Taurus Mountain
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Taurus Mountain
Taurus Mountain is a mountain summit located in British Columbia, Canada. Description Taurus Mountain is a 2,972-meter-elevation (9,751-foot) peak situated 12 kilometers (7.5 miles) 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 1,280 meters (4,200 feet) above Frances Creek in two kilometers (1.24 mile). 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 Geographic ...
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The Virgin (Purcell Mountains)
The Virgin is a mountain summit located in British Columbia, Canada. Description The Virgin is a 2,886-meter-elevation (9,470-foot) peak situated 12 kilometers (7.5 miles) 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 1,525 meters (5,000 feet) above Howser Creek in two kilometers (1.24 mile). 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 o ...
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Duncan Lake (British Columbia)
Duncan Lake is a man-made reservoir lake in the Kootenay region of British Columbia, Canada, formed by Duncan Dam and about 45 km in length. It is fed by the Duncan River, which forms part of the boundary between the Selkirk Mountains to the west and the Purcell Mountains to the east. Below Duncan Dam is the head of Kootenay Lake. Prior to inundation there was a lake of shorter length at the same location, also named Duncan Lake but also known as Upper Kootenay Lake or Upper Kootenai Lake. The name comes from the Duncan River's namesake, John "Jack" Duncan, prospector, who ran for election but did not win the Kootenay District seat on the colonial Legislative Council of British Columbia. See also *Columbia River Treaty * Duncan Lake known as Amazay Lake located in the Omineca Mountains of the Northern Interior of British Columbia British Columbia (commonly abbreviated as BC) is the westernmost province of Canada, situated between the Pacific Ocean and the Rocky Mo ...
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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 15,000 km2 (5,800 sq. mi.) 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 ...
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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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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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Eugen Rosenstock-Huessy
Eugen Rosenstock-Huessy (July 6, 1888 – February 24, 1973) was a historian and 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, initially at H ...
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First Ascent
In mountaineering, a first ascent (abbreviated to FA in guide books) is the first successful, documented attainment of the top of a mountain or the first to follow a particular climbing route. First mountain ascents are notable because they entail genuine exploration, with greater risks, challenges and recognition than climbing a route pioneered by others. The person who performs the first ascent is called the first ascensionist. In free climbing, a first ascent (or first free ascent, abbreviated FFA) of a climbing route is the first successful, documented climb of a route without using equipment such as anchors or ropes for aiding progression or resting. History The details of the first ascents of even many prominent mountains are scanty or unknown; sometimes the only evidence of prior summiting is a cairn, artifacts, or inscriptions at the top. Today, first ascents are generally carefully recorded and usually mentioned in guidebooks. The term is also used when referrin ...
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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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Conrad Kain
Conrad Kain (10 August 1883, 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 Alps and from 1898 to 1904 he worked at stone quarries in Veitsch and 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 Matterhorn, La Meije and several first ascents.
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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 estates ...
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Topographic Relief
Terrain or relief (also topographical relief) involves the vertical and horizontal dimensions of land surface. The term bathymetry is used to describe underwater relief, while hypsometry studies terrain relative to sea level. The Latin word (the root of ''terrain'') means "earth." 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. 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, drai ...
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