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Old Goat Mountain
Old Goat Mountain is a mountain summit located in Kananaskis Country of Alberta, Canada. Description Old Goat Mountain is situated near the south end of the Goat Range which is a subrange of the Canadian Rockies, and is the highest point in the Goat Range. The east flank of the mountain is within Spray Valley Provincial Park, whereas the west aspect is within Banff National Park, with the boundary line between the two parks running roughly north-to-south over its summit. Precipitation runoff from the mountain drains to the Spray Lakes Reservoir. Topographic relief is significant as the summit rises over 1,400 meters (4,600 feet) above Spray Lake in three kilometers (1.86 mile). The nearest higher peak is Wind Mountain, to the east. Old Goat Mountain can be seen from Alberta Highway 742, the Smith-Dorrien/Spray Trail. History The mountain was named "Old Goat" in memory of Rick Collier, a founding member of the Old Goats Climbing Club, who had climbed this peak numer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Goat Range (Kananaskis)
The Goat Range is a mountain range of the Canadian Rockies in southwestern Alberta, Canada. It is a part of the Front Ranges of the Southern Continental Ranges and lies on the western edge of Kananaskis Country, on the boundary between Spray Valley Provincial Park and Banff National Park. To the east, the Spray Lakes Reservoir separates the Goat Range from the Kananaskis Range, to the north-east, Goat Creek separates it from Mount Rundle, and to the south-west, the Spray River separates it from Sundance Range The Sundance Range is a mountain range in the Canadian Rockies, south of the town of Banff. It is located on the Continental Divide, which forms the boundary between British Columbia and Alberta Alberta ( ) is one of the thirteen provinces .... It covers an area of about 115 km², extending about 25 km in a NNW-SSE direction with a width ranging between 4 and 6 km. The highest peak is Old Goat Mountain (3109 m), located near the southern end of the range. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Three-thousanders Of Alberta
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term may refer to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Ande ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spray River
The Spray River is a tributary of the Bow River in western Alberta, Canada. The Spray River originates in the southern area of Banff National Park in the Canadian Rockies and soon enters the Spray Lakes Reservoir formed in 1951 after the construction of the ''Canyon Dam.'' At that point, the river briefly touches the Spray Valley Provincial Park before returning to Banff National Park. The river originally continued to flow north-northwest between the Goat Range and the Sundance Range before merging with Goat Creek at the northern end of the Goat Range and eventually meeting the Bow River in the Town of Banff, just below Bow Falls. However since the construction of the dam the Spray River bed is mostly dry north-northwest of the Spray Lakes Reservoir as the Dam diverts most of the water towards the Spray Powerhouse in Canmore. The river regains some water from Goat Creek and other smaller tributaries before arriving at the town of Banff. Meanwhile most of the Spray River's w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cone Mountain
Cone Mountain is a summit in the Canadian Rockies of Alberta, Canada. It is the southernmost peak in the Sundance Range. Cone Mountain was so named in 1915 on account of its shape. The mountain's name became official in 1924 by the Geographical Names Board of Canada. __NOTOC__ Climate Based on the Köppen climate classification, Cone Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . Precipitation Surface runoff, runoff from Cone Mountain drains into the Bow River which is a tributary of the Saskatchewan River. Geology The mountain 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. See also *Geography of Alberta References {{Canadian Rockies, state=collapsed Two-thousanders of Alberta Canadian Rockies ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Nestor (Alberta)
Mount Nestor is a mountain summit located in Kananaskis Country in the Canadian Rockies of Alberta, Canada. It is named after , a destroyer sunk in the Battle of Jutland during World War I. Mount Nestor is situated at the south end of the Goat Range along the west shore of Spray Lakes Reservoir. Nestor's east flank is within Spray Valley Provincial Park, while the west aspect is within Banff National Park, with the boundary line between the two parks running roughly north-to-south over its summit. The nearest higher peak is Old Goat Mountain, to the north. Mount Nestor can be seen from Alberta Highway 742, the Smith-Dorrien/Spray Trail. History The first ascent of the mountain was made in 1913 by the Interprovincial Boundary Commission. The mountain's name was officially adopted in 1922 by the Geographical Names Board of Canada. Geology Mount Nestor is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Buller (Alberta)
Mount Buller was named in 1922 after Lieutenant Colonel H.C. Buller DSO, a casualty of World War I. It is located in the Kananaskis Range in Alberta. __NOTOC__ Geology Buller 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, Buller is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . Precipitation runoff from the mountain drains west into Spray Lakes Reservoir. See also * 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 t ... * References Buller Alberta's R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Bogart
Mount Bogart is a summit located in Kananaskis Country in the Canadian Rockies of Alberta, Canada. Mount Bogart's nearest higher peak is Wind Mountain, to the north. Mount Bogart is situated northwest of Mount Kidd, and both can be seen from Highway 40 near the Kananaskis Village junction. History Mount Bogart was named by Donaldson Bogart Dowling (1858-1925), after his mother, whose maiden name was Bogart. Donaldson Dowling, an engineer with the Geological Survey of Canada, explored the area in 1904. The first ascent of the peak was made in 1930 by Kate Gardiner and Walter Feuz. The duo also made first ascents of Mount Lyautey and Mount Galatea in 1930.Thorington p. 19, 56 The mountain's name was officially adopted in 2006 by the Geographical Names Board of Canada. Geology Mount Bogart 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 th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Sparrowhawk
Mount Sparrowhawk is a mountain summit located in Kananaskis Country in the Canadian Rockies of Alberta, Canada. Mount Sparrowhawk's nearest higher peak is Mount Bogart, to the southeast. Sparrowhawk's south slope was a candidate to be used as a ski hill for the alpine events at the 1988 Winter Olympics, but nearby Mount Allan's Nakiska was selected instead. History Mount Sparrowhawk was named in 1917 for , a British destroyer that sank during the Battle of Jutland in World War I. This mountain's name was officially adopted in 1922 by the Geographical Names Board of Canada. The first ascent of the peak was made in 1947 by R.C. Hind, L. Parker, Mr. and Mrs. H.H. Rans. Mount Shark and Mount Sparrowhawk were designated as sites to host alpine skiing events in Calgary's bid for the 1988 Winter Olympics, however, the venue for the alpine skiing events moved to Nakiska shortly after Calgary was awarded the Games. Geology Mount Sparrowhawk is composed of sedimentary rock laid do ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Lougheed
Mount Lougheed is a triple-peak mountain located between Spray Lakes Reservoir and the Wind Valley of Kananaskis Country in the Canadian Rockies of Alberta, Canada. The highest summit is known as Peak 2 (3,107 metres). Peak 1 to the northwest is 3,080 metres. Peak 3 to the southeast is 3,010 metres. The nearest higher peak is Wind Mountain, to the southeast. Mount Lougheed is a conspicuous landmark that can be seen from Highway 1, the Trans-Canada Highway at Dead Man's Flats which is east of Canmore. __NOTOC__ History Mount Lougheed was named after Sir James Lougheed (1854–1925), a prominent lawyer, politician, senator, and cabinet minister. The mountain was originally named Wind Mountain by Eugène Bourgeau of the Palliser expedition, but was renamed in 1928 to honor Lougheed after his passing. The mountain's name was officially adopted in 1928 by the Geographical Names Board of Canada. The first ascent was made in 1889 by A. St. Cyr, W.S. Drewry, and Tom Wilson. Mount Lou ... [...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] |
