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Big Bend Peak
Big Bend Peak is a mountain summit located in the upper North Saskatchewan River valley in Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Saskatchewan, to the south. Big Bend Peak is situated on the west side of the Icefields Parkway four kilometres southwest of the "big bend" in the road, hence the peak's name origin. Geology Like other mountains in Banff Park, Big Bend Peak is composed of sedimentary rock laid down from 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, Big Bend Peak is 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. Precipitation runoff from Big Bend Peak drains into the North Saskatchewan River. Gallery File:Big Bend Peak.jpg, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Big Bend Ranges
The Big Bend Ranges are a subrange of the Selkirk Mountains of the Columbia Mountains in southeastern British Columbia, Canada, located in Big Bend of the Columbia River north of the Illecillewaet River. Sub-ranges * Adamant Range *Sir Sandford Range *Windy Range Gallery File:Downie Peak, British Columbia.jpg, Aerial view of the Big Bend Ranges, camera pointed north, with Downie Peak Downie Peak is a mountain summit located in British Columbia, Canada. Description Part of the Selkirk Mountains, Downie Peak is situated north of Revelstoke and east of Lake Revelstoke. Prominently visible from nearly every peak in the Nor ... centered References *Big Bend Rangesin the Canadian Mountain Encyclopedia Kootenay Land District {{BritishColumbiaInterior-mountain-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. 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'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Athabasca
Mount Athabasca is in the Columbia Icefield of Jasper National Park in Canada. The mountain was named in 1898 by J. Norman Collie, who made the first ascent on August 18 of that year. Athabasca is the Cree language name for "where there are reeds", which originally referred to Lake Athabasca. Mount Athabasca is unusual, in that water flows to the Pacific Ocean from the western slope, the Arctic Ocean from the northeastern slope, and to Hudson Bay from the southeastern slope.Geography of Alberta __NOTOC__ Routes There are several climbing routes, including: * North Glacier (Normal Route) II * Silverhorn II * AA Col II * Regular North Face III 5.8 * North Ridge III 5.5 * The Hourglass 300m, III, AI3-4 One of the most prominent features of Mount Athabasca is a horned-shaped tip near the top called the "Silverhorn". The Silverhorn is one of the easier routes to the summit but requires more caution and ability than the normal route because of blue ice and falling ice from other pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saskatchewan Glacier
The Saskatchewan Glacier is located in Banff National Park, Alberta, Canada, approximately northwest of the town of Banff, and can be accessed from the Icefields Parkway. Saskatchewan Glacier is the largest outflow glacier from the Columbia Icefield, which rests along the Continental Divide. The glacier is a primary water source for the North Saskatchewan River. The glacier is approximately long and covers an area of 30 km2 (11.5 mi2) and was measured in 1960 to be over thick at a distance of from the terminal snout. Between the years 1893 and 1953, Saskatchewan Glacier had receded a distance of , with the rate of retreat between the years 1948 and 1953 averaging per year. The glacier, which flows northeast, exhibits a prominent medial morraine. See also *List of glaciers in Canada A comprehensive list of glaciers in Canada began with glacial surveys by the Water Survey of Canada (WSC) from 1945 to 1980, including an inventory begun for the International Ge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Castleguard Mountain
Castleguard Mountain, also known as Mount Castleguard, is an isolated mountain located near the southern edge of the Columbia Icefield at the northern edge of Banff National Park in Alberta, Canada. In 1918, Irish land surveyor Arthur Oliver Wheeler named the mountain because of its castle-like appearance, which seemed to stand guard over the southern portion of the Columbia Icefield. Castleguard was first ascended in 1919 by the Interprovincial Boundary Commission, which determined the exact location of the boundary between British Columbia and Alberta along the continental divide. Author Lewis Freeman, in his 1925 book ''Roof of the Rockies'', described the view from the summit: Geology Castleguard 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, Castleguard is loc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Coleman (Alberta)
Mount Coleman is a mountain summit located in the upper North Saskatchewan River valley in Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Cirrus Mountain, to the north. Mount Coleman is situated along the east side the Icefields Parkway midway between Saskatchewan Crossing and Sunwapta Pass. __NOTOC__ History Mount Coleman was named in 1898 after Arthur P. Coleman (1852-1939), a Canadian geologist and among the first white men to explore the area that is now Jasper National Park. Geology Like other mountains in Banff Park, Mount Coleman is composed of sedimentary rock laid down from 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 Coleman is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirrus Mountain
Cirrus Mountain is a mountain summit located in the upper North Saskatchewan River valley on the shared boundary between Banff National Park and White Goat Wilderness Area, in the Canadian Rockies of Alberta, Canada. Cirrus Mountain is situated along the east side the Icefields Parkway midway between Saskatchewan Crossing and Sunwapta Pass. Topographic relief is significant as the summit rises above the parkway in . The nearest higher peak is Mount Stewart, to the north-northeast. History In 1928, Morrison P. Bridgland suggested the name ''Mount Huntington'' for the mountain, but it was not adopted. However, the Huntington name endures as the name of the ''Huntington Glacier'' below the eastern aspect of the summit. The mountain was instead named Cirrus Mountain, and that toponym was officially adopted in 1935 by the Geographical Names Board of Canada. The first ascent of the mountain was accomplished in 1939 by C.B. Sissons and H.J. Sissons. Geology Like other mountains i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Parker Ridge
Parker Ridge is a mountain ridge located in the upper North Saskatchewan River valley in Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Athabasca, to the west. Parker Ridge is situated along the west side of the Icefields Parkway and southeast of Sunwapta Pass. Parker Ridge is a ski-touring destination in the winter and popular hiking destination in the summer because it is situated beside the Icefields Parkway allowing easy access, and is nearly entirely above treeline allowing good views of the surrounding mountain landscape. A trail gains of elevation from the highway to the top of the ridge. Wandering east or west along the ridge provides views of Cirrus Mountain, the north face of Mount Saskatchewan, Saskatchewan Glacier, Mount Athabasca, Hilda Peak, and Nigel Peak among others. History Parker Ridge was named for Elizabeth Parker (1856–1944), co-founder of the Alpine Club of Canada in 1906 along with Arthur Olive ... [...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. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains Of Canada
Most mountain peaks of Canada lie in the west, specifically in British Columbia, Alberta, and the Yukon. Mountains can be found all over British Columbia while those in Alberta are mainly situated on the eastern side of the Canadian Rockies. The Saint Elias Mountains in the Yukon hold some of country's highest mountains, including the highest, Mount Logan Mount Logan ( ) is the highest mountain in Canada and the second-highest peak in North America after Denali (McKinley). The mountain was named after Sir William Edmond Logan, a Canadian geologist and founder of the Geological Survey of Canada ... at . Alberta ;Highest peaks Mts. Columbia & King Edward.jpg, Mount Columbia & Mount King Edward, King Edward in background The Twins - South and North (l-r).jpg, The Twins massif - South Twin Peak, South Twin and North Twin (l-r) Mount Assiniboine massif.jpg, Mount Assiniboine seen from above Lake Magog Columbia Icefields - panoramio (1).jpg, Snow Dome seen from Icefields Pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surface Runoff
Surface runoff (also known as overland flow or terrestrial runoff) is the unconfined flow of water over the ground surface, in contrast to ''channel runoff'' (or ''stream flow''). It occurs when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is #Saturation excess overland flow, saturated by water to its full capacity, and the rain arrives #Infiltration excess overland flow, more quickly than the soil can absorb it. Surface runoff often occurs because wikt:impervious#Adjective, impervious areas (such as roofs and Road surface, pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or human-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of Soil erosion#Rainfall and runoff, soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
