Mount Bell | |
---|---|
Highest point | |
Elevation | 3,269 m (10,725 ft) [1] [2] |
Prominence | 799 m (2,621 ft) [1] |
Parent peak | Mount Waddington (4,019 m) [2] |
Isolation | 9.96 km (6.19 mi) [1] |
Listing | Mountains of British Columbia |
Coordinates | 51°24′52″N125°25′49″W / 51.41444°N 125.43028°W [3] |
Geography | |
Interactive map of Mount Bell | |
Location | British Columbia, Canada |
District | Range 2 Coast Land District |
Parent range | Coast Mountains Waddington Range [1] |
Topo map | NTS 92N6 Mount Waddington [3] |
Climbing | |
First ascent | 1936 |
Mount Bell is a 3,269-metre (10,725-foot) mountain summit in British Columbia, Canada.
Mount Bell is set in the Waddington Range in a remote wilderness area that few visit. Mount Bell is located 290 km (180 mi) northwest of Vancouver and 7.46 km (4.64 mi) northwest of Mount Waddington, which is the highest peak of the entire Coast Mountains range. [1] Mount Bell is highly glaciated with the Remote Glacier on the northwest slope, Cannonade Glacier on the northeast slope, Bell Glacier to the east, and Dorothy Glacier to the south. Precipitation runoff and glacial meltwater from Mount Bell's slopes drains into tributaries of the Klinaklini River. [1] Topographic relief is significant as the summit rises 2,270 meters (7,450 feet) above Bell Creek in four kilometers (2.5 miles).
The mountain was named in 1928 by Don Munday and the toponym was officially adopted on April 3, 1928, by the Geographical Names Board of Canada to honor Dr. Frederick C. Bell (1883–1971), a founding member of the Alpine Club of Canada and club president from 1926 through 1928. [4] Mount Bell in Aberta is also named after him.
The first ascent of the summit was made on July 26, 1936, by Bestor Robinson, Ken Austin, Raffi Bedayn, and Hervey Voge. [4]
Based on the Köppen climate classification, Mount Bell is located in the marine west coast climate zone. [5] 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 several glaciers which surround the slopes of Mount Bell.
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.
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.
Mount Tiedemann 3,838 m (12,592 ft), prominence 848 m (2,782 ft), 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.
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.
Mount Spetch is a 2,579-metre (8,461-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is part of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated 25 km (16 mi) east of Pemberton, midway between Mount Matier and Slalok Mountain, both one kilometre either side of Spetch. The mountain's name was submitted by Karl Ricker of the Alpine Club of Canada to honor Samuel W. Spetch, who operated the general store at Birken, and other businesses in Pemberton. The name was officially adopted on January 23, 1979, by the Geographical Names Board of Canada. The first ascent of the mountain was made in 1971 by J. Oswald and G. Walter. Precipitation runoff from the peak drains into Joffre Creek and Twin One Creek, both tributaries of the Lillooet River. The mountain and its climate supports the Matier Glacier on the northern slope.
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.
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.
Sessel Mountain is a 2,746-metre (9,009-foot) mountain summit located in the Thiassi Range of the Coast Mountains, in southwestern British Columbia, Canada. It is the fourth-highest point in the Thiassi Range. Sessel is situated 46 km (29 mi) northwest of Pemberton, and 4.3 km (3 mi) northwest of Mount Sampson, which is its nearest higher peak. An unnamed icefield rests on the northern side of the peak, and the Boomerang Glacier lies at the base of the south slopes. Precipitation runoff from the peak drains into tributaries of the Lillooet and Hurley Rivers. The mountain's descriptive name was submitted by mountaineer Karl Ricker of the Alpine Club of Canada for its similar shape to a sessel, the German word for "armchair". The name was officially adopted January 23, 1979, by the Geographical Names Board of Canada. The first ascent of the mountain was made in 1974 by John Clarke.
Tremor Mountain is a prominent 2,691-metre (8,829-foot) summit 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 Spearhead Range, which is a subset of the Garibaldi Ranges. It is situated 13 km (8 mi) southeast of Whistler, and 8.7 km (5 mi) south of Wedge Mountain, its nearest higher peak. Precipitation runoff from the south side of the peak as well as meltwater from the Platform Glacier drains into Fitzsimmons Creek which is a tributary of the Green River. Meltwater from the Tremor Glacier on the northwestern slope drains to Wedge Creek, and meltwater from the Shudder Glacier on the northeast slope drains into Billygoat Creek, a tributary of the Lillooet River. Tremor Mountain is often climbed as part of the Spearhead Traverse. The first ascent of the mountain was made in 1928 by A.J. Campbell Garibaldi survey party. The mountain's name origin refers to unexplained earth tremors when the first ascent party was on the summit. The mountain's toponym was officially adopted on September 6, 1951, by the Geographical Names Board of Canada.
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