black o r c e are not too large, but are unique to the u rs p o in H T bears, wolves, coyotes, and a secretive e Rocky Mountains. The Burgess Shale site, O tt g e A population of grizzly bears. The mountain n rt i a one of the most important fossil sites in the k il Alberta C c re i I K e B.C. goat is Yoho’s most numerous large mammal k world, is located in the park and was Riv N er with a population estimated at around 400. For more information, contact: declared a World Heritage Site in 1981. S More than 200 species of birds, including The Superintendent Yoho, (along with Jasper, Kootenay and Golden and Bald Eagles, have been identified. Yoho National Park Banff National Parks and Mount Robson, Kootenay Box 99 Ic National The park's major watersheds contain rainbow Hamber and Mount Assiniboine e Field, British Columbia V0A 1G0 Park trout, brook trout, lake trout, northern pike, Provincial Parks) was declared a N Telephone: (250) 343-6783 R iv and whitefish. Reptiles and amphibians are Fax: (250) 343-6012 e UNESCO World Heritage Site in 1985 on r scarce because of the severe climate. Only Website: www.pc.gc.ca/yoho the park's 100th anniversary. 0 8 655 m one species of toad, three frogs, one © Parks Canada Glacier/Icefield salamander, and two types of snakes have been recorded. Yoho National Park of Canada Spring 2005 Yoho Location Yoho and Glacier National Park were both declared Vegetation National Park of Canada Canada's second national parks on the same day. Three distinct vegetation zones exist in this Yoho was established in 1886. Located in mountainous region, largely because of the southeastern British Columbia on the Alberta border, inherent changes in elevation. The montane Climate Yoho is part of the world-famous Rocky Mountains. 2 zone is the lowest of the three, and is The 1 313 km park is about 8 km west of Lake Louise, Dramatic variations in Yoho's climate are characterized by grassy meadows, and forests Alberta, and represents the Rocky Mountain Natural caused by a combination of elevation, rain of Douglas fir, white spruce, trembling aspen, Region, part of the Central Rockies ecosystem. Yoho shadow effects, and latitude. Generally, and lodgepole pine. The eastern limit of is part of the Montane Cordillera Ecozone. winters are long and summers cool and interior western hemlock forest is found in short, with only occasional hot spells. the park. The subalpine zone of the slopes Average January highs are -7oC, while July supports a largely closed coniferous forest of averages to 22oC. These temperatures Engelmann spruce, subalpine fir, and apply to valley bottoms. At higher lodgepole pine. Some open meadowland in elevations temperatures are about 5 to 7oC upper regions can also be found. During the cooler. Annual precipitation ranges from summer, these meadows are covered with a thick carpet of wildflowers. The highest of the less than 380 mm at lower elevations to Banff over 1 250 mm at higher elevations. National three zones, the alpine region, cannot Activities R Park support trees. Vegetation is sparse, with some alpine meadows, and as one goes O Visitors to Yoho can enjoy a multitude of Geology higher up still, one enters the exclusive activities, including camping at one of five C domain of hardy lichens that cling to the bare campgrounds, hiking along backcountry The Western and Eastern Main Ranges of the Rocky Mountains are found in Yoho, K rock. trails, canoeing on the park's larger lakes and ponds, and driving the scenic and are composed of limestone, Y Y o roadways. The park, which attracts visitors h sandstone, and shale. The mountains A o m i s k from all over the world each year, offers occasionally show folded layers of these w i R iv Wildlife fishing, mountain climbing, cycling, sedimentary bedrocks that are among the e r horseback riding, and cross-country skiing. oldest in the whole mountain chain. It is M R Emerald iv Yoho, like all of the Rocky Mountain Parks, is e Commercial services offer ski rentals, dog r Lake believed that the Rockies have seen at least O er famous for its wildlife. Some 60 mammal Riv sledding, and mountain guiding. four ice ages. Yoho is a region of waterfalls, U species are found here, including moose, elk, rock walls, and igneous formations, which Field P N white-tailed deer, mule deer, cougars, black o r c e are not too large, but are unique to the u rs p o in H T bears, wolves, coyotes, and a secretive e Rocky Mountains. The Burgess Shale site, O tt g e A population of grizzly bears. The mountain n rt i a one of the most important fossil sites in the k il Alberta C c re i I K e B.C. goat is Yoho’s most