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Valley Of The Ten Peaks
Valley of the Ten Peaks (french: Vallée des Dix Pics) is a valley in Banff National Park in Alberta, Canada, which is crowned by ten notable peaks and also includes Moraine Lake. The valley can be reached by following the Moraine Lake road near Lake Louise. The ten peaks were originally named by Samuel Allen, an early explorer of the region, who simply referred to them by using the numerals from one to ten in the Stoney First Nations Language. He may have learned the terms from his Native American guides, who helped him with the horses. The Nakoda–also known as the Stoney Indians–is a tribe whose culture and dialect are closely related to that of the Assiniboine First Nation, from whom they are believed to have separated in the mid-1700s, and who roamed large parts of the prairies and mountains of western Alberta well into British Columbia. The secluded Valley of the Ten Peaks was part of their original homeland. Gradually, though, all but three of the mountains were rename ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moraine Lake
Moraine Lake is a glacially fed lake in Banff National Park, outside the hamlet of Lake Louise, Alberta, Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately . The lake has a surface area of . The lake, being glacially fed, does not reach its crest until middle to late June. When it is full, it reflects a distinctive shade of azure blue. The unique colour is due to the refraction of light off the rock flour deposited in the lake on a continual basis by surrounding glaciers. Tourism Hiking trails The area around the lake has several walking/hiking trails that are, from time to time, restricted. The trail most commonly taken by tourists is The Rockpile Trail, which is along the actual moraine. The trail is approximately long, with an elevation change of . The view of the lake from the top of the rockpile is one of the most photographed locations in all of Canada. That view of the mountains behind the lake in Valley of the Ten Peaks is known ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Allen (Canada)
Mount Allen is a mountain in the Canadian Rockies, located on the Continental Divide, which forms the provincial boundary between British Columbia and Alberta in this region. J. Monroe Thorington named this mountain for Samuel Evans Stokes Allen in 1924. Allen was an American cartographer who mapped this area of the Rockies in 1894-95. Allen had named this mountain "Shappee", the Stoney language word for "six", as part of his naming of the ten mountains in the Valley of the Ten Peaks. The peak forms part of the backdrop to Moraine Lake in Banff National Park. Geology The mountains in Banff Park are 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, the mountain has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20&nbs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bank Of Canada
The Bank of Canada (BoC; french: Banque du Canada) is a Crown corporation and Canada's central bank. Chartered in 1934 under the ''Bank of Canada Act'', it is responsible for formulating Canada's monetary policy,OECD. OECD Economic Surveys: Canada 2000'. OECD Publishing; 30 August 2000. . p. 45–. and for the promotion of a safe and sound financial system within Canada.Financial Stability and Central Banks: A Global Perspective'. Routledge; November 2002. . p. 41–. The Bank of Canada is the sole issuing authority of Canadian banknotes,Gene Swimmer. How Ottawa Spends, 1996-97: Life Under the Knife'. MQUP; 15 May 1996. . p. 379–. provides banking services and money management for the government, and loans money to Canadian financial institutions. The contract to produce the banknotes has been held by the Canadian Bank Note Company since 1935. The Bank of Canada headquarters are located at the Bank of Canada Building, 234 Wellington Street in Ottawa, Ontario. The building als ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neil Colgan Hut
The Neil Colgan Hut is an alpine hut located at an altitude of on the Fay Glacier in Kootenay National Park in British Columbia, Canada. It is in a col between Mount Little and Mount Bowlen, one of the peaks overlooking the Valley of the Ten Peaks. The hut is maintained by the Alpine Club of Canada and is the highest permanent structure in Canada. It is named for hiker and adventurer Neil M. Colgan (1953–1979). The hut can accommodate 18 in the summer and 16 in the winter and is equipped with propane-powered lamps and a stovetop. There is one outdoor drum toilet at the facility. Reaching the hut from Fay Hut requires approximately 4 to 6 hours of glacier travel, or 8 to 12 hours climbing the Perren Route from Moraine Lake Moraine Lake is a glacially fed lake in Banff National Park, outside the hamlet of Lake Louise, Alberta, Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately . The lake has a surface area of . The lake ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canadian Twenty Dollar Bill
The Canadian $20 note is one of the most common banknotes of the Canadian dollar; it is the primary banknote dispensed from Canadian automatic teller machines (ATMs). The newest version, the Frontier Series polymer note, was released to the general public on November 7, 2012, replacing the banknote from the Canadian Journey Series. Present note The present $20 banknote was first issued on November 7, 2012. It is a polymer-based note featuring Queen Elizabeth II on the face and the Vimy Ridge memorial on the back. The window displays the Peace Tower. On January 18, 2013, a Canadian botanist complained that a foreign maple leaf was used as the emblem on the polymer notes instead of the sugar maple that the country has on its national flag, along with the $50 and $100 notes. After the death of Elizabeth II, the banknotes with her image will continue to be legal tender. It is undecided whether they will be replaced in circulation with notes bearing an image of her successor Cha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eiffel Peak
