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Waputik Mountains
The Waputik Mountains are a mountain range of the Canadian Rockies, located on the Continental Divide of the Americas, Continental Divide between Banff National Park, Banff and Yoho National Park. Covering an area of , the range is located west of the Howse River, Howse, Blaeberry River, Blaeberry and Amiskwi Rivers and east of the Bow River, Bow and Mistaya Rivers and south to Kicking Horse Pass. Named in 1884 by George Mercer Dawson, George M. Dawson, "waputik" is the Nakoda (Stoney), Stoney Indian word for Mountain goat, white goat. Many of the highest peaks of the range are heavily glaciated as they sit within the Waputik Icefield, Waputik and Wapta Icefields. The range is further divided into the President Range and Waputik Range This range includes the following mountains and peaks: See also * Ranges of the Canadian Rockies References

Mountain ranges of Alberta Mountain ranges of British Columbia Ranges of the Canadian Rockies Ranges of the Rocky Mountains Al ...
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Canada
Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by total area. Its southern and western border with the United States, stretching , is the world's longest binational land border. Canada's capital is Ottawa, and its three largest metropolitan areas are Toronto, Montreal, and Vancouver. Indigenous peoples have continuously inhabited what is now Canada for thousands of years. Beginning in the 16th century, British and French expeditions explored and later settled along the Atlantic coast. As a consequence of various armed conflicts, France ceded nearly all of its colonies in North America in 1763. In 1867, with the union of three British North American colonies through Confederation, Canada was formed as a federal dominion of four provinces. This began an accretion of provinces an ...
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George Mercer Dawson
George Mercer Dawson (August 1, 1849 – March 2, 1901) was a Canadian geologist and surveyor. Biography He was born in Pictou, Nova Scotia, the eldest son of Sir John William Dawson, Principal of McGill University and a noted geologist, and his wife, Lady Margaret Dawson. By age 11, he was afflicted with tuberculosis of the spine ( Pott's disease) that resulted in a deformed back and stunted growth. Physical limitations, however, did not deter Dawson from becoming one of Canada's greatest scientists. Tutors and his father provided his education during his slow recovery from the illness. Dawson later attended the High School of Montreal and McGill University (part-time) before moving to London to study geology and paleontology at the Royal School of Mines (now part of Imperial College London) in 1869. Dawson graduated after three years with the highest marks in his class. Dawson began his career in the 1870s as a professor of chemistry at Morrin College in Quebec City ...
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Mount Sarbach
Mount Sarbach is a mountain located in Banff National Park between Mistaya River and Howse River and is visible from the Icefields Parkway. The mountain is named after Peter Sarbach, a mountain guide from Switzerland, who guided the first ascent by J. Norman Collie and G.P. Baker in 1897. Mount Sarbach is situated south of Saskatchewan River Crossing, where the Icefields Parkway intersects with the David Thompson Highway. __NOTOC__ Geology Like other mountains in Banff Park, Mount Sarbach 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. A glacier shared with Kaufmann Peaks resides in the southeast cirque. Climate Based on the Köppen climate classification, Mount Sarbach 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 ...
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Mont Des Poilus
Mont des Poilus is a mountain summit located in Yoho National Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Mount Baker, to the north. Both are part of the Waputik Mountains. History It was named by Arthur Wheeler one week following the armistice which ended World War I to honor the Poilu, the common soldiers of the French Army. The first ascent of Mont des Poilus was made 1901 by James Outram, Edward Whymper, guided by C. Kaufmann, C. Klucker and J. Pollinger. The mountain's name became official in 1924 when approved by the Geographical Names Board of Canada. Geology Mont des Poilus is composed of sedimentary rock laid down during the Cambrian period. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. The Glacier des Poilus lies on the east aspect of the peak, and is part of the larger Waputik Icefield. Climate Based on the Köppen climate classification, Mo ...
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Mount Gordon (Waputik Range)
Mount Gordon is a mountain summit located immediately west of the Continental Divide, in the Waputik Range of the Canadian Rockies in British Columbia, Canada. It is a glaciated dome situated in Yoho National Park, and is the highest point of the Wapta Icefield. Its nearest higher peak is Mount Baker, to the northwest. History The first ascent of the mountain was made in August 1897 by George Percival Baker, J. Norman Collie, H. B. Dixon, Charles Ernest Fay, Arthur Michael, C. L. Noyes, H. C. Parker, and Charles Sproull Thompson, with Peter Sarbach as guide. The mountain was named in 1897 by Charles Sproull Thompson of the first ascent party for John Hamilton-Gordon, 1st Marquess of Aberdeen and Temair, at the time Governor General of Canada from 1893 to 1898. After descending from the summit of Mount Gordon, Thompson fell into a crevasse and became lodged which required rescue by the team. Mount Thompson, six kilometres to the north of Mount Gordon, was one of several peaks ...
