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Waputik Icefield
The Waputik Icefield is located 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 40 km2 (15 miles²) and is located 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 icefiel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Skiing Up The Waputik To Mt Balfour; Doug&Vic
Skiing is the use of skis to glide on snow. Variations of purpose include basic transport, a recreational activity, or a competitive winter sport. Many types of competitive skiing events are recognized by the International Olympic Committee (IOC), and the International Ski Federation (FIS). History Skiing has a history of almost five millennia. Although modern skiing has evolved from beginnings in Scandinavia, it may have been practiced more than 100 centuries ago in what is now China, according to an interpretation of ancient paintings. However, this continues to be debated. The word "ski" comes from the Old Norse word "skíð" which means to "split piece of wood or firewood". Asymmetrical skis were used in northern Finland and Sweden until at least the late 19th century. On one foot, the skier wore a long straight non-arching ski for sliding, and a shorter ski was worn on the other foot for kicking. The underside of the short ski was either plain or covered with animal s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Takakkaw Falls
Takakkaw Falls (; also spelled Takkakaw) is a waterfall located in Yoho National Park, near Field, British Columbia in Canada. The falls have a total height of , making them the second tallest waterfall in Canada. The main drop of the waterfall has a height of . "Takakkaw" translates to "magnificent” in Cree. The falls are fed by the meltwater of the Daly Glacier, which is part of the Waputik Icefield. The glacier keeps the volume of the falls up during the warm summer months, and they are a tourist attraction, particularly in late spring after the heavy snow melts, when the falls are at peak condition. Height Various sources place the total vertical height of Takakkaw Falls between and . The waterfall was formerly thought to be the tallest in Canada, but a new survey in 1985 found that it is actually shorter than Della Falls on Vancouver Island. The results of that survey also concluded that the main drop of the falls is high. In popular culture The Takakkaw Falls were fe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Fields Of British Columbia
Ice is water frozen into a solid state, typically forming at or below temperatures of 0 degrees Celsius or Depending on the presence of impurities such as particles of soil or bubbles of air, it can appear transparent or a more or less opaque bluish-white color. In the Solar System, ice is abundant and occurs naturally from as close to the Sun as Mercury to as far away as the Oort cloud objects. Beyond the Solar System, it occurs as interstellar ice. It is abundant on Earth's surfaceparticularly in the polar regions and above the snow lineand, as a common form of precipitation and deposition, plays a key role in Earth's water cycle and climate. It falls as snowflakes and hail or occurs as frost, icicles or ice spikes and aggregates from snow as glaciers and ice sheets. Ice exhibits at least eighteen phases ( packing geometries), depending on temperature and pressure. When water is cooled rapidly (quenching), up to three types of amorphous ice can form depending on its hist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Fields Of Alberta
Ice is water frozen into a solid state, typically forming at or below temperatures of 0 degrees Celsius or Depending on the presence of impurities such as particles of soil or bubbles of air, it can appear transparent or a more or less opaque bluish-white color. In the Solar System, ice is abundant and occurs naturally from as close to the Sun as Mercury to as far away as the Oort cloud objects. Beyond the Solar System, it occurs as interstellar ice. It is abundant on Earth's surfaceparticularly in the polar regions and above the snow lineand, as a common form of precipitation and deposition, plays a key role in Earth's water cycle and climate. It falls as snowflakes and hail or occurs as frost, icicles or ice spikes and aggregates from snow as glaciers and ice sheets. Ice exhibits at least eighteen phases ( packing geometries), depending on temperature and pressure. When water is cooled rapidly (quenching), up to three types of amorphous ice can form depending on its hist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Glaciers
