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Association Peak
Association Peak is a mountain summit located in Alberta, Canada. Description Association Peak is situated in Don Getty Wildland Provincial Park and the Fairholme Range which is a subset of the Canadian Rockies along the range's eastern front. It is set northeast of Canmore and six km north of Mount John Laurie. The nearest major city is Calgary, to the east. The mountain is visible from the Trans-Canada Highway which traverses the Bow Valley between Calgary and Banff National Park. Precipitation runoff from Association Peak drains north to the South Ghost River, and southeast to the Bow River via Old Fort Creek. Topographic relief is significant as the summit rises above the creek in . History The mountain's well-established toponym was officially adopted March 17, 1967, by the Geographical Names Board of Canada. Association Peak is named for the Indian Association of Alberta which was co-founded in 1939 by John Laurie, who had the mountain to the south named after hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fairholme Range
The Fairholme Range is a mountain range east of the Bow River valley in the Canadian Rockies. The range is bounded on the west side by the Trans-Canada Highway as it passes through the towns of Exshaw and Canmore, while the northern section of the range extends into Banff National Park to the southern shores of Lake Minnewanka. John Palliser named the range in 1859 after his sister Grace Fairholme, who had married William Fairholme. Peaks of this range include: Anû Kathâ Îpa, the last entry in the table above, is the official name as of 2020 of a mountain that previously held a racist and offensive name. In the spring and summer of 2003, Parks Canada performed a prescribed burn A controlled or prescribed burn, also known as hazard reduction burning, backfire, swailing, or a burn-off, is a fire set intentionally for purposes of forest management, farming, prairie restoration or greenhouse gas abatement. A control ... in selected areas of the range in order to redu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bow Valley
Bow Valley is a valley located along the upper Bow River in Alberta, Canada. The name "Bow" refers to the reeds that grew along its banks and which were used by the local First Nations people to make bows; the Blackfoot language name for the river is , meaning "river where bow weeds grow". about the river. Community There are several communities in the Bow Valley, including Banff, , Kananaskis, and the hamlets of ...[...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'' i ... [...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, 70 to 80 million years ago, and ended 35 to 55 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 propose ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...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 fos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated 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 movement, which are called agents of denudation. Biological detritus was 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 as dissolved minerals precipita ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Association Peak From Yamnuska
Association may refer to: * Club (organization), an association of two or more people united by a common interest or goal * Trade association, an organization founded and funded by businesses that operate in a specific industry * Voluntary association, a body formed by individuals to accomplish a purpose, usually as volunteers Association in various fields of study *Association (archaeology), the close relationship between objects or contexts. * Association (astronomy), combined or co-added group of astronomical exposures *Association (chemistry) * Association (ecology), a type of ecological community *Genetic association, when one or more genotypes within a population co-occur *Association (object-oriented programming), defines a relationship between classes of objects * Association (psychology), a connection between two or more concepts in the mind or imagination * Association (statistics), a statistical relationship between two variables * File association, associates a file w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stoney 142, 143, 144
Stoney 142, 143, 144 is an Indian reserve of the Stoney Nakoda First Nation, comprising Bearspaw, Chiniki, and Wesley First Nations in Alberta, located between the Municipal District of Bighorn No. 8 and Rocky View County. The largest community of the Nakoda people, it is 56 kilometers west of Calgary. The community is spread along both sides of the Trans-Canada Highway, east of Banff National Park and north of Kananaskis Improvement District. In addition to Kananaskis, it is also bordered by Bighorn No. 8, Rocky View County, and the town of Cochrane. By land area, it is the third-largest Indian reserve in Canada (after Blood 148 and Siksika 146, both also in Alberta). According to the Canada 2011 Census: *Population: 3,494 *% Change (1996–2001): 0.7 *% Change (2001–2011): 38.16 *Dwellings: 795 *Area (km2): 444.94 *Density (persons per km2): 7.85 History Most of the film ''Buffalo Bill and the Indians, or Sitting Bull's History Lesson'' was shot on location on the rese ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nakoda People
The Nakoda (also known as Stoney or ) are an Indigenous people in Western Canada and, originally, the United States. They used to inhabit large parts of what is now Alberta, Saskatchewan and Montana, but their reserves are now located in Alberta and in Saskatchewan, where they are scarcely differentiated from the Assiniboine. Through their language they are related to the Dakota and Lakota nations of the Great Plains and the Rocky Mountains, part of the large Sioux Nation. They refer to themselves in their own language as " Nakoda", meaning ''friend'', ''ally''. The name "Stoney" was given them by white explorers, because of their technique of using fire-heated rocks to boil broth in rawhide bowls. They are very closely related to the Assiniboine, who are also known as ''Stone Sioux'' (from the Ojibwe ). Alberta's Nakoda First Nation comprises three bands: Bearspaw, Chiniki and Wesley. The Stoney were "excluded" from Banff National Park between 1890 and 1920. In 2010 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geographical Names Board Of Canada
The Geographical Names Board of Canada (GNBC) is a national committee with a secretariat in Natural Resources Canada, part of the Government of Canada, which authorizes the names used and name changes on official federal government maps of Canada created since 1897. The board consists of 27 members, one from each of the provinces and territories, and others from departments of the Government of Canada. The board also is involved with names of areas in the Antarctic through the Antarctic Treaty. Structure The secretariat is provided by Natural Resources Canada. In addition to the provincial and territorial members are members from the following federal government departments: Aboriginal Affairs and Northern Development Canada, Canada Post Corporation, Fisheries and Oceans Canada, Elections Canada, Library and Archives Canada, Department of National Defence, Natural Resources Canada (including Geological Survey of Canada and Canada Centre for Mapping and Earth Observatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Topographic Relief
Terrain or relief (also topographical relief) involves the vertical and horizontal dimensions of land surface. The term bathymetry is used to describe underwater relief, while hypsometry studies terrain relative to sea level. The Latin word (the root of ''terrain'') means "earth." In physical geography, terrain is the lay of the land. This is usually expressed in terms of the elevation, slope, and orientation of terrain features. Terrain affects surface water flow and distribution. Over a large area, it can affect weather and climate patterns. Importance The understanding of terrain is critical for many reasons: * The terrain of a region largely determines its suitability for human settlement: flatter alluvial plains tend to have better farming soils than steeper, rockier uplands. * In terms of environmental quality, agriculture, hydrology and other interdisciplinary sciences; understanding the terrain of an area assists the understanding of watershed boundaries, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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