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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] |
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 ... [...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 Observation), Pa ... [...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 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trans-Canada Highway
The Trans-Canada Highway ( French: ; abbreviated as the TCH or T-Can) is a transcontinental federal–provincial highway system that travels through all ten provinces of Canada, from the Pacific Ocean on the west coast to the Atlantic Ocean on the east coast. The main route spans across the country, one of the longest routes of its type in the world. The highway system is recognizable by its distinctive white-on-green maple leaf route markers, although there are small variations in the markers in some provinces. While by definition the Trans-Canada Highway is a highway ''system'' that has several parallel routes throughout most of the country, the term "Trans-Canada Highway" often refers to the main route that consists of Highway 1 (British Columbia, Alberta, Saskatchewan, and Manitoba), Highways 17 and 417 (Ontario), Autoroutes 40, 20 and 85 (Quebec), Highway 2 (New Brunswick), Highways 104 and 105 (Nova Scotia) and Highway 1 (Newfoundland). This ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Afton
Mount Afton is a mountain summit located in Glacier National Park in the Selkirk Mountains of British Columbia, Canada. It is situated near the north end of Asulkan Ridge, south of Rogers Pass, northeast of Revelstoke, and west of Golden. The first ascent of the mountain was made in 1893 by Herbert Lambert, Miss MacLeod, Harold A. Perley, William H. Rau, and William Stables via the east buttress. The mountain was climbed in 1895 via the south ridge by Philip Stanley Abbot, Charles Ernest Fay, and Charles S. Thompson who named the mountain after themselves using an amalgamation of letters from their surnames, ("A"bbot "F"ay "T"homps"on"). The mountain's name was officially adopted March 31, 1924, when approved by the Geographical Names Board of Canada. Climate Based on the Köppen climate classification, Mount Afton 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Sir Donald
Mount Sir Donald is a mountain summit located in the Rogers Pass area of Glacier National Park in the Selkirk Mountains of British Columbia, Canada. Its good rock quality and classic Matterhorn shape make it popular for alpine rock climbers, and the Northwest Arete route is included in the popular book ''Fifty Classic Climbs of North America''. It was originally named Syndicate Peak in honor of the group who arranged the finances for the completion of the Canadian Pacific Railway, but was later renamed after Donald Smith, 1st Baron Strathcona and Mount Royal, head of the syndicate. The first ascent was made in 1890 by Emil Huber and Carl Sulzer of Switzerland and porter Harry Cooper. As of the 1910s, an average of three or four ascents per year were being made. Climate Based on the Köppen climate classification, the mountain has a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Prec ... [...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] |
Ursus Major Mountain
Ursus Major Mountain is a mountain summit located in Glacier National Park, in the Hermit Range of the Selkirk Mountains in British Columbia, Canada. Ursus Major Mountain is situated west of Rogers Pass, northeast of Revelstoke, and west of Golden. Its nearest higher peaks are Catamount Peak, to the southwest, and Ursus Minor Mountain, to the northeast. The first ascent of the mountain was made August 5, 1902, by a Dominion Topographic Survey party. The mountain's name was adopted in 1906, then re-approved September 8, 1932, by the Geographical Names Board of Canada. It was so-named by the survey party because of its proximity above Bear Creek (since renamed Connaught Creek), and in keeping with the bear theme of other nearby features such as Ursus Minor Mountain, Grizzly Mountain, Bruins Pass, and Balu Pass. The high point on Ursus Major's east ridge is unofficially called ''Balu Peak''. Climate Based on the Köppen climate classification, Ursus Major Mountain is loca ... [...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] |
List Of Mountains Of Canada
Most mountain peaks of Canada lie in the west, specifically in British Columbia, Alberta, and the Yukon. Mountains can be found all over British Columbia while those in Alberta are mainly situated on the eastern side of the Canadian Rockies. The Saint Elias Mountains in the Yukon hold some of country's highest mountains, including the highest, Mount Logan at . Alberta ;Highest peaks Mts. Columbia & King Edward.jpg, Mount Columbia & King Edward in background The Twins - South and North (l-r).jpg, The Twins massif - South Twin and North Twin (l-r) Mount Assiniboine massif.jpg, Mount Assiniboine seen from above Lake Magog Columbia Icefields - panoramio (1).jpg, Snow Dome seen from Icefields Parkway British Columbia Mount Assiniboine.jpg, Mount Assiniboine Mount Robson South.jpg, Mount Robson, highest in Canadian Rockies Garibaldi black tusk.jpg, The Black Tusk Snow Dome+Dome Glacier.jpg, Snow Dome and Dome Glacier Mount Mackenzie from Mount Revelstoke NP.jpg, Mou ... [...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] |
