Whitecap Mountain | |
---|---|
Highest point | |
Elevation | 2,918 m (9,573 ft) [1] |
Prominence | 1,533 m (5,030 ft) [1] |
Isolation | 71.44 km (44.39 mi) [1] |
Listing | Highest major summits of Canada Ultras of North America Isolated major summits of Canada Mountain peaks of Canada Mountains of British Columbia |
Coordinates | 50°42′58″N122°30′32″W / 50.71611°N 122.50889°W [2] |
Geography | |
Location | British Columbia, Canada |
District | Lillooet Land District |
Parent range | Coast Mountains Bendor Range [1] |
Topo map | NTS 92J10 Birkenhead Lake |
Whitecap Mountain is a 2,918-metre (9,573-foot) summit in British Columbia, Canada.
Whitecap Mountain is the highest point in the Bendor Range which is a subrange of the Coast Mountains. [1] [3] The remote glaciated peak is located 50 kilometres (31 mi) north-northeast of Pemberton and 40 kilometres (25 mi) west of Lillooet. Precipitation runoff from this mountain's south slope drains to Anderson Lake via Connel Creek, the northwest slope drains to Carpenter Lake via Keary Creek, and the east slope drains to Seton Lake via Whitecap Creek. This is all within the Fraser River watershed. [1] Whitecap Mountain is notable for its steep rise above local terrain as topographic relief is significant with the summit rising over 1,300 metres (4,265 ft) above the Connel Creek valley in 2.5 kilometres (1.6 mi). The mountain's local descriptive toponym was officially adopted on March 31, 1924, by the Geographical Names Board of Canada. [2]
Based on the Köppen climate classification, Whitecap Mountain is located in a tundra climate zone. [4] 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 three unnamed glaciers on the north, northwest, and east slopes of the mountain.
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.
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.
Lydia Mountain is a 2,100-metre (6,890-foot) summit located in the Tantalus Range, in Tantalus Provincial Park, in southwestern British Columbia, Canada. It is situated 14.5 km (9 mi) northwest of Squamish, and 5.46 km (3 mi) south-southeast of Mount Tantalus, which is the highest peak in the Tantalus Range. The nearest higher neighbor is The Red Tusk, 0.5 km (0 mi) to the west, and Mount Niobe lies 2.17 km (1 mi) to the east-southeast. Lake Lovely Water lies below the eastern slope of the peak and precipitation runoff from the peak drains east to the Squamish River, and west to the Clowhom River via Red Tusk Creek. Topographic relief is significant as Lydia Mountain rises 1,400 meters (4,600 feet) above Red Tusk Creek in approximately three kilometers (two miles). The mountain's name was officially adopted on June 6, 1957, by the Geographical Names Board of Canada. The mountain was named for mythic Lydia, of which Tantalus was a primordial ruler in Greek mythology. Several peaks in the Tantalus Range are named in association with Tantalus. The first ascent of Lydia Mountain was made in 1914 by Basil Darling and Allan Morkill.
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