Parapet Peak | |
---|---|
Highest point | |
Elevation | 2,463 m (8,081 ft) [1] [2] |
Prominence | 66 m (217 ft) [1] |
Parent peak | Isosceles Peak [2] |
Isolation | 0.77 km (0.48 mi) [1] |
Listing | Mountains of British Columbia |
Coordinates | 49°54′18″N122°54′17″W / 49.90500°N 122.90472°W [3] |
Naming | |
Etymology | Parapet |
Geography | |
Interactive map of Parapet Peak | |
Country | Canada |
Province | British Columbia |
District | New Westminster Land District [4] |
Protected area | Garibaldi Provincial Park |
Parent range | Garibaldi Ranges Coast Mountains |
Topo map | NTS 92G15 Mamquam Mountain [3] |
Climbing | |
First ascent | August 1922 |
Parapet Peak is a 2,463-metre (8,081-foot) mountain summit located in British Columbia, Canada.
Parapet Peak is set within Garibaldi Provincial Park and is part of the Garibaldi Ranges of the Coast Mountains. [1] It is situated 68 km (42 mi) north of Vancouver and 0.77 km (0 mi) north of Isosceles Peak, the nearest higher neighbor. [2] Precipitation runoff and glacial meltwater from the south side of the peak drains into the headwaters of the Pitt River, whereas the northern slope drains to Cheakamus Lake via Isosceles Creek. Topographic relief is significant as the summit rises 1,260 meters (4,134 feet) above Pitt River in 3 kilometers (1.9 miles).
The first ascent of Parapet Peak was made in August 1922 by Don Munday, his wife Phyllis Munday, Neal Carter, Harold O'Connor, and Clausen Thompson. [5] [6] The mountain's toponym was officially adopted on September 2, 1930, by the Geographical Names Board of Canada. [3]
Based on the Köppen climate classification, Parapet Peak is located in the marine west coast climate zone of western North America. [7] 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 the Isosceles Glacier on the east slope, the Gray Glacier on the north slope, and an unnamed glacier on the west slope of the peak.
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.
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 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.
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.
Spearman Peak is a 3,365-metre (11,040-foot) summit located in British Columbia, Canada.
Mount Carr is a 2,590-metre (8,497-foot) mountain summit located in British Columbia, Canada.
Spire Peaks is a 2,279-metre (7,477-foot) mountain located in British Columbia, Canada.
Isosceles Peak is a 2,488-metre (8,163-foot) mountain summit located in British Columbia, Canada.
Phyllis's Engine is a 2,517-metre (8,258-foot) granite pinnacle located in British Columbia, Canada.
Whirlwind Peak is a 2,427-metre (7,963-foot) mountain summit in southwestern British Columbia, Canada.
Hour Peak is a 2,329-metre (7,641-foot) mountain summit located in British Columbia, Canada.
Gentian Peak is a 2,197-metre (7,208-foot) summit in British Columbia, Canada.
Deception Peak is a 2,233-metre (7,326-foot) summit in British Columbia, Canada.
Jubilee Mountain is a 2,751-metre (9,026-foot) mountain summit in British Columbia, Canada.
Mount Sir Richard is a 2,681-metre (8,796-foot) glaciated summit in British Columbia, Canada.
Mount Neal is a 2,552-metre (8,373-foot) glaciated summit in British Columbia, Canada.
Shudder Mountain is a 2,671-metre (8,763-foot) summit in British Columbia, Canada.
Combatant Mountain, also called Mount Combatant, is a 3,762-metre (12,343-foot) summit in British Columbia, Canada.
Mount Pitt is a 2,487-metre (8,159-foot) summit in British Columbia, Canada.