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Mount Assiniboine Park Management Plan Part of the Canadian Rocky Mountain Parks World Heritage Site November 2012 Cover Page Photo Credit: Christian Kimber (Park Ranger) This document replaces the direction provided in the Mount Assiniboine Provincial Park Master Plan (1989). Mount Assiniboine Park Management Plan Approved by: November 15, 2012 ______________________________ __________________ Tom Bell Date Regional Director, Kootenay Okanagan Region BC Parks November 15, 2012 ______________________________ __________________ Brian Bawtinheimer Date Executive Director, Parks Planning and Management Branch BC Parks Plan Highlights The management vision for Mount Assiniboine Park is that the park continues to be an international symbol of the pristine scenic grandeur of British Columbia’s wilderness and the recreational enjoyment it offers. Key elements of the management plan include strategies to: Implement a zoning plan that enhances the emphasis on Mount Assiniboine Park’s value both as a component of a UNESCO World Heritage Site (which protects significant examples of Canadian Rocky Mountain ecosystems) and as the location of an internationally recognized wilderness recreation feature associated with heritage structures from the earliest days of facility-based backcountry tourism in the Canadian Rockies. Approximately 86% of the park is zoned as Wilderness Recreation, 13% is zoned as Nature Recreation, less than 1% is zoned as Special Feature and less than 0.01% is zoned as Intensive Recreation. Develop an ecosystem management strategy that coordinates management of vegetation and wildlife in the park with that of adjacent protected areas under other agencies’ jurisdiction and with activities on adjacent provincial forest lands. This includes a proposal to prepare a vegetation management strategy to maintain or restore natural disturbance regimes (i.e., insects, disease and fire) wherever possible. -
CANADA's MOUNTAIN Rocky Mountain Goats
CANADA'S MOUNTAIN Rocky Mountain Goats CANADA'S MOUNTAIN PLAYGROUNDS BANFF • JASPER • WATERTON LAKES • YOHO KOOTENAY ° GLACIER • MOUNT REVELSTOKE The National Parks of Canada ANADA'S NATIONAL PARKS are areas The National Parks of Canada may, for C of outstanding beauty and interest that purposes of description, be grouped in three have been set apart by the Federal Govern main divisions—the scenic and recreational ment for public use. They were established parks in the mountains of Western Canada; the to maintain the primitive beauty of the land scenic, recreational, wild animals, and historic scape, to conserve the native wildlife of the parks of the Prairie Provinces; and the scenic, country, and to preserve sites of national his recreational, and historic parks of Eastern Can toric interest. As recreational areas they pro ada. In these pages will be found descriptions vide ideal surroundings for the enjoyment of of the national parks in the first group—areas outdoor life, and now rank among Canada's which lie within the great mountain regions outstanding tourist attractions. of Alberta and British Columbia. Canada's National Park system teas estab * * * lished in 1SS5, when a small area surrounding mineral hot springs at Banff in the Rocky This publication is compiled in co-operation Mountains was reserved as a public posses with the National Parks Branch, Department sion. From this beginning has been developed of Northern Affairs and National Resources. the great chain of national playgrounds note Additional information concerning these parks stretching across Canada from the Selkirk may be obtained from the Park Superintend Mountains in British Columbia to the Atlantic ents, or from the Canadian Government Travel Coast of Nova Scotia. -
Glacier Fluctuations in the Canadian Rockies
GLACIER FLUCTUATIONS IN THE CANADIAN ROCKIES Calvin J. HEUSSER Department of Exploration ann Field Hesl'an'h .\Ilh'ri{'H II (;t'ographi{'al Soeiel:-" :\"t' W York. :\"t>w York Synopsis Through the use of survey and botanieal teehniques. reeent gladPI' fluctuations ill the Canadian Ho(:kies were measured and dated. Twelve gladers in nritish Columbia Hn<1 Alberta were studied between the )Iount Hobson area in the northwest and the vicinity of Kicking Horse Pass in the southeast. Two of them. Rob~ol\ and Yoho (;laeiers. are on the western slopes; ten, Angel, Columbia, Dome, Atha basku, unnamed at the head of Hilda Creek, Saskatchewan, Southeast LyeJJ , Fresh field, Peyto, and How Glaeiers drain on the east. Some of these flow from the salll(, i(,e field: ::<onw from independent nev<'~s, a])(1 some are merely hanging iee masses. (;laeier advun(,es arc dated from iee-tilted trees. glaeier retreat from the age of trees that have beeOlne established on reeessional'moraines. Re(,ords of this study show that glaeiers attained maxima and receded between the late seventeenth and late nineteenth eenturies. Bow Glaeier reeeded as e~lI'ly as lG7H; six glaciers receded frolll maxima in the eighteenth century and five withdrew during t.he nineteenth eentury. These data eompare with results of similar studies elsewhere in British Columbia, in Oregon, and in Alaska. Ko evidence of major twentieth ('entur~' ad Vt\lH'P was oiJservpd as is known for certain ('oastal Aluskan glaciers. Introduction Thb paper constitutes a report or the 19,,8 field work on twelve gill<'iers draining the northeast and southwest slopes of the Hocky Mountains in Alberta a.nd British Columhia, Dominion of Canada. -
