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Commonwealth Peak
Commonwealth Peak is a mountain summit in the Spray Mountains, a sub-range of the Canadian Rockies in Alberta, Canada. The mountain is situated in Peter Lougheed Provincial Park. Its nearest higher peak is Mount Birdwood, to the west. Both can be seen from Alberta Highway 742, also known as Smith-Dorrien/Spray Trail in Kananaskis Country. __NOTOC__ History Commonwealth Peak was named in 1979 to commemorate the 1978 Commonwealth Games that were held in Edmonton, Alberta. The mountain's name was officially adopted in 1979 by the Geographical Names Board of Canada. The first ascent of the peak was made in 1970 by Charlie Locke and Lloyd McKay. Geology Commonwealth 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, Commonwealth Peak is located in a subarctic climate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spray Mountains
The Spray Mountains is a mountain range of the Canadian Rockies located in southwestern Alberta, Canada. List of mountains This range includes the following mountains and peaks: References Spray Mountains, {{AlbertaRockies-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock (geology), rock formed by the cementation (geology), cementation of sediments—i.e. particles made of minerals (geological detritus) or organic matter (biological detritus)—that have been accumulated or deposited at Earth's surface. Sedimentation is any process that causes these particles to settle in place. Geological detritus originates from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or Mass wasting, mass movement, which are called agents of denudation. Biological detritus is formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur when dissolved minerals precipitate from aqueous solution, water solution. The sedimentary rock cover of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snow Peak (Alberta)
Snow Peak is a mountain summit in the Spray Mountains, a sub-range of the Canadian Rockies in Alberta, Canada. The mountain is situated on the shared border of Peter Lougheed Provincial Park and Banff National Park. The nearest higher peak is Mount Birdwood, to the northeast. The mountain is primarily used for hiking. __NOTOC__ Geology Snow 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, Snow Peak is located in a subarctic climate The subarctic climate (also called subpolar climate, or boreal climate) is a continental 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 ... with cold, snowy winters, and mild summers. Winter temperatures can drop below −2 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Sir Douglas
Mount Sir Douglas is located on the border of Alberta and British Columbia on the Continental Divide, at the northern end of Height of the Rockies Provincial Park and east of Invermere. It is Alberta's 18th highest peak, and 28th prominence mountain as well as British Columbia's 28th highest peak. It was named in 1916 by interprovincial boundary surveyors after Field Marshal Sir Douglas Haig. __NOTOC__ Geology Mount Sir Douglas 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, Mount Sir Douglas is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. See also * List of mountains in the Canadian Rockies * List of peaks on the Alberta–British Columbia border This is a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Burstall
Mount Burstall is a summit in Alberta, 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 coun .... Mount Burstall was named for H. E. Burstall, a British army officer who commanded Canadian troops during World War I. References Two-thousanders of Alberta Spray Mountains {{AlbertaRockies-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kananaskis Range
The Kananaskis Range is a mountain range west of the Kananaskis River in the Continental Ranges of the Canadian Rockies. Many of the peaks are named after ships and people involved in the Battle of Jutland. 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. List of mountains Peaks of this range include: References External links * * {{Canadian Rockies, state=collapsed Kananaskis Range, * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Galatea
Mount Galatea is the highest peak of the Kananaskis Range, a subrange of the Canadian Rockies in the province of Alberta. It is located in the upper Spray Lakes Valley of the Kananaskis Country system of provincial parks. The mountain was named after the Royal Navy cruiser HMS ''Galatea''. Geology Mount Galatea 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, Mount Galatea is located in a subarctic climate The subarctic climate (also called subpolar climate, or boreal climate) is a continental 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 ... zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill fact ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Alberta
Alberta is one of the thirteen provinces and territories of Canada. Located in Western Canada, the province has an area of and is bounded to the south by the United States state of Montana along 49° north for ; to the east at 110° west by the province of Saskatchewan for ; and at 60° north the Northwest Territories for . The southern half of the province borders British Columbia along the Continental Divide of the Americas on the peaks of the Rocky Mountains, while the northern half borders British Columbia along the 120th meridian west. Along with Saskatchewan it is one of only two landlocked provinces or territories. Terrain Alberta's landscape is marked by the impact of the Wisconsin Glaciation, about 75,000 to 11,000 years ago, when the entire future province was covered in ice. As the ice sheet receded, the landscape was changed, and large amounts of glacial till were left behind. The southern portion consists chiefly of plains that are almost entirely treeless. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scrambles In The Canadian Rockies
''Scrambles in the Canadian Rockies'' is a climbing guidebook by Alan Kane describing scrambling routes of mountains in the Canadian Rockies. It is published by Rocky Mountain Books, located in Calgary, Alberta Alberta is a Provinces and territories of Canada, province in Canada. It is a part of Western Canada and is one of the three Canadian Prairies, prairie provinces. Alberta is bordered by British Columbia to its west, Saskatchewan to its east, t .... The third edition , released in May 2016, has been updated and contains route descriptions for 175 peaks. The peaks are rated from easy to difficult and information on trail heads and the standard routes are covered. '' Backpacker'' magazine has twice featured the book as an expedition guide. The '' Canadian Alpine Journal'' referred to it as a "scree gospel". The book is solely responsible for creating a widespread interest in scrambling up mountain peaks, whether the peaks are in USA or Western Canada. Since first publishe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a continental 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°N to 70°N, poleward of the humid continental climates. Like other Class D climates, they are rare in the Southern Hemisphere, only found at some isolated highland elevations. 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 on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. 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'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laramide Orogeny
The Laramide orogeny was a time period of mountain building in western North America, which started in the Late Cretaceous, 80 to 70 million years ago, and ended 55 to 35 million years ago. The exact duration and ages of beginning and end of the orogeny are in dispute. The Laramide orogeny occurred in a series of pulses, with quiescent phases intervening. The major feature that was created by this orogeny was deep-seated, thick-skinned deformation, with evidence of this orogeny found from Canada to northern Mexico, with the easternmost extent of the mountain-building represented by the Black Hills of South Dakota. The phenomenon is named for the Laramie Mountains of eastern Wyoming. The Laramide orogeny is sometimes confused with the Sevier orogeny, which partially overlapped in time and space. The orogeny is commonly attributed to events off the west coast of North America, where the Kula and Farallon Plates were sliding under the North American Plate. Most hypotheses propo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
