Goat Peak | |
---|---|
Highest point | |
Elevation | 2,473 m (8,114 ft) [1] [2] |
Prominence | 744 m (2,441 ft) [1] |
Parent peak | Face Mountain (2,485 m) [1] [2] |
Isolation | 10.14 km (6.30 mi) [2] |
Listing | Mountains of British Columbia |
Coordinates | 50°32′48″N122°57′18″W / 50.54667°N 122.95500°W [3] |
Geography | |
Interactive map of Goat Peak | |
Country | Canada |
Province | British Columbia |
District | Lillooet Land District |
Parent range | Coast Mountains |
Topo map | NTS 92J10 Birkenhead Lake |
Goat Peak is a 2,473-metre (8,114-foot) summit located in the Pemberton Valley of British Columbia, Canada.
Goat Peak is situated in the Coast Mountains, 28 km (17 mi) north-northwest of Pemberton and one kilometer immediately west of Tenquille Mountain. [4] Precipitation runoff from the mountain's slopes drains south into Wolverine Creek and west into Mowich Creek which are both tributaries of the Lillooet River; and north to Hurley River. Goat Peak is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 2,230 meters (7,316 ft) above Lillooet River and Pemberton Valley in less than 5 km (3.1 mi). The mountain is on unceded territory of the Lil'wat and N'Quatqua, which is an important spiritual, cultural and food gathering area. [5] The surrounding area is habitat for the South Chilcotin grizzly bear, black bear, mountain goat, wolverine, wolf, and deer. The mountain's toponym was officially adopted December 31, 1970, by the Geographical Names Board of Canada. [3] The landform was originally identified as "Goat Mountain" in 1936 by the Canadian Alpine Journal. [4]
Based on the Köppen climate classification, Goat Peak is located in a subarctic 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. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports unnamed glaciers on the north and northeast slopes. The months July through September offer the most favorable weather for viewing or climbing Goat Peak.
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.
Joffre Peak is a 2,721-metre (8,927-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the second-highest point of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated 26 km (16 mi) east of Pemberton and 11 km (7 mi) northeast of Lillooet Lake. Joffre is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,500 meters (4,920 ft) above Cayoosh Creek in 4 km (2.5 mi). The nearest higher peak is Mount Matier, 1.6 km (1 mi) to the south. The mountain's climate supports the Matier Glacier on the southwest slope, and the Anniversary Glacier on the southeast slope. Precipitation runoff from the peak drains into Joffre Creek and Cayoosh Creek which are both within the Fraser River watershed.
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 Hartzell is a 2,615-metre (8,579-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 Mount Spetch, each a half kilometre either side of Hartzell. The mountain's name was submitted by Karl Ricker of the Alpine Club of Canada to honor Carl A. Hartzell, an early settler and postmaster at Pemberton. The name was officially adopted on January 23, 1979, by the Geographical Names Board of Canada. 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 Hartzell Glacier on the southeast slope, and the Matier Glacier on the northern slope.
Mount Sampson is a 2,811-metre (9,222-foot) mountain summit located in the Thiassi Range of the Coast Mountains, in the Pemberton Valley of southwestern British Columbia, Canada. It is the highest point in the Thiassi Range. Sampson is situated 41 km (25 mi) northwest of Pemberton, and 21.5 km (13 mi) southeast of Mount Ethelweard, which is its nearest higher peak. Precipitation runoff from the peak drains into tributaries of the Lillooet and Hurley Rivers.
Duffey Peak is a 2,219-metre (7,280-foot) mountain summit located in southwest British Columbia, Canada.
Handcar Peak is a 2,338-metre (7,671-foot) mountain summit located in the Railroad Group of the Coast Mountains, in the Pemberton Valley of southwestern British Columbia, Canada. It is situated 38 km (24 mi) northwest of Pemberton and 3 km (2 mi) west of Locomotive Mountain. Precipitation runoff from the peak drains into Sampson Creek and Buck Creek which are both tributaries of the Lillooet River. Handcar Peak is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising over 2,050 meters (6,725 ft) above Lillooet River and Pemberton Valley in approximately 4 km (2.5 mi). The mountain's name was proposed in 1978 by mountaineer Karl Ricker of the Alpine Club of Canada, in association with Railroad Pass, Railroad Creek and other railroad-related names of the immediate vicinity. The toponym was officially adopted January 23, 1979, by the Geographical Names Board of Canada.
Face Mountain is a 2,485-metre (8,153-foot) mountain summit located in British Columbia, Canada.
Ipsoot Mountain is a 2,576-metre (8,451-foot) glaciated summit located in southwest British Columbia, Canada.
Tenquille Mountain is a 2,391-metre (7,844-foot) summit located in the Pemberton Valley of British Columbia, Canada.
Sun God Mountain is a 2,421-metre (7,943-foot) summit located in British Columbia, Canada.
Seven O'clock Mountain is a 2,341-metre (7,680-foot) summit located near the Pemberton Valley of British Columbia, Canada.
Mount Ronayne is a 2,290-metre (7,513-foot) summit located in the Pemberton Valley of British Columbia, Canada.
Mount Barbour is a 2,290-metre (7,513-foot) summit located in the Pemberton Valley of British Columbia, Canada.
Vantage Peak is a 2,235-metre (7,333-foot) mountain summit located in the Coast Mountains of British Columbia, Canada. It is part of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated 28.5 km (18 mi) east of Pemberton on the boundary of the Nlháxten/Cerise Creek Conservancy. Precipitation runoff from the peak drains southwest into Twin One Creek thence Lillooet Lake; the north slope drains into headwaters of Cerise Creek; and the east slope drains into Caspar Creek thence Cayoosh Creek which is within the Fraser River watershed. Vantage Peak is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,135 meters (3,724 ft) above Twin One Creek in 4 km (2.5 mi). The nearest higher neighbor is Mount Duke, 2.08 km (1 mi) to the southeast.
Mount Howard is a 2,551-metre (8,369-foot) mountain summit located in the Coast Mountains of British Columbia, Canada. It is part of the Joffre Group, which is a subset of the Lillooet Ranges. Mount Howard is situated 27 km (17 mi) east of Pemberton and immediately southeast of Mount Matier. Precipitation runoff from the peak drains into Twin One Creek thence Lillooet Lake which is within the Lillooet River watershed. Mount Howard is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,650 meters (5,413 ft) above Twin One Creek in 4 km (2.5 mi).
Whitecap Mountain is a 2,918-metre (9,573-foot) summit in British Columbia, Canada.
Carcajou Peak is a 2,239-metre (7,346-foot) mountain summit in British Columbia, Canada.
Twin Goat Mountain is a 2,128-metre (6,982-foot) summit in British Columbia, Canada.