Cheakamus Mountain | |
---|---|
Highest point | |
Elevation | 2,588 m (8,491 ft) [1] |
Prominence | 298 m (978 ft) [1] |
Parent peak | Mount Benvolio (2613 m) [1] |
Listing | Mountains of British Columbia |
Coordinates | 50°00′00″N122°48′07″W / 50.00000°N 122.80194°W [2] |
Geography | |
Location | Garibaldi Provincial Park British Columbia, Canada |
District | New Westminster Land District |
Parent range | Fitzsimmons Range Garibaldi Ranges Coast Ranges |
Topo map | NTS 92G15 Mamquam Mountain [2] |
Climbing | |
First ascent | 1950 |
Easiest route | class 3 North Face/West Ridge [1] |
Cheakamus Mountain is a 2,588-metre (8,491-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 fourth-highest peak of the Fitzsimmons Range, which is a subset of the Garibaldi Ranges. [3] It is situated 16 km (10 mi) southeast of Whistler, and its nearest higher peak is Mount Benvolio, 1.65 km (1 mi) to the northwest. [3] The Diavolo Glacier spreads out below the north aspect of the peak, and precipitation runoff from the peak with meltwater from the glacier drains into tributaries of the Cheakamus River. The peak was named in association with the river, which in turn is anglicized from Tseearkamisht, a Squamish word meaning "people who use the cedar rope fishing net". [4] [5] The mountain's name was officially adopted on September 2, 1930, by the Geographical Names Board of Canada. [2] The first ascent of the mountain was made in 1950 by Roy Hooley, Jimmy Kilborn, and Ian Kirk. [1]
Based on the Köppen climate classification, Cheakamus Mountain is located in the marine west coast climate zone of western North America. [6] 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. The months July through September offer the most favorable weather for climbing Cheakamus Mountain.
Tricouni Peak is a mountain located south of Cypress Peak on the Squamish-Cheakamus divide within the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It was named in 1931 by Tom Fyles et al., the first ascent party. According to Tom Fyles himself, "Tricouni Mountain was the name suggested for the peak, as from a distance it had the appearance of three cones". A misinterpreted "resemblance to a 3-pointed tricouni boot nail" was mentioned only much later, and not by Fyles. The name "Tricouni Peak" was adopted on 22 June 1967.
Mount Weart is a 2,835-metre (9,301-foot) triple-summit mountain located in the Garibaldi Ranges of the Coast Mountains, in northwestern Garibaldi Provincial Park of southwestern British Columbia, Canada. It is situated 14 km (9 mi) northeast of Whistler, and its nearest higher peak is Wedge Mountain, 3.7 km (2 mi) to the south, which is the only peak within the park higher than Weart. The Armchair Glacier rests below the west aspect of the summit, and the massive Weart Glacier spans the northern and eastern aspects of the mountain. Precipitation runoff from the peak and meltwater from the glaciers drains into Wedgemount Lake and tributaries of the Lillooet River.
Rethel Mountain is a 2,408-metre (7,900-foot) mountain summit located in the Garibaldi Ranges of the Coast Mountains, in northwestern Garibaldi Provincial Park of southwestern British Columbia, Canada. It is situated 11 km (7 mi) northeast of Whistler, on the south side of Wedgemount Lake and west side of Wedgemount Glacier. Its nearest higher peak is Parkhurst Mountain, 1.3 km (1 mi) to the southeast. Rethel is set 3.2 km (2 mi) northwest of Wedge Mountain, the highest peak in Garibaldi Park, and 2.9 km (2 mi) southwest of Mount Weart, the second-highest in the park. Precipitation runoff from the peak drains into Wedgemount Creek and Rethel Creek, both tributaries of the Green River, which in turn is a tributary of the Lillooet River. It was named in association from Rethel station on the Pacific Great Eastern Railway route. The mountain's name was officially adopted on February 27, 1978, by the Geographical Names Board 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.
Mount Fitzsimmons is a 2,603-metre (8,540-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 third-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 Mount Benvolio, 0.5 km (0 mi) to the west-southwest. The Diavolo Glacier spreads out below the southeast aspect of the summit, and the Fitzsimmons Glacier descends the northwest slopes. 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 on August 19, 1924, by a party of the British Columbia Mountaineering Club. The peak was named for prospector James Fitzsimmons, who built a trail along Fitzsimmons Creek in an effort to haul supplies to a small copper mine he staked and worked. The mountain's name was officially adopted on September 2, 1930, by the Geographical Names Board of Canada.
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 Davidson is a 2,516-metre (8,255-foot) mountain summit located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. Visible from the Whistler Blackcomb ski area, it is situated 18 km (11 mi) south of Whistler, and its nearest higher peak is Castle Towers Mountain, 3 km (2 mi) to the west. The Cheakamus Glacier lies between these two summits, and precipitation runoff from the peak and meltwater from the glacier drains into tributaries of the Cheakamus River. The first ascent of the mountain was made in 1929 by Neal M. Carter and Emmy Milledge. The mountain is named after Professor John Davidson, who contributed a large amount of botanical knowledge about Garibaldi Park. The mountain's name was officially adopted on September 2, 1930, by the Geographical Names Board of Canada.
Decker Mountain is a 2,421-metre (7,943-foot) flat-topped 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 9 km (6 mi) southeast of Whistler, and 3.9 km (2 mi) west-northwest of Tremor Mountain, which is the highest point in the Spearhead Range. Precipitation runoff from the south side of the peak drains into Fitzsimmons Creek which is a tributary of the Cheakamus River, and meltwater from the Decker Glacier on the northeastern slope drains to Wedge Creek.
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.
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 Cheakamus 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 name was officially adopted on September 6, 1951, by the Geographical Names Board of Canada.
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