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Survey Peak (Alberta)
Survey Peak is a mountain summit in Alberta, Canada. Description Survey Peak is located in the Canadian Rockies of Banff National Park. It is situated at the intersection of the North Saskatchewan River valley and Howse River valley. Topographic relief is modest as the summit rises 1,200 metres (3,937 ft) above Glacier Lake in . The nearest higher named peak is Mount Erasmus, to the west. Survey Peak can be seen from the Icefields Parkway west of Saskatchewan Crossing. An ascent of the peak involves 1,400 metres of elevation gain covering 16 km round-trip distance, part of which is on the Glacier Lake Trail.Andrew Nugara (2011), ''Snowshoeing in the Canadian Rockies'', Rocky Mountain Books, History The first ascent of the summit was made in August 1898 by J. Norman Collie and Hugh E.M. Stutfield. Collie so named the peak after conducting a plane table survey from the summit. The mountain's toponym was officially adopted on March 31, 1924, by the Geographical Na ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 total area. Its southern and western border with the United States, stretching , is the world's longest binational land border. Canada's capital is Ottawa, and its three largest metropolitan areas are Toronto, Montreal, and Vancouver. Indigenous peoples have continuously inhabited what is now Canada for thousands of years. Beginning in the 16th century, British and French expeditions explored and later settled along the Atlantic coast. As a consequence of various armed conflicts, France ceded nearly all of its colonies in North America in 1763. In 1867, with the union of three British North American colonies through Confederation, Canada was formed as a federal dominion of four provinces. This began an accretion of provinces an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plane Table
A plane table (plain table prior to 1830) is a device used in surveying site mapping, exploration mapping, coastal navigation mapping, and related disciplines to provide a solid and level surface on which to make field drawings, charts and maps. The early use of the name ''plain table'' reflected its simplicity and plainness rather than its flatness. History The earliest mention of a plane table dates to 1551 in Abel Foullon's ''"Usage et description de l'holomètre"'', published in Paris.Turner, Anthony, ''Early Scientific Instruments, Europe 1400-1800'', Sotheby's Publishing, 1987, . page 81 However, since Foullon's description was of a complete, fully developed instrument, it must have been invented earlier. A brief description was also added to the 1591 edition of Digge's ''Pantometria''. The first mention of the device in English was by Cyprian Lucar in 1590.Turner, Gerard L'E., ''Scientific Instruments 1500-1900, An Introduction'', University of California Press, 1998 . ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Amery
Mount Amery is a mountain summit located in the North Saskatchewan River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Saskatchewan, to the northwest, but they are separated by the Alexandra River. Mount Amery can be seen from the Icefields Parkway north of Saskatchewan Crossing, with optimum photography conditions in the early morning light. Precipitation runoff from Mount Amery drains into tributaries of the Saskatchewan River The Saskatchewan River (Cree: ''kisiskāciwani-sīpiy'', "swift flowing river") is a major river in Canada. It stretches about from where it is formed by the joining together of the North Saskatchewan and South Saskatchewan Rivers to Lake Winn .... __NOTOC__ History Mount Amery honors Leo Amery (1873-1955), who was a British politician and journalist who twice visited the Canadian Rockies. Unusually, he (along with Brian Meredith and Edward Feuz Jr.) made the first ascent of the mounta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Outram
Mount Outram is a mountain summit located in the Howse River Valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Forbes, to the southwest. Glacier Lake is situated to the north, and the Sir James Glacier lies below the south aspect of the peak. Mount Outram can be seen from the Icefields Parkway southwest of Saskatchewan Crossing, with optimum photography conditions in morning light. History Mount Outram was named in 1920 for James Outram (1864-1925), a mountaineer who made numerous first ascents in the Canadian Rockies including Mount Assiniboine, Chancellor Peak, Cathedral Mountain, and Mount Wilson. The first ascent of the mountain was made in 1924 by F.V. Field, W.O. Field, and L. Harris, with guides Edward Feuz Jr. and J. Biner. The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada. Geology Like other mountains in Banff Park, Mount Outram is composed of sedimentary ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Sarbach
Mount Sarbach is a mountain located in Banff National Park between Mistaya River and Howse River and is visible from the Icefields Parkway. The mountain is named after Peter Sarbach, a mountain guide from Switzerland, who guided the first ascent by J. Norman Collie and G.P. Baker in 1897. Mount Sarbach is situated south of Saskatchewan River Crossing, where the Icefields Parkway intersects with the David Thompson Highway. __NOTOC__ Geology Like other mountains in Banff Park, Mount Sarbach 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. A glacier shared with Kaufmann Peaks resides in the southeast cirque. Climate Based on the Köppen climate classification, Mount Sarbach is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Murchison (Alberta)
Mount Murchison is a mountain summit located at the convergence of the North Saskatchewan River valley and Mistaya River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. The main summit has two high points: the Southeast Peak is 3,353 m, whereas the Northwest Peak is 3,333 m and separated by 700 m distance. Its nearest higher peak is Mount Cline, to the north. Mount Murchison is situated immediately southeast of the confluence of the North Saskatchewan River, Mistaya River, and Howse River near Saskatchewan Crossing, where the Icefields Parkway intersects with the David Thompson Highway. History Named by James Hector as he traversed the Mistaya Valley in September of 1858, Mount Murchison honors Sir Roderick Impey Murchison (1792-1871), a prominent English geologist and director of the Geological Survey of Great Britain. The mountain's name became official in 1924. The first ascent of the Northwest Peak was in 1902 by Norman Collie, H.E.M. Stutfie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Wilson (Alberta)
Mount Wilson is a mountain summit located in the North Saskatchewan River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Cline, to the northeast. Mount Wilson is situated immediately north of the confluence of the North Saskatchewan River, Mistaya River, and Howse River near Saskatchewan Crossing, where the Icefields Parkway intersects with the David Thompson Highway.__NOTOC__ History Mount Wilson honours Tom Wilson (1859–1933) who was an early explorer in the Canadian Rockies. The mountain was named in 1898 by Norman Collie. The first ascent of the mountain was made in 1902 by James Outram and Christian Kaufmann. The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada. Geology Like other mountains in Banff Park, Mount Wilson is composed of sedimentary rock laid down from the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east a ... [...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. As ... [...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] |
Survey Peak Formation
The Survey Peak Formation is a stratigraphic unit of latest Cambrian to earliest Ordovician age. It is present on the western edge of the Western Canada Sedimentary Basin in the Canadian Rockies of Alberta and British Columbia. It was named for Survey Peak near Mount Erasmus in Banff National Park by J.D. Aitken and B.S. Norford in 1967. The Survey Peak Formation is fossiliferous and includes remains of trilobites and other marine invertebrates, as well as conodonts, stromatolites, and thrombolites. Lithology and deposition The Survey Peak Formation formed as a shallow and at times emergent marine shelf along the western shoreline of the North American Craton during latest Cambrian to earliest Ordovician time.Aitken, J.D. 1966. Middle Cambrian to Middle Ordovician cyclic sedimentation, southern Rocky Mountains of Alberta. Bulletin of Canadian Petroleum Geology, vol. 14, no. 6, p. 405-441. It consists of limestones, calcareous shales and mudstones, and siltstones, and can be ... [...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] |
