Octopus Mountain | |
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![]() North aspect, centered at top | |
Highest point | |
Elevation | 2,932 m (9,619 ft) [1] [2] |
Prominence | 570 m (1,870 ft) [3] |
Parent peak | Indian Peak (2,992 m) [3] |
Listing | Mountains of British Columbia |
Coordinates | 50°54′27″N115°48′34″W / 50.90750°N 115.80944°W [4] |
Geography | |
Country | Canada |
Province | British Columbia |
District | Kootenay Land District [5] |
Protected area | Mount Assiniboine Provincial Park |
Parent range | Mitchell Range [3] Canadian Rockies |
Topo map | NTS 82J13 Mount Assiniboine [4] |
Geology | |
Age of rock | Cambrian |
Type of rock | Sedimentary rock |
Octopus Mountain is a 2,932-metre (9,619-foot) mountain summit located in Mount Assiniboine Provincial Park of British Columbia, Canada.
Octopus Mountain is situated 12 km (7.5 mi) west of the Continental Divide and is part of the Mitchell Range which is a sub-range of the Canadian Rockies. [3] Precipitation runoff from the peak's southeast slope drains into the Mitchell River and all other slopes drain into tributaries of the Simpson River. Topographic relief is modest as the summit rises 1,330 metres (4,364 ft) above Lachine Creek in 3 km (1.9 mi) and 1,300 metres (4,265 ft) above the Mitchell River in 4 km (2.5 mi).
The mountain was named in 1913 by surveyor Robert Daniel McCaw (1884–1941) but the reason for the name is unknown. [1] [2] The mountain's toponym was officially adopted on September 9, 1924, by the Geographical Names Board of Canada. [4] A forest fire burned the slopes of Octopus Mountain in 2012 and consumed 932 hectares of land. [6]
Octopus Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. [7]
Based on the Köppen climate classification, Octopus Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. [8] Winter temperatures can drop below −20 °C with wind chill factors below −30 °C.
Mount Hector is a 3,394-metre (11,135-foot) mountain summit located in the Bow River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. The mountain was named in 1884 by George M. Dawson after James Hector, a geologist on the Palliser expedition. The mountain is located beside the Icefields Parkway, 17 km (11 mi) north of Lake Louise.
Mount Lyautey is a 3,045-metre (9,990-foot) mountain summit located in Kananaskis Country in the Canadian Rockies of Alberta, Canada. Mount Lyautey is situated 2.0 kilometres east of the Continental Divide, within Peter Lougheed Provincial Park. Its nearest higher peak is Mount Joffre, 8.0 km (5.0 mi) to the south. Mount Lyautey can be seen from Upper Kananaskis Lake and Alberta Highway 40.
The Monarch is a 2,895-metre (9,498-foot) mountain summit located in the Ball Range of the Canadian Rockies in British Columbia, Canada. The Monarch is situated on the boundary between Kootenay National Park and Mount Assiniboine Provincial Park, four kilometres to the west side of the Continental Divide. Although not visible from roads, The Monarch is a prominent feature seen from the slopes above Sunshine Village ski resort. Its nearest higher peak is Mount Bourgeau, 10.35 km (6.43 mi) to the north-northeast.
Wedgwood Peak is a 3,024-metre (9,921-foot) mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Mount Assiniboine, 2.0 km (1.2 mi) to the south. The mountain is situated northwest of Lake Magog and 1.0 km (0.62 mi) south of Sunburst Peaks.
The Marshall is a 3,180-metre (10,430-foot) mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Mount Assiniboine, 3.0 km (1.9 mi) to the east-southeast. The mountain is situated west of Wedgwood Peak.
Sunburst Peaks is a 2,849-metre (9,347-foot) mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Wedgwood Peak, 1.0 km (0.62 mi) to the south. The mountain is situated immediately southeast of Sunburst Lake, west of Lake Magog, and south of Cerulean Lake.
Mount Watson is a 2,955-metre (9,695-foot) mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. The nearest higher peak is The Marshall, 2.0 km (1.2 mi) to the southeast.
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Mount Outram is a 3,245-metre (10,646-foot) mountain summit located in the Howse River Valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Forbes, 4.37 km (2.72 mi) to the southwest. Glacier Lake is situated 4.0 km (2.5 mi) to the north, and the Sir James Glacier lies below the south aspect of the peak. Mount Outram can be seen from the Icefields Parkway southwest of Saskatchewan Crossing, with optimum photography conditions in morning light.
Mount Harkin is a 2,979-metre (9,774-foot) mountain summit located in the Kootenay River Valley along the eastern border of Kootenay National Park. Park visitors can see the peak from Highway 93, also known as the Banff–Windermere Highway. It is part of the Mitchell Range, which is a sub-range of the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Mount Assiniboine, 14.0 km (8.7 mi) to the northeast.
Nub Peak is a 2,746-metre (9,009-foot) mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Nestor Peak, 4.0 km (2.5 mi) to the west. The mountain is situated north of Sunburst Peaks, with Elizabeth Lake and Cerulean Lake in between. The Continental Divide and Assiniboine Pass are situated 3.5 km (2.2 mi) to the east. Nub Peak is famous for its panoramic view of Mount Assiniboine with its surrounding lakes and peaks. The mountain's descriptive name was officially adopted in 1924. An arm extending southwest from Nub is officially known as Chucks Ridge, and an arm extending southeast is officially called Nublet. Nub Peak is composed of sedimentary rock laid down during the Cambrian period and pushed east over the top of younger rock during the Laramide orogeny.
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