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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 Icefie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banff National Park
Banff National Park is Canada's oldest National Parks of Canada, national park, established in 1885 as Rocky Mountains Park. Located in Alberta's Rockies, Alberta's Rocky Mountains, west of Calgary, Banff encompasses of mountainous terrain, with many glaciers and ice fields, dense pinophyta, coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, Alberta, Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, Alberta, Banff, in the Bow River valley. The Canadian Pacific Railway was instrumental in Banff's early years, building the Banff Springs Hotel and Chateau Lake Louise, and attracting tourists through extensive advertising. In the early 20th century, roads were built in Banff, at times by war internees from Wor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caldron Peak
Caldron Peak is a mountain peak of the Waputik Range, located in Alberta, Canada. It is prominently visible from the Peyto Lake Overlook in Banff National Park. It was named after Caldron Lake which is from its summit. __NOTOC__ Geology Like other mountains in Banff Park, Caldron Peak 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, Caldron Peak 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 Caldron Peak Peak drains into the Mistaya River which is a tributary of the North Saskatchewan River The North Saskatchewan River is a glacier-fed river that flows from the Canadian Rockies continental divide east to central Saskatchewan, where it j ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1 Peyto Lake Pano 2019
1 (one, unit, unity) is a number representing a single or the only entity. 1 is also a numerical digit and represents a single unit of counting or measurement. For example, a line segment of ''unit length'' is a line segment of length 1. In conventions of sign where zero is considered neither positive nor negative, 1 is the first and smallest positive integer. It is also sometimes considered the first of the infinite sequence of natural numbers, followed by 2, although by other definitions 1 is the second natural number, following 0. The fundamental mathematical property of 1 is to be a multiplicative identity, meaning that any number multiplied by 1 equals the same number. Most if not all properties of 1 can be deduced from this. In advanced mathematics, a multiplicative identity is often denoted 1, even if it is not a number. 1 is by convention not considered a prime number; this was not universally accepted until the mid-20th century. Additionally, 1 is the s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wapta Icefield
The Wapta Icefield is located on the Continental Divide in the Waputik Mountains of the Canadian Rockies, in the provinces of British Columbia and Alberta. The icefield is shared by Banff and Yoho National Parks and numerous outlet glaciers extend from the icefield, including the Vulture, Bow and Peyto Glaciers. Runoff from the icefields and outlet glaciers supply water to both the Kicking Horse and Bow Rivers, as well as numerous streams and lakes. The icefield is one of the most studied in the Canadian Rockies and all evidence supports the conclusion that the icefield is shrinking in area, especially near the lowest altitudes of its outlet glaciers, including Peyto Glacier, in which the glacier has become both shorter in length and thinner in thickness. In the 1980s the icefield covered an area of approximately . The icefield is easily accessible by mountaineers in both the summer and winter. Both ski trips in the winter and glacier hiking trips in the summer often combine a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peyto Glacier
__NOTOC__ The Peyto Glacier is situated in the Canadian Rockies in Banff National Park, Alberta, Canada, approximately northwest of the town of Banff, and can be accessed from the Icefields Parkway. Geography Peyto Glacier is an outflow glacier from the Wapta Icefield, which rests along the Continental divide. The glacier snout is subject to high melt rates from season to season and there is marked surface lowering on several parts of the glacier. Glacial silt, which is carried from the glacier by streams, ensures a turquoise appearance to Peyto Lake, a popular touring destination. As is true for the vast majority of glaciers worldwide, Peyto Glacier has been retreating rapidly, especially since the last half of the 20th century, and has reportedly lost 70% of its mass since it was first researched (Demuth and Keller, 2006). Between 1896 and 1966, the total volume loss of the Peyto Glacier was 1088.5 x 106 m3 (Wallace, 1995). A 1896's photograph by Walter D. Wilcox was the fi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Parks Canada
Parks Canada (PC; french: Parcs Canada),Parks Canada is the applied title under the Federal Identity Program; the legal title is Parks Canada Agency (). is the agency of the Government of Canada which manages the country's 48 National Parks, three National Marine Conservation Areas, 172 National Historic Sites, one National Urban Park, and one National Landmark. Parks Canada is mandated to "protect and present nationally significant examples of Canada's natural and cultural heritage, and foster public understanding, appreciation, and enjoyment in ways that ensure their ecological and commemorative integrity for present and future generations". The agency also administers lands and waters set aside as potential national parklands, including 10 National Park Reserves and one National Marine Conservation Area Reserve. More than of lands and waters in national parks and national marine conservation areas has been set aside for such purposes. Parks Canada cooperatively manages a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock Flour
