Big Snow Mountain | |
---|---|
Highest point | |
Elevation | 2,357 m (7,733 ft) [1] [2] |
Prominence | 1,196 m (3,924 ft) [1] |
Parent peak | Mount Saugstad (2,908 m) [1] |
Isolation | 8.2 km (5.1 mi) [1] |
Listing | Mountains of British Columbia |
Coordinates | 52°14′17″N126°41′15″W / 52.23806°N 126.68750°W [3] |
Geography | |
Interactive map of Big Snow Mountain | |
Country | Canada |
Province | British Columbia |
District | Range 3 Coast Land District |
Parent range | Coast Mountains |
Topo map | NTS 93D2 South Bentinck Arm [3] |
Big Snow Mountain is a 2,357-metre (7,733-foot) mountain summit located in British Columbia, Canada. [4]
Big Snow Mountain is a glaciated peak situated in the Coast Mountains, in a remote wilderness area that few visit. Big Snow is set 16 km (9.9 mi) south-southeast of Bella Coola and 430 km (270 mi) northwest of Vancouver. Precipitation runoff and glacier meltwater from Big Snow drains to Thorsen Creek → Bella Coola River → North Bentinck Arm, and to South Bentinck Arm via Brynildsen Creek → Smitley River → Noeick River. Topographic relief is significant as the summit rises 1,550 meters (5,085 feet) above Brynildsen Creek in 2.5 kilometers (1.55 mile). The mountain was named by a 1951 climbing party, [4] and the landform's toponym was officially adopted April 15, 1984, by the Geographical Names Board of Canada. [3]
Based on the Köppen climate classification, Big Snow Mountain is located in the marine west coast climate zone of western North America. [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 glaciers on the north, east and west slopes of Big Snow.
Nusatsum Mountain, is a mountain in the Pacific Ranges of the Coast Mountains of British Columbia, Canada, located near the Nusatsum River and south of and between the communities of Firvale and Hagensborg. The peak can be seen from Highway 20. The mountain is the equivalent of Mount Ararat in the traditions of the Nuxalk, as the place where survivors found refuge from the Great Flood. The landform's toponym was officially adopted March 13, 1947, by the Geographical Names Board of Canada. Other spellings of Nusatsum seen on older maps include "Nootsatsum", "Noosatum" and "Nutsatsum".
Defiance Mountain is a 2,659-metre-elevation (8,724-foot) summit in the northernmost Pacific Ranges of the Coast Mountains of British Columbia, Canada. It is located to the south of the Bella Coola River between the communities of Firvale and Hagensborg. Nusatsum Mountain is to its northwest and Stupendous Mountain to the northeast. The peak can be seen from Highway 20. The landform's toponym was officially adopted March 13, 1947, by the Geographical Names Board of Canada.
Mount Matier is a prominent 2,783-metre (9,131-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the highest point of the Joffre Group, which is a subset range of the Coast Mountains. It is situated 26 km (16 mi) east of Pemberton, and 9 km (6 mi) northeast of Lillooet Lake. Its nearest higher peak is Mount Weart, 30 km (19 mi) to the southwest. The slopes of the mountain are covered by the Matier Glacier on the northwest, Anniversary Glacier on the northeast, Twin One Glacier on the southeast, and Hartzell Glacier to the south. Precipitation runoff from the peak drains into Joffre Creek and Twin One Creek, both tributaries of the Lillooet River.
Slalok Mountain, originally known as Rex's Pillar, is a 2,653-metre (8,704-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the third-highest point of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated 24 km (15 mi) east of Pemberton, and 8 km (5 mi) northeast of Lillooet Lake. It is 4 km (2 mi) northeast of Duffey Peak and the nearest higher peak is Mount Matier, 1.9 km (1 mi) to the east. Precipitation runoff from the peak drains into Joffre Creek and Twin One Creek, both tributaries of the Lillooet River. The first ascent of the mountain was made in 1963 by C. Adam, T. Anderson, and G. Richardson. The mountain's name Slalok is the traditional name for the settlement of nearby Mount Currie. The name was officially adopted on June 11, 1979, by the Geographical Names Board of Canada. The mountain and its climate supports the Matier Glacier, Stonecrop Glacier, and Tszil Glacier on the northern slopes.
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.
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.
Otter Mountain is a prominent 2,693-metre (8,835-foot) glaciated summit located in the Coast Mountains of British Columbia, Canada. It is situated 16 kilometers northeast of Stewart, British Columbia, and the nearest higher peak is Mount Pattullo, 25.4 km (15.8 mi) to the north. Otter ranks as the 23rd most topographically prominent summit of Canada. Topographic relief is significant as the summit rises 2,380 meters above Bitter Creek Valley in 5 kilometers. This mountain's toponym was adopted as "Mount Otter" on 24 July 1945, and officially renamed Otter Mountain on 5 November 1953 by the Geographical Names Board of Canada. Precipitation runoff from the mountain drains west into Bitter Creek which is a tributary of the Bear River, or east to Nelson Creek which is part of the Nass River drainage basin, and all ultimately finds its way to the Inside Passage.
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