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Mount Owen (British Columbia)
Mount Owen is a summit in British Columbia, Canada. Description Mount Owen is located in Yoho National Park, in the Bow Range of the Canadian Rockies. Precipitation runoff from Mount Owen drains into tributaries of the Ottertail River which in turn is a tributary of the Kicking Horse River. Mount Owen is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising approximately 1,700 meters (5,577 ft) above the Ottertail River Valley in . The nearest higher neighbor is Odaray Mountain, to the north-northeast. History The first ascent of the mountain was made in 1892 by Canadian surveyor James J. McArthur who named the mountain for his survey party member, Frank Owen. The mountain's toponym was officially adopted on March 31, 1924, by the Geographical Names Board of Canada. Geology Mount Owen is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bow Range
The Bow Range is a mountain range of the Canadian Rockies in Alberta and British Columbia, Canada. The range is named in associated with the Bow River and was officially adopted on March 31, 1917 by the Geographic Board of Canada. It is a part of the Banff- Lake Louise Core Area of the Southern Continental Ranges, located on the Continental Divide, west of the Bow River valley, in Banff National Park and Kootenay National Park. The Bow Range covers a surface area of 717 km2 (277 mi2), has a length of 34 km (from north to south) and a maximum width of 43 km. The highest peak is Mount Temple, with an elevation of . The range also covers the Valley of the Ten Peaks, with the tallest of the ten being Mount Hungabee at 3492 metres. The range also has hiking areas such as the Consolation Lakes, Sentinel Pass-Larch Valley, Wenkchenma Pass-Eiffel Lake, the Beehive plain of the Six Glaciers system and Saddle Back Pass. __NOTOC__ Peaks and mountains See also * R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
James J
James is a common English language surname and given name: *James (name), the typically masculine first name James * James (surname), various people with the last name James James or James City may also refer to: People * King James (other), various kings named James * Saint James (other) * James (musician) * James, brother of Jesus Places Canada * James Bay, a large body of water * James, Ontario United Kingdom * James College, a college of the University of York United States * James, Georgia, an unincorporated community * James, Iowa, an unincorporated community * James City, North Carolina * James City County, Virginia ** James City (Virginia Company) ** James City Shire * James City, Pennsylvania * St. James City, Florida Arts, entertainment, and media * ''James'' (2005 film), a Bollywood film * ''James'' (2008 film), an Irish short film * ''James'' (2022 film), an Indian Kannada-language film * James the Red Engine, a character in ''Thomas the Tank En ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Three-thousanders Of British Columbia
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term may refer to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Ande ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Columbia Highway 1
Highway 1 is a Provincial highways in British Columbia, provincial highway in British Columbia, Canada, that carries the main route of the Trans-Canada Highway (TCH). The highway is long and connects Vancouver Island, the Greater Vancouver region in the Lower Mainland, and the British Columbia Interior, Interior. It is the westernmost portion of the main TCH to be numbered "Highway 1", which continues through Western Canada and extends to the Manitoba–Ontario boundary. The section of Highway 1 in the Lower Mainland is the second-busiest freeway in Canada, after Ontario Highway 401 in Toronto. The highway's western terminus is in the provincial capital of Victoria, British Columbia, Victoria, where it serves as a city street and freeway in the suburbs. Highway 1 travels north to Nanaimo, British Columbia, Nanaimo and reaches the Lower Mainland at Horseshoe Bay, British Columbia, Horseshoe Bay via a BC Ferries route across the Strait of Georgia. The highway bypasses Vancouver on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Goodsir
Mount Goodsir (or the Goodsir Towers) is the highest mountain in the Ottertail Range, a subrange of the Park Ranges in British Columbia. It is located in Yoho National Park, near its border with Kootenay National Park. The mountain has two major summits, the South Tower (the higher summit) and the North Tower, . The mountain was named by James Hector in 1859 after two brothers, John Goodsir, a professor of anatomy at the University of Edinburgh, and Harry Goodsir, a surgeon on the ship HMS Erebus. The standard route on the South Tower is the southwest ridge, a straightforward but long climb ( Grade III), which consists primarily of non-technical terrain, but includes short sections of narrow ridge graded YDS 5.4. Access to any route on either Tower requires a long hike. See also * Mountain peaks of Canada * List of mountain peaks of North America This article comprises three sortable tables of major mountain peaksThis article defines a significant summit as a summi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Park Mountain
Park Mountain is a mountain summit located above the southwest shore of Lake McArthur in Yoho National Park, in the Bow Range of the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Mount Biddle, to the east. Park Mountain is situated four kilometres west of the Continental Divide, and southeast of Field, British Columbia. History The mountain was named in 1915 because of the "park-like" setting of the area. The Lake O'Hara area that the mountain is located in is a gem within a park, the best that the Canadian Rockies has to offer. The first ascent of the mountain was made in 1904 by a survey party. The mountain's toponym was officially adopted in 1952 when approved by the Geographical Names Board of Canada. Geology Park 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 Base ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Duchesnay
Mount Duchesnay is a summit in British Columbia, Canada. Description Mount Duchesnay is located in Yoho National Park, in the Bow Range of the Canadian Rockies. Precipitation runoff from Mount Duchesnay drains into tributaries of the Kicking Horse River which is a tributary of the Columbia River. Mount Duchesnay is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising over 1,700 meters (5,577 ft) above the Kicking Horse Valley in less than . The peak is visible from Highway 1 (the Trans-Canada Highway). The nearest higher neighbor is Mount Stephen, to the north-northeast. History At the suggestion of James Outram, the mountain was named in 1902 by David McNicoll (vice-president of Canadian Pacific Railway) to remember Charles-Edmond Juchereau Duchesnay (June 23, 1854 – September 4, 1901), Assistant General Superintendent of the railway's Western Division and son of Elzéar-He ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of British Columbia
British Columbia is the westernmost province of Canada, bordered by the Pacific Ocean. With an area of it is Canada's third-largest province. The province is almost four times the size of the United Kingdom and larger than every United States state except Alaska. It is bounded on the northwest by the U.S. state of Alaska, directly north by Yukon and the Northwest Territories, on the east by Alberta, and on the south by the U.S. states of Washington, Idaho, and Montana. Formerly part of the British Empire, the southern border of British Columbia was established by the 1846 Oregon Treaty. The province is dominated by mountain ranges, among them the Canadian Rockies but dominantly the Coast Mountains, Cassiar Mountains, and the Columbia Mountains. Most of the population is concentrated on the Pacific coast, notably in the area of Vancouver, located on the southwestern tip of the mainland, which is known as the Lower Mainland. It is the most mountainous province of Canada. Statist ... [...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] |
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] |
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] |