Rock flour, or glacial flour, consists of fine-grained, silt-sized particles of rock, generated by mechanical grinding of bedrock by glacial erosion or by artificial grinding to a similar size. Because the material is very small, it becomes suspended in meltwater making the water appear cloudy, which is sometimes known as glacial milk. When the sediments enter a river, they turn the river's colour grey, light brown, iridescent blue-green, or milky white. If the river flows into a glacial lake, the lake may appear turquoise in colour as a result. When flows of the flour are extensive, a distinct layer of a different colour flows into the lake and begins to dissipate and settle as the flow extends from the increase in water flow from the glacier during snow melts and heavy rain periods. Examples of this phenomenon may be seen at Lake Pukaki and Lake Tekapo in New Zealand, Lake Louise, Moraine Lake, Emerald Lake, and Peyto Lake in Canada, Gjende lake in Norway, and several lakes ( ... [...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 Peak
Peyto Peak is a mountain in the Waputik Range, part of the Canadian Rockies in Alberta, Canada. It lies at the north end of the Wapta Icefield, in Banff National Park, about one km (0.6 mi) east of the border with British Columbia and north of the town of Field. Five kilometres to the northeast lies Bow Pass, one of the high points of the Icefields Parkway. Between the peak and the pass lies picturesque Peyto Lake. Three kilometres southwest of Peyto Peak is Mount Baker, the highest point in the immediate vicinity. History Peyto Peak was named in 1896 by Walter Wilcox for Ebenezer William "Bill" Peyto, an early outfitter, trail guide and trapper in the Banff and Lake Louise areas. The first ascent of the peak was in 1933 by famed mountaineer Conrad Kain and party. The mountain's name became official in 1928 by the Geographical Names Board of Canada. Geology Like other mountains in Banff Park, Peyto Peak is composed of sedimentary rock laid down during the Precambrian to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waputik Range
The Waputik Range lies west of the upper Bow Valley, east of Bath Creek, and south of Balfour Creek in the Canadian Rockies. "Waputik" means "white goat" in Stoney. The range was named in 1884 by George Mercer Dawson of the Geological Survey of Canada. The President Range lies within the Waputik Range. The Waputik Range should not be confused with the much larger Waputik Mountains which encompasses this range and other peaks along the Continental Divide in Yoho National Park. Peaks * Howse Peak , highest in the Waputik Mountains * Mount Balfour 3272m * Mount Patterson 3191m * Mount Baker 3180m * Mont des Poilus 3166m * Mount Gordon 3161m * The President 3123m * Caldron Peak 2909m * Wapta Mountain Wapta Mountain is a mountain located in the Canadian Rockies between Emerald Lake and Yoho Valley in Yoho National Park, British Columbia, Canada. It stands just north of the ridge containing the Burgess Shale fossil beds. Along with The Vice Pres ... 2782m * Waputik Peak 2755m * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alberta
Alberta ( ) is one of the thirteen provinces and territories of Canada. It is part of Western Canada and is one of the three prairie provinces. Alberta is bordered by British Columbia to the west, Saskatchewan to the east, the Northwest Territories (NWT) to the north, and the U.S. state of Montana to the south. It is one of the only two landlocked provinces in Canada (Saskatchewan being the other). The eastern part of the province is occupied by the Great Plains, while the western part borders the Rocky Mountains. The province has a predominantly continental climate but experiences quick temperature changes due to air aridity. Seasonal temperature swings are less pronounced in western Alberta due to occasional Chinook winds. Alberta is the fourth largest province by area at , and the fourth most populous, being home to 4,262,635 people. Alberta's capital is Edmonton, while Calgary is its largest city. The two are Alberta's largest census metropolitan areas. More tha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bill Peyto
Ebenezer William Peyto ( ; 14 February 1869 – 23 March 1943) was an English-Canadian pioneer, mountain guide, and early park warden of Banff National Park. Life and career Peyto was born in Welling, Kent in 1869 and immigrated to Canada, settling in Calgary in February 1887. He found his way to the Canadian Rocky Mountains where he initially worked as a railway labourer. By the mid-1890s Peyto had built a small log cabin close to the Bow River where he kept his outfitting and trapping gear. Peyto eventually found work as a mountain guide under Tom Wilson, and led early expeditions to attempt to climb Mount Assiniboine, including once with James Outram in the 1890s. He was also chosen to lead Edward Whymper to Vermilion Pass. Peyto enlisted to serve in Lord Strathcona's Horse Regiment during the Boer War in 1899, and during World War I in Belgium and France with the Twelfth Mounted Regiment and Machine Gun Brigade. He was wounded in his right leg at the Battle of Ypres. Peyt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