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Mount Baker (Waputik Mountains)
Mount Baker is a mountain on the Continental Divide, in Alberta and British Columbia, in the Waputik Mountains of the Canadian Rockies. It was named in 1898 by J. Norman Collie after his friend and climbing partner George Percival Baker (1855–1951), textile manufacturer, plantsman and gardener, and keen mountaineer. Baker described his visit to this area which took place in 1897.Mountaineering memories of the past. Privately printed 1951 In this small volume Baker noted that Collie also proposed to name a pass after him. Collie and Baker were accompanied by Peter Sarbach, and for the first week by H. B. Dixon as well as American members of the Appalachian Mountain Club. Mount Sarbach was named at the same time, as well as several other peaks: "We now named the peaks, after presidents of the Club of our time, Freshfield, Dent, Pilkington, and Walker." The mountain has been wrongly identified as "Stremotch Mountain" on subsequent maps and documents after a first map that was sub ...
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Mount Chephren
Mount Chephren is a mountain located in the Mistaya River Valley of Banff National Park, Canada. Mount Chephren was named after Chephren, the 4th Dynasty Egyptian pharaoh. The mountain was originally named Pyramid Mountain in 1897 by J. Norman Collie, but it conflicted with an identically named peak in Jasper National Park, so it was renamed in 1924 to its present name. Routes Scramble Mount Chephren is rated a difficult scramble on the south face due to its steep upper slopes with possible snow and ice difficulties. Considerable snow on the route would likely require crampons and an ice axe, thereby pushing the climb into the realm of technical mountaineering. The best conditions for scrambling would normally be late July and August. The trail head is located at the west end of the Waterfowl Lakes campground off the Icefields Parkway in Banff National Park. The elevation gain from the trail head to the summit is . Technical There are three main routes: * South Face/West Rid ...
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Mount Balfour
Mount Balfour is a mountain located on the Continental Divide, part of the border between British Columbia and Alberta, in the Waputik Range in the Park Ranges of the Canadian Rockies.It is the 71st highest peak in Alberta and the 113th highest in British Columbia; it is also the 52nd most prominent in Alberta. The mountain was named by James Hector in 1859 after Professor John Hutton Balfour, a Scottish botanist and instructor at the University of Edinburgh where Hector had studied. Climbing History Early attempts to climb the mountain were made from Niles Pass via Sherbrooke Lake. The first ascent was made on August 18, 1898 by C.L. Noyes, C.S. Thompson, G.M. Weed; members of the Appalachian Mountain Club. The party started their ascent from Hector Lake which they had reached by crossing Dolomite Pass to Bow Lake and then continuing south. C.E. Fay had also attempted the mountain in 1898 via the Sherbrooke Lake/Niles Pass approach but were eventually turned back by p ...
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White Pyramid (Banff)
White Pyramid is a mountain summit located between the Howse River valley and Mistaya River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Howse Peak, to the south. Topographic relief is significant as the summit rises 1,460 meters (4,790 ft) above Chephren Lake in 2.5 km (1.5 mile). White Pyramid is visible from the Icefields Parkway in the vicinity of Waterfowl Lakes. History It was named in 1901 by J. Norman Collie to distinguish it from Mount Chephren, which back then was named Pyramid Mountain. The two peaks are nearly the same in height, and separated by only one kilometre. However, White Pyramid has a glacier on its north aspect, which Chephren does not. The first ascent of White Pyramid was made in 1939 by Kate (Katie) Gardiner and guide Edward Feuz Jr. The climbing duo made many first ascents in the Canadian Rockies during the 1930s. The mountain's name was made official in 1961 when approved by the G ...
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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 * ...
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President Range
The President Range is a mountain range of the Canadian Rockies, located in the northwestern section of Yoho National Park. The range is named for the highest peak in the range, The President (mountain), The President. This range includes the following mountains and peaks: References

* Ranges of the Canadian Rockies Mountain ranges of British Columbia {{BritishColumbiaInterior-geo-stub ...
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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 ...
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