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Taurus Mountain
Taurus Mountain is a mountain summit located in British Columbia, Canada. Description Taurus Mountain is a peak situated southeast of The Bugaboos, in the Purcell Mountains which are a subrange of the Columbia Mountains. Precipitation runoff from Taurus Mountain drains southwest into the headwaters of Howser Creek thence Duncan Lake; and from the north slope into headwaters of Frances Creek and eventually the Columbia River. Topographic relief is significant as the summit rises over above Frances Creek in . History The name Taurus was applied to the mountain by Arthur O. Wheeler during his survey trip across Bugaboo Pass in 1910. Conrad Kain said that Wheeler called the mountain Taurus "because it was like a bull." From the Bugaboo region its general appearance suggests a formidable bull. The mountain's toponym was officially adopted June 9, 1960, by the Geographical Names Board of Canada. The first ascent of the summit was made July 28, 1946, by Edward F. Little, Eugen Ros ...
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The Virgin (Purcell Mountains)
The Virgin is a mountain summit located in British Columbia, Canada. Description The Virgin is a peak situated southeast of The Bugaboos and three kilometers southwest of Taurus Mountain. The mountain is part of the Purcell Mountains which are a subrange of the Columbia Mountains. Precipitation runoff from The Virgin drains into the headwaters of Howser Creek which empties at Duncan Lake. Topographic relief is significant as the summit rises above Howser Creek in . History The mountain was discovered and named in 1946 by the climbing team which made the first ascent of nearby Taurus Mountain. The climbers, Edward F. Little and Eugen Rosenstock-Huessy, wrote: "The white snow-draped terraces of the peak were a beautiful sight, and this appearance, along with the stellar name of the neighbor which, though hidden, we knew was nearby, prompted us to name it for purposes of our own reference, 'Virgo' or the 'Virgin'." The mountain's toponym was officially adopted October 29, 1962 ...
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Duncan Lake (British Columbia)
Duncan Lake or Lake Duncan or ''variation'', may refer to: Places Lakes A lake, one of many lakes around the world. Canada One of several lakes in Canada: * Duncan Lake (British Columbia) in British Columbia. Four lakes by this name. * Duncan Lake (Manitoba) in Manitoba * Duncan Lake (Northwest Territories) in the Northwest Territories * Duncan Lake (Ontario) in Ontario. Natural Resources Canada website lists seven lakes in the province. * Duncan Lake (Quebec) in Quebec * Duncan Lake (Saskatchewan) in Saskatchewan. Two lakes by this name. United States One of several lakes in the United States: * Lake Duncan (Oklahoma), a reservoir for Duncan City, Oklahoma; near Fuqua Lake * Duncan Lake (Michigan) * Duncan Lake (Minnesota) * Duncan Lake (Montana) * Duncan Lake (New Hampshire) * Duncan Lake (Tennessee) * Duncan Lake (Texas) * Duncan Lake (Wyoming) Other places Places that are not lakes: * Duncan Lake 1, British Columbia, and Indian Reserve in British Columbia Other uses * ''L ...
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Purcell Supergroup
The Purcell Supergroup is composed primarily of argillites, carbonate rocks, quartzites, and mafic igneous rocks of late Precambrian (Mesoproterozoic) age. It is present in an area of about in southwestern Alberta and southeastern British Columbia, Canada, and it extends into the northwestern United States where it is called the Belt Supergroup. It was named for the Purcell Mountains of British Columbia by R.A. Daly in 1912. Fossil stromatolites and algal structures are common in some of the Purcell Supergroup rocks,O'Connor, M.P. 1972. Classification and environmental interpretation of the cryptalgal organosedimentary "Molar-Tooth" structure from the Late Precambrian Belt-Purcell Supergroup. Journal of Geology, vol. 80, no. 5, p. 592-610.McMechan, M.E. 1981. The Middle Proterozoic Purcell Supergroup in the southwestern Rocky and southeastern Purcell Mountains, British Columbia, and the initiation of the Cordilleran Miogeocline, southern Canada and adjacent United States. Bulletin ...
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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. St ...
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Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a continental 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°N to 70°N, poleward of the humid continental climates. Like other Class D climates, they are rare in the Southern Hemisphere, only found at some isolated highland elevations. 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 on ...
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Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. 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'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ...
