Grenelle Mountain

Last updated
Grenelle Mountain
Grenelle Mountain.jpg
Northwest aspect
Highest point
Elevation 3,047 m (9,997 ft) [1]
Prominence 255 m (837 ft) [1]
Parent peak Mount Waddington (4,019 m) [2]
Isolation 3.06 km (1.90 mi) [2]
Listing Mountains of British Columbia
Coordinates 51°19′16″N125°08′19″W / 51.32111°N 125.13861°W / 51.32111; -125.13861 [3]
Geography
Canada British Columbia relief location map.jpg
Red triangle with thick white border.svg
Grenelle Mountain
Location in British Columbia
Canada relief map 2.svg
Red triangle with thick white border.svg
Grenelle Mountain
Grenelle Mountain (Canada)
Location British Columbia, Canada
DistrictRange 2 Coast Land District
Parent range Coast Mountains
Waddington Range
Topo map NTS 92N6 Mount Waddington [3]
Climbing
First ascent 1950
Easiest route Expedition

Grenelle Mountain is a 3,047-metre (9,997-foot) mountain summit located in British Columbia, Canada. [1]

Contents

Description

Grenelle Mountain is a glaciated peak situated in the Waddington Range of the Coast Mountains, in a remote wilderness area that few visit. Grenelle Mountain is set 150 km (93 mi) north of the community of Campbell River and 10 km (6.2 mi) southeast of Mount Waddington, the highest peak of the entire Coast Mountains range. Other neighbors between Waddington and Grenelle include Spearman Peak, Mount Munday, Arabesque Peaks and Bravo Peak. Precipitation runoff and glacier meltwater from Grenelle Mountain drains to Bute Inlet via the Homathko River. [1] Topographic relief is significant as the summit rises 1,500 meters (4,920 feet) above the Tiedemann Glacier in two kilometers (1.2 mile).

History

The name "Crenelle Mountain" was originally submitted in January 1928 by mountaineer Don Munday and officially adopted 19 December 1968. [4] Munday so-named it because of its likeness to crenelles and battlements. The spelling "Grenelle", although misconstrued, is firmly entrenched in the mountaineering community, according to April 1978 advice from Dr. Glenn Woodsworth, Geological Survey of Canada and Alpine Club of Canada representative to the Geographical Names Board of Canada. [4] The "Grenelle Mountain" toponym was officially adopted May 1, 1978, by the Geographical Names Board of Canada. [3]

The first ascent of the summit was made in July 1950 by Allen Steck, William W. Dunmire, Oscar Cook, Richard Houston, James Wilson, Philip Bettler, William Long and Raymond de Saussure. [5] [6]

Climate

Based on the Köppen climate classification, Grenelle Mountain has an ice cap climate. [7] Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall. As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Temperatures can drop below −20 °C with wind chill factors  below −30 °C. This climate supports the Waddington, Splendour and Tiedemann glaciers which cover the slopes of Grenelle Mountain.

See also

Related Research Articles

<span class="mw-page-title-main">Mount Waddington</span> Mountain in British Columbia, Canada

Mount Waddington, once known as Mystery Mountain, is the highest peak in the Coast Mountains of British Columbia, Canada. Although it is lower than Mount Fairweather and Mount Quincy Adams, which straddle the United States border between Alaska and British Columbia, Mount Waddington is the highest peak that lies entirely within British Columbia. It and the subrange which surround it, known as the Waddington Range, stand at the heart of the Pacific Ranges, a remote and extremely rugged set of mountains and river valleys.

<span class="mw-page-title-main">Mount Munday</span>

Mount Munday is one of the principal summits of the Pacific Ranges of the Coast Mountains in British Columbia, Canada. It is 3,356 m (11,010 ft) in elevation and stands in the Waddington Range six kilometres southeast of Mount Waddington 4,019 m (13,186 ft), which is the highest summit in the Coast Mountains.

<span class="mw-page-title-main">Mount Tiedemann</span>

Mount Tiedemann 3838m, prominence 848m, is one of the principal summits of the Pacific Ranges subdivision of the Coast Mountains of British Columbia. It is located 3 km (1.9 mi) northeast of Mount Waddington in the Waddington Range massif between the Homathko and Klinaklini Rivers.

