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Mount Byng
Mount Byng is a mountain summit located in the upper Spray River Valley of southern Banff National Park, in the Canadian Rockies of Alberta, Canada. It is the second-highest point in the Blue Range. Mount Byng's nearest higher peak is Mount Alcantara, to the west-southwest. The mighty Mount Assiniboine is situated to the northwest of Byng. History Mount Byng was named in 1918 for Julian Byng, 1st Viscount Byng of Vimy, a British Field marshal (United Kingdom), Field Marshal who served during the World War I, First World War where he commanded the Canadian Corps, and later served as Governor General of Canada. The mountain's name was made official in 1928 by the Geographical Names Board of Canada. The first ascent was made in 1934 by H.S. Crosby, with guide Rudolph Aemmer. Geology Mount Byng is composed of sedimentary rock laid down during the Precambrian to Jurassic periods and was later pushed east and over the top of younger rock during the Laramide orogeny. Climate Ba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blue Range
The Blue Range is a mountain range of the Canadian Rockies, located on the Continental Divide of the Americas, Continental Divide in Banff National Park, Canada. The range was so named on account of its blueish colour when viewed from afar. Mount Alcantara is the highest point in the range. This range includes the following mountains and peaks: Notes Mountain ranges of Alberta Ranges of the Canadian Rockies Mountains of Banff National Park {{AlbertaRockies-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Governor General Of Canada
The governor general of Canada (french: gouverneure générale du Canada) is the federal viceregal representative of the . The is head of state of Canada and the 14 other Commonwealth realms, but resides in oldest and most populous realm, the United Kingdom. The , on the advice of Canadian prime minister, appoints a governor general to carry on the Government of Canada in the 's name, performing most of constitutional and ceremonial duties. The commission is for an indefinite period—known as serving ''at Majesty's pleasure''—though five years is the usual length of time. Since 1959, it has also been traditional to alternate between francophone and anglophone officeholders—although many recent governors general have been bilingual. The office began in the 17th century, when the French crown appointed governors of the colony of Canada. Following the British conquest of the colony, the British monarch appointed governors of the Province of Quebec (later the Canadas) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Turner
Mount Turner is a mountain summit located in the upper Spray River Valley of southern Banff National Park, in the Canadian Rockies of Alberta, Canada. Mount Turner in not visible from any road in Banff Park, however, it can be seen from Alberta Highway 742, also known as the Smith-Dorrien/Spray Trail in Kananaskis Country. Mount Turner's nearest higher peak is Cone Mountain, to the north. History Mount Turner was named in 1918 for Sir Richard Ernest William Turner (1871–1961), a Lieutenant-general in the Canadian Army who served during the Second Boer War and the First World War, and was a recipient of the Victoria Cross.Mount Turner PeakFinder Earlier in his career, he served in the |
Marvel Peak
Marvel Peak is a mountain summit located in the southern tip of Banff National Park, in the Canadian Rockies of Alberta, Canada. Marvel Peak is situated in the Blue Range, three kilometers from the Continental Divide, and not visible from any road. Marvel Peak's nearest higher peak is Wonder Peak, to the north-northwest. History Like so many of the mountains in and around Kananaskis Country, Marvel Peak 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. It was named in 1917 by the Interprovincial Boundary Survey after HMS ''Marvel'' which was a destroyer involved in the Battle of Jutland. An alternate view is the name is simply descriptive, similar to Wonder Peak to the north. The mountain's toponym was officially adopted in 1934 by the Geographical Names Board of Canada. Geology Like other mountains in Banff Park, Marvel Peak is composed of sedimentary rock laid down during the Precamb ... [...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] |
Spray Lakes Reservoir
Spray Lakes Reservoir is a reservoir in Alberta, Canada. The Spray Lakes were a string of lakes formed along the Spray River, a tributary of the Bow River. With the damming of the river, the lakes were united in the Spray Lakes Reservoir. It lies between the Goat Range and the Three Sisters ridge, at an elevation of . The lake is followed by Highway 742 (Smith-Dorrien Trail) in the northern part. The Lake is impounded by two embankment dams; the 28-metre-high ''Canyon Dam'' is located near the southern end of the reservoir and blocks the main outlet of the river in a north-northwestern direction, while the secondary 13-metre-high ''Three Sisters Dam'' at the northern end of the reservoir provides the outlet for the diverted water way and contains a small 3 MW powerhouse. The two dams and the lake were created in 1951 as part of the Spray Hydro Electric Project. From the Three Sisters Dam the water is diverted into a secondary reservoir known as the ''Goat Pond'' which direc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...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] |
Precambrian
The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. The Precambrian accounts for 88% of the Earth's geologic time. The Precambrian is an informal unit of geologic time, subdivided into three eons ( Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago ( Ga) to the beginning of the Cambrian Period, about million years ago ( Ma), when hard-shelled creatures first appeared in abundance. Overview Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian fossil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
