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Mount Cline
Mount Cline is a mountain in western Alberta, Canada, north of Saskatchewan Crossing, southwest of Nordegg. The mountain is located in the North Saskatchewan River Valley, west of Resolute Mountain. It was named in 1898 by J. Norman Collie, after Michel Klyne (also called Michael Cline), French Canadian postmaster of Jasper House from 1824 to 1835. __NOTOC__ Geology Mount Cline 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 Cline 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. Gallery File:Mount Cline 2.jpg, Mount Cline See also * List of mountains in the Canadian Rockies A list of highest mountains and peaks in the Canadian Rockies over ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cline Range
Cline may refer to: Science * Cline (biology), a measurable gradient in a single trait in a species across its geographical range * Cline (hydrology), a fluid layer with a property that varies * Cline (mathematics) or generalised circle, a circle or straight line in inverse geometry * Cline (linguistics): ** Cline of instantiation, a concept in systemic functional linguistics ** Cline of grammaticality in grammaticalization Other * Cline (fish) (''Clinitrachus argentatus''), a shallow water fish * Cline (surname), a given name and a family name (including a list of persons with the name) * Cline River, in Alberta, Canada * Cline, Texas in Uvalde County, Texas * Cline Avenue, a road in Indiana, US * Antonov An-32, a military transport aircraft, whose NATO reporting name is "Cline" See also * Clines, a surname * Clinal, a torsion angle in alkane stereochemistry * Clyne (other) * Kline (other) * Klein (other) Klein may refer to: People *Kl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
French Canadian
French Canadians, referred to as Canadiens mainly before the nineteenth century, are an ethnic group descended from French people, French colonists first arriving in Canada (New France), France's colony of Canada in 1608. The vast majority of French Canadians live in the province of Quebec. During the 17th century, French settlers originating mainly from the west and north of France settled Canada. It is from them that the French Canadian ethnicity was born. During the 17th to 18th centuries, French Canadians expanded across North America and colonized various regions, cities, and towns. As a result, people of French Canadian descent can be found across North America. Between 1840 and 1930, many French Canadians emigrated to New England, an event known as the Quebec diaspora, Grande Hémorragie. Etymology French Canadians get their name from the Canada (New France), French colony of Canada, the most developed and densely populated region of New France during the period of Fr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains In The Canadian Rockies
A list of highest mountains and peaks in the Canadian Rockies over is shown below. Sources for the elevation, prominence and first ascent can be found in their respective pages and/or Wikidata Wikidata is a collaboratively edited multilingual knowledge graph hosted by the Wikimedia Foundation. It is a common source of open data that Wikimedia projects such as Wikipedia, and anyone else, are able to use under the CC0 public domain .... Gallery File:Mt. Robson from Berg Lake, reflected.jpg, Mount Robson from Berg Lake Mt. Columbia (vertical).jpg, Mount Columbia North Twin from Columbia Icefield approach.jpg, North Twin Peak References ;Notes {{reflist, group=notes Canadian Rockies, *• Canadian Rockies Mountains, Rockies Mountains, Rockies ... [...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] |
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 143.1 Mya. The Jurassic constitutes the second and middle period of the Mesozoic, Mesozoic Era as well as the eighth period of the Phanerozoic, Phanerozoic Eon 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 (CAMP). The beginning of the Toarcian Age started around 183 million years ago and is marked by the Toarcian Oceanic Anoxic Event, a global episode of Anoxic event, oceanic anoxia, ocean acidification, and elevated global temperatures associated with extinctions, likely caused by the eruption of the Kar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precambrian
The Precambrian ( ; or pre-Cambrian, sometimes abbreviated pC, 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 Latinized 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 ... [...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] |
Jasper House
Jasper House National Historic Site, in Jasper National Park, Alberta, is the second site of a trading post on the Athabasca River that functioned from 1813 to 1884 as a major staging and supply post for travel through the Canadian Rockies. The post was originally named Rocky Mountain House, but was renamed to avoid confusion with the Rocky Mountain House trading post on the North Saskatchewan River, becoming "Jasper's House" after the postmaster, Jasper Hawes, who operated the post from 1815 or 1817 to 1821. The first location was on the west shore of Brûlé Lake (Alberta), Brûlé Lake. The second Jasper House was established at the northern end of Jasper Lake (Alberta), Jasper Lake in 1830, primarily serving travellers crossing Yellowhead Pass or Athabasca Pass. The site operated until 1853, and was occasionally used until 1858 when it was reopened seasonally by Henry John Moberly, who operated it into the 1860s. The post was officially closed in 1884 after years of inactiv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Michel Klyne
Michel Klyne (2 July 1781 – 1868) was an employee of the North West Company and later the Hudson's Bay Company, serving as postmaster at Jasper House in the Rocky Mountains. Early life Klyne was born in the Province of Quebec in 1781, son of a Hessian soldier, Johan Adam Klein (or Jean Adam Klyne) who fought in the American Revolutionary War, and his French Canadian wife, Marie-Geneviève Bisson. He had one sister, also named Marie-Geneviève, and several half-siblings through his father. The North West Company and Hudson's Bay Company Klyne entered the employ of the North West Company in the late 1790s as a fur trader. Following the 1821 merger of the NWC and the HBC, he was put in charge of Jasper House, near modern Jasper, Alberta. He served as postmaster for 11 years, from 1824 to 1834. In 1835, he retired to the Red River. Alberta's Cline River and Mount Cline [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canadian Rockies
The Canadian Rockies () or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part of the Canadian Cordillera, which is the northern segment of the North American Cordillera, the expansive system of interconnected mountain ranges between the Interior Plains and the Pacific Coast that runs northwest–southeast from central Alaska to the Isthmus of Tehuantepec in Mexico. Canada officially defines the Rocky Mountains system as the mountain chains east of the Rocky Mountain Trench extending from the Liard River valley in northern British Columbia to the Albuquerque Basin in New Mexico, not including the Mackenzie, Richardson and British Mountains/ Brooks Range in Yukon and Alaska (which are all included as the "Arctic Rockies" in the United States' definition of the Rocky Mountains system). The Canadian Rockies, being the northern segment of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
