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Mount Bonney
Mount Bonney, is a mountain summit located in Glacier National Park in the Selkirk Mountains of British Columbia, Canada. Mount Bonney is surrounded by ice including the Bonney Glacier, Clarke Glacier, Swanzy Glacier, and Bonney Névé. Its nearest higher peak is Mount Sir Donald, to the northeast. Mount Bonney is visible from Highway 1, the Trans-Canada Highway at Rogers Pass. History The first ascent of the mountain was made in 1888 by Reverend William S. Green and Rev. Henry Swanzy. The first ascent by a lady was in 1904 by Henrietta L. Tuzo with guide Christian Bohren. Mount Bonney, Bonney Glacier, and Bonney Névé were each named in 1888 by Reverend Green for Thomas George Bonney (1833–1923), president of the Geological Society of London and president of the Alpine Club of London. BC Geographical Names The mountain's na ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier National Park (Canada)
Glacier National Park is part of a system of 43 parks and park reserves across Canada, and one of seven national parks in British Columbia. Established in 1886, the park encompasses , and includes a portion of the Selkirk Mountains which are part of the larger grouping of mountains, the Columbia Mountains. It also contains the Rogers Pass National Historic Site. The park's history is closely tied to two primary Canadian transportation routes, the Canadian Pacific Railway (CPR), completed in 1885, and the Trans-Canada Highway, completed in 1963. Rogers Pass in the centre of the park eluded explorers until 1881. The railway brought with it tourism, the establishment of Glacier National Park and the construction of a popular alpine hotel. The heavy winter snows and steep, avalanche-prone valleys of the park have been a major obstacle to transportation, necessitating much railway engineering and avalanche control measures. The park contains high peaks, large, active glaciers, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geological Society Of London
The Geological Society of London, known commonly as the Geological Society, is a learned society based in the United Kingdom. It is the oldest national geological society in the world and the largest in Europe with more than 12,000 Fellows. Fellows are entitled to the postnominal FGS (Fellow of the Geological Society), over 2,000 of whom are Chartered Geologists (CGeol). The Society is a Registered Charity, No. 210161. It is also a member of the Science Council, and is licensed to award Chartered Scientist to qualifying members. The mission of the society is: "Making geologists acquainted with each other, stimulating their zeal, inducing them to adopt one nomenclature, facilitating the communication of new facts and ascertaining what is known in their science and what remains to be discovered". History The Society was founded on 13 November 1807 at the Freemasons' Tavern, Great Queen Street, in the Covent Garden district of London. It was partly the outcome of a previous cl ... [...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, Ande ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Green
Mount Green is a mountain summit located in Glacier National Park, in the Selkirk Mountains of British Columbia, Canada. It is situated north-northwest of Mount Bonney, southwest of Rogers Pass, northeast of Revelstoke, and west of Golden. The mountain was named by Arthur Oliver Wheeler for Rev. William Spotswood Green (1847–1919), who explored, mapped, named, climbed, and wrote about the Selkirk Mountains. His book "''Among the Selkirk Glaciers''", published in 1890, introduced the world to the Selkirk Mountains. He is credited with recommending the location for a small chalet to the Canadian Pacific Railway that would grow to become the Chateau Lake Louise hotel, as well as making the first ascent of Mount Bonney.R. W. Sandford, Introduction to William Spotswood Green, Among the Selkirk Glaciers'. London: Macmillan and Co., 1890, reprint 1998 by Aquila Books, Calgary. The mountain's name was officially adopted September 8, 1932, when approved by the Geographical Name ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Donkin
Mount Donkin is a summit in British Columbia, Canada. Description Mount Donkin is located in Glacier National Park and is part of the Selkirk Mountains. Precipitation runoff from the mountain drains into tributaries of the Incomappleux River. Mount Donkin is more notable for its steep rise above local terrain than for its absolute elevation. Topographic relief is significant as the summit rises 1,840 metres (6,037 ft) above the Incomappleux River in . The nearest higher neighbor is Michel Peak on Mount Dawson, to the east. History While in the Selkirks in 1888, Rev. William Spotswood Green, Alpine Club, London, named this mountain after fellow club member William Frederick Donkin (1845–1888), Honorary Secretary of the Alpine Club, who perished that year in the Caucasus. The nearby Mount Fox was also named in memory of another member of the club, Harry Fox, who also perished with Donkin during their attempt to be the first to climb Koshtan-Tau. The bodies of Do ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Swanzy