Eiffel Peak is a mountain summit in Banff National Park in Alberta, Canada. It's part of the Bow Range, which is a sub-range of the Canadian Rockies. The nearest higher peak is Mount Temple (Alberta), Mount Temple, to the northeast. History The first ascent was made in 1901 by Charles S. Thompson and G.M. Weed, with Hans Kaufmann as guide. The peak was named in 1908 by Arthur O. Wheeler on account of its great height; its name is an allusion to the Eiffel Tower. The mountain's name was made official in 1952 by the Geographical Names Board of Canada. Geology Eiffel 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, Eiffel Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill fact ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Babel (Alberta)
Mount Babel is a mountain peak of the Bow Range in Banff National Park, Alberta, Canada. The mountain can be seen from the Valley of the Ten Peaks. Mount Babel was first climbed by A Hart, Edward Oliver Wheeler, L. Wilson and H. Worsfold in 1910. Geology Like other mountains in Banff Park, Mount Babel 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, Mount Babel 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. Tower of Babel The Tower of Babel is a conspicuous quartzite monolith at the northern end of the mountain, and is apparent to park visitors at Moraine Lake. It was named in 1899 by Walter D. Wilcox because its profile reminded him of the biblical Tower ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Temple (Alberta)
Mount Temple is a mountain in Banff National Park of the Canadian Rockies of Alberta, Canada. Mt. Temple is located in the Bow River Valley between Paradise Creek and Moraine Creek and is the highest peak in the Lake Louise area. The peak dominates the western landscape along the Trans-Canada Highway from Castle Junction to Lake Louise. History The mountain was named by George Mercer Dawson in 1884 after Sir Richard Temple who visited the Canadian Rockies that same year. Mt. Temple was the first peak to be climbed in the Canadian segment of the Rocky Mountains. Tragedy * On July 11, 1955, in one of Canada's most tragic mountaineering accidents, seven American male teenagers were killed on the southwest ridge route. A warm summer day had caused several nearby avalanches. They finally decided to turn back and during the descent, an avalanche swept 10 members of the party down the snowfield through a bottleneck of rocks. Unfortunately, the entire party only had one ice axe a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wenkchemna Peak
Wenkchemna Peak is located on the border of Alberta and British Columbia. It was named in 1894 by Samuel E. S. Allen. Wenkchemna is the 10th peak in The Valley of the Ten Peaks, as they are normally numbered (left to right as seen from Moraine Lake). It is an extension into the valley of the ridge formed by Mount Hungabee and Ringrose Peaks. Geology Wenkchemna 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, Wenkchemna Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. See also * List of peaks on the Alberta–British Columbia border * Mountains of Alberta * Mountains of British Columbia Further reading * Brian Patton, Bart Robinson, 'Walks ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neptuak Mountain
Neptuak Mountain was named by Samuel E.S. Allen in 1894. "Neptuak" is the Stoney Indian word for "nine" as Neptuak Mountain is peak #9 in the Valley of the Ten Peaks. It is located on the Continental Divide, which is also the British Columbia-Alberta border in this region, and is in the Bow Range of the Park Ranges of the Canadian Rockies. The summit is a tripoint for Banff National Park, Kootenay National Park, and Yoho National Park, where the three parks share a common border. Geology Like other mountains in Banff Park, Neptuak 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, Neptuak 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deltaform Mountain
Deltaform Mountain is one of the mountains in the Valley of the Ten Peaks, located on the Continental Divide on the border of British Columbia and Alberta, and also on the border between Banff and Kootenay National Parks in Canada. The mountain was originally named Saknowa by Samuel Allen but Walter Wilcox named it to its official title in 1897 as it resembles the Greek letter delta. Deltaform was first climbed in 1903 by August Eggers and Herschel Clifford Parker who were guided by Christian and Hans Kaufmann. __NOTOC__ Climbing routes The two main climbing routes are: * North-West Ridge (Normal Route) II 5.5 * North Face, The Supercouloir IV 5.8 Geology Deltaform 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, Deltaform is located in a subarctic c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Tuzo
Mount Tuzo, previously "Peak Seven" or "Shagowa", was named in 1907 after its first ascendant Henrietta L. Tuzo. It is located within the Valley of the Ten Peaks in the Canadian Rockies, along the Continental Divide, which forms the boundary between British Columbia and Alberta in this region. __NOTOC__ Geology Like other mountains in Banff Park, Mount Tuzo is composed of sedimentary rock laid down from 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, Mount Tuzo is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C. See also * List of peaks on the Alberta–British Columbia border This is a list of peaks on the Alberta–British Columbia border, being the spine of the Continental Divide from the Canada–Unite ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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