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Mount Coulthard
Mount Coulthard is a mountain straddling the border between Alberta and British Columbia in Canada. It is part of the Flathead Range which is a subset of the Canadian Rockies. The mountain is set on the Continental Divide, in Castle Wildland Provincial Park. It is situated in the Crowsnest Pass area and can be seen from Highway 3, the Crowsnest Highway. Mount Coulthard is named after Major Robert Wilson Coulthard (born December 6, 1875), a prominent Canadian mining engineer. He was general manager of the West Canadian Coal Company, engineer at Crow's Nest Pass Coal Company from 1901–1908, and a Major with the 2nd Canadian Tunnelling Company. The mountain's toponym was officially adopted in 1928 by the Geographical Names Board of Canada. Geology Mount Coulthard is composed of limestone, a 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 Cretaceous period rock during t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andy Good Peak
Andy Good Peak is located just south of Crowsnest Pass on the Canadian provincial boundary between Alberta and British Columbia on the Continental Divide. It was named in 1916 after Andy Good, a hotel owner in nearby Crowsnest Pass whose bar straddled the provincial border. See also *List of peaks on the Alberta–British Columbia border Gallery File:McLaren, Andy Good, Parrish.jpg, Mt. McLaren, with Andy Good Peak (behind), and Mt. Parrish (right) File:Flathead Range Crowsnest Pass area.jpg, Flathead RangeLeft to rightː Mount Coulthard, Andy Good Peak, Mount Parrish, Chinook Peak Chinook Peak is a summit located on the eastern border of Mount Rainier National Park. It is also on the shared border of Pierce County, Washington, Pierce County and Yakima County, Washington, Yakima County in Washington (U.S. state), Washingto .... References {{Canadian Rockies, state=collapsed Two-thousanders of Alberta Two-thousanders of British Columbia Canadian Rockies Kootenay ... [...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 Observation), Pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Two-thousanders Of Alberta
Two-thousanders are mountains that have a height of at least 2,000 metres above sea level, but less than 3,000 metres. The term is used in Alpine circles, especially in Europe (e.g. German: ''Zweitausender''). The two photographs show two typical two-thousanders in the Alps that illustrate different types of mountain. The Säuling (top) is a prominent, individual peak, whereas the Schneeberg (bottom) is an elongated limestone massif. In ranges like the Allgäu Alps, the Gesäuse or the Styrian-Lower Austrian Limestone Alps the mountain tour descriptions for mountaineers or hikers commonly include the two-thousanders, especially in areas where only a few summits exceed this level. Examples from these regions of the Eastern Alps Eastern Alps is the name given to the eastern half of the Alps, usually defined as the area east of a line from Lake Constance and the Alpine Rhine valley up to the Splügen Pass at the Alpine divide and down the Liro River to Lake Como in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chinook Peak (Alberta)
Chinook Peak is a mountain summit located in the Canadian Rockies of Alberta, Canada. Description Chinook Peak is situated 10 kilometers southwest of the town of Coleman in the Crowsnest Pass area and can be seen from Highway 3, the Crowsnest Highway. It is set on land managed by Castle Wildland Provincial Park. Precipitation runoff from the mountain drains into tributaries of the nearby Crowsnest River. Topographic relief is significant as the summit rises 1,300 meters (4,265 feet) above the river in 4.5 kilometers (2.8 miles). Sentry Mountain is to the northwest and the nearest higher neighbor is Andy Good Peak, to the southeast on the Continental Divide. History Chinook Peak was named by Jim Kerr, a resident of the Crowsnest Pass. Jim knew that when snow started blowing from the top from the west, a chinook wind would soon follow. When mapping this area, Dr. Raymond A. Price of the Geological Survey of Canada mapping this area, used this name to identify the peak.Aphro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Parrish
Mount Parrish is a mountain summit located in Alberta, Canada. Description Mount Parrish is situated eight kilometers southwest of the town of Coleman in the Crowsnest Pass area and can be seen from Highway 3, the Crowsnest Highway. It is part of the Flathead Range which is a subset of the Canadian Rockies. The peak is set one kilometer east of the Continental Divide, in Castle Wildland Provincial Park. Precipitation runoff from the mountain drains into tributaries of the nearby Crowsnest River. Topographic relief is significant as the summit rises 1,190 meters (3,900 feet) above the river in 5 kilometers (3.1 miles). Chinook Peak is to the northwest of Mt. Parrish and the nearest higher neighbor is Andy Good Peak, to the south. History Mount Parrish is named after Sherman Parrish, an early settler in the Crowsnest Pass area in 1898.Dave Birrell (2000), ''50 Roadside Panoramas in the Canadian Rockies'', Rocky Mountain Books, , p. 138 He homesteaded at th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount McLaren
Mount McLaren is a mountain summit located in Alberta, Canada. Description Mount McLaren is situated six kilometers southwest of the town of Coleman in the Crowsnest Pass area and can be seen from the Crowsnest Highway (Highway 3). It is part of the Flathead Range which is a subset of the Canadian Rockies. The peak is set two kilometers east of the Continental Divide, in Castle Wildland Provincial Park. Precipitation runoff from the mountain drains into Star and North York creeks which are tributaries of the nearby Crowsnest River. Topographic relief is significant as the summit rises over 945 meters (3,100 feet) above the river in 5 kilometers (3.1 miles). Chinook Peak is to the west of Mt. McLaren and the nearest higher neighbor is Mount Parrish, to the southwest. History Mount McLaren is named after Peter McLaren (1833–1919), a Canadian politician and Senator from Perth, Ontario.Dave Birrell (2000), ''50 Roadside Panoramas in the Canadian Rockies'' ... [...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] |
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] |
Cave
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorgani ... [...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 Plate, Kula and Farallon Plates were sliding under the North American plate. Most hypothes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ... [...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] |
