Mount Neal | |
---|---|
Highest point | |
Elevation | 2,552 m (8,373 ft) [1] |
Prominence | 481 m (1,578 ft) [2] |
Parent peak | Wedge Mountain [1] |
Isolation | 3.93 km (2.44 mi) [2] |
Listing | Mountains of British Columbia |
Coordinates | 50°09′16″N122°41′37″W / 50.15444°N 122.69361°W [3] |
Naming | |
Etymology | Neal Carter |
Geography | |
Interactive map of Mount Neal | |
Location | British Columbia, Canada |
District | Lillooet Land District [3] |
Protected area | Garibaldi Provincial Park |
Parent range | Pacific Ranges [2] |
Topo map | NTS 92J2 Whistler |
Climbing | |
First ascent | 1949 |
Mount Neal is a 2,552-metre (8,373-foot) glaciated summit in British Columbia, Canada.
Mount Neal is located in the Coast Mountains, and 23 kilometres (14 mi) east-northeast of Whistler in Garibaldi Provincial Park. [3] Precipitation runoff and glacial meltwater from this mountain's slopes drains to the Lillooet River via Ure, Kakila, and Chaos creeks. [2] Mount Neal is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,250 metres (4,100 ft) above Chaos Creek in three kilometres (1.9 mi).
The mountain was named in 1929 by A.J. Campbell to honor Neal Carter (1902–1978), in recognition of Carter's excellent mapping of a large section of Garibaldi Park in the early days as a mountaineer. [4] Carter was a prominent member of the British Columbia Mountaineering Club and was credited with many first ascents in Garibaldi Park in 1922–23. The toponym was officially adopted October 4, 1932, by the Geographical Names Board of Canada instead of the originally proposed toponym, Mount Carter. [4]
The first ascent of the summit was made September 6, 1949, by three members of the University of British Columbia's Varsity Outdoor Club: Arnie Ede, Fleming McConnell, and Bob Nicholson. [5]
Based on the Köppen climate classification, Mount Neal is located in the marine west coast 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 the Carter Glacier on the east slope of the peak, as well as the Needles Glacier to the west. The months of July and August offer the most favorable weather for climbing Mount Neal.
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.
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.
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