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Roche Noire (Alberta)
Roche Noire is a mountain located in Alberta, Canada. Description The mountain is set within Jasper National Park, in the Trident Range of the Canadian Rockies. The town of Jasper is situated to the east-northeast, Muhigan Mountain is to the east, and the Continental Divide is to the west. The peak is composed of sedimentary rock laid down from the Precambrian to the Jurassic periods and pushed east and over the top of younger rock during the Laramide orogeny. Precipitation runoff from Roche Noire drains into tributaries of the Miette River. Topographic relief is significant as the summit rises 1,400 meters (4,593 feet) above Meadow Creek in three kilometers (1.9 mile). History The mountain was named in 1916 by Morrison P. Bridgland, and the words "Roche Noire" are French, meaning "black rock", referring to the color of the summit.Morrison Parsons Bridgland, Robert Douglas, Édouard Deville (1917), ''Description of & Guide to Jasper Park'', Canada Department ...
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Pyramid Lake (Alberta)
Pyramid Lake is a kidney-shaped lake in Jasper National Park, Alberta, Canada. It lies at the foot of Pyramid Mountain Pyramid Mountain can refer to: ;Antarctica * Pyramid Mountain (Antarctica), in the Quartermain Mountains ;Canada *Pyramid Mountain (Alberta) in Jasper National Park, Alberta * Pyramid Mountain (Garibaldi Provincial Park) in Garibaldi Provincial P ..., a natural landmark that overlooks the town of Jasper. It has a total area of and discharges in Athabasca River through the long Pyramid Creek. Several picnic sites are established on the shores of the lake, as well as boat ramps. Pyramid Lake Resort is located on the southeast point of the lake. Pyramid Island is a short distance from the resort, there is a small parking area which can be accessed by a road or hiking trails, then you cross a small wood foot bridge to the island itself, which has benches, picnic tables and a small open wooden shelter. Pyramid Lake is connected to the town of Jasper by Pyramid ...
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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 ...
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Two-thousanders Of Alberta
Two-thousanders are mountains that have a height of at least 2,000 metres above sea level, but less than 3,000 metres. The term is used in Alpine circles, especially in Europe (e.g. German: ''Zweitausender''). The two photographs show two typical two-thousanders in the Alps that illustrate different types of mountain. The Säuling (top) is a prominent, individual peak, whereas the Schneeberg (bottom) is an elongated limestone massif. In ranges like the Allgäu Alps, the Gesäuse or the Styrian-Lower Austrian Limestone Alps the mountain tour descriptions for mountaineers or hikers commonly include the two-thousanders, especially in areas where only a few summits exceed this level. Examples from these regions of the Eastern Alps are: * the striking Nebelhorn (2,224 m) near Oberstdorf or the Säuling (2,047 m) near Neuschwanstein, * the Admonter Reichenstein (2,251 m), Eisenerzer Reichenstein (2,165 m), Großer Pyhrgas (2,244 m) or Hochtor (2,369  ...
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Yellowhead Pass
The Yellowhead Pass is a mountain pass across the Continental Divide of the Americas in the Canadian Rockies. It is located on the provincial boundary between the Canadian provinces of Alberta and British Columbia, and lies within Jasper National Park and Mount Robson Provincial Park. Due to its modest elevation of and its gradual approaches, the pass was recommended by Sir Sandford Fleming as a route across the Rocky Mountains for the planned Canadian Pacific Railway. The proposal was rejected in favour of a more direct and southerly route, through the more difficult Kicking Horse Pass, which was opened in 1886. However, both the Grand Trunk Pacific and Canadian Northern Railways used the Yellowhead Pass for their main lines, built c. 1910–1913, and the main line of their successor, the Canadian National Railway, still follows the route. Via Rail's premier passenger train, the ''Canadian''; the Jasper – Prince Rupert train; and the Jasper section of the '' Rocky Moun ...