<span class="mw-page-title-main">Mount Bute</span>

Mount Bute, also known as Bute Mountain, is a 2,810-metre (9,220-foot) mountain located in the Coast Mountains of British Columbia, Canada. Situated at the southern extreme of the Homathko Icefield, Mount Bute has an impressive 800-metre sheer granite west face, and Bute Glacier dominates the north aspect. This imposing mountain is visible from Waddington Harbour at the head of Bute Inlet, in a remote wilderness area that few visit. Its nearest higher peak is Mount Grenville, 13.0 km (8.1 mi) to the east-northeast. Mount Grenville is the highest summit of the icefield. Mount Bute is 63.0 km (39.1 mi) southeast of Mount Waddington, the highest peak of the entire Coast Mountains range.

<span class="mw-page-title-main">Overlord Mountain</span> Mountain in the country of Canada

Overlord Mountain is a 2,625-metre (8,612-foot) glacier-clad peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is the highest point of the Fitzsimmons Range, which is a subset of the Garibaldi Ranges, and can be readily seen from the Whistler Blackcomb ski area. It is situated 15 km (9 mi) southeast of Whistler, and its nearest higher peak is Mount Macbeth, 3 km (2 mi) to the north-northeast. The Benvolio Glacier rests below the south aspect of the summit, the Fitzsimmons Glacier on the east aspect, and the expansive Overlord Glacier spans the northern and western aspects of the mountain. Precipitation runoff from the peak and meltwater from its glaciers drains into tributaries of the Cheakamus River. The first ascent of the mountain was made in 1923 by Phyllis Munday and Don Munday via the Benvolio Glacier. The mountain's descriptive name was recommended by the Garibaldi Park Board and officially adopted on September 2, 1930, by the Geographical Names Board of Canada.

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Mount Macbeth is a 2,639-metre (8,658-foot) glacier-clad peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is part of the Spearhead Range, which is a subset of the Garibaldi Ranges. It is situated 14 km (9 mi) southeast of Whistler, and 2 km (1 mi) south of Tremor Mountain, which is the highest point in the Spearhead Range. The Naden Glacier spreads out below the eastern aspect of the summit, the Macbeth Glacier lies below the south aspect, and the Curtain Glacier descends the northern slope. Precipitation runoff from the peak and meltwater from its glaciers drains into Fitzsimmons Creek which is a tributary of the Cheakamus River. Macbeth is most often climbed as part of the Spearhead Traverse. The first ascent of the mountain was made in 1969 by P. Starr, E. Bass, B. Ellis, and P. Macec via the northeast ridge. The peak was named in 1964 by an Alpine Club of Canada climbing party, to commemorate the 400th anniversary of William Shakespeare's birth. The mountain's name was officially adopted on August 27, 1965, by the Geographical Names Board of Canada.

<span class="mw-page-title-main">Mount Benvolio</span> Mountain in the country of Canada

Mount Benvolio is a 2,613-metre (8,573-foot) glacier-clad peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is the second-highest point of the Fitzsimmons Range, which is a subset of the Garibaldi Ranges. It is situated 15 km (9 mi) southeast of Whistler, and its nearest higher peak is Overlord Mountain, 0.7 km (0 mi) to the northwest. The Benvolio Glacier is set on the western slope of the peak, the Diavolo Glacier spreads out below the eastern aspect of the summit, and the Fitzsimmons Glacier descends the north slope. Precipitation runoff from the peak and meltwater from its glaciers drains into tributaries of the Cheakamus River.

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References

  1. 1 2 3 4 "Grenelle Mountain, British Columbia". Peakbagger.com. Retrieved 2022-12-06.
  2. 1 2 "Grenelle Mountain, Peakvisor.com" . Retrieved 2022-12-06.
  3. 1 2 3 "Grenelle Mountain". Geographical Names Data Base . Natural Resources Canada . Retrieved 2022-12-06.
  4. 1 2 "Grenelle Mountain". BC Geographical Names . Retrieved 2022-12-06.
  5. William W. Dunmire (2019), From Climbing Peaks to Saving Our Planet: Outdoor Adventures that Shaped My Life, FriesenPress, ISBN   9781525545665
  6. Oscar A. Cook (1951), A.A.C., Sierra Nevada Section, Americanalpineclub.org
  7. Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11. ISSN   1027-5606.