Mount Wilcox (Alberta)
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Mount Wilcox (Alberta)
Mount Wilcox (also known as Wilcox Peak) is a mountain summit located in the Canadian Rockies of Alberta, Canada. It is located in Jasper National Park right beside the Columbia Icefield visitor centre with the Icefields Parkway traversing the western base of the mountain. Its nearest higher peak is Nigel Peak, to the northeast. Mount Wilcox is a moderate scramble from Wilcox Pass. Due to its location, it provides one of the best views of the Athabasca Glacier. History The mountain was named Wilcox Peak by J. Norman Collie in 1899 after Walter D. Wilcox, an early explorer of the Canadian Rockies who also made the first ascent of the peak in 1896. The mountain's ''Wilcox Peak'' name was officially adopted in 1924 by the Geographical Names Board of Canada. The Board changed it to Mount Wilcox in 1928, until ultimately reverting to Wilcox Peak in 1956. Climate Based on the Köppen climate classification, Wilcox Peak is located in a subarctic climate with cold, snowy winters, and ...
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Columbia Icefield
The Columbia Icefield is the largest ice field in North America's Rocky Mountains. Located within the Canadian Rocky Mountains astride the Continental Divide along the border of British Columbia and Alberta, Canada, the ice field lies partly in the northwestern tip of Banff National Park and partly in the southern end of Jasper National Park. It is about in area, to in depth and receives up to of snowfall per year. History The Columbia Icefield was formed during the Great Glaciation, or Illinoisan period (238,000 to 126,000 BCE).Sandford 1993, p. 23. The initial advancement of the ice field ended during the latter millennia of the Early Wisconsinan period (73,000 to 62,000 BCE), around the time ''Homo sapiens'' began to appear on the earth. The next major advance of the ice field occurred during the Late Wisconsinan period (18,000 to 9,000 BCE), which marked the end of the major intercontinental land mass bridges. During the Crowfoot Glacier advance (9,000 to 7,000 BCE) ...
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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 Observation), Pa ...
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Scrambles In The Canadian Rockies
''Scrambles'' is the fifth studio album by Bomb the Music Industry!, released digitally and physically on February 15th, 2009. The album was released a year and a half after Get Warmer, making it the longest gap between the release of two chronologically adjacent Bomb the Music Industry! albums. Frontman Jeff Rosenstock aimed to record the album on a limited budget of $50; up to that point, the band had never spent that much money on the recording of an album. In 2019, to celebrate the album's 10th anniversary, a compilation of demos for the album was released by Rosenstock. Recording and composition In November 2007, the band announced they were in the demo and writing phase for their next album; alongside this, they posted a demo of "25" on their Myspace profile. A demo for "Fresh Attitude Young Body" was posted online on March 30, 2008, followed by several others for a limited time. In September 2008, the band played a few East Coast shows with the Riot Before. On October 6, ...
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List Of Mountains In The Canadian Rockies
A list of highest peaks in the Canadian Rockies is shown below: References ;Notes {{reflist, group=notes *• Canadian Rockies The Canadian Rockies (french: Rocheuses canadiennes) or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part ... Mountains, Rockies Mountains, Rockies ...
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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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Mount Andromeda (Alberta)
Mount Andromeda is located within the Columbia Icefield on the boundary of Banff and Jasper national parks. The mountain can be seen from the Icefields Parkway (#93) near Sunwapta Pass and is 2.3 km WSW of Mount Athabasca. Mt. Andromeda was named in 1938 by Rex Gibson, former president of the Alpine Club of Canada, after Andromeda, the wife of Perseus In Greek mythology, Perseus (Help:IPA/English, /ˈpɜːrsiəs, -sjuːs/; Greek language, Greek: Περσεύς, Romanization of Greek, translit. Perseús) is the legendary founder of Mycenae and of the Perseid dynasty. He was, alongside Cadmus .... From the Climber's Guide: * "A deservedly popular peak, well seen and easily accessible from the Icefields campground via the road to the snowmobile parking lot." Routes There are several mountaineering and climbing routes on Andromeda. The ''Skyladder'' is the normal and very popular glacier route. References External linksMt. Andromeda on SummitPost Three-thousanders ...
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Tangle Ridge
Tangle Ridge is a mountain summit located in Jasper National Park, in the Canadian Rockies of Alberta, Canada. Tangle Ridge is situated south of Beauty Creek and north of Tangle Creek, in the Sunwapta River valley. Topographic relief is significant as the summit rises 1,200 metres (3,937 ft) above Beauty Creek in . Views from the top of Tangle Ridge provide photographers with an opportunity to capture the peaks surrounding the Columbia Icefield, some of which, such as Mount Columbia and Mount Alberta, are otherwise hidden from view along the Icefields Parkway. __NOTOC__ History The mountain was named by Mary Schäffer in 1907 for the difficulty that climbers had descending down Tangle Creek from the ridge. The mountain's toponym was officially adopted in 1935 by the Geographical Names Board of Canada. Climate Based on the Köppen climate classification, Tangle Ridge is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures ...
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Athabasca River
The Athabasca River (French: ''Rivière Athabasca'') is a river in Alberta, Canada, which originates at the Columbia Icefield in Jasper National Park and flows more than before emptying into Lake Athabasca. Much of the land along its banks is protected in national and provincial parks, and the river is designated a Canadian Heritage River for its historical and cultural importance. The scenic Athabasca Falls is located about upstream from Jasper. Etymology The name ''Athabasca'' comes from the Woods Cree word , which means "herethere are plants one after another", likely a reference to the spotty vegetation along the river. Course The Athabasca River originates in Jasper National Park, in an unnamed lake at the toe of the Columbia Glacier within the Columbia Icefield, between Mount Columbia, Snow Dome, and the Winston Churchill Range, at an elevation of approximately . It travels before draining into the Peace-Athabasca Delta near Lake Athabasca south of Fort Chipewyan. Fr ...
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Sunwapta River
The Sunwapta River is a major tributary of the Athabasca River in Jasper National Park in Alberta, Canada. Course The headwaters of the Sunwapta River are near the Columbia Icefield in the valley west-northwest of Sunwapta Pass, which divides Jasper National Park from Banff National Park. Several kilometres down the valley from the pass is Sunwapta Lake, at the toe of the Athabasca Glacier, which is considered the nominal source for the river. The Sunwapta River then continues to run northwest through Jasper National Park, following the Icefields Parkway, and finally joins the Athabasca River shortly after Sunwapta Falls. ''Sunwapta'' is a Stoney language word meaning "turbulent river". Geologist A. P. Coleman named the river in 1892.Karamitsanis, Aphrodite (1991). ''Place Names of Alberta, Volume 1''. Calgary: University of Calgary Press, pg. 240 Tributaries *Kitchener Creek *Tangle Creek *Woolley Creek *Beauty Creek *Diadem Creek *Grizzly Creek *Jonas Creek *Poboktan Cree ...
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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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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 ...
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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'' indi ...
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