Gimli (mountain)
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Gimli (mountain)
Gimli is a mountain summit located in the Valhalla Ranges of the Selkirk Mountains in British Columbia, Canada. Gimli is the sixth-highest point in the Valhalla Ranges, with the highest being Gladsheim Peak, to the north-northwest. It is situated in southern Valhalla Provincial Park, east of Gimli Peak, and west of Slocan and Slocan Lake. Gimli is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,500 meters (4,920 ft) above Mulvey Creek in . History The name "Valhalla Mountains" first appeared in George Mercer Dawson's Geological Survey of Canada map published in 1890. Dawson applied names derived from Scandinavian mythology to several of the mountain ranges and peaks in Southern Kootenay. This landform's toponym was officially adopted as "Mount Dag" on March 3, 1971, at the request of the Kootenay Mountaineering Club, but it was officially changed to Gimli on April 29 ...
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Gimli Peak
Gimli Peak is a mountain summit located in the Valhalla Ranges of the Selkirk Mountains in British Columbia, Canada. Gimli Peak is the fourth-highest point in the Valhalla Ranges, with the highest being Gladsheim Peak, to the north. Its nearest higher peak is Midgard Peak, to the northwest. It is situated in southern Valhalla Provincial Park, immediately southwest of Mulvey Lakes, and west of Slocan and Slocan Lake. The name "Valhalla Mountains" first appeared in George Mercer Dawson's Geological Survey of Canada map published in 1890. Dawson applied names derived from Scandinavian mythology to several of the mountain ranges and peaks in Southern Kootenay. In keeping with the Valhalla theme, this peak was originally labelled "Mount Gimli" on a 1900 Geological Survey of Canada publication, and it was officially adopted April 29, 1998, by the Geographical Names Board of Canada as Gimli Peak. According to Norse mythology, Gimli is the place where the righteous survivors of ...
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George Mercer Dawson
George Mercer Dawson (August 1, 1849 – March 2, 1901) was a Canadian geologist and surveyor. Biography He was born in Pictou, Nova Scotia, the eldest son of Sir John William Dawson, Principal of McGill University and a noted geologist, and his wife, Lady Margaret Dawson. By age 11, he was afflicted with tuberculosis of the spine ( Pott's disease) that resulted in a deformed back and stunted growth. Physical limitations, however, did not deter Dawson from becoming one of Canada's greatest scientists. Tutors and his father provided his education during his slow recovery from the illness. Dawson later attended the High School of Montreal and McGill University (part-time) before moving to London to study geology and paleontology at the Royal School of Mines (now part of Imperial College London) in 1869. Dawson graduated after three years with the highest marks in his class. Dawson began his career in the 1870s as a professor of chemistry at Morrin College in Quebec City ...
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Geography Of British Columbia
British Columbia is the westernmost province of Canada, bordered by the Pacific Ocean. With an area of it is Canada's third-largest province. The province is almost four times the size of the United Kingdom and larger than every United States state except Alaska. It is bounded on the northwest by the U.S. state of Alaska, directly north by Yukon and the Northwest Territories, on the east by Alberta, and on the south by the U.S. states of Washington, Idaho, and Montana. Formerly part of the British Empire, the southern border of British Columbia was established by the 1846 Oregon Treaty. The province is dominated by mountain ranges, among them the Canadian Rockies but dominantly the Coast Mountains, Cassiar Mountains, and the Columbia Mountains. Most of the population is concentrated on the Pacific coast, notably in the area of Vancouver, located on the southwestern tip of the mainland, which is known as the Lower Mainland. It is the most mountainous province of Canada. Statist ...
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List Of Mountains Of Canada
Most mountain peaks of Canada lie in the west, specifically in British Columbia, Alberta, and the Yukon. Mountains can be found all over British Columbia while those in Alberta are mainly situated on the eastern side of the Canadian Rockies. The Saint Elias Mountains in the Yukon hold some of country's highest mountains, including the highest, Mount Logan at . Alberta ;Highest peaks Mts. Columbia & King Edward.jpg, Mount Columbia & King Edward in background The Twins - South and North (l-r).jpg, The Twins massif - South Twin and North Twin (l-r) Mount Assiniboine massif.jpg, Mount Assiniboine seen from above Lake Magog Columbia Icefields - panoramio (1).jpg, Snow Dome seen from Icefields Parkway British Columbia Mount Assiniboine.jpg, Mount Assiniboine Mount Robson South.jpg, Mount Robson, highest in Canadian Rockies Garibaldi black tusk.jpg, The Black Tusk Snow Dome+Dome Glacier.jpg, Snow Dome and Dome Glacier Mount Mackenzie from Mount Revelstoke NP.jpg, Mou ...