numerous large mammal k world, is located in the park and was Riv N er with a population estimated at around 400. For more information, contact: declared a World Heritage Site in 1981. S More than 200 species of birds, including The Superintendent Yoho, (along with Jasper, Kootenay and Golden and Bald Eagles, have been identified. Yoho National Park Banff National Parks and Mount Robson, Kootenay Box 99 Ic National The park's major watersheds contain rainbow Hamber and Mount Assiniboine e Field, British Columbia V0A 1G0 Park trout, brook trout, lake trout, northern pike, Provincial Parks) was declared a N Telephone: (250) 343-6783 R iv and whitefish. Reptiles and amphibians are Fax: (250) 343-6012 e UNESCO World Heritage Site in 1985 on r scarce because of the severe climate. Only Website: www.pc.gc.ca/yoho the park's 100th anniversary. 0 8 655 m one species of toad, three frogs, one © Parks Canada Glacier/Icefield salamander, and two types of snakes have been recorded..
Load more

Recommended publications
  • Okanagan Range Ecoregion
    Selecting Plants for Pollinators A Guide for Gardeners, Farmers, and Land Managers In the Okanagan Range Ecoregion Keremeos and Hedley Table of CONTENTS Why Support Pollinators? 4 Getting Started 5 Okanagan range 6 Meet the Pollinators 8 Plant Traits 10 Developing Plantings 12 Farms 13 Public Lands 14 Home Landscapes 15 Plants That Attract Pollinators 16 Habitat hints 20 Habitat and Nesting requirements 21 S.H.A.R.E. 22 Checklist 22 This is one of several guides for different regions of North America. Resources and Feedback 23 We welcome your feedback to assist us in making the future guides useful. Please contact us at [email protected] 2 Selecting Plants for Pollinators Selecting Plants for Pollinators A Guide for Gardeners, Farmers, and Land Managers In the Okanagan Range Ecoregion Keremeos and Hedley A NAPPC and Pollinator Partnership Canada™ Publication Okanagan Range 3 Why support pollinators? IN THEIR 1996 BOOK, THE FORGOTTEN POLLINATORS, Buchmann and Nabhan estimated that animal pollinators are needed for the reproduction “Flowering plants of 90% of fl owering plants and one third of human food crops. Each of us depends on these industrious pollinators in a practical way to provide us with the wide range of foods we eat. In addition, pollinators are part of the across wild, intricate web that supports the biological diversity in natural ecosystems that helps sustain our quality of life. farmed and even Abundant and healthy populations of pollinators can improve fruit set and quality, and increase fruit size. In farming situations this increases production per hectare. In the wild, biodiversity increases and wildlife urban landscapes food sources increase.
    [Show full text]
  • Ecoregions with Grasslands in British Columbia, the Yukon, and Southern Ontario
    83 Chapter 4 Ecoregions with Grasslands in British Columbia, the Yukon, and Southern Ontario Joseph D. Shorthouse Department of Biology, Laurentian University Sudbury, Ontario, Canada P3E 2C6 Abstract. The second largest grasslands of Canada are found in south-central British Columbia in valleys between mountain ranges and on arid mountain-side steppes or benchlands. The province contains five ecozones, with most of the grassland habitat in the Montane Cordillera Ecozone. This ecozone consists of a series of plateaux and low mountain ranges and comprises 17 ecoregions, 7 of which contain grasslands. Dominant grasses here are bunchgrasses. A few scattered grasslands are found in the Yukon in the Boreal Cordillera Ecozone within three ecoregions. Grasslands in southwestern Ontario consist of about 100 small remnants of what was once much more abundant tallgrass prairie. These grasslands grow in association with widely spaced deciduous trees and are remnants of a past prairie peninsula. Grasslands called alvars are also found on flat limestone bedrock in southern Ontario. This chapter briefly describes the physiography, climate, soils, and prominent flora of each ecoregion for the benefit of future biologists wishing to study the biota of these unique grasslands. Résumé. Les prairies du centre-sud de la Colombie-Britannique sont les deuxièmes plus vastes au Canada. Elles se trouvent dans les vallées séparant les chaînes de montagnes, et sur les steppes ou replats arides à flanc de montagne. La province renferme cinq écozones, et l’habitat de prairies se trouve principalement dans l’écozone de la cordillère alpestre. Cette écozone est constituée d’une série de plateaux et de chaînes de montagnes basses et se divise en 17 écorégions, dont 7 renferment des prairies.
