Mount Inglismaldie

Mount Inglismaldie
Mount Inglismaldie
	Mount Inglismaldie in winter
Highest point
Elevation	2,964 m (9,724 ft)
Prominence	160 m (520 ft)
Coordinates	51°14′30″N115°25′15″W / 51.24167°N 115.42083°W
Geography
	Mount Inglismaldie Location in Alberta Mount Inglismaldie Location in Canada
Location	Alberta, Canada
Parent range	Fairholme Range ; Canadian Rockies
Topo map	NTS 82O3 Canmore
Geology
Rock age	Cambrian
Rock type	sedimentary rock
Climbing
First ascent	1933
Easiest route	Scramble

Last updated December 04, 2024

Mount Inglismaldie is the second-highest peak of the Fairholme Range in Banff National Park. It is located immediately west of Mount Girouard in the Bow River valley south of Lake Minnewanka.

Geology

Like other mountains in Banff National Park, Mount Inglismaldie is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.^[3] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.^[4]

Climate

Based on the Köppen climate classification, Mount Inglismaldie is located in a subarctic climate with cold, snowy winters, and mild summers.^[5] Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Inglismaldie drains into Lake Minnewanka and the Bow River.

Gallery

Mount Inglismaldie (left) and Mount Girouard (right)
Lake Minnewanka with Mount Inglismaldie (right) and Mount Girouard (left)

Related Research Articles

Mount Girouard is the highest peak of the Fairholme Range in Banff National Park, Alberta, Canada. Mt. Girouard is located in the Bow River valley south of Lake Minnewanka.

Mount Peechee is the third highest peak of the Fairholme Range in Banff National Park. Mt. Peechee is located immediately southeast of Mount Girouard in the Bow River valley south of Lake Minnewanka.

Mount Charles Stewart is a mountain located in the Bow River valley of Banff National Park in Canada.

Princess Margaret Mountain is a mountain located in the Bow River valley of Banff National Park, 2.5 km (1.6 mi) west of Mount Charles Stewart.

Mount Louis is a 2,682-metre (8,799-foot) mountain summit located in southeast Banff National Park in Alberta, Canada. It is part of the Sawback Range which is a subset of the Canadian Rockies.

Copper Mountain is a mountain in Banff National Park, 20 km (12 mi) north of the town of Banff. The mountain was named in 1884 by George M. Dawson after he had climbed to a mining site set up by Joe Healy and J.S. Dennis in 1881. Healy and Dennis claimed they had found a copper deposit at the site. It was also at this point that Dawson spotted and named Mount Assiniboine.

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.

<span class="mw-page-title-main">Pilot Mountain (Alberta)</span> Mountain in Banff National Park, Alberta, Canada

Pilot Mountain is a mountain in the Bow River valley of Banff National Park in Alberta, Canada. It is located southeast of Redearth Creek and directly west of the Trans-Canada Highway.

Mount Sarbach is a mountain located in Banff National Park between Mistaya River and Howse River and is visible from the Icefields Parkway. The mountain is named after Peter Sarbach, a mountain guide from Switzerland, who guided the first ascent by J. Norman Collie and G.P. Baker in 1897. Mount Sarbach is situated south of Saskatchewan River Crossing, where the Icefields Parkway intersects with the David Thompson Highway.

Mount Astley is a 2,869-metre (9,413-foot) mountain summit located in the Palliser Range of the Canadian Rockies in Alberta, Canada. It is situated in Banff National Park above Lake Minnewanka. It was named after Charles D'Oyley Astley, who ran the boat concession on the lake in the late 1800s.

Mount Perren is located on the border of Alberta and British Columbia on the Continental Divide. It was named in 1968 after Walter Perren, a Swiss climbing guide and Parks Canada service warden. The peak forms part of the backdrop to Moraine Lake in the Valley of the Ten Peaks of Banff National Park.

Crowfoot Mountain is a mountain within Banff National Park in Alberta, Canada. The Crowfoot Glacier sits on the northeastern flank of the mountain.

Mount Costigan is a 2,973-metre (9,754-foot) summit in Alberta, Canada.

Mount Thompson is a 3,089-metre (10,135-foot) mountain summit located four kilometres west of Bow Lake in Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Baker, 5.0 km (3.1 mi) to the west. Mount Thompson is situated east of the Wapta Icefield, and is a member of the Waputik Mountains. Mount Thompson can be seen from the Icefields Parkway at Bow Lake.

