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Mist Mountain
Mist Mountain is a mountain located alongside Alberta Highway 40, Highway 40 in the Canadian Rockies of Alberta, Canada. It reaches an elevation of and is visible from Highway 40 and the Sheep River (Alberta), Sheep River. The mountain was named in 1884 by George M. Dawson after he experienced a prolonged period of poor weather while near the western slopes of the range. Mist Mountain is composed of sedimentary rock that was pushed east and over the top of younger rock during the Laramide orogeny. Hot springs near its base as well as panoramic views from the peak mean it is a popular hike for locals and tourists visiting the lower Kananaskis area. __NOTOC__ Climate Based on the Köppen climate classification, Mist Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, June through September are the best months to climb Mist Mou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Misty Range
The Misty Range is a mountain range of the Canadian Rockies located east of the Alberta Highway 40, Bighorn Highway within Kananaskis Country, Canada. It is a sub-range of the High Rock Range in the Southern Continental Ranges. List of Mountains This range includes the following mountains: See also *Ranges of the Canadian Rockies References {{Canadian Rockies, state=collapsed Alberta's Rockies High Rock Range ... [...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] |
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] |
Mist Mountain Formation
The Mist Mountain Formation is a geologic formation of latest Jurassic to earliest Cretaceous age in the Western Canada Sedimentary Basin that is present in the southern and central Canadian Rockies. It was named for outcrops along the western spur of Mist Mountain in Alberta by D.W. Gibson in 1979. The Mist Mountain Formation contains economically important coal seams that have been mined in southeastern British Columbia and southwestern Alberta.Gibson, D.W. 1979. The Morrissey and Mist Mountain formations - newly described lithostratigraphic units of the Jura-Cretaceous Kootenay Group, Alberta and British Columbia. Bulletin of Canadian Petroleum Geology 27: 183-208. Lithology The Mist Mountain Formation consists of interbedded light to dark grey siltstone, silty shale, mudstone, and sandstone, with localized occurrences of chert- and quartzite-pebble conglomerate and conglomeratic sandstone, as well as a series of economically important coal seams.Glass, D.J. (editor) 1997. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Highwood River
The Highwood River is a tributary of the Bow River in southwestern Alberta, Canada. Course The Highwood originates in the Canadian Rockies in Peter Lougheed Provincial Park, in the Highwood Pass below Mount Arethusa. It flows south and is paralleled by the Alberta Highway 40, Kananaskis Trail between Elbow-Sheep Wildland Provincial Park, Don Getty Wildland Provincial Park, and ''Emerson Creek Park''. It turns east and flows along Highway 541 and through the community of Longview, Alberta, Longview. Continuing east, it passes through High River, ending when it enters the Bow River southeast of Calgary. Recreation The river is known for flyfishing. A variety of trout species live in the river, including native bull trout. In springtime when the snow is melting the river offers white water rafting. Flooding The Highwood River is subject to frequent flooding. Flood events of exceptional magnitude occurred in 1894, 1899, 1902, 1908, 1912, 1923, 1929, 1932, 1942, 1995, 2005 and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surface Runoff
Surface runoff (also known as overland flow or terrestrial runoff) is the unconfined flow of water over the ground surface, in contrast to ''channel runoff'' (or ''stream flow''). It occurs when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is #Saturation excess overland flow, saturated by water to its full capacity, and the rain arrives #Infiltration excess overland flow, more quickly than the soil can absorb it. Surface runoff often occurs because wikt:impervious#Adjective, impervious areas (such as roofs and Road surface, pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or human-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of Soil erosion#Rainfall and runoff, soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. ... [...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] |
George M
''George M!'' is a Broadway theatre, Broadway musical based on the life of George M. Cohan, the biggest Broadway star of his day who was known as "The Man Who Owned Broadway." The book for the musical was written by Michael Stewart (playwright), Michael Stewart, John Pascal, and Francine Pascal. Music and lyrics were by George M. Cohan himself, with revisions for the musical by Cohan's daughter, Mary Cohan. The story covers the period from the late 1880s until 1937 and focuses on Cohan's life and show business career from his early days in vaudeville with his parents and sister to his later success as a Broadway singer, dancer, composer, lyricist, theatre director and theatre producer, producer. The show includes such Cohan hit songs as "Give My Regards To Broadway", "You're a Grand Old Flag", and "Yankee Doodle Dandy." Productions The musical opened on Broadway at the Palace Theatre (New York City), Palace Theatre on April 10, 1968, and closed on April 26, 1969, after 433 pe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of 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 70 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sheep River (Alberta)
The Sheep River is located in southwestern Alberta, Canada, and is part of the Bow River watershed. The river begins in the mountain valleys of Elbow-Sheep Wildland Provincial Park, passes through Sheep River Provincial Park, and joins the about 8 km east of . The Sheep River provides drinking water for the towns of [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