    [Show full text]
  • MOTHS and BUTTERFLIES LEPIDOPTERA DISTRIBUTION DATA SOURCES (LEPIDOPTERA) * Detailed Distributional Information Has Been J.D
    MOTHS AND BUTTERFLIES LEPIDOPTERA DISTRIBUTION DATA SOURCES (LEPIDOPTERA) * Detailed distributional information has been J.D. Lafontaine published for only a few groups of Lepidoptera in western Biological Resources Program, Agriculture and Agri-food Canada. Scott (1986) gives good distribution maps for Canada butterflies in North America but these are generalized shade Central Experimental Farm Ottawa, Ontario K1A 0C6 maps that give no detail within the Montane Cordillera Ecozone. A series of memoirs on the Inchworms (family and Geometridae) of Canada by McGuffin (1967, 1972, 1977, 1981, 1987) and Bolte (1990) cover about 3/4 of the Canadian J.T. Troubridge fauna and include dot maps for most species. A long term project on the “Forest Lepidoptera of Canada” resulted in a Pacific Agri-Food Research Centre (Agassiz) four volume series on Lepidoptera that feed on trees in Agriculture and Agri-Food Canada Canada and these also give dot maps for most species Box 1000, Agassiz, B.C. V0M 1A0 (McGugan, 1958; Prentice, 1962, 1963, 1965). Dot maps for three groups of Cutworm Moths (Family Noctuidae): the subfamily Plusiinae (Lafontaine and Poole, 1991), the subfamilies Cuculliinae and Psaphidinae (Poole, 1995), and ABSTRACT the tribe Noctuini (subfamily Noctuinae) (Lafontaine, 1998) have also been published. Most fascicles in The Moths of The Montane Cordillera Ecozone of British Columbia America North of Mexico series (e.g. Ferguson, 1971-72, and southwestern Alberta supports a diverse fauna with over 1978; Franclemont, 1973; Hodges, 1971, 1986; Lafontaine, 2,000 species of butterflies and moths (Order Lepidoptera) 1987; Munroe, 1972-74, 1976; Neunzig, 1986, 1990, 1997) recorded to date.
    [Show full text]
  • RBA Cragg Fonds
    Kamloops Museum and Archives R.B.A. Cragg fonds 1989.009, 0.2977, 0.3002, 1965.047 Compiled by Jaimie Fedorak, June 2019 Kamloops Museum and Archives 2019 KAMLOOPS MUSEUM AND ARCHIVES 1989.009, etc. R.B.A. Cragg fonds 1933-1979 Access: Open. Graphic, Textual 2.00 meters Title: R.B.A. Cragg fonds Dates of Creation: 1933-1979 Physical Description: ca. 80 cm of photographs, ca. 40 cm of negatives, ca. 4000 slides, and 1 cm of textual records Biographical Sketch: Richard Balderston Alec Cragg was born on December 5, 1912 in Minatitlan, Mexico while his father worked on a construction contract. In 1919 his family moved to Canada to settle. Cragg gained training as a printer and worked in various towns before being hired by the Kamloops Sentinel in 1944. Cragg worked for the Sentinel until his retirement at age 65, and continued to write a weekly opinion column entitled “By The Way” until shortly before his death. During his time in Kamloops Cragg was active in the Kamloops Museum Association, the International Typographical Union (acting as president on the Kamloops branch for a time), the BPO Elks Lodge Kamloops Branch, and the Rock Club. Cragg was married to Queenie Elizabeth Phillips, with whom he had one daughter (Karen). Richard Balderson Alec Cragg died on January 22, 1981 in Kamloops, B.C. at age 68. Scope and Content: Fonds consists predominantly of photographic materials created by R.B.A. Cragg during his time in Kamloops. Fonds also contains a small amount of textual ephemera collected by Cragg and his wife Queenie, such as ration books and souvenir programs.