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Slocan River
Slocan may refer to: Communities * Slocan, British Columbia or Slocan City, a village in the Slocan Valley, British Columbia, Canada * Slocan Valley or Slocan Country or Silvery Slocan, a valley in British Columbia, Canada * Slocan Park, British Columbia, an unincorporated settlement in the Slocan Valley, British Columbia, Canada * South Slocan, British Columbia, an unincorporated community on the Kootenay River, British Columbia, Canada * Slocan (electoral district), a provincial electoral district in the Canadian province of British Columbia from 1903 to 1920 Rivers and lakes * Slocan River, tributary of the Kootenay River in British Columbia, Canada ** Little Slocan River, a tributary of the Slocan River in British Columbia, Canada * Slocan Lake, a lake in the Slocan Valley, British Columbia, Canada See also * Kaslo-Slocan, a provincial electoral district in the Canadian province of British Columbia from 1924 to 1963 * Kaslo and Slocan Railway, a narrow gauge railway in the ...
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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 ...
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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 ...
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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 ...
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Ragnarök
In Norse mythology, (; non, Ragnarǫk) is a series of events, including a great battle, foretelling the death of numerous great figures (including the gods Odin, Thor, Týr, Freyr, Heimdallr, and Loki), natural disasters, and the submersion of the world in water. After these events, the world will rise again, cleansed and fertile, the surviving and returning gods will meet and the world will be repopulated by two human survivors. is an important event in Norse mythology and has been the subject of scholarly discourse and theory in the history of Germanic studies. The event is attested primarily in the ''Poetic Edda'', compiled in the 13th century from earlier traditional sources, and the ''Prose Edda'', written in the 13th century by Snorri Sturluson. In the ''Prose Edda'' and in a single poem in the ''Poetic Edda'', the event is referred to as (), a usage popularised by 19th-century composer Richard Wagner with the title of the last of his ''Der Ring des Nibelungen'' ...
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Gimlé
In Norse mythology, Gimlé (alternately Gimli as in Icelandic) is a place where the worthy survivors of Ragnarök are foretold to live. It is mentioned in the ''Prose Edda'' and the Eddic poem "Völuspá" and described as the most beautiful place in Asgard, more beautiful than the sun. Etymology The meaning of the name is "fire-lea" or "fire-shelter", or in scholar Lee M. Hollander's view, more likely "gem-roof". Descriptions Within Asgard, the realm of the gods, Gimlé is a golden-roofed building where righteous people go when they die. In the ''Prose Edda'', Snorri Sturluson places it in Víðbláinn, which he describes as third heaven currently inhabited only by light elves. In "Völuspá", which he quotes in one of his accounts of Gimlé, the hall is on Gimlé, presumably a mountain, rather than being itself called Gimlé. Snorri presents Gimlé as a pagan heaven. Scholars including Hollander and Rudolf Simek have seen the description of Gimlé as influenced by the Christi ...
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Norse Mythology
Norse, Nordic, or Scandinavian mythology is the body of myths belonging to the North Germanic peoples, stemming from Old Norse religion and continuing after the Christianization of Scandinavia, and into the Nordic folklore of the modern period. The northernmost extension of Germanic mythology and stemming from Proto-Germanic folklore, Norse mythology consists of tales of various deities, beings, and heroes derived from numerous sources from both before and after the pagan period, including medieval manuscripts, archaeological representations, and folk tradition. The source texts mention numerous gods such as the thunder-god Thor, the raven-flanked god Odin, the goddess Freyja, and numerous other deities. Most of the surviving mythology centers on the plights of the gods and their interaction with several other beings, such as humanity and the jötnar, beings who may be friends, lovers, foes, or family members of the gods. The cosmos in Norse mythology consists of Nine Worl ...
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Geographical Names Board Of Canada
The Geographical Names Board of Canada (GNBC) is a national committee with a secretariat in Natural Resources Canada, part of the Government of Canada, which authorizes the names used and name changes on official federal government maps of Canada created since 1897. The board consists of 27 members, one from each of the provinces and territories, and others from departments of the Government of Canada. The board also is involved with names of areas in the Antarctic through the Antarctic Treaty. Structure The secretariat is provided by Natural Resources Canada. In addition to the provincial and territorial members are members from the following federal government departments: Aboriginal Affairs and Northern Development Canada, Canada Post Corporation, Fisheries and Oceans Canada, Elections Canada, Library and Archives Canada, Department of National Defence, Natural Resources Canada (including Geological Survey of Canada and Canada Centre for Mapping and Earth Observation), Pa ...
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