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Mount French (Alberta)
Mount French is a summit in the Spray Mountains range of the Canadian Rockies in Alberta, Canada. The mountain is situated in Peter Lougheed Provincial Park of Kananaskis Country. French is the second highest point in the Spray Mountains Range. Its nearest higher peak, and highest in the Spray Range, is Mount Sir Douglas, to the west. Mount French can be seen from Alberta Highway 742, the Smith-Dorrien/Spray Trail. History It was named in 1915 by Morrison P. Bridgland (1878-1948), a Dominion Land Surveyor after Sir John French (1852-1925). French was Commander-in-chief of the British Forces (1914-1915) during the first 16 months of World War I, and in 1922 he was named the first Earl of Ypres. The first ascent was made in 1921 by M. Morton Jr. and H.S. Hall Jr., with Edward Feuz Jr. as guide. The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada. Geology Mount French is composed of sedimentary rock laid down during the Precambrian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spray Mountains
The Spray Mountains is a mountain range of the Canadian Rockies located in southwestern Alberta, Canada Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by tot .... This range includes the following mountains and peaks: References Mountain ranges of Alberta Ranges of the Canadian Rockies {{AlbertaRockies-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
World War I
World War I (28 July 1914 11 November 1918), often abbreviated as WWI, was one of the deadliest global conflicts in history. Belligerents included much of Europe, the Russian Empire, the United States, and the Ottoman Empire, with fighting occurring throughout Europe, the Middle East, Africa, the Pacific, and parts of Asia. An estimated 9 million soldiers were killed in combat, plus another 23 million wounded, while 5 million civilians died as a result of military action, hunger, and disease. Millions more died in genocides within the Ottoman Empire and in the 1918 influenza pandemic, which was exacerbated by the movement of combatants during the war. Prior to 1914, the European great powers were divided between the Triple Entente (comprising France, Russia, and Britain) and the Triple Alliance (containing Germany, Austria-Hungary, and Italy). Tensions in the Balkans came to a head on 28 June 1914, following the assassination of Archduke Franz Ferdin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Jellicoe
Mount Jellicoe is a mountain summit located in Peter Lougheed Provincial Park in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Smith-Dorrien, to the north. The Haig Glacier lies below the west aspect of Jellicoe, and the Smith-Dorrien Glacier lies to the north. The Continental Divide is to the west. Like so many of the mountains in Kananaskis Country, Mount Jellicoe received its name from the persons and ships involved in the 1916 Battle of Jutland, the only major sea battle of the First World War. History Mount Jellicoe was named in 1918 to honor Admiral of the Fleet John R. Jellicoe (1859–1935), the commander of the British Grand Fleet who led the Royal Navy into the Battle of Jutland in World War I. The first ascent of the peak was made in 1922 by E.W. Crawford, W. Gillespie, M.D. Geddes, M.P. Hendrie, and N.D.B. Hendrie. The mountain's toponym was officially adopted in 1924 by the Geographical Names Board of Canada. Geology Mount Je ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Inflexible
Mount Inflexible is a mountain in the Kananaskis Range of Alberta, Canada. It was named in 1922 after , a battlecruiser of the Royal Navy serving during the First World War. Geology Mount Inflexible 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, Mount Inflexible is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below with wind chill factors below . 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 ... References Three-thousanders of Alberta Alberta's Rockies ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Murray (Alberta)
Mount Murray is a mountain summit in the Spray Mountains range of the Canadian Rockies in Alberta, Canada. The mountain is situated in Peter Lougheed Provincial Park of Kananaskis Country. Its nearest higher peak is Mount French, to the south-southwest. Mount Murray can be seen from Alberta Highway 742, the Smith-Dorrien/Spray Trail. __NOTOC__ History The mountain was named in 1918 for General Sir A. J. Murray, (1860-1945). Murray was a British Army officer who served in the Second Boer War and the First World War as Commander-in-Chief of the Egyptian Expeditionary Force from 1916 to 1917. The mountain's name was officially adopted in 1928 by the Geographical Names Board of Canada. Geology Mount Murray 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, Mount Mu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Burstall
Mount Burstall is a summit in Alberta, Canada Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by tot .... Mount Burstall was named for H. E. Burstall, a British army officer who commanded Canadian troops during World War I. References Two-thousanders of Alberta Alberta's Rockies {{AlbertaRockies-geo-stub ... [...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] |
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 ... [...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] |
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] |