    [Show full text]
  • National Par Ks British Columbia
    NATIONAL FOREWORD The National Parks of Canada are areas of natural beauty and special interest that have been "dedicated to the people PAR KS of Canada for their benefit, education, and enjoyment". Established primarily for the preservation of the unspoiled natural landscape and for the protection of the native wildlife, they are to be "maintained and made use of so as to leave them unimpaired for the enjoyment of future generations". BRITISH The discovery of hot mineral springs, bubbling from the slopes of Sulpltur Mountain, by engineers exploring the route for Canada's first transcontinental railway, led to the establish­ ment of Canada's first national park. From this small area of ten square miles at Banff, Alberta, set apart in 1885, the COLUMBIA national parks system has been extended until it embraces 37 separate areas totalling more than 29,000 square miles. Although a few parks have been devoted chiefly to the con­ servation of certain species of big game animals once threatened with extinction, some contain sites memorable in the early history of Canada. Others have been developed so that park visitors may more conveniently view the magnificent scenery and relax in the enjoyment of the inspirational and peaceful environment. From the sea-girt hills on the Atlantic Coast across the rivers and lakes of Central Canada to tlie alpine vistas of the Rockies and Selkirks, these national playgrounds provide ideal areas for nature study and for recreation. It is the responsibility of the National Parks Branch of the Department of Northern Affairs and National Resources to administer these natural areas for the enjoyment of Canada's present and future generations.
    [Show full text]
  • Canadian Rockies Hiking Trail List
    Canadian Rockies Hiking Trail List The following hiking trails are detailed in the Canadian Rockies Trail Guide: BANFF NATIONAL PARK Banff—Lake Minnewanka Sunshine Meadows 25. Sunshine Meadows Loop 1. C Level Cirque Trail 26. Quartz Hill—Citadel Pass Trail 2. Johnson Lake Trail 27. Simpson Pass—Healy Meadows Trail 3. Lake Minnewanka Trail 4. Alymer Lookout Trail Bow Valley Highline 5. Cascade Amphitheatre Trail 28. Healy Pass—Egypt Lake Trail 6. Elk Lake Trail 29. Egypt Lake via Pharaoh Creek Trail 7. Stoney Squaw Trail 30. Redearth Creek—Shadow Lake Trail 8. Fenland Trail 31. Twin Lakes Trail 9. Tunnel Mountain Trail 32. Arnica Lake—Twin Lakes Trail 10. Sulphur Mountain Trail 33. Bow Valley Highline Trail 11. Sundance Canyon Trail 34. Boom Lake Trail 12. Mount Rundle Trail 35. Smith Lake Trail 13. Spray River Circuit Trail 36. Taylor Lake Trail 14. Goat Creek Trail 15. Rundle Riverside Trail Lake Louise—Moraine Lake 37. Lake Louise Lakeshore Trail Bow Valley Parkway—Sawback Range 38. Fairview Lookout Trail 16. Cory Pass—Mt. Edith Trail 39. Lake Agnes Trail 17. Edith Pass via Forty Mile Creek Trail 40. Plain of the Six Glaciers Trail 18. Muleshoe Trail 41. Saddleback Trail 19. Johnston Canyon—Ink Pots Trail 42. Paradise Valley Loop 20. Sawback Trail 43. Larch Valley—Sentinel Pass Trail 21. Sawback Range Circuit 44. Eiffel Lake—Wenkchemna Pass Trail 22. Rockbound Lake Trail 45. Consolation Lakes Trail 23. Castle Lookout Trail 46. Moraine Lakeshore Trail 24. Bourgeau Lake Trail Boulder Pass—Skoki Valley 47. Boulder Pass—Skoki Valley Trail 48.
