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Mary Barclay's Mountain
Mary Barclay's Mountain is a summit located in the Kananaskis Range of the Canadian Rockies of Alberta, Canada. Mary Barclay's Mountain can be seen from Highway 40 in Kananaskis Country. The mountain's nearest higher neighbor is Skogan Peak, to the west, and Mount Lorette is to the immediate southwest. __NOTOC__ History This summit honors Mary Belle Barclay (1912-1983), who founded the first of the Canadian Youth Hostels in 1933 at Bragg Creek near Calgary, Alberta. With her sister, Catherine, together they officially founded and registered the Canadian Youth Hostel Association in 1938. Geology Mary Barclay's 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, Mary Barclay's Mountain is located in a subarctic climate zone with cold, snowy winters, and m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kananaskis Range
The Kananaskis Range is a mountain range west of the Kananaskis River in the Canadian Rockies. Many of the peaks are named after ships and people involved in the Battle of Jutland The Battle of Jutland (german: Skagerrakschlacht, the Battle of the Skagerrak) was a naval battle fought between Britain's Royal Navy Grand Fleet, under Admiral John Jellicoe, 1st Earl Jellicoe, Sir John Jellicoe, and the Imperial German Navy .... Mount Bogart is named after D.B. Dowling. Bogart was his mother's maiden name and his middle name. D.B. Dowling surveyed the area in the early 1900s for the Geographical Society of Canada. Tower was named after Francis George Towers an early homesteader of the region. Mt McDougal another early homesteader Archie McDougal of Carstairs. Mts. Evans Thomas named after Thomas Oldham Evans an early homesteader. Peaks of this range include: References Ranges of the Canadian Rockies Mountain ranges of Alberta {{AlbertaRockies-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precambrian
The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. The Precambrian accounts for 88% of the Earth's geologic time. The Precambrian is an informal unit of geologic time, subdivided into three eons ( Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago ( Ga) to the beginning of the Cambrian Period, about million years ago ( Ma), when hard-shelled creatures first appeared in abundance. Overview Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian fossil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nakiska
Nakiska is a ski resort in western Canada, in the Kananaskis Country region of the province of Alberta. It is located from Calgary, west on Highway 1 (Trans-Canada Highway) and south on Highway 40 (Kananaskis Trail). "Nakiska" is a Cree word meaning "to meet" or "meeting place." Set on the east face of the southern end of Mount Allan, Nakiska has 64 trails with four chairlifts (3 high-speed quads and 1 double), 1 Reg Magic Carpet and 1 Monster Carpet) set up over an area of . The longest run has , from a top lift-served elevation of to the base at . Nakiska is owned by Resorts of the Canadian Rockies, which also owns the Fernie, Kimberley, Kicking Horse Mountain Resort, Mont Sainte Anne, and Stoneham ski resorts. History The site was selected in 1983 and opened for skiing in the fall of 1986, in preparation for the 1988 Winter Olympics. Pre-Olympic races on the North American Cup circuit (Nor-Am) were held in December 1986 and World Cup downhill and super G races were h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Baldy (Alberta)
Mount Baldy is a mountain located in the Kananaskis River valley alongside Highway 40 in the Canadian Rockies. During World War II, prisoners in a nearby internment camp were occasionally permitted to make the ascent of Mt. Baldy as long as they promised to return. A University of Calgary research centre now occupies the former location of the camp. Up until 1984, when it was given its current day official name, it was commonly referred to as Barrier Mountain, due to its proximity to Barrier Lake. Photos Image:Mt-Baldy-Alberta-south-and-west-peaks.jpg, South and west peaks from the summit of the north peak Image:Mt Baldy-Kananaskis.JPG, View from Barrier Lake Barrier Lake is a man made reservoir at the north end of Kananaskis Country in Alberta, Canada. Highway 40 runs between the lake and Mount Baldy, on the eastern shore. It is entirely located in the Bow Valley Provincial Park. Barrier Lake was ... Image:Barrier Lake Kananaskis Aerial.jpg, Towering over Barrier L ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barrier Lake
Barrier Lake is a man made reservoir at the north end of Kananaskis Country in Alberta, Canada. Highway 40 runs between the lake and Mount Baldy, on the eastern shore. It is entirely located in the Bow Valley Provincial Park. Barrier Lake was created for hydroelectric power generation on the Kananaskis River. The dam that impounds the lake is at the north end of the lake. The lake is also used for recreational activities, with hiking paths surrounding the lake (and cross-country skiing trails in the winter). A visitor centre is located on the eastern shore. - from Alberta Community Development
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Heart Mountain (Alberta)
Heart Mountain is a mountain located in the Bow River valley just south of Exshaw, Alberta, Exshaw, Alberta. The peak was named in 1957 for the heart shaped layer of limestone near the top. The summit can be reached by following the northwest ridge starting from the Heart Creek Trail. It is an easy scramble with one moderate step. Being in the front ranges and only an hour from Calgary, it sees many visitors year-round. A circuit route can be completed by following the ridge line as it circles left and then descends to Quaite Creek. See also * List of mountains of Canada References External links Two-thousanders of Alberta Alberta's Rockies {{AlbertaRockies-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains Of Canada