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Basilica Mountain
Basilica Mountain is a summit A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. The topography, topographic terms acme, apex, peak (mountain peak), and zenith are synonymous. The term (mountain top) is generally used ... in Alberta, Canada located between Clairvaux Creek and Meadow Creek. Basilica Mountain was so named on account of its basilica-shaped outline. See also * List of mountains in the Canadian Rockies References Two-thousanders of Alberta Alberta's Rockies {{AlbertaRockies-geo-stub ...
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Tonquin Valley
The Tonquin Valley is located in Jasper National Park, Alberta, Canada, next to the border of the provinces of Alberta and British Columbia, an area which is also the continental divide, running along the peaks of the South Jasper Range (including The Ramparts subrange) which rise above Amethyst Lake. Tonquin Creek drains Moat Lake and flows west into Mount Robson Provincial Park in British Columbia, and empties into the Fraser River. The Astoria River drains south and east into the Athabasca River. The Tonquin Valley leads to Tonquin Pass which cradles the Amythyst Lakes at its crest beneath the Precambrian quartzite wall of the Ramparts. The valley was named after the Pacific Fur Company ship '' Tonquin'', destroyed in Clayoquot Sound in 1811. Recreation Within the valley there is the scenic Amethyst Lake and Moat Lake. It is a popular destination for back-country hikers, ski touring and horseback trips to the two outfitters camps on the shores of Amethyst Lake. There are ...
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Yellowhead Highway
The Yellowhead Highway (french: Route Yellowhead) is a major interprovincial highway in Western Canada that runs from Winnipeg to Graham Island off the coast of British Columbia via Saskatoon and Edmonton. It stretches across the four western Canadian provinces of British Columbia, Alberta, Saskatchewan, and Manitoba and is part of the Trans-Canada Highway system and the larger National Highway System, but should not be confused with the more southerly, originally-designated Trans-Canada Highway. The highway was officially opened in 1970. Beginning in 1990, the green and white Trans-Canada logo was used to designate the roadway. The highway is named for the Yellowhead Pass, the route chosen to cross the Canadian Rockies. The pass and the highway are named after a fur trader and explorer named Pierre Bostonais. He had yellow streaks in his hair, and was nicknamed " Tête Jaune" (Yellowhead). Almost the entire length of the highway is numbered as 16, except for the section ...
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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 ...
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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 ...
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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 ...
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Geographical Names Board Of Canada
The Geographical Names Board of Canada (GNBC) is a national committee with a secretariat in Natural Resources Canada, part of the Government of Canada, which authorizes the names used and name changes on official federal government maps of Canada created since 1897. The board consists of 27 members, one from each of the provinces and territories, and others from departments of the Government of Canada. The board also is involved with names of areas in the Antarctic through the Antarctic Treaty. Structure The secretariat is provided by Natural Resources Canada. In addition to the provincial and territorial members are members from the following federal government departments: Aboriginal Affairs and Northern Development Canada, Canada Post Corporation, Fisheries and Oceans Canada, Elections Canada, Library and Archives Canada, Department of National Defence, Natural Resources Canada (including Geological Survey of Canada and Canada Centre for Mapping and Earth Observatio ...
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Dominion Land Survey
The Dominion Land Survey (DLS; french: links=no, arpentage des terres fédérales, ATF) is the method used to divide most of Western Canada into one-square-mile (2.6 km2) sections for agricultural and other purposes. It is based on the layout of the Public Land Survey System used in the United States, but has several differences. The DLS is the dominant survey method in the Prairie provinces, and it is also used in British Columbia along the Railway Belt (near the main line of the Canadian Pacific Railway), and in the Peace River Block in the northeast of the province. (Although British Columbia entered Confederation with control over its own lands, unlike the Northwest Territories and the Prairie provinces, British Columbia transferred these lands to the federal Government as a condition of the building of the Canadian Pacific Railway. The federal government then surveyed these areas under the DLS.)
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