    [Show full text]
  • National Park System: a Screening Level Assessment
    Environment Canada Parks Canada Environnement Canada Parcs Canada Edited by: Daniel Scott Adaptation & Impacts Research Group, Environment Canada and Roger Suffling School of Planning, University of Waterloo May 2000 Climate change and Canada’s national park system: A screening level assessment Le Changement climatique et le réseau des parcs nationaux du Canada : une évaluation préliminaire This report was prepared for Parks Canada, Department of Canadian Heritage by the Adaptation & Impacts Research Group, Environment Canada and the Faculty of Environmental Studies, University of Waterloo. The views expressed in the report are those of the study team and do not necessarily represent the opinions of Parks Canada or Environment Canada. Catalogue No.: En56-155/2000E ISBN: 0-662-28976-5 This publication is available in PDF format through the Adaptation and Impacts Research Group, Environment Canada web site < www1.tor.ec.gc.ca/airg > and available in Canada from the following Environment Canada office: Inquiry Centre 351 St. Joseph Boulevard Hull, Quebec K1A 0H3 Telephone: (819) 997-2800 or 1-800-668-6767 Fax: (819) 953-2225 Email: [email protected] i Climate change and Canada’s national park system: A screening level assessment Le Changement climatique et le réseau des parcs nationaux du Canada : une évaluation préliminaire Project Leads and Editors: Dr. Daniel Scott1 and Dr. Roger Suffling2 1 Adaptation and Impacts Research Group, Environment Canada c/o the Faculty of Environmental Studies, University of Waterloo Waterloo, Ontario N2L 3G1 519-888-4567 ext. 5497 [email protected] 2 School of Planning Faculty of Environmental Studies, University of Waterloo Waterloo, Ontario N2L 3G1 Research Team: Derek Armitage - Ph.D.
    [Show full text]
  • Integrating Biophysical and Eco-Cultural Fire in Canada Doi: 10.4996/Fireecology.0701074 Page 74
    Fire Ecology Volume 7, Issue 1, 2011 White et al.: Integrating Biophysical and Eco-Cultural Fire in Canada doi: 10.4996/fireecology.0701074 Page 74 FORUM ARTICLE BURNING AT THE EDGE: INTEGRATING BIOPHYSICAL AND ECO-CULTURAL FIRE PROCESSES IN CANADA’S PARKS AND PROTECTED AREAS Clifford A. White1*, Daniel D.B. Perrakis2, Victor G. Kafka3, and Timothy Ennis4 1Parks Canada Agency, P.O. Box 900, Banff National Park, Banff, Alberta, Canada T1L 1K2 2 British Columbia Ministry of Natural Resource Operations, Wildfire Management Branch, P.O. Box 9502 Station Provincial Government Victoria, British Columbia, Canada V8W 9C1 3Parks Canada Agency, Ecosystem Conservation Service, 3 passage du Chien d’Or, C.P. 6060, Haute-Ville, Québec, Province of Québec, Canada G1R 4V7 4 Nature Conservancy of Canada, 200-825 Broughton Street, Victoria, British Columbia, Canada V8W 1E5 *Corresponding author: Tel.: 001-403-760-0203; e-mail: [email protected] ABSTRACT Currently, high intensity, large-area lightning fires that burn during droughts dominate Canada’s fire regimes. However, studies from several disciplines clearly show that hu- mans historically ignited burns within this matrix of large fires. Two approaches for fire research and management have arisen from this pattern: a “large-fire biophysical para- digm” related to lightning-ignited fires, and an “eco-cultural paradigm” related to human- caused burning. Working at the edge between biophysically driven fires and eco-cultural burns, and their associated management and research paradigms, presents unique chal- lenges to land managers. We proceed by describing fire frequency trends across Canada, and how an interaction between changing climatic and cultural factors may provide better causal explanations for observed patterns than either group of factors alone.
