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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] |
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] |
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, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Kananaskis Village
Kananaskis Village is an unincorporated community in Alberta's Rockies within the Kananaskis Country park system in the Kananaskis Improvement District of Alberta, Canada. It is located approximately south of the Trans-Canada Highway ( Highway 1), west of Highway 40 (Kananaskis Trail) via Mt. Allan Drive and Centennial Drive. The community is located on the west shore of the Kananaskis River at the base of Mount Kidd. The village was the host of the 28th G8 summit in 2002. Kananaskis Improvement District's municipal office is located in Kananaskis Village. Attractions Kananaskis Village is a resort community. It features hotel-style accommodation and numerous amenities. Amenities include a 36-hole golf course (Kananaskis Country Golf Course), downhill skiing (Nakiska Ski Area), equestrian facilities (Boundary Ranch), and trails for hiking, mountain cycling, and cross-country skiing. See also *List of communities in Alberta The province of Alberta, Canada, is divide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Kidd
Mount Kidd is a double-summit massif centrally located in Kananaskis Country in the Canadian Rockies of Alberta, Canada. Mount Kidd is situated within Spray Valley Provincial Park, and its nearest higher neighbor is Mount Sparrowhawk, to the northwest. Mount Kidd is a landmark that can be seen from Highway 40 in the Kananaskis Village area, and from the Kananaskis Country Golf Course which lies at the eastern base of the mountain. History In 1907, Dr. Donaldson Bogart Dowling, an engineer with the Geological Survey of Canada, named the mountain for John Alfred (Fred) Kidd, who was a resident of nearby Morley, Alberta. From 1902 to 1907, Kidd ran the Morley general store and outfitted expeditions and geological survey crews such as Dowling's with supplies. The first ascent of the mountain was made in 1947 by R. C. Hind and J. F. Tarrant. The mountain's name was officially adopted in 1953 by the Geographical Names Board of Canada. In June 1986, Mount Kidd was the sce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Wedge (Alberta)
The Wedge is a mountain in Alberta, Canada. It is part of the Fisher Range of the Southern Continental Ranges of the Canadian Rockies. It is located east of Highway 40 just southeast from the K-Country golf course, immediately southeast of Wedge Pond in Kananaskis Country. Scramble gain, mostly easy with a moderate section just above the tree line and a short difficult section on the ridge. The trail starts from the wedge pond parking lot. Either follow the shore counter clock wise until a trail takes off into the trees or follow the cutline south (right) from the gate to find a trail that soon joins the other and heads up the hill. It's a nice treed walk up to the tree line. Once on the rocks the best route up is to keep to the right, beside the cliffs until you can get on top then it's an easy walk up to the false summit. From there a ridge walk leads to the true summit. One short section of the ridge is too narrow to walk on so one has to find hand and foot holds and ... [...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] |
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] |
Mountains Of Alberta
Most of Alberta's mountains are found on the western edge of the province of Alberta, consisting of the eastern slopes of the Canadian Rockies, which run through the province from Alberta's mid-point to its southern border with the United States. Other elevated spots can be found in the Caribou Mountains and the Cypress Hills. The peaks of the Canadian Rockies are majestic, many of them reaching a height of more than three kilometres above sea level. Alberta's southwestern boundary is traced on the Continental Divide, along the high ranges of the Rocky Mountains, and many peaks are located on the Alberta–British Columbia border. The peak of Mount Columbia, within Jasper National Park, is the highest point in Alberta, second highest in the Canadian Rockies and 28th highest in Canada. The Caribou Mountains are located in the northern extremity of Alberta, forming an elevated plateau in the northern plains and wetlands. They reach an altitude of 1,030 m, almost 700&n ... [...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] |
