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Dungeon Peak
Dungeon Peak is a mountain summit located on the shared border of Jasper National Park in Alberta, and Mount Robson Provincial Park in British Columbia, Canada. Dungeon Peak is part of The Ramparts in the Tonquin Valley. The descriptive name was applied in 1916 by Morrison P. Bridgland (1878-1948), a Dominion Land Surveyor who named many peaks in Jasper Park and the Canadian Rockies. The mountain's name was made official in 1935 by the Geographical Names Board of Canada. __NOTOC__ Climate Based on the Köppen climate classification, Dungeon Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. See also *List of peaks on the British Columbia–Alberta border *Tonquin Valley The Tonquin Valley is located in Jasper National Park, Alberta, Canada, next to the border of the provinces of Alberta and British Columbia, an area which is also the continental divide, running ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oubliette Mountain
Oubliette Mountain is a mountain summit located on the shared border of Jasper National Park in Alberta, and Mount Robson Provincial Park in British Columbia, Canada. Situated in the Tonquin Valley, Oubliette Mountain is part of The Ramparts in the Canadian Rockies. The nearest higher neighbor is Dungeon Peak, to the northwest. Not coincidentally, an oubliette is a secret dungeon with access only through a trapdoor in its ceiling. The mountain's descriptive name was coined by Cyril G. Wates. History The first ascent was made in July 1932 by William Hainsworth and Max Strumia, with guide Hans Fuhrer. The first ascent of the East Buttress was made July 27, 1962 by Fred Beckey, Brian Greenwood, and Don Gordon. This climbing route is included in Beckey's book titled "''Fred Beckey's 100 Favorite North American Climbs''". Climate Based on the Köppen climate classification, Oubliette Mountain is located in a subarctic climate zone with cold, snowy winters, and mild sum ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Ramparts (Canada)
The Ramparts are a mountain range in the Canadian Rockies. Part of the Park Ranges, they straddle the Continental Divide and lie partly within Jasper National Park in Alberta and Mount Robson Provincial Park in British Columbia. There are 10 named summits in the group, the highest of which is Mount Geikie. Most were named by the Alpine Club of Canada and carry military engineering themed names such as Bastion, Parapet, Redoubt, Postern, and Dungeon. They form a western boundary for the Tonquin Valley. Amethyst Lake lies to the east, while the headwaters of the Fraser River The Fraser River is the longest river within British Columbia, Canada, rising at Fraser Pass near Blackrock Mountain in the Rocky Mountains and flowing for , into the Strait of Georgia just south of the City of Vancouver. The river's annual d ... bound it to the west. References {{reflist Mountain ranges of British Columbia Mountain ranges of Alberta Ranges of the Canadian Rockies Mou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Three-thousanders Of British Columbia
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term may refer to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Andes) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Peaks On The British Columbia–Alberta Border
A ''list'' is any set of items in a row. List or lists may also refer to: People * List (surname) Organizations * List College, an undergraduate division of the Jewish Theological Seminary of America * SC Germania List, German rugby union club Other uses * Angle of list, the leaning to either port or starboard of a ship * List (information), an ordered collection of pieces of information ** List (abstract data type), a method to organize data in computer science * List on Sylt, previously called List, the northernmost village in Germany, on the island of Sylt * ''List'', an alternative term for ''roll'' in flight dynamics * To ''list'' a building, etc., in the UK it means to designate it a listed building that may not be altered without permission * Lists (jousting), the barriers used to designate the tournament area where medieval knights jousted * ''The Book of Lists'', an American series of books with unusual lists See also * The List (other) * Listing ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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'' i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Observatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dominion Land Survey
The Dominion Land Survey (DLS; french: links=no, arpentage des terres fédérales, ATF) is the method used to divide most of Western Canada into one-square-mile (2.6 km2) sections for agricultural and other purposes. It is based on the layout of the Public Land Survey System used in the United States, but has several differences. The DLS is the dominant survey method in the Prairie provinces, and it is also used in British Columbia along the Railway Belt (near the main line of the Canadian Pacific Railway), and in the Peace River Block in the northeast of the province. (Although British Columbia entered Confederation with control over its own lands, unlike the Northwest Territories and the Prairie provinces, British Columbia transferred these lands to the federal Government as a condition of the building of the Canadian Pacific Railway. The federal government then surveyed these areas under the DLS.) [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tonquin Valley
The Tonquin Valley is located in Jasper National Park, Alberta, Canada, next to the border of the provinces of Alberta and British Columbia, an area which is also the continental divide, running along the peaks of the South Jasper Range (including The Ramparts subrange) which rise above Amethyst Lake. Tonquin Creek drains Moat Lake and flows west into Mount Robson Provincial Park in British Columbia, and empties into the Fraser River. The Astoria River drains south and east into the Athabasca River. The Tonquin Valley leads to Tonquin Pass which cradles the Amythyst Lakes at its crest beneath the Precambrian quartzite wall of the Ramparts. The valley was named after the Pacific Fur Company ship '' Tonquin'', destroyed in Clayoquot Sound in 1811. Recreation Within the valley there is the scenic Amethyst Lake and Moat Lake. It is a popular destination for back-country hikers, ski touring and horseback trips to the two outfitters camps on the shores of Amethyst Lake. There are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Robson Provincial Park
Mount Robson Provincial Park is a provincial park in the Canadian Rockies with an area of 2,249 km². The park is located entirely within British Columbia, bordering Jasper National Park in Alberta. The B.C. legislature created the park in 1913, the same year as the first ascent of Mount Robson by a party led by Conrad Kain. It is the second oldest park in the provincial system. The park is named for Mount Robson, which has the highest point in the Canadian Rockies and is located entirely within the park. History The first recreational trail was built in 1913 by Jasper outfitter Donald "Curly" Phillips along the Robson River to Berg Lake. From May to September, the Mt. Robson Visitor Information Centre is open to the public, and is a common stop on the Yellowhead Highway. The only commercial services within the park are at a combination coffee-shop gas station complex at the same viewpoint. There are two government campgrounds near the Visitor Centre and one near Yellowhea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Redoubt Peak
Redoubt Peak is a mountain summit located on the shared border of Jasper National Park in Alberta, and Mount Robson Provincial Park in British Columbia, Canada. Redoubt Peak is part of The Ramparts in the Canadian Rockies. It was named in 1920 because it has an appearance similar to that of a redoubt on a castle. Its nearest higher peak is Dungeon Peak, to the southeast. History The first ascent was made in 1927 by F. H. Slark and F. Rutishauser, who both perished on the descent. Their summit record was found on the top the following summer (in 1928). The mountain's name became official in 1935 by the Geographical Names Board of Canada. Climate Based on the Köppen climate classification, Redoubt Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Redoubt Peak drains into the Athabasca River on its east side, and the Fraser River from the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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