Mount Swanzy is a mountain summit located in Glacier National Park (Canada), Glacier National Park in the Selkirk Mountains of British Columbia, Canada. Mount Swanzy is surrounded by ice including the Bonney Glacier, Clarke Glacier, and Swanzy Glacier. Its nearest higher peak is Mount Bonney, to the west. History The mountain was named in 1895 by Messrs. Philip Stanley Abbot, Abbot, Charles Ernest Fay, Fay, and Thompson, for the Reverend Henry Swanzy, who with the Reverend William Spotswood Green introduced the world to the Selkirk Mountains following their 1888 first ascents of Mount Bonney and others. The first ascent of the mountain was made in 1900 by Arthur Michael, Sydney Spencer, Edouard Feuz Sr, and Friedrich Michel. The mountain's name was officially adopted in 1932 when approved by the Geographical Names Board of Canada. Climate Based on the Köppen climate classification, Mount Swanzy is located in a subarctic climate zone with cold, snowy winters, and mild summer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cheops Mountain
Cheops Mountain, is a mountain summit located in Glacier National Park in the Selkirk Mountains of British Columbia, Canada. Cheops Mountain is situated in the Hermit Range, and the summit provides a good view of the Hermit and Sir Donald Ranges. Its nearest higher peak is Ursus Major Mountain, to the northwest. Cheops is visible from Highway 1, the Trans-Canada Highway at Rogers Pass. History The first ascent of the mountain was made in 1893 by Samuel E. S. Allen and Walter D. Wilcox. The 1910 Rogers Pass avalanche was the deadliest avalanche in Canadian history, resulting in the deaths of 62 Canadian Pacific Railway workers. In the late afternoon of March 4, 1910, an avalanche swept down the slopes of Cheops, burying the railroad tracks in snow. The men were working to clear the tracks when shortly before midnight the deadly slide hit, coming from the opposite side of the valley down Avalanche Mountain. The mountain's current name was officially adopted in 1951 when ap ... [...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. Statist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Incomappleux River
The Incomappleux River is in the West Kootenay region of southeastern British Columbia, Canada. Entering the Beaton Arm of Upper Arrow Lake, the river is a major tributary of the Columbia River. The upper reaches of the Incomappleux valley are home to some of the only inland temperate rainforest in the world. First Nations The name "Incomappleux" is derived from the Okanagan word ''nk'mapeleqs'', meaning "point at end (of lake)". This refers to the northeastern tip of Upper Arrow Lake into which the river empties. The names of the creek and adjacent mountain are also derived from this word. A Sinixt village by this name formerly existed somewhere in the confluence area. European presence In 1865, James Turnbull, surveyor and mapmaker, explored the Incomappleux Valley. After the mid-1880s, visitors could enter the valley from the Canadian Pacific Railway (CP) main line, moving southward through the Glacier National Park area into the valley and following the river to its mouth. Eu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Illecillewaet River
The Illecillewaet River is a tributary of the Columbia River located in British Columbia, Canada. Fed by the Illecillewaet Glacier in Glacier National Park, the river flows approximately to the southwest,About the Illecillewaet Watershed , Columbia Mountains Institute where it flows into the north end of at Revelstoke. The river's is . History The Illecillewaet has been of impor ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surface Runoff
Surface runoff (also known as overland flow) is the flow of water occurring on the ground surface when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is saturated by water to its full capacity, and the rain arrives more quickly than the soil can absorb it. Surface runoff often occurs because impervious areas (such as roofs and pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or man-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. Runoff that occurs on the ground surface before reaching a channel can be a nonpoint source of pollution, as it can carry man-made contaminants or natural forms of pollution (such as rotting leaves). Man-made contaminants in runoff i ... [...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 ave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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