Midgard Peak
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Midgard Peak
Midgard Peak is a mountain summit located in the Valhalla Ranges of the Selkirk Mountains in British Columbia, Canada. Midgard Peak is the third-highest point in the Valhalla Ranges, with the highest being Gladsheim Peak, to the east-northeast. The nearest higher neighbor is Asgard Peak, to the northeast. It is situated on the southern border of Valhalla Provincial Park, northwest of Gimli Peak, and west of Slocan and Slocan Lake. Etymology 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's name was submitted February 1970 by Robert Dean of the Kootenay Mountaineering Club for consideration, and the toponym was officially adopted March 3, 1971, by the Geographical Names Board of Canada. According to Norse mythology, Midgard is the home ...
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Valhalla Ranges
The Valhalla Ranges are a subrange of the Selkirk Mountains of the Columbia Mountains in southeastern British Columbia, Canada, located between Lower Arrow Lake of the Arrow Lakes and 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 C .... The ranges were named by G.M. Dawson for the hall of immortality where Norse heroes went after their death in battle. Sub-ranges * Ruby Range References *Valhalla Rangesin the Canadian Mountain Encyclopedia External links * Selkirk Mountains {{BritishColumbiaInterior-geo-stub ...
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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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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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Midgard
In Germanic cosmology, Midgard (an anglicised form of Old Norse ; Old English , Old Saxon , Old High German , and Gothic ''Midjun-gards''; "middle yard", "middle enclosure") is the name for Earth (equivalent in meaning to the Greek term , "inhabited") inhabited by and known to humans in early Germanic cosmology. The Old Norse form plays a notable role in Norse cosmology. Etymology The Old Norse name is cognate with Gothic (attested in the Gospel of Luke as a translation of the Greek ), Old Saxon (in ''Heliand''), Old High German (in ''Muspilli''), and Old English . The latter, which appears in both prose and poetry, was transformed to or ("Middle-earth") in Middle English literature. All these forms stem from Common Germanic , a compound of ("middle") and ("yard, enclosure"). In early Germanic cosmology, it stands alongside the term ''world'' (cf. Old English , Old Saxon , Old High German , Old Frisian , Old Norse ), itself from a Common Germanic compound ''*wira-alđi ...
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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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Geological Survey Of Canada
The Geological Survey of Canada (GSC; french: Commission géologique du Canada (CGC)) is a Canadian federal government agency responsible for performing geological surveys of the country, developing Canada's natural resources and protecting the environment. A branch of the Earth Sciences Sector of Natural Resources Canada, the GSC is the country's oldest scientific agency and was one of its first government organizations. History In September 1841, the Province of Canada legislature passed a resolution that authorized the sum of £1,500 sterling be granted to the government for the estimated expense of performing a geological survey of the province. In 1842, the Geological Survey of Canada was formed to fulfill this request.Christy Vodden (1992)No Stone Unturned: The First 150 years of the Geological Survey of Canada Geological Survey of Canada Web site William Edmond Logan was in Montreal at the time and made it known that he was interested in participating in this survey. G ...
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