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Mt. Lefroy
Mount Lefroy is a mountain on the Continental Divide, at the border of Alberta and British Columbia in western Canada. The mountain is located on the eastern side of Abbot Pass which separates Lake Louise in Banff National Park from Lake O'Hara in Yoho National Park. Mount Victoria lies immediately on the western side of the pass. The mountain was named by George M. Dawson in 1894 for Sir John Henry Lefroy (1817–1890), an astronomer who had traveled over in Canada's north between 1842 and 1844 making meteorological and magnetic observations. The mountain is the site of the first fatal climbing accident in Canada. In 1896 during a failed summit bid, Philip Stanley Abbot slipped on rocks after just coming off an icy section and plummeted down the rock face to his death. The first successful ascent was made in 1897 by J. Norman Collie, Arthur Michael, H. Dixon; Charles Fay, Peter Sarbach, R. Vanderlip, C. Noyes, Charles Thompson, and H. Parker. A prominent painting ... [...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] |
John Henry Lefroy
Sir John Henry Lefroy (28 January 1817 – 11 April 1890) was an English military man and later colonial administrator who also distinguished himself with his scientific studies of the Earth's magnetism. Biography Lefroy was a son of the Rev. John Henry George Lefroy, of Ewshot House (subsequently Itchel) in Hampshire, England, and his wife, Sophia Cottrell. His sister Anne married the Irish landowner and politician John McClintock, who was created the 1st Baron Rathdonnell in 1868. Lefroy was also a first cousin to Thomas Lefroy (1776-1869), the future Chief Justice of Ireland whom Jane Austen apparently had in mind when she created the character of Mr. Darcy in 'Pride and Prejudice'. Lefroy entered the Royal Military Academy, Woolwich in London in 1831 and became a 2nd lieutenant of the Royal Artillery in 1834. When the British government launched a project under the direction of Edward Sabine to study terrestrial magnetism, he was chosen to set up and supervise the observa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Gallery Of Canada
The National Gallery of Canada (french: Musée des beaux-arts du Canada), located in the capital city of Ottawa, Ontario, is Canada's national art museum. The museum's building takes up , with of space used for exhibiting art. It is one of the largest art museums in North America by exhibition space. The institution was established in 1880 at the Second Supreme Court of Canada building, and moved to the Victoria Memorial Museum building in 1911. In 1913, the Government of Canada passed the ''National Gallery Act'', formally outlining the institution's mandate as a national art museum. The museum was moved to the Lorne building in 1960. In 1988, the museum was relocated to a new building designed for this purpose. The National Gallery of Canada is situated in a glass and granite building on Sussex Drive, with a notable view of the Canadian Parliament buildings on Parliament Hill. The building was designed by Israeli architect Moshe Safdie and opened in 1988. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Mitre (Alberta)
The Mitre is a mountain summit located in the Lake Louise area of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Lefroy, to the west. Mount Aberdeen is to the north-northeast, Lefroy Glacier immediately north, Mitre Glacier southwest, and Paradise Valley to the southeast. History The Mitre was named in 1893 by Samuel E.S. Allen presumably because the mountain resembles a Bishop's mitre. The first ascent of the peak was made in 1901 by Christian Kaufmann, J. Pollinger, G. Collier, E. Tewes, and G. Bohren. The mountain's name was officially adopted in 1952 by the Geographical Names Board of Canada. Geology Like other mountains in Banff Park, The Mitre 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, The Mitr ... [...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] |
Cambrian
The Cambrian Period ( ; sometimes symbolized C with bar, Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million years ago (mya) to the beginning of the Ordovician Period mya. Its subdivisions, and its base, are somewhat in flux. The period was established as "Cambrian series" by Adam Sedgwick, who named it after Cambria, the Latin name for 'Cymru' (Wales), where Britain's Cambrian rocks are best exposed. Sedgwick identified the layer as part of his task, along with Roderick Murchison, to subdivide the large "Transition Series", although the two geologists disagreed for a while on the appropriate categorization. The Cambrian is unique in its unusually high proportion of sedimentary deposits, sites of exceptional preservation where "soft" parts of organisms are preserved as well as their more resistant shells. As a result, our understanding of the Ca ... [...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 precipitate from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lawren Harris
Lawren Stewart Harris LL. D. (October 23, 1885 – January 29, 1970) was a Canadian painter, best known as a leading member of the Group of Seven. He played a key role as a catalyst in Canadian art and as a visionary in Canadian landscape art. Early years Lawren Stewart Harris was born on October 23, 1885 in Brantford, Ontario. He was the son of Thomas Morgan Harris and Annabelle Stewart. His father was secretary to the firm of A. Harris, Sons & Company Ltd., merchants of farm machinery, which merged with the Massey firm in 1891, forming the Massey-Harris Company, later known as Massey Ferguson. Lawren Harris's share of the fortune that resulted made him free from financial cares the rest of his life. Although born to wealth, he was an individual who made his own path in his own individual way. In 1894, his father died and the family moved to Toronto. In 1899, he began to board at St. Andrew's College, which was located in Rosedale in Toronto at the time, then in 1903 attended ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Group Of Seven (artists)
The Group of Seven, once known as the Algonquin School, was a group of Canadian landscape painters from 1920 to 1933, originally consisting of Franklin Carmichael (1890–1945), Lawren Harris (1885–1970), A. Y. Jackson (1882–1974), Frank Johnston (1888–1949), Arthur Lismer (1885–1969), J. E. H. MacDonald (1873–1932), and Frederick Varley (1881–1969). Later, A. J. Casson (1898–1992) was invited to join in 1926, Edwin Holgate (1892–1977) became a member in 1930, and LeMoine FitzGerald (1890–1956) joined in 1932. Two artists commonly associated with the group are Tom Thomson (1877–1917) and Emily Carr (1871–1945). Although he died before its official formation, Thomson had a significant influence on the group. In his essay "The Story of the Group of Seven", Harris wrote that Thomson was "a part of the movement before we pinned a label on it"; Thomson's paintings '' The West Wind'' and ''The Jack Pine'' are two of the group's most icon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peter Sarbach
Peter Sarbach (1844 – 1930) was born in St. Niklaus, Switzerland, near the village of Zermatt; which is a historic village in the Shadow of the Matterhorn, the great mountain which divides the watershed from Switzerland and Italy. Prominence In 1864, Peter Sarbach was a porter for Sir Edward Whymper in one of his attempts to ascend the Matterhorn. Subsequently, he became a guide in the Swiss Alps and surrounding area. The competent guiding skills of Peter Sarbach were well renowned. At age 53, he was invited to Canada for an 1897 first ascent expedition of Mt. Lefroy; and hence he became the first Swiss guide to work in the Canadian Rockies. Canadian accomplishment The guiding skills of Peter Sarbach were commissioned, in a roundabout way, at the request of Edwin Hale Abbot, the father of Philip Stanley Abbot. Hence, together with John Norman Collie, Professor Harold Baily Dixon, George Percival Baker, Professor Charles Ernest Fay, and others, Peter Sarbach lead a memori ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