Most mountain peaks of Canada lie in the west, specifically in British Columbia, Alberta, and the Yukon. Mountains can be found all over British Columbia while those in Alberta are mainly situated on the eastern side of the Canadian Rockies. The Saint Elias Mountains in the Yukon hold some of country's highest mountains, including the highest, Mount Logan at . Alberta ;Highest peaks Mts. Columbia & King Edward.jpg, Mount Columbia & King Edward in background The Twins - South and North (l-r).jpg, The Twins massif - South Twin and North Twin (l-r) Mount Assiniboine massif.jpg, Mount Assiniboine seen from above Lake Magog Columbia Icefields - panoramio (1).jpg, Snow Dome seen from Icefields Parkway British Columbia Mount Assiniboine.jpg, Mount Assiniboine Mount Robson South.jpg, Mount Robson, highest in Canadian Rockies Garibaldi black tusk.jpg, The Black Tusk Snow Dome+Dome Glacier.jpg, Snow Dome and Dome Glacier Mount Mackenzie from Mount Revelstoke NP.jpg, Mou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alberta's Rockies
Alberta's Rockies comprise the Canadian Rocky Mountains in Alberta, Canada. On the southwestern part of the province along the British Columbia border, the region covers all but the south of Census Division 15. The main industry in this region is tourism. Geography This human region is almost identical to the Alberta Mountain forests ecozone. The region contains the Central Front Ranges and the Continental Ranges of the Canadian Rocky Mountains, and includes the Banff National Park and Jasper National Park, as well as the Kananaskis Country park system and the Willmore Wilderness. The main transportation corridors run through the Kicking Horse Pass and the Yellowhead Pass from east to west, while the Bow Valley and Athabasca River valley are followed by the longitudinal Icefields Parkway. Another important waterway that crosses this region is the North Saskatchewan River. Tourism Some of the best ski resorts of the Rockies are located in this region, and are important tou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bow River
The Bow River is a river in Alberta, Canada. It begins within the Canadian Rocky Mountains and 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 runs through the city of Calgary, taking in the Elbow River at the historic site of Fort Calgary near downtown. The Bow River pathway, developed along the river's banks, is considered a part of Calgary's self-image. First Nations made varied use of the river for sustenance before settlers of European origin arrived, such as using its valleys in the buffalo hunt. The name ''Bow ''refers to the reeds that grew along its banks and were used by the First Nations to make bows; the Blackfoot language name for the river is , meaning "river where bow reeds grow". The river is an important source of water for irrigation and drinking water. Between the years 1910 and 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kananaskis River
The Kananaskis River is a mountain river in western Alberta, Canada. It is a tributary of the Bow River, crossing the length of Kananaskis Country. The river was named by John Palliser in 1858 after a Cree. Course The Kananaskis originates in the Canadian Rockies, east of the continental divide, in Peter Lougheed Provincial Park. It flows southeast to the Upper Kananaskis Lake, then turns north into the Lower Kananaskis Lake. From here it has a northbound course on the border of Spray Valley Provincial Park and Elbow-Sheep Wildland Provincial Park, where the Kananaskis Trail follows its itinerary. The lower course flows through Bow Valley Provincial Park, where Barrier Lake is formed along the river. Barrier Lake is an artificial lake used for hydroelectric power generation. The Kananaskis merges into the Bow River at Seebe, 30 km east of Canmore. The Kananaskis River has a total length of . The river contains three hydroelectric dams, each of which contains a powerhous ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surface Runoff
Surface runoff (also known as overland flow) is the flow of water occurring on the ground surface when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is saturated by water to its full capacity, and the rain arrives more quickly than the soil can absorb it. Surface runoff often occurs because impervious areas (such as roofs and pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or man-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. Runoff that occurs on the ground surface before reaching a channel can be a nonpoint source of pollution, as it can carry man-made contaminants or natural forms of pollution (such as rotting leaves). Man-made contaminants in runoff i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N, poleward of the humid continental climates. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification ''Dfc'', ''Dwc'', ''Dsc'', ''Dfd'', ''Dwd'' and ''Dsd''. Description This type of climate offers some of the most extreme seasonal temperature variations found on the planet: in winter, temperatures can drop to below and in summer, the temperature may exceed . However, the summers are short; no more than three months of the year (but at least one month) must have a 24-hour average temperature of at least to fall into this category of climate, and the coldest month should ave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
