Mount Sir Sandford | |
---|---|
Highest point | |
Elevation | 3,519 m (11,545 ft) [1] |
Prominence | 2,707 m (8,881 ft) [1] |
Listing | |
Coordinates | 51°39′24″N117°52′04″W / 51.65667°N 117.86778°W [2] |
Geography | |
District | Kootenay Land District |
Parent range | Sir Sandford Range |
Topo map | NTS 82N12 Mount Sir Sandford [2] |
Climbing | |
First ascent | 1912 [3] |
Easiest route | remote glacier/ice/rock climb |
Mount Sir Sandford is the highest mountain of the Sir Sandford Range and the highest mountain in the Selkirk Mountains of southeastern British Columbia, Canada. It is the 12th highest peak in the province. The mountain was named after Sir Sandford Fleming, a railway engineer for the Canadian Pacific Railway.
The mountain was first summited in 1912 after several attempts in prior years by a party of four, led by Edward W. D. Holway and including Howard Palmer, Edward Feuz Jr. and Rudolph Aemmer. [4]
Sir Sandford Fleming was a Scottish Canadian engineer and inventor. Born and raised in Scotland, he emigrated to colonial Canada at the age of 18. He promoted worldwide standard time zones, a prime meridian, and use of the 24-hour clock as key elements to communicating the accurate time, all of which influenced the creation of Coordinated Universal Time. He designed Canada's first postage stamp, produced a great deal of work in the fields of land surveying and map making, engineered much of the Intercolonial Railway and the first several hundred kilometers of the Canadian Pacific Railway, and was a founding member of the Royal Society of Canada and founder of the Canadian Institute.
Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain on the Great Divide, on the British Columbia/Alberta border in Canada.
Mount King Edward is a mountain located at the head of the Athabasca River valley in Jasper National Park, Canada. Mt. King Edward is situated on the Continental Divide with Mt. Columbia 51⁄2 km east. The mountain was named in 1906 by Mary Schäffer Warren after King Edward VII.
The Columbia Icefield is the largest ice field in North America's Rocky Mountains. Located within the Canadian Rocky Mountains astride the Continental Divide along the border of British Columbia and Alberta, Canada, the ice field lies partly in the northwestern tip of Banff National Park and partly in the southern end of Jasper National Park. It is about 325 square kilometres (125 sq mi) in area, 100 to 365 metres in depth and receives up to 7 metres (280 in) of snowfall per year.
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 from the border to Kinbasket Lake, at the now-deserted 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 Mountains to the northwest, are also part of the larger grouping of mountains known as the Columbia Mountains. A scenic highway loop, the International Selkirk Loop, encircles the southern portions of the mountain range.
The Columbia Mountains are a group of mountain ranges along the Upper Columbia River in British Columbia, Montana, Idaho and Washington. The mountain range covers 135,952 km². The range is bounded by the Rocky Mountain Trench on the east, and the Kootenai River on the south; their western boundary is the edge of the Interior Plateau. Seventy-five percent of the range is located in Canada and the remaining twenty-five percent in the United States; American geographic classifications place the Columbia Mountains as part of the Rocky Mountains complex, but this designation does not apply in Canada. Mount Sir Sandford is the highest mountain in the range, reaching 3,519 metres (11,545 ft).
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This article comprises three sortable tables of major mountain peaks of Canada.
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The Sir Sandford Range is a subrange of the Big Bend Ranges of the Selkirk Mountains of the Columbia Mountains in southeastern British Columbia, Canada, located between Gold (river) and Palmer Creek just southwest of the Gold Arm of Kinbasket Lake.
Hooker and Brown are two mythical mountains, once reputed to lie on the great Divide of the Canadian Rockies in Jasper National Park, bordering the Athabasca Pass, the old passage for the fur trade. These two peaks were reputed to be the highest mountains in North America at over 16,000 feet (4,900 m), and were maintained to be so on maps and atlases, for almost a hundred years, spurring the early mountaineers arriving on the railway (1890) to explore the Rockies and discover features such as the Columbia Icefield.
Mount Barnard is located on the border of Alberta and British Columbia, NW of the head of Waitabit Creek and North of Golden. It is the 30th highest peak in Alberta and the 42nd highest peak in British Columbia. It was named in 1917 by boundary surveyors after Sir Francis Stillman Barnard, a Lieutenant Governor of BC during the 1910s. It should not be confused with the higher Californian peak of the same name.
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Beaver Mountain is a 3,212-metre (10,538-foot) mountain summit in British Columbia, Canada.
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Adamant Mountain is a 3,345-metre (10,974-foot) mountain in British Columbia, Canada.
Austerity Mountain is a 3,337-metre (10,948-foot) mountain in British Columbia, Canada.