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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] |
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 - #Tonquin Hill Tonquin Hill is located on the border of Alberta and British Columbia. It was named in 1916 by E ... [...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 Na ... [...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] |
Icefields Parkway
Highway 93 is a north–south highway in Alberta, Canada. It is also known as the Banff-Windermere Parkway south of the Trans-Canada Highway ( Highway 1) and the Icefields Parkway north of the Trans-Canada Highway. It travels through Banff National Park and Jasper National Park and is maintained by Parks Canada for its entire length. It runs from the British Columbia border at Vermilion Pass in the south, where it becomes British Columbia Highway 93, to its terminus at the junction with the Yellowhead Highway ( Highway 16) at Jasper. The route takes its number from U.S. Route 93, which runs uninterrupted south to central Arizona, and was initially designated as '93' in 1959. Route description Banff-Windermere Highway The southern portion of the route is part of the Banff-Windermere Highway, a highway that travels from British Columbia Highway 95 at Radium Hot Springs, through Kootenay National Park and Vermilion Pass across the Continental Divide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
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 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] |
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] |
Marmot Basin
Marmot Basin is an alpine ski area located on Marmot Mountain in Alberta's Jasper National Park. It has 91 named runs on four mountain faces with 3,000 vertical feet of drop. The area has a lift capacity of close to 12,000 skiers per hour on seven lifts. The season runs from mid-November to early May. It is located twenty minutes south of Jasper and sees two million visitors a year. Amenities The Rental & Repair shop offers rentals of skis, snowboards, boots, and poles. The Snow Sports School offers lessons, clinics, and a variety of children's programs. There are three mountain day lodges: Caribou Chalet at the base area and Eagle and Paradise Chalets at mid-mountain. There is no current overnight on-mountain lodging at Marmot Basin. Marmot Basin has three terrain parks on the mountain, which feature various rail slides, table tops, and jumps. Marmot offers a terrain park in the Lower, Mid, and Upper Mountains. Lift system Former lifts * Tranquilizer Chair (Double Chair) - ... [...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] |
