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Mount Tekarra
Mount Tekarra is a mountain summit located in the Athabasca River valley of Jasper National Park, in the Canadian Rockies of Alberta, Canada. It is situated at the northwest end of the Maligne Range and is visible from Jasper and the Icefields Parkway. The nearest higher neighbor is The Watchtower, to the east. __NOTOC__ History The mountain was named by James Hector in 1859 for Tekarra, an Iroquois guide and hunter who accompanied Hector during his exploration of the Athabasca River during the Palliser Expedition. The first ascent of Mount Tekarra was made in 1915 by Morrison P. Bridgland (1878-1948), a Dominion Land Surveyor who named many peaks in Jasper Park and the Canadian Rockies. The mountain's name was officially adopted in 1947 by the Geographical Names Board of Canada. Geology Mount Tekarra is composed of sedimentary rock laid down during the Cambrian period and pushed east and over the top of younger rock during the Laramide orogeny. Climate Based on the Köppen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maligne Range
The Maligne Range is a mountain range of the Canadian Rockies located directly southeast of Jasper townsite in Jasper National Park, Canada. The southern tail-end of the range finishes at Endless Chain Ridge. __NOTOC__ Mountains This range includes the following mountains and peaks: See also * Ranges of the Canadian Rockies The Canadian Rockies are a segment of the North American Rocky Mountains found in the Canadian provinces of Alberta and British Columbia. List of ranges There is no universally accepted hierarchical division of the Canadian Rockies into subrang ... References {{Canadian Rockies, state=collapsed Mountain ranges of Alberta Ranges of the Canadian Rockies Mountains of Jasper National Park ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roche Bonhomme
Roche Bonhomme is a mountain summit located in Jasper National Park in Alberta, Canada. It is located in the Colin Range, which is a sub-range of the Canadian Rockies. The peak is situated northeast of the municipality of Jasper, and is a prominent landmark in the Athabasca Valley visible from Highway 16 and the Canadian. Its nearest higher peak is Grisette Mountain, to the east. Roche Bonhomme was named in 1878 by George Munro Grant for the fact it has an anthropomorphic shape. The French "Roche Bonhomme" translates to "Rock Fellow." The mountain's name was officially adopted in 1947 by the Geographical Names Board of Canada. Roche Bonhomme is composed of Permian and Carboniferous strata topped by darker Triassic siltstone of the Sulphur Mountain Formation. __NOTOC__ Climate Based on the Köppen climate classification, Roche Bonhomme is located in a subarctic climate The subarctic climate (also called subpolar climate, or boreal climate) is a climate with long, co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Whistlers
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, Alberta, Jasper is situated 7 kilometres to the northeast. Its nearest higher peak is Indian Ridge (Alberta), Indian Peak, to the southwest. The highest and longest aerial Jasper Skytram, 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 (Alberta), Monarch Mountain, Pyramid Mountain (Alberta), Pyramid Mountain, Hawk Mountain (Alberta), 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 wh ... [...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] |
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] |
Maligne River
The Maligne River ( ) is a medium-sized river in the Canadian Rockies. It runs through parts of Jasper National Park in Alberta, Canada. The Maligne is a major tributary of the Athabasca River. The river takes from the French word for malignant or wicked. It is theorised that a Belgian priest (Pieter Jan De Smet ) voyageur created this name in reference to the current of the river near its confluence with the Athabasca River. Geography The Maligne River begins south of Maligne Lake. Forming from the meltwater of Replica Peak, the river heads north, passing under Mount Mary Vaux, Lysfran Peak, Mount Unwin, and Mount Charleton before emptying into Maligne Lake. The Maligne River drains the north end of Maligne Lake and heads northwest to Medicine Lake. It then flows west, entering the Athabasca River.Mussio Ventures. ''Central Alberta Backroad Mapbook.'' Burnaby: Backroad Mapbooks (2002) Below Maligne Lake, it is a losing stream A losing stream, disappearing stream, infl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surface Runoff
Surface runoff (also known as overland flow) is the flow of water occurring on the ground surface when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is saturated by water to its full capacity, and the rain arrives more quickly than the soil can absorb it. Surface runoff often occurs because impervious areas (such as roofs and pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or man-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. Runoff that occurs on the ground surface before reaching a channel can be a nonpoint source of pollution, as it can carry man-made contaminants or natural forms of pollution (such as rotting leaves). Man-made contaminants in runoff i ... [...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] |
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] |
