Mount Madeline | |
---|---|
Highest point | |
Elevation | 2,536 m (8,320 ft) [1] [2] |
Prominence | 543 m (1,781 ft) [2] |
Parent peak | Mount Tūtoko [2] |
Isolation | 2.87 km (1.78 mi) [2] |
Listing | New Zealand #62 |
Coordinates | 44°36′51″S168°02′45″E / 44.61417°S 168.04583°E [2] |
Geography | |
Interactive map of Mount Madeline | |
Location | South Island |
Country | New Zealand |
Region | Southland [2] |
Protected area | Fiordland National Park |
Parent range | Darran Mountains |
Topo map(s) | NZMS260 D40 [3] Topo50 CA09 [4] |
Geology | |
Rock age | 136 ± 1.9 Ma |
Rock type | Gabbronorite, dioritic orthogneiss |
Climbing | |
First ascent | 1920 |
Mount Madeline is a 2,536-metre-elevation (8,320-foot) mountain in Fiordland, New Zealand.
Mount Madeline is the second-highest peak of the Darran Mountains. It is situated in the Southland Region of South Island, and set within Fiordland National Park which is part of the Te Wahipounamu UNESCO World Heritage Site. [2] Precipitation runoff from the mountain drains west to the Tūtoko River via Leader Creek, and east to the Hollyford River via Madeline, Cleft, and Glacier creeks. Topographic relief is significant as the summit rises 2,500 metres (8,202 feet) above the Hollyford Valley in four kilometres and 2,100 metres (6,890 feet) above the Tūtoko Valley in four kilometres.
In 1895, Malcolm Ross, Kenneth Ross, W.J. Hodgkin, and Tom Fyfe climbed the lower west peak (2,516 m) of Madeline. [4] The first ascent of the true summit was made in March 1920 by Alf Cowling and Samuel Turner. [4] The mountain was named in 1921 after Samuel Turner's daughter, Madeline. [3] [5]
Based on the Köppen climate classification, Mount Madeline is located in a marine west coast climate zone, with a subpolar oceanic climate (Cfc) at the summit. [6] 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 unnamed glaciers on the peak's slopes. The months of December through February offer the most favourable weather for viewing or climbing this peak. [7]
Climbing routes with the first ascents: [4]
Fiordland, is a non-administrative geographical region of New Zealand in the south-western corner of the South Island, comprising the western third of Southland. Most of Fiordland is dominated by the steep sides of the snow-capped Southern Alps, deep lakes, and its steep, glacier-carved and now ocean-flooded western valleys. The name "Fiordland" derives from an alternate spelling of the Scandinavian word for steep glacial valleys, "fjord". The geographic area of Fiordland is dominated by, and roughly coterminous with, Fiordland National Park, New Zealand's largest national park.
Lake Marian is an alpine lake at the southern end of the Darran Mountains in the Fiordland National Park in the South Island of New Zealand. The lake is located just above the treeline in a hanging valley leading northwest from the Hollyford Valley near The Divide pass. The valley is sheltered by steep snow-covered peaks of over 2,000 metres (6,600 ft) on all sides apart from the entrance.
Mount Tūtoko is the highest peak in Fiordland National Park, in southwest New Zealand. It lies between the Hollyford Valley and Milford Sound, 15 kilometres due north of the Homer Tunnel at the northern end of the Darran Mountains. The glacier-covered mountain rises to a height of 2,723 metres (8,934 ft) and is visible from the Hollyford Track. Two slightly lower summits lie just to the south of the main peak.
The Darran Mountains are a prominent range within New Zealand's Fiordland National Park, the country's biggest national park. They contain the park's highest peak, Mount Tūtoko.
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