Mount Talbot | |
---|---|
Highest point | |
Elevation | 2,105 m (6,906 ft) [1] [2] |
Prominence | 695 m (2,280 ft) [2] |
Isolation | 3.06 km (1.90 mi) [2] |
Coordinates | 44°45′03″S167°59′51″E / 44.750825°S 167.997525°E [2] |
Naming | |
Etymology | Arthur Ernest Talbot |
Geography | |
Interactive map of Mount Talbot | |
Location | South Island |
Country | New Zealand |
Region | Southland [2] |
Protected area | Fiordland National Park |
Parent range | Darran Mountains [3] |
Topo map | Topo50 CB09 [4] |
Geology | |
Rock age | 136 ± 1.9 Ma |
Rock type | Gabbronorite, dioritic orthogneiss |
Climbing | |
First ascent | 1924 |
Mount Talbot is a 2,105-metre-elevation (6,906-foot) mountain in Fiordland, New Zealand.
Mount Talbot is part of the Darran Mountains and is situated above the Homer Tunnel in the Southland Region of South Island. It is set within Fiordland National Park which is part of the Te Wahipounamu UNESCO World Heritage Site. [2] Precipitation runoff from the mountain drains north into the headwaters of the Gulliver River and south into the headwaters of the Hollyford River. Topographic relief is significant as the summit rises 1,600 metres (5,249 feet) above the Gulliver River in two kilometres and 1,245 metres (4,085 feet) above Gertrude Valley in one kilometre. The nearest higher peak is Mount Crosscut, 3.8 kilometres to the east-southeast. [2]
The mountain was named to honour Arthur Ernest Talbot (1876–1917), a New Zealand mountaineer and alpine explorer who was well known for explorations in northern Fiordland, particularly in 1910 discovering a route to Milford near this mountain. [4] He was killed in action in Europe during World War I. This mountain's toponym has been officially approved by the New Zealand Geographic Board. [4] The first ascent of the summit was made in 1924 by George Moir, Ken Roberts, Harry Slater, and Bob Sinclair. [3]
Climbing routes with first ascents: [3]
Based on the Köppen climate classification, Mount Talbot is located in a marine west coast climate zone. [5] Prevailing westerly winds blow moist air from the Tasman Sea onto the mountain, where the air is forced upward by the mountains (orographic lift), causing moisture to drop in the form of rain and snow. This climate supports small unnamed glaciers on the slopes. The months of December through February offer the most favourable weather for viewing or climbing this peak. [6]
Mount Waddington, once known as Mystery Mountain, is the highest peak in the Coast Mountains of British Columbia, Canada. Although it is lower than Mount Fairweather and Mount Quincy Adams, which straddle the United States border between Alaska and British Columbia, Mount Waddington is the highest peak that lies entirely within British Columbia. It and the subrange which surround it, known as the Waddington Range, stand at the heart of the Pacific Ranges, a remote and extremely rugged set of mountains and river valleys.
Mount Robson is the most prominent mountain in North America's Rocky Mountain range; it is also the highest point in the Canadian Rockies. The mountain is located entirely within Mount Robson Provincial Park of British Columbia, and is part of the Rainbow Range. Mount Robson is the second highest peak entirely in British Columbia, behind Mount Waddington in the Coast Range. The south face of Mount Robson is clearly visible from the Yellowhead Highway, and is commonly photographed along this route.
The Gulliver River is a river in the Fiordland area of New Zealand. It starts in the Darran Mountains on the north slope of Mount Talbot, and flows north and then west into the Cleddau River, which runs into Milford Sound. The river was named in 1906 by W.G. Grave for Alf Grenfell, who had a nickname of "Gulliver". A track along the Gulliver River from the Cleddau is suitable for day walks in summer and autumn and can be extended on the Grave Talbot Track into the Espereance valley, past the 59 m (194 ft) high De Lambert Falls and over the Grave Talbot Pass.
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