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Fairview Mountain (Alberta)
Fairview Mountain (sometimes called Mount Fairview) is a mountain in Banff National Park situated along the southeastern shoreline of Lake Louise. The mountain was named in 1894 by Walter Wilcox, which reflects the view from the top. An alternate name for the peak is ''Goat Mountain'' although it is rarely referred to as such. While imposing cliffs seen from Lake Louise may indicate a difficult climb, the mountain is easily ascended by experienced hikers via a trail around the backside on the southern slopes of the mountain. Geology Fairview Mountain is composed of sedimentary rock laid down during the Cambrian period. 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, Fairview is located 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bow Range
The Bow Range is a mountain range of the Canadian Rockies in Alberta and British Columbia, Canada. The range is named in associated with the Bow River and was officially adopted on March 31, 1917 by the Geographic Board of Canada. It is a part of the Banff- Lake Louise Core Area of the Southern Continental Ranges, located on the Continental Divide, west of the Bow River valley, in Banff National Park and Kootenay National Park. The Bow Range covers a surface area of 717 km2 (277 mi2), has a length of 34 km (from north to south) and a maximum width of 43 km. The highest peak is Mount Temple, with an elevation of . The range also covers the Valley of the Ten Peaks, with the tallest of the ten being Mount Hungabee at 3492 metres. The range also has hiking areas such as the Consolation Lakes, Sentinel Pass-Larch Valley, Wenkchenma Pass-Eiffel Lake, the Beehive plain of the Six Glaciers system and Saddle Back Pass. __NOTOC__ Peaks and mountains See also * R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cambrian
The Cambrian Period ( ; sometimes symbolized C with bar, Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million years ago (mya) to the beginning of the Ordovician Period mya. Its subdivisions, and its base, are somewhat in flux. The period was established as "Cambrian series" by Adam Sedgwick, who named it after Cambria, the Latin name for 'Cymru' (Wales), where Britain's Cambrian rocks are best exposed. Sedgwick identified the layer as part of his task, along with Roderick Murchison, to subdivide the large "Transition Series", although the two geologists disagreed for a while on the appropriate categorization. The Cambrian is unique in its unusually high proportion of sedimentary deposits, sites of exceptional preservation where "soft" parts of organisms are preserved as well as their more resistant shells. As a result, our understanding of the Ca ... [...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 Eastern Alps is the name given to the eastern half of the Alps, usually defined as the area east of a line from Lake Constance and the Alpine Rhine valley up to the Splügen Pass at the Alpine divide and down the Liro River to Lake Como in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Niblock
Mount Niblock is a mountain in Banff National Park near Lake Louise, Alberta, Canada. The mountain was named in 1904 after John Niblock, a superintendent with the Canadian Pacific Railway. Niblock was an early promoter of tourism in the Rockies and influenced the naming of some of the CPR stops in Western Canada. Mt. Niblock is a popular scramble in the Lake Louise area and is sometimes combined in the same day with Mount Whyte (), although the latter is a more difficult scramble. The best time for climbing Mt. Niblock is July through September when the normal route is usually free of snow. Attempting it in the spring or early summer may include significant avalanche hazard. To access Mt. Niblock, follow the trail as it begins near Chateau Lake Louise, passes Mirror Lake and then Lake Agnes. Follow the right hand shore line trail to the far end of the lake until it begins its left turn towards the Big Beehive. Here an obvious path can be found leading to the lower scree slop ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Whyte
Mount Whyte is a mountain in Alberta, Canada located in Banff National Park, near Lake Louise. The mountain can be seen from the Trans-Canada Highway, and offers views of the Valley of the Ten Peaks, including the Chateau Lake Louise. The mountain is also visible from the hiking trail that skirts the northern shore of Lake Agnes. The mountain was named in 1898 by Sir William Methuen after William Whyte, a representative of the Canadian Pacific Railway. Climbing Mt. Whyte is usually combined with Mount Niblock () when done as a scramble. However, while Mt. Niblock is rated a moderate scramble, Mt. Whyte is much more difficult due to additional exposure and loose rock. The scramble should not be attempted in snowy conditions due to considerable fall distance which would likely prove fatal. For rock climbers, the Perren Route (II 5.6) is another option. While mostly a scramble as well, a short section of difficult climbing near the top in addition to route finding challenges ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saddle Mountain (Alberta)
Saddle Mountain is a summit in Alberta, Canada. Description Saddle Mountain is located in the Bow Valley within Banff National Park, and it is part of the Bow Range of the Canadian Rockies. Lake Louise, Alberta, Lake Louise townsite is situated to the northeast and the Continental Divide is to the west. The nearest higher neighbor is Fairview Mountain (Alberta), Fairview Mountain, to the northwest. Precipitation runoff from Saddle Mountain drains into tributaries of the Bow River. Topographic relief is modest as the summit rises over 600 meters (1,968 ft) above Paradise Creek in one kilometer (0.6 mile) and nearly 900 meters (2,953 ft) above Bow River in . The peak is visible from Alberta Highway 1 to the east, and is prominent in the iconic photographs taken from Nicholas Morant, Morant's Curve. Access The Paradise Valley Trail leads from Lake Louise (Alberta), Lake Louise to Saddleback Pass, and from the pass an off-trail scramble leads to the top of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haddo Peak
Haddo Peak is a summit in Alberta, Canada. Haddo Peak is located in the Lake Louise area of Banff National Park. Haddo Peak honors the name of George Gordon, Lord Haddo. Named in 1916, the name became official in 1952. Geology Like other mountains in Banff Park, Haddo 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, Haddo Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below with wind chill factors below . Weather conditions during summer months are optimum for climbing. See also * List of mountains in the Canadian Rockies * Geology of Alberta The geology of Alberta encompasses parts of the Canadian Rockies and thick sedimentary sequences, bearing coal, oil and natural gas, atop complex Pre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Lefroy
Mount Lefroy is a mountain on the Continental Divide, at the border of Alberta and British Columbia in western Canada. The mountain is located on the eastern side of Abbot Pass which separates Lake Louise in Banff National Park from Lake O'Hara in Yoho National Park. Mount Victoria lies immediately on the western side of the pass. The mountain was named by George M. Dawson in 1894 for Sir John Henry Lefroy (1817–1890), an astronomer who had traveled over in Canada's north between 1842 and 1844 making meteorological and magnetic observations. The mountain is the site of the first fatal climbing accident in Canada. In 1896 during a failed summit bid, Philip Stanley Abbot slipped on rocks after just coming off an icy section and plummeted down the rock face to his death. The first successful ascent was made in 1897 by J. Norman Collie, Arthur Michael, H. Dixon; Charles Fay, Peter Sarbach, R. Vanderlip, C. Noyes, Charles Thompson, and H. Parker. A prominent painting by Can ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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, ... [...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 ave ... [...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'' indi ... [...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 Plate, Kula and Farallon Plates were sliding under the North American plate. Most hypothes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
