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Waputik Mountains
The Waputik Mountains are a mountain range of the Canadian Rockies, located on the Continental Divide between Banff and Yoho National Park. Covering an area of , the range is located west of the Howse, Blaeberry and Amiskwi Rivers and east of the Bow and Mistaya Rivers and south to Kicking Horse Pass. Named in 1884 by George M. Dawson, "waputik" is the Stoney Indian word for white goat. Many of the highest peaks of the range are heavily glaciated as they sit within the Waputik and Wapta Icefields. The range is further divided into the President Range and 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 ... Mountains and Peaks This range includes the following mountains and peaks: References {{Canadian Rockies, state=collapsed Kootenay Land District< ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canada
Canada is a country in North America. Its Provinces and territories of Canada, ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, making it the world's List of countries and dependencies by area, second-largest country by total area, with the List of countries by length of coastline, world's longest coastline. Its Canada–United States border, border with the United States is the world's longest international land border. The country is characterized by a wide range of both Temperature in Canada, meteorologic and Geography of Canada, geological regions. With Population of Canada, a population of over 41million people, it has widely varying population densities, with the majority residing in List of the largest population centres in Canada, urban areas and large areas of the country being sparsely populated. Canada's capital is Ottawa and List of census metropolitan areas and agglomerations in Canada, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bow River
The headwaters of the Bow River in Alberta, Canada, start at the Bow Glacier and Bow Lake (Alberta), Bow Lake in Banff National Park in the Canadian Rockies, Canadian Rocky Mountains. The glacial stream that feeds Bow Lake (Alberta), Bow Lake has a mean elevation of 2310 metres above sea level (7578 feet above sea level). From there, the river winds through the Alberta foothills onto the prairies, where it meets the Oldman River, the two then forming the South Saskatchewan River. These waters ultimately flow through the Nelson River into Hudson Bay. The Bow River Basin is the most highly populated basin in Alberta, with over 1.6 million people living within the watershed. Major population centres along the Bow River, listed from upstream to downstream, include Lake Louise, Alberta, Lake Louise (population 1,004), Banff, Alberta, Banff (population 10,944), Canmore, Alberta, Canmore (population 17,200), Cochrane, Alberta, Cochrane (population 38,014), and Calgary (population 1,48 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 by the Geographical Names Board of Canada 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 a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 poo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
First Ascent
In mountaineering and climbing, a first ascent (abbreviated to FA in climbing guidebook, guide books), is the first successful documented climb to the top of a mountain or the top of a particular climbing route. Early 20th-century mountaineers and climbers focused on reaching the tops of iconic mountains (e.g. the eight-thousanders) and climbing routes (e.g. the great north faces of the Alps) by whatever means possible, often using considerable amounts of aid climbing, and/or with large expedition style support teams that laid "siege" to the climb. As all the key tops were summited, the manner in which each top was reached became important, particularly the ability to complete the ascent without artificial aid, which is called free climbing. In free climbing, the term first free ascent (abbreviated FFA) is used where a mountain or climbing route is ascended without any artificial aid (devices for climbing protection, protection in the event of a fall could be used as long as the ... [...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 Yoho National Park ( ) is a National Parks of Canada, national park of Canada. It is located within the Canadian Rockies, Rocky Mountains along the western slope of the Continental Divide of the Americas in southeastern British Columbia, bordere .... Mountains and Peaks Gallery References {{Canadian Rockies, state=collapsed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
President Range
The President Range is a mountain range of the Canadian Rockies, located in the northwestern section of Yoho National Park Yoho National Park ( ) is a National Parks of Canada, national park of Canada. It is located within the Canadian Rockies, Rocky Mountains along the western slope of the Continental Divide of the Americas in southeastern British Columbia, bordere .... The range is named for the highest peak in the range, The President. List of Mountains This range includes the following mountains: References Kootenay Land District {{BritishColumbiaInterior-mountain-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wapta Icefield
The Wapta Icefield is a series of glaciers located on the Continental Divide of the Americas, Continental Divide in the Waputik Mountains of the Canadian Rockies, in the provinces of British Columbia and Alberta, in Yoho National Park in the Canadian Rocky Mountains, Rockies. The icefield is shared by Banff National Park, Banff and Yoho National Parks and numerous outlet glaciers extend from the icefield, including the Vulture Glacier (Alberta, Canada), Vulture, Bow Glacier, Bow and Peyto Glaciers. Runoff from the icefields and outlet glaciers supply water to both the Kicking Horse River, Kicking Horse and Bow Rivers, as well as numerous streams and lakes. The icefield is one of the most studied in the Canadian Rockies. Currently, all evidence supports the conclusion that the icefield is shrinking in area, especially near the lowest altitudes of its outlet glaciers. This is including Peyto Glacier, as the glacier has become both shorter in length and thinner in thickness. In the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waputik Icefield
The Waputik Icefield is on the Continental divide in the Canadian Rocky Mountains, in the provinces of British Columbia and Alberta. It is developed on the heights of the Waputik Range in the Central Main Ranges. The icefield is shared by Banff and Yoho National Parks, and numerous outlet glaciers extend from the icefield. Runoff from the Waputik Icefield provides water for numerous lakes, streams and rivers including Hector Lake, and the Bow, Kicking Horse and Yoho Rivers. Runoff from the Daly Glacier feeds Takakkaw Falls. The icefield encompasses and is northwest of Lake Louise, on the west side of the Icefields Parkway. 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 traverse of this icefield with a trip across the Wapta Icefield directly to the north. Glaciers The following glaciers are part of this icefield: *Waputik Glacier *Diableret Glacier *Glac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Goat
The mountain goat (''Oreamnos americanus''), also known as the Rocky Mountain goat, is a cloven-footed mammal that is endemic to the remote and rugged mountainous areas of western North America. A subalpine to truly alpine species, it is a sure-footed climber commonly seen on sheer rock faces, near-vertical cliffs and icy passages. Mountain goats generally avoid venturing down into lower elevations—except during seasonal food shortages or during particularly bad weather—as the extreme elevation which they inhabit is their primary defense against predators such as black and brown bears, pumas and wolves. Despite its vernacular name and both genera being in the same subfamily (Caprinae), the mountain goat is not a member of '' Capra'', the genus that includes all true goats (such as the wild goat (''Capra aegagrus''), from which the domestic goat is derived); rather, it is more closely allied with the other bovids known as “goat-antelopes”, including the European cham ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nakoda (Stoney)
The Nakoda (also known as Stoney, , or Stoney Nakoda) are an Indigenous people in Western Canada and the United States. Their territory used to be large parts of what is now Alberta, Saskatchewan, and Montana, but their reserves are now in Alberta and in Saskatchewan, where they are rarely differentiated from the Assiniboine. They refer to themselves in their language as , meaning 'friend, ally'. The name ''Stoney'' was given to them by Anglophone explorers, because of their technique of using fire-heated rocks to boil broth in rawhide bowls. They are very closely related to the Assiniboine, who are also known as Stone Sioux (from ). The Nakoda First Nation in Alberta comprises three bands: Bearspaw, Chiniki, and Goodstoney. The Stoney were "excluded" from Banff National Park between 1890 and 1920. In 2010 they were officially "welcomed back". Nakoda groups The Nakoda are descendants of individual bands of the Assiniboine, from whom they spun out as an independent g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
