|
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 Precambrian t ... [...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 in Banff National Park, Canada. The range was so named on account of its blueish colour when viewed from afar. Mount Alcantara Mount Alcantara is a mountain summit located in British Columbia, Canada. Description Mount Alcantara is the highest point in the Blue Range, a subrange of the Canadian Rockies. This remote peak is situated west of the Continental Divide and s ... 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] |
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 fos ... [...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 are: * the striking Nebelhorn (2,224 m) near Oberstdorf or the Säuling (2,047 m) near Neuschwanstein, * the Admonter Reichenstein (2,251 m), Eisenerzer Reichenstein (2,165 m), Großer Pyhrgas (2,244 m) or Hochtor (2,369 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Magog
Mount Magog is located on the border of Alberta and British Columbia on the Continental Divide in the Canadian Rockies. It also straddles the shared boundary of Banff National Park with Mount Assiniboine Provincial Park. It was named in 1930 after references in the Bible. __NOTOC__ Geology Mount Magog 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, Mount Magog is located in a 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, ge ... with cold, snowy winters, and mild summers. Temperatures can drop below -20°C with wind chill factors below -30°C. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Assiniboine
Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At , it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mount Assiniboine rises nearly above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mount Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mount Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of the Assiniboine people. Mount Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The mountain can be reached only by a six-hour hike or horse-pack , three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. Climbing Mt. Assiniboi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Gloria
Mount Gloria is located on the border of Alberta and British Columbia on the Continental Divide in Canada. It was named in 1913 by the Interprovincial Boundary Survey after Lake Gloria which lies directly north of the mountain. __NOTOC__ 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. Climate Based on the Köppen climate classification, Mount Gloria 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 °C. See also *List of peaks on the British Columbia–Alberta border A ''list'' is any set of items in a row. List or lists may also refer to: People * List (surname) Organizations * List College, an undergraduate division of the Jewish Theological Seminary of America * SC Germania List, Ge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Morrison (Alberta)
Mount Morrison is a mountain summit located in the upper Spray River Valley of southern Banff National Park, in the Canadian Rockies of Alberta, Canada. Mount Morrison 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 Morrison's nearest higher peak is Mount Turner, to the north. History Mount Morrison was named in 1918 for Sir Edward Whipple Bancroft Morrison (1867–1925), Major General in the Canadian Army during the First World War. Earlier in his career, he served in the Royal Canadian Dragoons with Sir Richard Ernest William Turner in 1900 during the Second Boer War under the command of Brigadier-General Horace Smith-Dorrien. Not coincidentally, Mount Morrison is situated two kilometres south of Mount Turner. The mountain's toponym was officially adopted in 1924 by the Geographical Names Board of Canada. The first ascent of the peak was made in 1955 by Do ... [...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 Royal Canadian Dragoons ...
[...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 a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