A glacier ( ) or () is a persistent body of dense ice that is constantly moving under its own weight; it forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries. Glaciers slowly deform and flow due to stresses induced by their weight, creating crevasses, seracs, and other distinguishing features. Because glacial mass is affected by long-term climate changes, e.g., precipitation, mean temperature, and cloud cover, glacial mass changes are considered among the most sensitive indicators of climate change. There are about 198,000 to 200,000 glaciers in the world. Glaciers by continent Africa Africa, specifically East Africa, has contained glacial regions, possibly as far back as the last glacier maximum 10 to 15 thousand years ago. Seasonal snow does exist on the highest peaks of East Africa as well as in the Drakensberg Range of South Africa, the Stormberg Mountains, and the Atlas Mountains in Morocco. Currently, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Balfour Hut
The R.J. Ritchie Hut (Balfour Hut) is an alpine hut located at an altitude of between the southern tip of the Wapta Icefield and the northern tip of the Waputik Icefield in Banff National Park. The hut is at the half-way mark for the Wapta traverse and is usually used in conjunction with the other huts in this chain while attempting a cross-glacier ski trip. The hut is maintained by the Alpine Club of Canada. The hut sleeps 18 in the summer and 16 in the winter. It is equipped with propane-powered lamps and stovetop. The hut requires approximately three to five hours of glacier travel to get to from the Bow Hut, or six to eight hours from the Scott Duncan Hut. Location The hut is found on low, rocky hills at the toe of the Vulture Glacier. It is east of Balfour Pass and the continental divide, just inside the boundary of Banff National Park.} History The original Balfour Hut, a fibreglass igloo built in 1965 at Balfour Pass in Banff National Park, was the first hut on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scott Duncan Hut
The Waputik Icefield is located 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 40 km2 (15 miles²) and is located 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 icefiel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Club Of Canada
The Alpine Club of Canada (ACC) is an amateur athletic association with its national office in Canmore, Alberta that has been a focal point for Canadian mountaineering since its founding in 1906. The club was co-founded by Arthur Oliver Wheeler, who served as its first president, and Elizabeth Parker, a journalist for the '' Manitoba Free Press''. Byron Harmon, whose 6500+ photographs of the Canadian Rockies in the early 20th century provide the best glimpse of the area at that time, was official photographer to the club at its founding. The club is the leading organization in Canada devoted to climbing, mountain culture, and issues related to alpine pursuits and ecology. It is also the Canadian regulatory organization for climbing competition, sanctioning local, regional and national events, and assembling, coaching and supporting the national team. The ACC is divided into 24 regional sections across Canada that serve local members and focus on local issues and access, linkin ... [...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] |
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] |
Lake Louise (Alberta)
Lake Louise (named Ho-run-num-nay (Lake of the Little Fishes) by the Stoney Nakota First Nations people) is a glacial lake within Banff National Park in Alberta, Canada. It is located west of the Hamlet of Lake Louise and the Trans-Canada Highway The Trans-Canada Highway ( French: ; abbreviated as the TCH or T-Can) is a transcontinental federal–provincial highway system that travels through all ten provinces of Canada, from the Pacific Ocean on the west coast to the Atlantic Ocean o ... (Alberta Highway 1, Highway 1). Lake Louise is named after the Princess Louise, Duchess of Argyll, Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Victoria of the United Kingdom, Queen Victoria and the wife of the John Campbell, 9th Duke of Argyll, Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The turquoise colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yoho River
The Yoho River is a silty, swift tributary of the Kicking Horse River in the Canadian province of British Columbia. The river is entirely within Yoho National Park. Course The Yoho River originates at the north end of Yoho National Park and flows generally south to join the Kicking Horse River some distance northeast of Field. It begins at the toe of the Yoho Glacier and flows within from its source it has already received the waters of Waves Creek, Twin Falls Creek, Fairy Creek & the Little Yoho River. It continues south for another to its confluence with the stream Takakkaw Falls Takakkaw Falls (; also spelled Takkakaw) is a waterfall located in Yoho National Park, near Field, British Columbia in Canada. The falls have a total height of , making them the second tallest waterfall in Canada. The main drop of the waterfall h ... is on. Along that stretch is a significant canyon in which the river drops over at least one major waterfall. The river also picks up the waters ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
