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Emerald Peak (Yoho)
__NOTOC__ Emerald Peak is a mountain summit located in Yoho National Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Mount Carnarvon, to the northwest. Both are part of the President Range which is a subset of the Waputik Mountains. Emerald Peak is visible from Emerald Lake, rising above the northwest shore. The mountain's name was officially adopted in 1924 when approved by the Geographical Names Board of Canada, in association with Emerald Lake, which in turn was named in 1900 on account of its color. Geology Emerald Peak is composed of sedimentary rock laid down during the Cambrian period. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate Based on the Köppen climate classification, Emerald Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30& ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
President Range
The President Range is a mountain range of the Canadian Rockies The Canadian Rockies (french: Rocheuses canadiennes) or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part ..., located in the northwestern section of Yoho National Park. The range is named for the highest peak in the range, The President. This range includes the following mountains and peaks: References * Ranges of the Canadian Rockies Mountain ranges of British Columbia {{BritishColumbiaInterior-geo-stub ... [...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] |
Two-thousanders Of British Columbia
Two-thousanders are mountains that have a height of at least 2,000 height above sea level, 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 mountaineering, 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 (mountain), Nebelhorn (2,224 m) near Oberstdorf or the Säuling (2,047 m) near Neuschwanstein, * the Admonter Reichenstein (2,251 m), Eisenerzer Reichenstein (2,165&nb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount King (British Columbia)
Mount King is a mountain summit located in Yoho National Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Mount Deville, to the northwest. Both are in the Van Horne Range, which has the oldest mountains in the Rockies, and as such they are highly eroded. Mount King is a landmark that can be seen from Highway 1, the Trans-Canada Highway in the Kicking Horse valley and Kicking Horse Pass areas. The mountain is situated 14 kilometres southwest of Emerald Lake, and 13 km southwest of Field, British Columbia. History The mountain was named by Otto Koltz in 1886 for William Frederick King (1854–1916), a Canadian surveyor, astronomer, and civil servant. The first ascent of Mount King was made in 1892 by James J. McArthur. The mountain's name was officially adopted in 1924 when approved by the Geographical Names Board of Canada. Geology Mount King is composed of sedimentary rock laid down during the Cambrian period. Formed in shallow seas, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Burgess
Mount Burgess, , is a mountain in Yoho National Park and is part of the Canadian Rockies. It is located in the southwest buttress of Burgess Pass in the Emerald River and Kicking Horse River Valleys. History It was named in 1886 by astronomer Otto Klotz after Alexander MacKinnon Burgess, the Deputy Minister of the Interior at the time when Klotz worked for a railway construction. In 1892, James J. McArthur was the first to ascend this mountain. He was completing a survey of the lands adjacent to the Canadian Pacific Railway. In 1909, geologist Charles D. Walcott discovered the Burgess Shale deposit of fossils with fine details on Mount Burgess. The Burgess Shale is a black shale fossil bed (Lagerstätte) named after nearby Burgess Pass, in which are found new and unique species, many in fact constituting entire new phyla of life, and even today some of these unique species have proven impossible to classify. The fossils are especially valuable because they include appendage ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wapta Mountain
Wapta Mountain is a mountain located in the Canadian Rockies between Emerald Lake and Yoho Valley in Yoho National Park, British Columbia, Canada. It stands just north of the ridge containing the Burgess Shale The Burgess Shale is a fossil-bearing deposit exposed in the Canadian Rockies of British Columbia, Canada. It is famous for the exceptional preservation of the soft parts of its fossils. At old (middle Cambrian), it is one of the earliest fos ... fossil beds. Along with The Vice President and Mount Burgess, Wapta Mountain forms the backdrop to Emerald Lake, and marks the southern end of the President Range. In 1901, James Outram, J. H. Scattergood, and their guide C. Bohren, became the first people to ascend Wapta Mountain. Wapta Mountain overlooks Takakkaw Falls (1,247 feet), the second tallest waterfall in western Canada. The word "Wapta" means "river" in the Stoney language. References {{Reflist, refs= {{cite bivouac , id=1655 , name=Wapta Mountain, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Michael Peak