Role of the Protected Area Provincial and Regional Context
Role of the Protected Area Provincial and Regional Context Height of the Rockies and Elk Lakes provincial parks lie in southeastern British Columbia in the Rocky Mountains, about 85 km southwest of Calgary, Alberta. They are flanked to the East by the Elk Valley and the Kananaskis Valley and to the West by the Park Ranges. The mountain ranges of the Kootenay District provide a wide diversity of natural values and recreation opportunities as evidenced by the numerous national and provincial parks in the District (Fig. 2). Over 16% of the land base in the East Kootenays is in protected areas. · Height of the Rockies and Elk Lakes provincial parks are a significant part of BC's system of protected areas. In conjunction with Banff National Park and Peter Lougheed Provincial Park in Alberta, they form a large, contiguous protected area that is rich in natural, recreational and cultural values. Also, these parks are critical links in the Yellowstone to Yukon Conservation Initiative (Y2Y)1. · The combined size of these two provincial parks contributes to the protection of biodiversity in the region and is integral to the conservation of wildlife populations, plant communities and biodiversity. · These parks offer a wide range of top caliber wilderness recreation opportunities and outstanding features. Plate 2 : Fish fossil in Elk Lakes Provincial Park 1 Proposal by Canada and U.S. conservation groups to create a thread of ecological connectivity linking protected areas in both countries from Yellowstone National Park to the Yukon. 11 Significance in the Protected Areas System Height of the Rockies and Elk Lakes provincial parks are a significant part of BC's system of protected areas. -
Banff to Jasper Bike Tour the 290 Kilometre (180 Mile) Bike Point
Banff to Jasper bike tour the 290 kilometre (180 mile) bike point. Continuing north descend to Saskatchewan e best time to do this bike tour is tour between Banff and Jasper is Crossing, where three rivers converge, and then climb in July and August but June and Sep - considered to be one of the most impressive to the Columbia Icefields, known for chilly tempera - tember are possible if the weather cooper - mountain rides in the world. e ride runs tures even in the middle of summer. is is where you ates. Fickle weather is the norm in the parallel to the Continental Divide, and can can take a motorized tour onto the glacier. mountains so come prepared for four seasons start in either Banff or Jasper, both of which are at any time. You might find snow patches at the exceptionally scenic towns. Mountain ride means North of the Columbia Icefield you’ll see Sunwapta top of some passes even in the summer. riding by mountains and not over them. Only 55 Mountain and the Endless Chain Ridge. e rest of kilometres from Banff is Lake Louise, considered to the bike tour takes you alongside the Sunwapta and e Banff Jasper corridor is easily accessible via Cal - be the hiking capital of Canada. If time isn’t of the Athabasca Rivers into Jasper. gary only 125 kilometres (80 miles) away to the east. essence then stay longer and explore. In particular, Edmonton is also a possibility though it’s 360 kilo - Lake Agnes and the Plain of Six Glaciers aren’t far e ride takes place entirely on the Parkway, a highway metres (215 miles) from Jasper. -
The Columbia Ice-Field
THE COLUMBIA ICE-FIELD THE COLUMBIA ICE-FIELD Department of Resources and Development Development Services Branch National Parks and Historic Sites Service Ottawa, Canada Athabasca Glacier—Columbia Ice-field showing Snow Dome in background. Jasper National Park, Alberta The Columbia Ice-field The Columbia Ice-field, centre of the greatest known accumulation of ice in the Rocky Mountains, is not only one of the most interesting ice-fields in North America, but certainly one of the most accessible. Near the Banff-Jasper Highway, it lies astride the British Columbia- Alberta boundary and at the dividing line between Banff and Jasper National Parks. With its outlet glaciers, the Columbia Ice-field covers an area of nearly 130 square miles, of which fully 50 square miles are more than 8,500 feet above sea level in the area of accumulation, usually called the "neve". From the great central ice reservoir, lying between Snow Dome, Mount Castleguard, and Mount Columbia and capping the Continental Divide for a distance of about 20 miles, three valleys radiate outward. Through them flow the Athabasca Glacier to the northeast, the Saskatchewan to the east, and the Columbia to the northwest. From other points smaller ice tongues flow into the surrounding valleys, and in a number of places ice tumbles over precipices to form reconstructed glaciers such as Dome Glacier at the head of Habel Creek, and the northward flowing glacier between Mounts Columbia and King Edward. The Columbia Ice-field is the source of three great rivers — the 765-mile Athabasca, a sub-tributary of the Mackenzie River, which flows into the Arctic Ocean; the Saskatchewan (1,205 miles) which crosses the Prairies and empties into Lake Winnipeg and, via the Nelson River, into Hudson Bay; and the Columbia (1,210 miles) which cascades its way through scenic gorges, crossing into the U.S.A before entering the Pacific Ocean. -
Island Bushwhacker Annual 2009
THE ALPINE CLUB OF CANADA VANCOUVER ISLAND SECTION ISLAND BUSHWHACKER ANNUAL VOLUME 37, 2009 VANCOUVER ISLAND SECTION of THE ALPINE CLUB OF CANADA SECTION EXECUTIVE – 2009 Chair Cedric Zala Secretary Rick Hudson Treasurer Geoff Bennett Banff Mountain Film Festival Lissa Zala Kari Frazer Bushwhacker Committee Sandy Briggs Lindsay Elms Rob Macdonald Russ Moir Bushwhacker Design & Layout Sandy Stewart Education Peter Rothermel Dave Campbell Equipment Mike Hubbard FMCBC Rep John Young Library/Archivist Judith Holm Membership Jain Alcock-White Members at Large Phee Hudson Russ Moir Mike Morley Dave Campbell National Rep Russ Moir Newsletter Cedric Zala Safety Selena Swets Schedule Karun Thanjavur Webmaster/Listserver Martin Hofmann ACC VI Section website: www.accvi.ca ACC National website: www.alpineclubofcanada.ca ISSN 0822 - 9473 Cover: Looking east from Springer Peak to Johnstone Strait, June 2009. PHOTO: DAVE CAMPBELL Printed on recycled paper Contents Message from the Chair Cedric Zala ..............................................................................................................................................................................................1 VANCOUVER ISLAND Colonel Foster – On a Sunny Summer’s Day Christine Fordham ............................................................................................3 Mount Phillips from Arnica Lakes Dave Campbell ....................................................................................................................4 Victoria Peak: First Winter Ascent -
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 -
JASPER from POINTS of INTEREST from Banff Jasper (Read Up) (Read Down) and BANFF - JASPER 184.5 "JASPER TOWNSITE (3,472')
Miles Miles THE BANFF-JASPER from POINTS OF INTEREST from Banff Jasper (read up) (read down) AND BANFF - JASPER 184.5 "JASPER TOWNSITE (3,472'). Headquarters, 0.0 Jasper National Park. Information Bureau, outdoor heated swimming pool, tennis courts, hotels, bungalows, camp COLUMBIA ICE-FIELD ground. Miette Hot Springs, 38 mi. 183.9 JUNCTION with road to Athabasca River, 0.6 HIGHWAY Old Fort Point and Lac Beauvert Loop, and 2 mi. 183.5 BUNGALOWS. 1.0 183.4 MIETTE RIVER. Confluence with Athabasca 1.1 River. Scenic beyond adequate description, this spectacular high 182.8 BUNGALOWS. 1.7 way ranks among the great "highroads" of the world. For 180.3 WHISTLERS CREEK. Bungalows. 4.2 its entire length of 185 miles it commands some of the most 178.2 PORTAL CREEK. 6.3 breath-taking and majestic scenery in the Canadian Rockies. A panorama of mountain ranges, unbroken but ever-changing, Columbia Ice-Field 176.3 *ASTORIA RIVER, drains Amethyst Lakes. 8.2 along both sides of this highway keeps the visitor enchanted 176.2 JUNCTION, MT. EDITH CAVELL ROAD. 8.3 and enthralled. Arrow signs along the road point to features Angel Glacier, 9 mi. Tea Room. 7| mi. to of special interest, many of which are listed in this publica start of Trail to Tonquin Valley. 8 mi. to tion. Canadian Youth Hostel Unit. 171.2 CONFLUENCE, Whirlpool and Athabasca 13.3 Rivers. Brook trout. At places the Banff-Jasper Highway reaches a height of nearly 7,000 feet above sea-level. Many of the mountains visible in 170.6 VALLEY OF CROOKED TREES. -
Grizzly Bear Population Dynamics Across Productivity and Human Influence Gradients
