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Bow Lake (Alberta)
Bow Lake is a small lake in western Alberta, Canada. It is located on the Bow River, in the Canadian Rockies, at an altitude of 1920 m. The lake lies south of the Bow Summit, east of the Waputik Range (views including Wapta Icefield, Bow Glacier, Bow Peak, Mount Thompson, Crowfoot Glacier and Crowfoot Mountain) and west of the Dolomite Pass, Dolomite Peak and Cirque Peak. Bow Lake is one of the lakes that line the Icefields Parkway in Banff National Park and Jasper National Park, other such lakes being Hector Lake, Lake Louise, Peyto Lake, ''Mistaya Lake'', ''Waterfowl Lakes'', ''Chephren Lake'' and ''Sunwapta Lake''. Historical Simpson's Num-Ti-Jah Lodge is located on the shores of Bow Lake at the foot of Mount Jimmy Simpson.Tim Whyte Bow Lake is the closest lake to the headwaters of Bow River, and has a total area of 3.21 km2. Water in the lake is meltwater of the Bow Glacier and its turquoise colouring is due to glacial till. Image gallery See also *Lakes of Alb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crowfoot Glacier
__NOTOC__ Crowfoot Glacier is located in Banff National Park, Alberta, Canada, northwest of Lake Louise, and can be viewed from the Icefields Parkway. The glacier is situated on the northeastern flank of Crowfoot Mountain. Geography Crowfoot Glacier is east of the continental divide, and runoff from the glacier supplies water to the Bow River. The glacier has retreated since the end of the Little Ice Age The Little Ice Age (LIA) was a period of regional cooling, particularly pronounced in the North Atlantic region. It was not a true ice age of global extent. The term was introduced into scientific literature by François E. Matthes in 1939. Ma ... and now has lost one entire lobe; it therefore no longer resembles the glacier which early explorers named. The glacier was measured to be . The Crowfoot glacier was once connected to the Wapta Icefield, and in the 1980s and was considered to be part of a smaller icefield of 5 km2 (1.9 mi2). See also * List ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Icefields Parkway
Highway 93 is a north–south highway in Alberta, Canada. It is also known as the Banff-Windermere Parkway south of the Trans-Canada Highway ( Highway 1) and the Icefields Parkway north of the Trans-Canada Highway. It travels through Banff National Park and Jasper National Park and is maintained by Parks Canada for its entire length. It runs from the British Columbia border at Vermilion Pass in the south, where it becomes British Columbia Highway 93, to its terminus at the junction with the Yellowhead Highway ( Highway 16) at Jasper. The route takes its number from U.S. Route 93, which runs uninterrupted south to central Arizona, and was initially designated as '93' in 1959. Route description Banff-Windermere Highway The southern portion of the route is part of the Banff-Windermere Highway, a highway that travels from British Columbia Highway 95 at Radium Hot Springs, through Kootenay National Park and Vermilion Pass across the Continental Divide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lakes Of Alberta
This is a list of lakes in Alberta, Canada. Most of Alberta's lakes were formed during the last glaciation, about 12,000 years ago. There are many different types of lakes in Alberta, from glacial lakes in the Canadian Rockies to small shallow lakes in the prairies, brown water lakes in the northern boreal forest and muskeg, kettle holes and large lakes with sandy beaches and clear water in the central plains. Distribution of the lakes throughout the province of Alberta is irregular, with many water bodies in the wet boreal plains in the north, and very few in the semi-arid Palliser's Triangle in the southeast. __TOC__ River basins Most of Alberta's waters are drained in a general north or northeastern direction, with six major rivers forming four major watersheds collecting the water and removing it from the province: [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alberta Highway 93
Highway 93 is a north–south highway in Alberta, Canada. It is also known as the Banff-Windermere Parkway south of the Trans-Canada Highway ( Highway 1) and the Icefields Parkway north of the Trans-Canada Highway. It travels through Banff National Park and Jasper National Park and is maintained by Parks Canada for its entire length. It runs from the British Columbia border at Vermilion Pass in the south, where it becomes British Columbia Highway 93, to its terminus at the junction with the Yellowhead Highway ( Highway 16) at Jasper. The route takes its number from U.S. Route 93, which runs uninterrupted south to central Arizona, and was initially designated as '93' in 1959. Route description Banff-Windermere Highway The southern portion of the route is part of the Banff-Windermere Highway, a highway that travels from British Columbia Highway 95 at Radium Hot Springs, through Kootenay National Park and Vermilion Pass across the Continental Divid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crowfoot Mountain (Alberta)
Crowfoot Mountain is a mountain within Banff National Park in Alberta, Canada. The Crowfoot Glacier sits on the northeastern flank of the mountain. The mountain was named in 1959 after the glacier. Geology Like other mountains in Banff Park, Crowfoot Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate Based on the Köppen climate classification, Crowfoot Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from Crowfoot Mountain drains into the Bow River which is a tributary of the Saskatchewan River. File:Bow_Lake_beim_Icefields_Parkway.jpg, Crowfoot Mountain near Bow Lake File:Crowfoot Mountain, Banff National Park - panoramio.jpg, Crowfoot Mountain File:Crowfoot Mountai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Till
image:Geschiebemergel.JPG, Closeup of glacial till. Note that the larger grains (pebbles and gravel) in the till are completely surrounded by the matrix of finer material (silt and sand), and this characteristic, known as ''matrix support'', is diagnostic of till. image:Glacial till exposed in roadcut-750px.jpg, Glacial till with tufts of grass Till or glacial till is unsorted glacier, glacial sediment. Till is derived from the erosion and entrainment of material by the moving ice of a glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines. Till is classified into primary deposits, laid down directly by glaciers, and secondary deposits, reworked by fluvial transport and other processes. Description Till is a form of ''glacial drift'', which is rock material transported by a glacier and deposited directly from the ice or from running water emerging from the ice. It is distinguished from other forms of drift in that it is d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meltwater