Michael Peak is a mountain summit located in Yoho National Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is The President, to the west-northwest. Both are part of the President Range which is a subset of the Waputik Mountains. Michael Peak is a landmark seen 4.5 kilometres north-northeast of Emerald Lake, three kilometres southwest of Takakkaw Falls, and 10 kilometres north of Field, British Columbia. History Originally known as Angle Peak, the mountain was renamed by Edward Whymper in 1901 for his friend Arthur Michael (1853–1942), an organic chemistry professor who participated in the 1897 first ascents of Mount Lefroy and Mount Victoria with J. Norman Collie, also a fellow Professor of Organic Chemistry. The first ascent of Michael Peak was made 1900 by James Outram, with Christian Kaufmann as guide. Outram wrote of it: ''"Making the ascent entirely on rocks we succeeded in obtaining quite an interesting scramble to the sharp pe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Takakkaw Falls
Takakkaw Falls (; also spelled Takkakaw) is a waterfall located in Yoho National Park, near Field, British Columbia in Canada. The falls have a total height of , making them the second tallest waterfall in Canada. The main drop of the waterfall has a height of . "Takakkaw" translates to "magnificent” in Cree. The falls are fed by the meltwater of the Daly Glacier, which is part of the Waputik Icefield. The glacier keeps the volume of the falls up during the warm summer months, and they are a tourist attraction, particularly in late spring after the heavy snow melts, when the falls are at peak condition. Height Various sources place the total vertical height of Takakkaw Falls between and . The waterfall was formerly thought to be the tallest in Canada, but a new survey in 1985 found that it is actually shorter than Della Falls on Vancouver Island. The results of that survey also concluded that the main drop of the falls is high. In popular culture The Takakkaw Falls were f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The President (mountain)
The President is a mountain peak on ''The President/Vice-President Massif'' of the President Range, in eastern British Columbia. It is just north of Emerald Lake in Yoho National Park, near the Alpine Club of Canada's Stanley Mitchell hut. History The President was named ''Shaugnessy'' in 1904 by Edward Whymper after Thomas Shaugnessy, the president of the Canadian Pacific Railway. In 1907, the mountain was renamed by the Alpine Club of Canada, after it was discovered that the name had already been used on a mountain in the Selkirks. Climate Based on the 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, nota ..., The President is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. Statis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kicking Horse River
The Kicking Horse River is in the Canadian Rockies of southeastern British Columbia, Canada. The river was named in 1858, when James Hector, a member of the Palliser Expedition, reported being kicked by his packhorse while exploring the river. Hector named the river and the associated pass as a result of the incident. The Kicking Horse Pass, which connects through the Rockies to the valley of the Bow River, was the route through the mountains subsequently taken by the Canadian Pacific Railway when it was constructed during the 1880s. The railway's Big Hill and associated Spiral Tunnels are in the Kicking Horse valley and were necessitated by the steep rate of descent of the river and its valley. Kicking Horse Pedestrian Bridge in Golden is the longest authentic covered timber-frame bridge in Canada. Planned as a community project by the Timber Framers Guild, local volunteers were joined by carpenters and timber framers from Canada, the United States and Europe. The bridge struct ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Emerald River
The Emerald River is a short river in British Columbia. It is about long and drains the waters of Emerald Lake to the Kicking Horse River. The river exits the lake's south end and flows in a southern direction for about to its mouth, which is at almost exactly the same place as the mouth of the Amiskwi River. It picks up three named tributaries; Hamilton Creek, Russell Creek and Kendel Creek. The name of the river was adopted in the 5th Report of the Geographic Board of Canada, 30 June 1904. See also *List of British Columbia rivers The following is a partial list of rivers of British Columbia, organized by watershed. Some large creeks are included either because of size or historical importance (See Alphabetical List of British Columbia rivers ). Also included are lakes th ... References Rivers of British Columbia Rivers of the Canadian Rockies Yoho National Park Kootenay Land District {{BritishColumbia-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
