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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 language, 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 of the Americas, Continental Divide in Yoho National Park. Peaks * Howse Peak , highest in the Waputik Mountains * Mount Balfour 3272m * Mount Patterson 3191m * Mount Baker (Waputik Mountains), Mount Baker 3180m * Mont des Poilus 3166m * Mount Gordon (Waputik Range), Mount Gordon 3161m * The President (mountain), The President 3123m * Caldron Peak 2909m * Wapta Mountain 2782m * Waputik Peak 2755m * Pulpit Peak 2720m Gallery References Ranges of the Canadian Rockies Mountain ranges of Alberta Mountain ... [...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] |
Yoho National Park
Yoho National Park ( ) is a national park of Canada. It is located within the Rocky Mountains along the western slope of the Continental Divide of the Americas in southeastern British Columbia, bordered by Kootenay National Park to the south and Banff National Park to the east in Alberta. The word ''Yoho'' is a Cree expression of amazement or awe, and it is an apt description for the park's spectacular landscape of massive ice fields and mountain peaks, which rank among the highest in the Canadian Rockies. Yoho covers , the smallest of the region's four contiguous national parks, which also include Jasper, Kootenay, and Banff National Parks, as well as three British Columbia provincial parks— Hamber Provincial Park, Mount Assiniboine Provincial Park, and Mount Robson Provincial Park. Together, these parks form the Canadian Rocky Mountain Parks World Heritage Site. Yoho's administrative and visitor centre is located in Field, British Columbia, beside the Trans-Canada High ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Alberta
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ranges Of The Canadian Rockies
The Canadian Rockies are a segment of the North American Rocky Mountains found in the Canadian provinces of Alberta and British Columbia. List of ranges There is no universally accepted hierarchical division of the Canadian Rockies into subranges. For ease of navigation only, this article follows and divides the Canadian Rockies into Far Northern Rockies, Northern Continental Ranges, Central Main Ranges, Central Front Ranges and Southern Continental Ranges, each of these subdivided in distinct areas and ranges. From north to south and west to east, these mountain ranges are: Far Northern Rockies The Far Northern Rockies lie in British Columbia, and run from Prince George almost to the Yukon border. * Muskwa Ranges ** Akie Range ** Battle of Britain Range ** Deserters Range ** Gataga Ranges ** Rabbit Plateau ** Sentinel Range ** Stone Range ** Terminal Range ** Tochieka Range ** Tower of London Range ** Truncate Range * Hart Ranges ** Misinchinka Ranges (from Pe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pulpit Peak
Pulpit Peak is a mountain summit located one km south of Hector Lake in Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Lilliput Mountain, to the southwest. Pulpit Peak is situated east of the Waputik Icefield, and is a member of the Waputik Mountains. Pulpit Peak can be seen from the Icefields Parkway towering above Hector Lake. History Pulpit Peak was named in 1898 by Charles Sproull Thompson (1869-1921), who participated in numerous first ascents in the Canadian Rockies. He believed the peak resembled a pulpit in a church. The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada. Geology Like other mountains in Banff Park, Pulpit 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 classificatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waputik Peak
__NOTOC__ Waputik Peak was named by George Mercer Dawson in 1884. It is located in the Waputik Range in Alberta. "Waputik" means "white goat" in the Stoney language. Geology Like other mountains in Banff Park, Waputik 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, Waputik Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures in winter can drop below −20 °C with wind chill factors below −30 °C. See also *Geology of Alberta *Geography of Alberta Alberta is one of the thirteen provinces and territories of Canada. Located in Western Canada, the province has an area of and is bounded to the south by the United States state of Montana along 49° north for ; to the east at 110° west by t ... References ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 The Burgess Shale is a fossil-bearing deposit exposed in the Canadian Rockies of British Columbia, Canada. It is famous for the exceptional preservation of the soft parts of its fossils. At old (middle Cambrian), it is one of the earliest fos ... fossil beds. Along with The Vice President and Mount Burgess, Wapta Mountain forms the backdrop to Emerald Lake, and marks the southern end of the President Range. In 1901, James Outram, J. H. Scattergood, and their guide C. Bohren, became the first people to ascend Wapta Mountain. Wapta Mountain overlooks Takakkaw Falls (1,247 feet), the second tallest waterfall in western Canada. The word "Wapta" means "river" in the Stoney language. References {{Reflist, refs= {{cite bivouac , id=1655 , name=Wapta Mountain, a ... [...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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The President (mountain)
The President is a mountain peak on ''The President/Vice-President Massif'' of the President Range, in eastern British Columbia. It is just north of Emerald Lake in Yoho National Park, near the Alpine Club of Canada's Stanley Mitchell hut. History The President was named ''Shaugnessy'' in 1904 by Edward Whymper after Thomas Shaugnessy, the president of the Canadian Pacific Railway. In 1907, the mountain was renamed by the Alpine Club of Canada, after it was discovered that the name had already been used on a mountain in the Selkirks. Climate Based on the Köppen climate classification The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, nota ..., The President is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 peak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Edward Whymper FRSE (27 April 184016 September 1911) was an English mountaineer, explorer, illustrator, and author best known for the first ascent of the Matterhorn in 1865. Four members of his climbing party were killed during the descent. Wh ..., guided by C. Kaufmann, Christian Klucker, 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 sha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 su ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
