Doubletop Mountain (British Columbia)
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Doubletop Mountain (British Columbia)
Doubletop Mountain is a mountain in British Columbia, Canada. Description Doubletop Mountain is part of the Adamant Range which is a subrange of the Selkirk Mountains. It is located northwest of Golden along the west side of the Rocky Mountain Trench. Precipitation runoff and glacial meltwater from the mountain drains to Kinbasket Lake via Swan and Double Eddy creeks. Topographic relief is significant as the summit rises 1,367 metres (4,485 ft) above Double Eddy Creek in and 1,367 metres (4,485 ft) above Swan Creek in . Doubletop Mountain is located immediately north of the Bill Putnam hut which is one of Canada's best ski mountaineering destinations.Chic Scott, ''Summits and Icefields: Columbia Mountains'', Rocky Mountain Books Ltd, 2003, , p. 54. The mountain's toponym was officially adopted on March 4, 1965, by the Geographical Names Board of Canada. Climate Based on the Köppen climate classification, Doubletop Mountain is located in a subarctic ...
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Adamant Range
The Adamant Range is a subrange of the Big Bend Ranges of the Selkirk Mountains of the Columbia Mountains in southeastern British Columbia, Canada, located on the west side of Columbia Reach, Kinbasket Lake Kinbasket Lake (or Kinbasket Reservoir) is a reservoir on the Columbia River in southeast British Columbia, north of the city of Revelstoke and the town of Golden. The reservoir was created by the construction of the Mica Dam. The lake includes tw ..., north of Glacier National Park. References *Adamant Rangein the Canadian Mountain Encyclopedia Big Bend Ranges {{BritishColumbiaInterior-geo-stub ...
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Two-thousanders Of British Columbia
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&n ...
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Sentinel Peak (Adamant Range)
Sentinel Peak is a mountain in British Columbia, Canada. Description Sentinel Peak is part of the Adamant Range which is a subrange of the Selkirk Mountains. It is located northwest of Golden and north of Glacier National Park. Sentinel Peak is highly glaciated with the Granite Glacier west of the peak, Echo Glacier in the north cirque, and the Gothics Glacier on the south and east slopes of the peak. Precipitation runoff and glacial meltwater from the mountain drains to Kinbasket Lake via Smith and Swan creeks. Topographic relief is significant as the summit rises 1,800 metres (5,905 ft) above Smith Creek in and 1,500 metres (4,921 ft) above Swan Creek in . Sentinel Peak is located south of the Bill Putnam hut which makes the peak an excellent ski mountaineering destination. The mountain's toponym was officially adopted on March 4, 1965, by the Geographical Names Board of Canada. Climate Based on the Köppen climate classification, Sentinel Peak i ...
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Houdini Needles
Houdini Needles is a mountain in British Columbia, Canada. Description Houdini Needles is part of the Adamant Range which is a subrange of the Selkirk Mountains. It is located northwest of Golden and north of Glacier National Park. Houdini Needles is glaciated with the Gothics Glacier to the south of the peaks. Precipitation runoff and glacial meltwater from the mountain drains to Kinbasket Lake via Smith Creek. Topographic relief is significant as the summit rises 1,560 metres (5,418 ft) above Smith Creek in . History The mountain's toponym was officially adopted on March 4, 1965, by the Geographical Names Board of Canada. The mountain was named by William Lowell Putnam III who explained "When we first saw them from the Echo Glacier they looked so impressive and impossible that we decided only Houdini could get them...." Putnam, along with Andrew Kauffman, Benjamin Ferris and Henry Pinkham, were the members of the party who made the first ascent of the peaks ...
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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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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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Ski Mountaineering
Ski mountaineering (abbreviated to skimo) is a skiing discipline that involves climbing mountains either on skis or carrying them, depending on the steepness of the ascent, and then descending on skis. There are two major categories of equipment used, free-heel Telemark skis and skis based on Alpine skis, where the heel is free for ascents, but is fixed during descent. The discipline may be practiced recreationally or as a competitive sport. Competitive ski mountaineering is typically a timed racing event that follows an established trail through challenging winter alpine terrain while passing through a series of checkpoints. Racers climb and descend under their own power using backcountry skiing equipment and techniques. More generally, ski mountaineering is an activity that variously combines ski touring, Telemark skiing, Telemark, backcountry skiing, and mountaineering. History Military patrol was an Military patrol at the 1924 Winter Olympics, official event at the 1924 W ...
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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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Selkirk Mountains
The Selkirk Mountains are a mountain range spanning the northern portion of the Idaho Panhandle, eastern Washington, and southeastern British Columbia which are part of a larger grouping of mountains, the Columbia Mountains. They begin at Mica Peak and Krell Hill near Spokane and extend approximately 320 km north (200 miles) from the border to Kinbasket Lake, at the now-inundated location of the onetime fur company post Boat Encampment. The range is bounded on its west, northeast and at its northern extremity by the Columbia River, or the reservoir lakes now filling most of that river's course. From the Columbia's confluence with the Beaver River, they are bounded on their east by the ''Purcell Trench'', which contains the Beaver River, Duncan River, Duncan Lake, Kootenay Lake and the Kootenay River. The Selkirks are distinct from, and geologically older than, the Rocky Mountains. The neighboring Monashee and Purcell Mountains, and sometimes including the Cariboo Mounta ...
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