    [Show full text]
  • Canadian Rockies by Rail Featuring Banff, Vancouver and the Rocky Mountaineer Train
    8 DAY HOLIDAY SAVE $ PER300 PERSON IF BOOKED BY 11/30/2019 Canadian Rockies by Rail featuring Banff, Vancouver and the Rocky Mountaineer Train July 19, 2020 Departure Date: Canadian Rockies by Rail Experience the best of Western 8 Days • 14 Meals Canada on an unforgettable adventure aboard the famed Rocky Mountaineer train through the Rockies while visiting the beautiful cities of Banff and Vancouver. TOUR HIGHLIGHTS 4 14 Meals (7 breakfasts, 3 lunches and 4 dinners) 4 Round trip airport transfers 4 Spend 1 night in Calgary, Alberta’s center of Cowboys and Culture 4 Take a panoramic sightseeing tour of Calgary and get your first glimpse of the Canadian Rockies from high atop the 626-foot tall Calgary Tower 4 Step back into Canada’s colorful past at Heritage Park with its fur-traders, blacksmith and collection of vintage automobiles 4 Spend 2 nights in the town of Banff inside Banff National Park, Canada’s first national park 4 Take a gondola ride to the top of Sulphur Mountain for a breathtaking view of the Banff village valley and surrounding mountains 4 Travel the scenic Icefields Parkway from Banff to Lake Louise 4 Visit Chateau Lake Louise located on the vibrant blue, glacier-fed waters of Lake Louise Banff National Park, Canada’s first national park 4 Spend 2 full days on board the Rocky Mountaineer Train in Silver Leaf Class as you pass some of the most breathtaking scenery in DAY 1 – Arrive in Calgary North America Welcome to one of North America's most rugged and beautiful 4 Spend 1 night in scenic Kamloops, nestled in the Rocky Mountains cities, Calgary.
    [Show full text]
  • Yoho National Park Map of the Park & Town of Field
    Yoho National Park Map of the park & town of Field T HE G WAPTA R E A Established in 1886, this park ICEFIELD T Y D O IV H boasts amazing waterfalls and Gordon ID O GL E 28 peaks that rise to over 3,000 Des Poilus A C ur Pass meters in height. Taken from I o ER Balf GLA DES POILUS the Cree word meaning awe CIE R Yoho Balfour and wonder, Yoho is filled with Peak breathtaking vistas. Twin Falls McArthur Isolated Size: 1,310 sq km (507 sq mi) Laughing WAPUTIK Peak Falls To JASPER ass ICEFIELD Amiskwi P NATIONAL iver I oho R DALY PARK C Y E ttle GLACIER i F Emergency telephone: 911 L Niles I Kiwetinok 4 E Left-hand turns L The President EMERALD TAKAKKAW on the Trans- D Telephone: 250-343-6783 S O GLACIER 5 FALLS Canada Highway tto River are permitted at P C A r signed intersec- R TTY: 1-866-787-6221 ee Emeral ass Paget 93 k Carnarvon Peak tions only. K B Sherbrooke W as ho PWapta in o Lake A Hamilton d Y 1 Y Horsey Lake EMERALD Ogden Kicking Burges Ross 7 LAKE Horse LAKE P Lake LOUISE a Field Wapta d Pass n ss a Amiskwi Emer 3 Lake o To Ban Hamilto s 3 R Falls (85 km from 2 e Spike Peak ook Narao r r al Field) and T i ocher Ridge B F d Peak KOOTENAY Burgess River a NATIONAL r Stephen act R PARK O iv 1 t e FIELD Cathedral te r r Catar Victoria he 2 O'Ha e t ad 6 V R Lak Abboss a iv Pa n Ho er Lefroy Dennis Duchesnay r Lake BANFF ne Rang Odaray O'Hara NATIONAL Opab PARK r P e e 1 YOHO o King v Lake Hungabee rc i in u R NATIONAL p McArthur P in e e s a ass r PARK Park ss P o Owen k Biddle e H e nkchemna r e g C W n O R i t r i k te u v c r e i ta h r t Hunter K il Riv r Hurd er A c KOOTENAY F I E L D M NATIONAL - CANAD PARK TRANS A HIG HWAY Ottertail km To Golden Vaux - 57 (57 km from Field) and Falls en Y r old 1 MOUNTB REVELSTOKE HANBUR i Goodsir k G anf s f e Ball AND GLA- 8CIER GLACIER d Pass d 5 Mt.