Meltwater is water released by the melting of snow or ice, including glacial ice, tabular icebergs and ice shelves over oceans. Meltwater is often found in the ablation zone of glaciers, where the rate of snow cover is reducing. Meltwater can be produced during volcanic eruptions, in a similar way in which the more dangerous lahars form. When meltwater pools on the surface rather than flowing, it forms melt ponds. As the weather gets colder meltwater will often re-freeze. Meltwater can collect or melt under the ice's surface. These pools of water, known as subglacial lakes can form due to geothermal heat and friction. Water source Meltwater provides drinking water for a large proportion of the world's population, as well as providing water for irrigation and hydroelectric plants. This meltwater can originate from seasonal snowfall, or from the melting of more permanent glaciers. Climate change threatens the precipitation of snow and the shrinking volume of glaciers. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Jimmy Simpson
__NOTOC__ Mount Jimmy Simpson is a summit located northwest of Bow Lake in Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Thompson, to the southwest. Mount Jimmy Simpson is a member of the Waputik Mountains, and is situated east of the Wapta Icefield and west of the Bow River valley. Mount Jimmy Simpson can be seen from the Icefields Parkway at Bow Lake. ''Jimmy Simpson Junior'' is a 2,721 meter sub-summit east of the mountain. History Mount Jimmy Simpson is named for Jimmy Simpson (1877–1972) who was a respected outfitter in the early explorations of the Canadian Rockies. Jimmy worked as a cook for Tom Wilson and learned the guide and outfitting business from Bill Peyto. In 1902, while working for Peyto, he was given the responsibility of leading James Outram's climbing expedition into the headwaters of the North Saskatchewan River and Columbia Icefield. Jimmy built a small log cabin for use with his outfitting business ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peyto Lake
Peyto Lake ( ) is a glacier-fed lake in Banff National Park in the Canadian Rockies. The lake itself is near the Icefields Parkway. It was named for Bill Peyto, an early trail guide and trapper in the Banff area. The lake is formed in a valley of the Waputik Range, between Caldron Peak, Peyto Peak and Mount Jimmy Simpson, at an elevation of . During the summer, significant amounts of glacial rock flour flow into the lake from a nearby glacier, and these suspended rock particles are what give the lake a unique bright, turquoise colour. Because of its bright colour, photos of the lake often appear in illustrated books, and the area around the lake is a popular sightseeing spot. In 2021, Parks Canada completed improvements to the lake viewpoint, trails and parking areas. The lake is best seen from Bow Summit, the highest point on the Icefields Parkway. The lake is fed by Peyto Creek, which drains water from Caldron Lake and Peyto Glacier (part of the Wapta Icefield The Wapta Ic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Louise, Alberta
Lake Louise is a Hamlet (place)#Canada, hamlet within Banff National Park in Alberta, Canada. Named after Princess Louise, Duchess of Argyll, it lies in Alberta's Rockies on the Bow River, northeast of Lake Louise (Alberta), the lake that shares its name. Initially settled in 1884 as an outpost for the Canadian Pacific Railway, Lake Louise sits at an elevation of , making it Canada's highest community. The nearby lake, framed by mountains, is one of the most famous mountain vistas in the world; the famous Chateau Lake Louise also overlooks the lake. History Prior to the arrival of Europeans, Indigenous peoples in Canada, Indigenous peoples lived in Rocky Mountain Foothills, the foothills and forests of the Rocky Mountains - including what is today Lake Louise, where they hunted bison and other big game animals. In the Stoney language of the Nakoda people the area is called , meaning "lake of the little fishes". During the 1870s, the construction of the Canadian Pacific Railw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hector Lake
Hector Lake is a small glacial lake in western Alberta, Canada. It is located on the Bow River, in the Waputik Range of the Canadian Rockies. It is named after James Hector, a geologist and naturalist with the Palliser Expedition. The lake is formed in a valley of the Waputik Range, north of the Waputik Icefield, between Pulpit Peak, Mount Balfour, Crowfoot Mountain and Bow Peak. Hector Glacier and Mount Hector rise on the opposite side of the Bow River. Hector Lake is one of the lakes that line the Icefields Parkway in Banff National Park and Jasper National Park, other such lakes being Bow Lake, Lake Louise, Peyto Lake Peyto Lake ( ) is a glacier-fed lake in Banff National Park in the Canadian Rockies. The lake itself is near the Icefields Parkway. It was named for Bill Peyto, an early trail guide and trapper in the Banff area. The lake is formed in a valley of ..., ''Mistaya Lake'', ''Waterfowl Lakes'', ''Chephren Lake'' and ''Sunwapta Lake''. Hector Lake is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jasper National Park
Jasper National Park is a national park in Alberta, Canada. It is the largest national park within Alberta's Rocky Mountains spanning . It was established as a national park in 1930 and declared a UNESCO World Heritage Site in 1984. Its location is north of Banff National Park and west of Edmonton. The park contains the glaciers of the Columbia Icefield, springs, lakes, waterfalls and mountains. History First Nations The territory encompassed by what is now Jasper National Park has been inhabited since time immemorial by Nakoda, Cree, Secwépemc, and Dane-zaa peoples. Plainview projectile points have been found at the head of Jasper Lake, dating back to between 8000 and 7000 BCE. In the centuries between then and the establishment of the park, First Nations land use has fluctuated according to climatic variations over the long term, and according to cyclical patterns of ungulate population numbers, particularly elk, moose, mule deer, and occasionally caribou. S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
