Corrie Peak | |
---|---|
Highest point | |
Elevation | 2,263 m (7,425 ft) [1] [2] |
Prominence | 437 m (1,434 ft) [1] |
Isolation | 2.92 km (1.81 mi) [1] |
Listing | Mountains of British Columbia |
Coordinates | 49°59′09″N122°57′18″W / 49.98583°N 122.95500°W [3] |
Naming | |
Etymology | Corrie (geology) |
Geography | |
Interactive map of Corrie Peak | |
Country | Canada |
Province | British Columbia |
District | New Westminster Land District |
Protected area | Garibaldi Provincial Park |
Parent range | Garibaldi Ranges Coast Mountains |
Topo map | NTS 92G15 Mamquam Mountain |
Corrie Peak is a 2,263-metre (7,425-foot) summit in British Columbia, Canada.
Corrie Peak is located within Garibaldi Provincial Park on the southwest side of Cheakamus Lake, [4] and is part of the Garibaldi Ranges of the Coast Mountains. [1] It is situated 81 km (50 mi) north of Vancouver and 5 km (3 mi) north of Castle Towers Mountain. [3] Precipitation runoff from the peak drains north to Cheakamus Lake which is within the Cheakamus River watershed. Topographic relief is significant as the summit rises 1,430 meters (4,692 feet) above the lake in 3 km (2 mi).
The peak was named in 1916 by Scottish-born botanist John Davidson. [4] In Scotland "Corrie" refers to a steep-sided hollow on a mountain, which in other parts of the world is called a cirque. The mountain's toponym was officially adopted on September 2, 1930, by the Geographical Names Board of Canada as labelled on a 1928 topographic map of Garibaldi Park. [3]
Based on the Köppen climate classification, Corrie Peak is located in the marine west coast climate zone of western North America. [5] Weather fronts originating in the Pacific Ocean 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. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports the Corrie Glacier on the southwest slope.
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.
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. 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. 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". The mountain's name was officially adopted on September 2, 1930, by the Geographical Names Board of Canada. The first ascent of the mountain was made in 1950 by Roy Hooley, Jimmy Kilborn, and Ian Kirk.
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