    [Show full text]
  • Article Is Available On- Anderson, E
    Hydrol. Earth Syst. Sci., 25, 2513–2541, 2021 https://doi.org/10.5194/hess-25-2513-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. The spatial extent of hydrological and landscape changes across the mountains and prairies of Canada in the Mackenzie and Nelson River basins based on data from a warm-season time window Paul H. Whitfield1,2,3, Philip D. A. Kraaijenbrink4, Kevin R. Shook1, and John W. Pomeroy1 1Centre for Hydrology, University of Saskatchewan, Saskatoon, SK, S7N 1K2, Canada 2Department of Earth Sciences, Simon Fraser University, Burnaby, BC, Canada 3Environment and Climate Change Canada, Vancouver, BC, Canada 4Geosciences, Utrecht University, Utrecht, the Netherlands Correspondence: Paul H. Whitfield (paul.h.whitfi[email protected]) Received: 24 November 2020 – Discussion started: 4 January 2021 Revised: 30 March 2021 – Accepted: 8 April 2021 – Published: 18 May 2021 Abstract. East of the Continental Divide in the cold inte- separating the Canadian Rockies and other mountain ranges rior of Western Canada, the Mackenzie and Nelson River in the west from the poorly defined drainage basins in the basins have some of the world’s most extreme and variable east and north. Three specific areas of change were iden- climates, and the warming climate is changing the landscape, tified: (i) in the mountains and cold taiga-covered subarc- vegetation, cryosphere, and hydrology. Available data consist tic, streamflow and greenness were increasing while wetness of streamflow records from a large number (395) of natu- and snowcover were decreasing, (ii) in the forested Boreal ral (unmanaged) gauged basins, where flow may be peren- Plains, particularly in the mountainous west, streamflows nial or temporary, collected either year-round or during only and greenness were decreasing but wetness and snowcover the warm season, for a different series of years between were not changing, and (iii) in the semi-arid to sub-humid 1910 and 2012.
    [Show full text]
  • The Amazing Race How Does Agriculture Make Regions Unique?
    Learning Sources PROJECT Agriculture Project-Based Learning and Teaching Series The Amazing Race How does agriculture make regions unique? www.albertamilk.com/teacher-resources/ PROJECT Agriculture Learning Source: The Amazing Race 1 ©Alberta Milk 2017 Permission is granted to make copies of any or all parts of this resource for educational, not-for-profit use only. Readers should be aware that Internet websites offered as citations and/or sources for further information may have changed or disappeared between the time this was written and when it is read. Teachers are cautioned that all websites listed in this resource should be checked for appropriateness and suitability before being provided to, or used with, students. Every effort has been made to acknowledge sources used in the PROJECT Agriculture resources. In the event of questions arising as to the use of any material, we will be pleased to make the necessary corrections in future printings. Please contact Patricia Shields-Ramsay at InPraxis Learning at 780.421.7163. This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License. To view a copy of this license, visit http:// creativecommons.org/licenses/by-nc-sa/4.0/ or send a letter to Creative Commons, PO Box 1866, Mountain View, CA 94042, USA. 2 PROJECT Agriculture Learning Source: The Amazing Race Learning Source: The Amazing Race Cross Country Canada How do geographers define a region? Regions are areas that share common characteristics. They are identified by the natural features or geographic characteristics that an area shares. Regions are often named by the main physical or geographic feature.
    [Show full text]