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Eugen Rosenstock-Huessy
Eugen Rosenstock-Huessy (; July 6, 1888February 24, 1973) was a historian and social philosophy, social philosopher, whose work spanned the disciplines of history, theology, sociology, linguistics and beyond. Born in Berlin, Germany into a non-observant Jewish family, the son of a prosperous banker, he converted to Christianity in his late teens, and thereafter the interpretation and reinterpretation of Christianity was a consistent theme in his writings. He met and married Margrit Hüssy in 1914. In 1925, the couple legally combined their names. They had a son, Hans, in 1921. Rosenstock-Huessy served as an officer in the German army during World War I. His experience caused him to reexamine the foundations of liberal Western culture. He then pursued an academic career in Germany as a specialist in medieval law, which was disrupted by the rise of Nazism. In 1933, after Adolf Hitler became Chancellor of Germany, he emigrated to the United States where he began a new academic career, ...
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First Ascent
In mountaineering and climbing, a first ascent (abbreviated to FA in climbing guidebook, guide books), is the first successful documented climb to the top of a mountain or the top of a particular climbing route. Early 20th-century mountaineers and climbers focused on reaching the tops of iconic mountains (e.g. the eight-thousanders) and climbing routes (e.g. the great north faces of the Alps) by whatever means possible, often using considerable amounts of aid climbing, and/or with large expedition style support teams that laid "siege" to the climb. As all the key tops were summited, the manner in which each top was reached became important, particularly the ability to complete the ascent without artificial aid, which is called free climbing. In free climbing, the term first free ascent (abbreviated FFA) is used where a mountain or climbing route is ascended without any artificial aid (devices for climbing protection, protection in the event of a fall could be used as long as the ...
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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. History It was created in December 1897, by Order in Council, as the Geographic Board of Canada. It consisted of one Board member from each of four Government of Canada departments, as well as the Surveyor General of Dominion Lands, while a secretariat was provided by the then-extant Department of the Interior. In December 1899, the Order in Council was amended to give the Canadian provinces and territories the right to nominate one official, each, to be a Board member. The board was succeeded by the Canadian Board on Geographic Names in 1948, then reorganized as the Canadian Permanent Committee on Geographic Names (CPCGN) in 1961. Structure , the Board consists of 27 members, one from each of the provinces and territories, and ot ...
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Conrad Kain
Conrad Kain (10 August 1883, Schwarzau im Gebirge, Nasswald – 2 February 1934, Cranbrook, British Columbia) was an Austrian mountain guide who guided extensively in Europe, Canada, and New Zealand, and was responsible for the first ascents of more than 60 routes in British Columbia. He is particularly known for pioneering climbs in the Purcell Mountains and the first ascents of Mount Robson (1913), Mount Louis (1916) and Bugaboo Spire (1916). Life Kain was born in poverty in a small village in Lower Austria. His father was a miner who died when Kain was 8. In his youth he worked as a goatherd in the Rax-Schneeberg Group, Rax Alps and from 1898 to 1904 he worked at stone quarries in Veitsch and Reichenau an der Rax, Hirschwang. His free time he spent climbing, and by 1904 he guided his first clients, becoming an officially recognized professional guide in 1906. He guided his clients not only in Austria (including the Dolomites), but also in Switzerland and France, including the ...
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Arthur Oliver Wheeler
Arthur Oliver Wheeler (May 1, 1860 – May 20, 1945) was born in Ireland and immigrated to Canada in 1876 at the age of 16. He became a land surveyor and surveyed large areas of western Canada, including photo-topographical surveys of the Selkirk Mountains and the British Columbia-Alberta boundary along the continental divide through the Canadian Rockies. In 1906, he and journalist Elizabeth Parker were the principal founders of the Alpine Club of Canada (ACC). He was its first president, from 1906 to 1910, and editor of the '' Canadian Alpine Journal'' from 1907 to 1930. He remained Honorary President of the ACC from 1926 until his death in 1945. The Arthur O. Wheeler hut of the ACC is named after him. Early life Wheeler was born on May 1, 1860, at ''The Rocks'', the Wheeler family estate near Kilkenny, Ireland. He was educated at Ballinasloe College, County Galway, and at Dulwich College, London. The family fell upon hard times in Ireland, and in 1876 they sold their estate ...
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Topographic Relief
Terrain (), alternatively relief or topographical relief, is the dimension and shape of a given surface of land. In physical geography, terrain is the lay of the land. This is usually expressed in terms of the elevation, slope, and orientation of terrain features. Terrain affects surface water flow and distribution. Over a large area, it can affect weather and climate patterns. Bathymetry is the study of underwater relief, while hypsometry studies terrain relative to sea level. Importance The understanding of terrain is critical for many reasons: * The terrain of a region largely determines its suitability for human settlement: flatter alluvial plains tend to have better farming soils than steeper, rockier uplands. * In terms of environmental quality, agriculture, hydrology and other interdisciplinary sciences; understanding the terrain of an area assists the understanding of watershed boundaries, drainage characteristics, drainage systems, groundwater systems, water ...
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