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Peveril Peak
Peveril Peak is a mountain summit located in Alberta, Canada. Description Peveril Peak is set within Jasper National Park, in the Trident Range of the Canadian Rockies. The town of Jasper is situated to the north and the Continental Divide is to the west. The nearest higher neighbor is Terminal Mountain, to the north. The peak is visible from the Icefields Parkway to the east. Precipitation runoff from Peveril Peak drains into Portal Creek, a tributary of the Athabasca River. Topographic relief is significant as the summit rises 850 meters (2,790 feet) above the creek in one kilometer (0.6 mile). History The summit was first reached in 1926 by Bradley B. Gilman and his crew, who called it "Portal Peak."''The American Alpine News'' Issues 176-199 (1986), American Alpine Club, p. 17. The peak was named in 1932 after Sir Walter Scott's 1823 novel '' Peveril of the Peak'', and in turn the title refers to Peveril Castle. The mountain's toponym was officially ad ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trident Range
The South Jasper Ranges are mountain ranges of the Rocky Mountains in Alberta and British Columbia, Canada. It is a part of the Central Main Ranges of the Canadian Rockies, located on the Continental Divide, in Jasper National Park (Alberta) and Mount Robson Provincial Park (British Columbia). It contains the Meadow-Clairvaux, Fraser-Rampart, Trident Range and, most prominently, the Cavell Group of mountains and the headwaters of the Athabasca and Fraser River. The South Jasper Ranges covers a surface of 1,196 km2 (462 mi2), has a length of 39 km (from north to south) and a width of 49 km. Peaks and mountains #Mount Edith Cavell - # Simon Peak - # Throne Mountain - #Manx Peak - # Blackhorn Peak - #Roche Noire - #Chevron Mountain - #Terminal Mountain - # Lectern Peak - # Peveril Peak - # Muhigan Mountain - #Marmot Mountain - #The Whistlers The Whistlers is a mountain summit located in Jasper National Park, in the Trident Range of the Canadian R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peveril Of The Peak
''Peveril of the Peak'' (1823) is the longest novel by Sir Walter Scott. Along with ''Ivanhoe'', ''Kenilworth'', and ''Woodstock'' this is one of the English novels in the Waverley novels series, with the main action taking place around 1678 in the Peak District, the Isle of Man, and London, and centring on the Popish Plot. Plot introduction Julian Peveril, a Cavalier, is in love with Alice Bridgenorth, a Roundhead's daughter, but both he and his father are accused of involvement with the "Popish Plot" of 1678. Most of the story takes place in Derbyshire, London, and on the Isle of Man. The title refers to Peveril Castle in Castleton, Derbyshire. Composition and sources On 25 February 1822 Scott informed his Edinburgh publisher Archibald Constable that he was thinking of writing a novel about the Popish Plot. He seems to have begun composition of ''Peveril of the Peak'' immediately after completing ''The Fortunes of Nigel'' at the beginning of May and the first volume was compl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lectern Peak
Lectern Peak is a mountain summit located in Alberta, Canada. Description Lectern Peak is set within Jasper National Park, in the Trident Range of the Canadian Rockies. The town of Jasper is situated to the north and the Continental Divide is to the west. The nearest higher neighbor is Aquila Mountain, to the south. The peak is visible from the Icefields Parkway to the east. Precipitation runoff from Lectern Peak drains into Portal Creek and Astoria River which are both tributaries of the Athabasca River. Topographic relief is significant as the summit rises 900 meters (2,950 feet) above the creek in two kilometers (1.2 mile). A partial ascent of the mountain was made in 1913 by Geoffrey E. Howard who named the peak for its resemblance to a church lectern.Howard Palmer, James Monroe Thorington (1921), ''A Climber's Guide to the Rocky Mountains of Canada'', American Alpine Club, p. 151 He was accompanied by Arnold L. Mumm and Moritz Inderbinen on the exped ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marmot Mountain
Marmot Mountain is a mountain summit located in Alberta, Canada. Description Marmot Mountain is set within Jasper National Park, in the Trident Range of the Canadian Rockies. The town of Jasper is situated to the north and the Continental Divide is to the west. The nearest higher neighbor is Terminal Mountain, to the southwest. Precipitation runoff from Marmot Mountain drains into Portal Creek and Whistlers Creek which are both tributaries of the Athabasca River. Topographic relief is modest as the summit rises 1,550 meters (5,085 feet) above the Athabasca Valley in six kilometers (3.7 miles). The mountain was named in 1916 and the toponym was officially adopted February 7, 1951, by the Geographical Names Board of Canada. The name refers to the marmot, which are large ground squirrels which inhabit the slopes. The Whistlers, Siffleur Mountain and Arctomys Peak also owe their names to the marmot, an indication that the animal was a favorite of the early explore ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Whistlers (Alberta)
The Whistlers is a mountain summit located in Jasper National Park, in the Trident Range of the Canadian Rockies of Alberta, Canada. The municipality of Jasper is situated 7 kilometres to the northeast. Its nearest higher peak is Indian Peak, to the southwest. The highest and longest aerial tramway in Canada ascends to a lookout at 2,277 meters elevation, still 193 meters below the summit, but a hiking trail continues to the summit. Some of the mountains that can be seen (weather permitting) from the top include Mount Robson, Mount Bridgland, Monarch Mountain, Pyramid Mountain, Hawk Mountain, Mount Colin, Grisette Mountain, Mount Tekarra, Mount Hardisty, Mount Kerkeslin, Terminal Mountain, and Manx Peak. History The descriptive name ''The Whistlers'' was applied in 1916 by Édouard-Gaston Deville of the Geological Survey of Canada for the whistling inhabitants of the mountain, the hoary marmot. The mountain's name was officially adopted in 1951 by the Geographical Nam ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oldhorn Mountain
Oldhorn Mountain is a summit in Alberta, Canada. Description Oldhorn Mountain is located within Jasper National Park, in the Trident Range of the Canadian Rockies. The town of Jasper is situated to the north-northeast and the Continental Divide is to the west. The nearest higher neighbor is Throne Mountain, to the southeast. Precipitation runoff from Oldhorn drains south into the Astoria River and topographic relief is significant as the summit rises 1,320 meters (4,330 feet) above the river in two kilometers (1.2 mile). History The landform was named in 1916 by William Pittman Hinton (1871–1955), who attributed the shape of the mountain to that of a horn. The Oldhorn name appeared in print in the 1921 guidebook, ''"A Climber's Guide to the Rocky Mountains of Canada"''. The first ascent of the summit was made in 1924 by Lawrence Coolidge, George Higginson, and Joe Johnson, with guide Alfred Streich. The mountain's toponym was officially adopted on March 5, ... [...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] |
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] |
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 fossil ... [...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] |
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] |