Grizzly bear population dynamics across productivity and human influence gradients by Clayton T. Lamb A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Ecology Department of Biological Sciences University of Alberta © Clayton T. Lamb, 2019 Abstract Coexistence with large carnivores is one of the greatest conservation challenges across the globe, in part because mechanisms of coexistence are unknown or contested. Large carnivores can be conflict-prone and pose real or perceived threats to human life and property. In North America, grizzly bears (Ursus arctos) typify the struggle to conserve and coexist with large carnivores amongst a matrix of competing land uses. Grizzly bears are a symbol of wildness to society, but the management of this species can divide communities, derail collaborative conservation initiatives, and are the focus of high-profile media coverage and lawsuits. At the center of this controversy is scientific uncertainty around population dynamics of the species, primarily relating to population size, limiting factors, and the ecology of conflict. The contemporary threats of wilderness loss, human population expansion, and climate change pose both a no-analog future for grizzly bears, but also opportunity. Leveraging novel ecological tools, and the ongoing human-induced landscape and climate change, considerable opportunity exists to investigate the mechanisms driving grizzly bear population dynamics and those promoting coexistence—enduring populations of wildlife in human-dominated landscapes. The goal of this dissertation was to test the factors limiting grizzly bear population dynamics across ecosystems, update local population estimates, and to identify the mechanisms promoting carnivore coexistence and those exacerbating it. -
Accommodations
14_837292 bindex.qxp 1/5/06 8:45 PM Page 261 Index See also Accommodations and Restaurant indexes below. GENERAL INDEX driving tours, 73-83 frontcountry camping, 29, 129–134 highlights, 61–63 ccommodations. See A information and reservations, 20–21, Accommodations index 24–25 Adventure outings, 38–40 nightlife, 142–143 Airplane tours, 231 organized tours, 38–39, 83–85 Air travel, 30 rules and regulations, 54–56 Alpine Club of Canada, 24, 73, 110, visitor centers, 53–54 125, 135–136, 205–206 winter sports, 9, 61–62, 113–117 Amethyst Lake, 18, 187 Banff Park Radio, 52 Angel Glacier, 13, 44 Banff Summer Arts Festival, 8, 70 Arnica Lake, 59 Banff Townsite, 61, 62, 67–68, 70–73 Athabasca Falls, 159 Banff Transit, 63 Athabasca Glacier, 157 Bankhead, 7, 73, 86, 90 Athabasca River, 167–168 Banks/ATMs, 56, 151 Beauty Creek, 179 Beehives, 95 ackcountry, 28–29, 33–36, 66, B Birdwatching, 74–75, 224, 257–259 102–107, 185–188 Boating permits, 29 Backpacking, 6–7, 14, 34–35, Books, 24–25 102–104 Boom Lake, 92–93 Bald Hills, 13, 171, 182 Bourgeau Lake, 5, 93 Banff Centre, 38, 49, 61, 70 Bow Falls, 62, 68 Banff Centre for Mountain Culture, Bow Glacier Falls, 99 49, 70 Bow Lake, 66, 70, 82, 99 Banff Festival of the Arts, 61 Bow Pass, 82 Banff Festival of Mountain Films, 61 Bow River, 62, 70 Banff Gondola, 59, 71 Bow Summit, 66, 101 Banff Information Centre, 58, 64, Bow Valley Parkway, 59, 62, 64, 74, 67, 85 92–94 Banff/Lake Louise Tourism Centre, 24 Brazeau Loop, 159, 185 Banff Mountain Film Festival, 8, Brazeau Valley, 100 70–71 Buffalo National Luxton Museum, 71 Banff Mountain Norquay, 114 Burgess Shale, 229–230 Banff National Park Bus travel, 31, 211 access/entry points, 52–53 COPYRIGHTEDaccommodations, 18–19, 118–129 MATERIAL backcountry, 10, 29, 102–107, -Level Cirque, 86 134–137 C Campgrounds, 10, 17–18, 59, 67, day hikes. -
Jasper National Park
Jasper Cover: Maligne Lake Ice bridge on Athabasca Glacier Rocky Mountain sheep A park naturalist explains the wonders of nature Introducing a park and an idea Some of the more common shrubs in the park are wild Canada covers half a continent, fronts on three oceans rose, buffalo berry, willow, alder, juniper, shrubby cinque- and stretches from the extreme Arctic more than halfway foil, silverberry, saskatoon berry, Labrador tea, red osier National Park dogwood and bearberry. to the equator. There is a great variety of landforms in this immense country, and Canada's national parks have been created to preserve important examples for you and The animals: each seeks its own habitat for generations to come. Animals, like plantlife, depend on suitable environment The National Parks Act of 1930 specifies that national for their survival. The mountain goat, marmot and pika parks are "dedicated to the people . for their benefit, usually inhabit the higher regions. Mountain sheep and education and enjoyment" and must remain "unimpaired elk are seen on the lower slopes, while the moose, mule for the enjoyment of future generations." deer, beaver and muskrat stay near the valley bottom. Jasper National Park, 4,200 square miles in area and In winter, animals which do not hibernate move to one of the largest parks on the North American continent, snow-free slopes or into the valleys, where food is more Alberta is notable for its magnificent mountain scenery and unique plentiful. natural wonders - relics of the Ice Age. Other mammals, such as the lynx, coyote, porcupine, The park is situated some 235 miles west of Edmonton black and grizzly bear, wolverine, marten and badger also and 258 miles northwest of Calgary.