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Mount Lorette (Alberta)
Mount Lorette is a summit centrally located in Kananaskis Country in the Canadian Rockies of Alberta, Canada. Mount Lorette's nearest higher peak is Skogan Peak, to the north-northwest. Mount Lorette is a landmark that can be seen from Highway 40 north of the Kananaskis Village area. __NOTOC__ History It was named in 1922 for Lorette Spur, a ridge to the north of Vimy Ridge which was the scene of very heavy fighting during World War I. Capturing Lorette Spur marked a significant battle in French military history. The first ascent of the peak was made in 1952 by R.C. Hind, B. Richardson, L. Keeling, J. Manry, J. Dodds, and C. McAllister. The mountain's name was officially adopted in 1953 by the Geographical Names Board of Canada. Geology Mount Lorette 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alberta
Alberta ( ) is one of the thirteen provinces and territories of Canada. It is part of Western Canada and is one of the three prairie provinces. Alberta is bordered by British Columbia to the west, Saskatchewan to the east, the Northwest Territories (NWT) to the north, and the U.S. state of Montana to the south. It is one of the only two landlocked provinces in Canada (Saskatchewan being the other). The eastern part of the province is occupied by the Great Plains, while the western part borders the Rocky Mountains. The province has a predominantly continental climate but experiences quick temperature changes due to air aridity. Seasonal temperature swings are less pronounced in western Alberta due to occasional Chinook winds. Alberta is the fourth largest province by area at , and the fourth most populous, being home to 4,262,635 people. Alberta's capital is Edmonton, while Calgary is its largest city. The two are Alberta's largest census metropolitan areas. More tha ... [...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] |
Mount Lougheed
Mount Lougheed is a triple-peak mountain located between Spray Lakes Reservoir and the Wind Valley of Kananaskis Country in the Canadian Rockies of Alberta, Canada. The highest summit is known as Peak 2 (3,107 metres). Peak 1 to the northwest is 3,080 metres. Peak 3 to the southeast is 3,010 metres. The nearest higher peak is Wind Mountain, to the southeast. Mount Lougheed is a conspicuous landmark that can be seen from Highway 1, the Trans-Canada Highway at Dead Man's Flats which is east of Canmore. __NOTOC__ History Mount Lougheed was named after Sir James Lougheed (1854–1925), a prominent lawyer, politician, senator, and cabinet minister. The mountain was originally named Wind Mountain by Eugène Bourgeau of the Palliser expedition, but was renamed in 1928 to honor Lougheed after his passing. The mountain's name was officially adopted in 1928 by the Geographical Names Board of Canada. The first ascent was made in 1889 by A. St. Cyr, W.S. Drewry, and Tom Wilson. Mount Lou ... [...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] |
Wasootch Peak
Wasootch Peak is a mountain summit located in the Fisher Range of Kananaskis Country in the Canadian Rockies of Alberta, Canada. The peak is situated on the northern end of the ridge that separates Wasootch Creek from Porcupine creek. Wasootch Peak's nearest higher peak is Old Baldy, to the southeast. The peak may be seen from Highway 40, and is prominently featured from the ski slopes at Nakiska. ''Wasootch'' is from the Stoney language word ''wazi'', which translated means ''unique''.Canadian Mountain Place Names, Authors: Glen W. Boles, Roger W. Laurilla, William L. Putnam, Publisher: Rocky Mountain Books, 2006 Geology Wasootch 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, Wasootch Peak is located in a subarctic climate zone with cold, snowy winters, ... [...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 The University of Calgary (U of C or UCalgary) is a public research university located in Calgary, Alberta, Canada. The University of Calgary started in 1944 as the Calgary branch of the University of Alberta, founded in 1908, prior to being ins ... 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 Image:Barrier Lake Kananaskis Aerial.jpg, Towering over Barrier La ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Geology Of Alberta
The geology of Alberta encompasses parts of the Canadian Rockies and thick sedimentary sequences, bearing coal, oil and natural gas, atop complex Precambrian crystalline basement rock. Geologic history, stratigraphy & tectonics The Precambrian granite and gneiss crystalline basement rocks beneath Alberta are extremely ancient, dating to the Archean and Proterozoic. The Slave Craton and Southern Alberta craton are the oldest units at more 2.5 billion years old, while younger units from the Proterozoic include the Wopmay orogeny, Great Slave Lake shear zone, Pre-Taltston basement, Taltson magmatic zone, Athabasca polymetamorphic terrane, Red Earth granulite domain, Kimiwan isotopic anomaly, Ksituan magmatic arc, Virgin River shear zone, Central Alberta intrusions and Lacombe domain. In many cases, Proterozoic deformation overprinted older Archean rocks. The Hudsonian Orogeny from 1.9 to 1.6 billion years ago was the last major regional metamorphic event. Paleozoic (539-251 million ... [...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] |