Mount Jimmy Simpson is a 2,966-metre (9,731-foot) summit located 3 kilometres northwest of Bow Lake in Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Thompson, 3.0 km (1.9 mi) to the southwest. Mount Jimmy Simpson is a member of the Waputik Mountains, and is situated east of the Wapta Icefield and west of the Bow River valley. Mount Jimmy Simpson can be seen from the Icefields Parkway at Bow Lake. Jimmy Simpson Junior is a 2,721 meter sub-summit east of the mountain.

Bow Peak is a 2,840-metre (9,320-foot) mountain summit located in the Bow River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Crowfoot Mountain, 2.11 km (1.31 mi) to the east. Bow Peak is situated north of Hector Lake, southeast of Bow Lake, and can be seen from the Icefields Parkway. Although not of remarkable elevation, the mountain is a conspicuous landmark and visible from as far away as the Lake Louise area. Its position in the Waputik Mountains provides magnificent views from the summit.

Tonsa, or Tonsa Peak, is a 3,053-metre (10,016 ft) mountain summit located on the border of Alberta and British Columbia on the Continental Divide in the Canadian Rockies. The mountain forms part of the backdrop to Moraine Lake in the Valley of the Ten Peaks of Banff National Park. It was named in 1894 by Samuel E.S. Allen for the Stoney Indian word for the number four.

Mount Andromache is a 3,033-metre (9,951-foot) mountain summit located in the Bow River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. The nearest higher neighbor is Mount Hector, 4.00 km (2.49 mi) to the south. Mount Andromache can be seen from the Icefields Parkway as the road traverses the western base of the peak. Topographic relief is significant as the summit rises 1,180 m (3,870 ft) above the parkway in 1.5 km (0.93 mi). The Molar Glacier is situated on the northeast aspect of the mountain. Precipitation runoff from Mount Andromache drains into tributaries of the Bow River.

Portal Peak is a 2,926-metre (9,600-foot) mountain summit located four kilometers west of Bow Lake in Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Thompson, 1.0 km (0.62 mi) to the northwest. Portal Peak is situated east of the Wapta Icefield, and is a member of the Waputik Mountains. Portal Peak can be seen from the Icefields Parkway at Bow Lake.

Little Temple is a 2,653-metre (8,704-foot) mountain summit located in Banff National Park of the Canadian Rockies of Alberta, Canada. Little Temple is situated in the Bow River Valley between Paradise Creek and Moraine Creek, 6.0 km (3.7 mi) south of Lake Louise, Alberta. The mountain can be seen from the Icefields Parkway along with its nearest higher peak, Mount Temple, 1.07 km (0.66 mi) to the southwest.

References

1 2 3 4 5 "Mount Inglismaldie". cdnrockiesdatabases.ca. Retrieved 2019-09-13.
↑ "Mount Inglismaldie". Bivouac.com. Retrieved 2006-09-27.
↑ Belyea, Helen R. (1960). The Story of the Mountains in Banff National Park (PDF). parkscanadahistory.com (Report). Ottawa: Geological Survey of Canada. Archived (PDF) from the original on 2015-10-02. Retrieved 2019-09-13.
↑ Gadd, Ben (2008). "Geology of the Rocky Mountains and Columbias" (PDF). Archived from the original (PDF) on 2012-04-02. Retrieved 2010-01-01.
↑ Peel, M. C.; Finlayson, B. L. & McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11 (5): 1633–1644. Bibcode:2007HESS...11.1633P. doi: 10.5194/hess-11-1633-2007 . ISSN 1027-5606.

External links

Parks Canada web site: Banff National Park
Mount Inglismaldie weather: Mountain Forecast

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[pf-1] 1 2 3 4 5 "Mount Inglismaldie". cdnrockiesdatabases.ca. Retrieved 2019-09-13.

[bivouac-2] "Mount Inglismaldie". Bivouac.com. Retrieved 2006-09-27.

[3] Belyea, Helen R. (1960). The Story of the Mountains in Banff National Park (PDF). parkscanadahistory.com (Report). Ottawa: Geological Survey of Canada. Archived (PDF) from the original on 2015-10-02. Retrieved 2019-09-13.

[gadd-4] Gadd, Ben (2008). "Geology of the Rocky Mountains and Columbias" (PDF). Archived from the original (PDF) on 2012-04-02. Retrieved 2010-01-01.

[Peel-5] Peel, M. C.; Finlayson, B. L. & McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11 (5): 1633–1644. Bibcode:2007HESS...11.1633P. doi: 10.5194/hess-11-1633-2007 . ISSN 1027-5606.

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