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Mount Julian (Alberta)
Mount Julian is a peak located at the southern end of Maligne Lake in Jasper National Park, Alberta, Canada. The mountain was named in 1928 by Leo Amery for his son Julian David Faber - ''Speaking for England''. The mountain was first climbed in 1930 by J.A. Corry, C.G. Crawford, E.M. Gillespie, J. McAuley, M. Percy, R. Rushworth, G. Shanger, and I. Vanderberg. Geology Mount Julian 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 Julian is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. See also * * Geography of Alberta Alberta is one of the thirteen provinces and territories of Canada. Located in Western Canada, the province has an area ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Julian Amery
Harold Julian Amery, Baron Amery of Lustleigh, (27 March 1919 – 3 September 1996) was a British Conservative Party politician, who served as a Member of Parliament (MP) for 39 of the 42 years between 1950 and 1992. He was appointed to the Privy Council in 1960. Amery was created a life peer upon his retirement from the House of Commons in 1992. For three decades, he was a leading figure in the Conservative Monday Club. He was the son-in-law of Conservative prime minister Harold Macmillan. His brother, John, was hanged for high treason for supporting Nazi Germany and Fascist Italy during the Second World War. Early and family life Amery was born in Chelsea, London. His father was Leo Amery, a British statesman and Conservative politician. He was educated at Eaton House, Summer Fields School, Eton College and Balliol College, Oxford. While an undergraduate, he had a brief romance with the future novelist Barbara Pym, who was six years his senior. Military service B ... [...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] |
Mount Paul
Mount Paul is a mountain summit towering 1134 metres above the east shore of Maligne Lake in Jasper National Park, in the Canadian Rockies of Alberta, Canada. The nearest higher peak is Maligne Mountain, to the north-northwest. Mount Paul is situated north of Monkhead and they are often seen together in the background of iconic calendar photos of Spirit Island and Maligne Lake. __NOTOC__ History Mount Paul was named by Mary Schäffer after Paul Sharples, Mary's nine year old nephew who accompanied her on her second expedition to Maligne Lake in 1911. Mary originally referred to this mountain as ''The Thumb'' during her first successful expedition to Maligne Lake in 1908. The first ascent of Mount Paul was made in 1928 by W.R. Hainsworth and M.M. Strumia This mountain's name was officially adopted in 1946 by the Geographical Names Board of Canada. Climate Based on the Köppen climate classification, Mount Paul is located in a subarctic climate with cold, snowy winters, and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Alberta
Alberta is one of the thirteen provinces and territories of Canada. Located in Western Canada, the province has an area of and is bounded to the south by the United States state of Montana along 49° north for ; to the east at 110° west by the province of Saskatchewan for ; and at 60° north the Northwest Territories for . The southern half of the province borders British Columbia along the Continental Divide of the Americas on the peaks of the Rocky Mountains, while the northern half borders British Columbia along the 120th meridian west. Along with Saskatchewan it is one of only two landlocked provinces or territories. Terrain Alberta's landscape is marked by the impact of the Wisconsin Glaciation, about 75,000 to 11,000 years ago, when the entire future province was covered in ice. As the ice sheet receded, the landscape was changed, and large amounts of glacial till were left behind. The southern portion consists chiefly of plains that are almost entirely treeless. As ... [...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 a ... [...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] |
David Faber (schoolmaster)
David James Christian Faber (born 7 July 1961) is a schoolmaster and former Conservative member of the Parliament of the United Kingdom. He did not seek re-election in 2001, after which he became an author, before in 2010 being appointed as head master of Summer Fields School, Oxford. He is the grandson of the late former Conservative Prime Minister Harold Macmillan (1894–1986). Family and early life The son of Julian and Lady Caroline Faber, Faber comes from an aristocratic political family drawn from the Whig and latterly the Conservative traditions. His maternal grandfather Harold Macmillan was Prime Minister at the time of his birth. His maternal grandmother, Lady Dorothy Cavendish, was descended from three Prime Ministers, the 4th Duke of Devonshire (1756–1757), the 2nd Earl of Shelburne (1782–1783) and the 3rd Duke of Portland (1783 and 1807–1809). Faber's great-great-great-granduncle was Lord Hartington and his great-grandfather Victor Cavendish, 9th Duke of Dev ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Queen Elizabeth Ranges
The Queen Elizabeth Ranges is a group of mountain ranges in the Canadian Rockies on the southeastern side of Jasper National Park, Canada. The northern end of the ranges begins east of Medicine Lake and extends in a southeasterly direction past the southern shore of Maligne Lake. The group was named in 1953 to celebrate the coronation of Elizabeth II The coronation of the British monarch, coronation of Elizabeth II took place on 2 June 1953 at Westminster Abbey in London. She acceded to the throne at the age of 25 upon the death of her father, George VI, on 6 February 1952, being Proclamati ... as Canada's sovereign. These ranges include the following mountains and peaks: References Mountains of Jasper National Park Mountain ranges of Alberta Queen Elizabeth Ranges {{AlbertaRockies-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Julian Amery, Baron Amery Of Lustleigh
Harold Julian Amery, Baron Amery of Lustleigh, (27 March 1919 – 3 September 1996) was a British Conservative Party politician, who served as a Member of Parliament (MP) for 39 of the 42 years between 1950 and 1992. He was appointed to the Privy Council in 1960. Amery was created a life peer upon his retirement from the House of Commons in 1992. For three decades, he was a leading figure in the Conservative Monday Club. He was the son-in-law of Conservative prime minister Harold Macmillan. His brother, John, was hanged for high treason for supporting Nazi Germany and Fascist Italy during the Second World War. Early and family life Amery was born in Chelsea, London. His father was Leo Amery, a British statesman and Conservative politician. He was educated at Eaton House, Summer Fields School, Eton College and Balliol College, Oxford. While an undergraduate, he had a brief romance with the future novelist Barbara Pym, who was six years his senior. Military service Befo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
