GUNUNG · Selandia Baru
Mitre Peak
Mitre Peak / Rahotu
SourcePhoto: source
—
- Feels like
- —
- Humidity
- —
- Wind
- —
Source: Open-Meteo
Information
- Elevation
- 1.683 m
- Country
- Selandia Baru (NZ)
- Location / Range
- Fiordland National Park (bagian Te Wāhipounamu World Heritage), Pulau Selatan
- Mountain type
- Puncak ikonik yang menjulang hampir tegak lurus dari perairan Milford Sound; sebenarnya gugusan lima puncak yang dari kejauhan tampak sebagai satu titik — batuan hasil ukiran glasial Fiordland, bukan gunung berapi
- Volcanic?
- No (non-volcanic)
- Coordinates
- -44.6330, 167.8560
- Difficulty
- Sangat berat: meski tak terlalu tinggi, pendakian dimulai dari permukaan laut menembus hutan Fiordland yang lebat lalu menyusuri punggungan sempit yang sangat terekspos. Tali dianjurkan; umumnya butuh 2 hari dan ascent-nya jarang dilakukan
- Best Season
- Januari–Maret, ketika cuaca Fiordland paling stabil dan garis salju tinggi
- Permits & Rules
- Tidak perlu izin khusus untuk mendaki, tetapi akses lewat perahu/taksi air dari Milford Sound ke Sinbad Bay; kawasan DOC Fiordland. Sangat bergantung cuaca — Milford Sound menerima curah hujan hingga ±7 meter per tahun
- Hazards
- Eksposur ekstrem dengan jurang ribuan kaki langsung ke fiord, tidak ada sumber air di punggungan (harus membawa semua air), hutan sangat lebat, curah hujan tinggi, batu licin, dan keterpencilan yang menyulitkan evakuasi
Description
Mitre Peak (Rahotu), about 1,683 metres high, is one of New Zealand's most iconic mountains, rising almost sheer from the waters of Milford Sound in Fiordland National Park, part of the Te Wāhipounamu World Heritage Area. Although it looks like a single sharp point from afar, Mitre Peak is actually a closely grouped set of five peaks, and its rock is glacially carved rather than volcanic. Despite its modest height, climbing it is a serious undertaking because it begins at sea level: climbers usually take a boat to Sinbad Bay, push through very dense Fiordland bush, then follow a narrow ridge with fearsome exposure straight down to the fiord thousands of feet below. Ropes are recommended for some sections, and water must be carried in because there is none on the ridge. Dry weather windows are hard to find — Milford Sound is one of the wettest places on Earth with up to about 7 metres of rain a year — so ascents of Mitre Peak are relatively infrequent and best attempted from January to March.
Gallery
Foto bersumber dari Wikimedia Commons — klik untuk memperbesar & lihat sumbernya.
Routes
Pendakian berpemandu (guided ascent)
Sangat berat (dipandu, dengan tali pengaman pada seksi terekspos)Several professional mountain guiding operators offer guided ascents of Mitre Peak, using rope protection on the most exposed sections and scheduling around Fiordland's weather windows. It suits those who want to reach this iconic summit without handling the navigation and technical risk alone.
SourceRute standar via Sinbad Bay (punggungan selatan)
Sangat berat (mountaineering: hutan lebat, punggungan sangat terekspos, tali dianjurkan)The most common route: climbers take a boat or water taxi from Milford Sound to near Sinbad Bay, climb through very dense Fiordland bush to the ridge, then follow the narrow, highly exposed ridge to the summit. There is no water on the ridge, so it must be carried. It is usually done over two days, though strong climbers sometimes complete it in a single push. It depends heavily on a rare dry-weather window.
SourceClimbing Experiences
Accounts of climbing Mitre Peak almost all stress that it is far harder than its height suggests. Because it starts at sea level, climbers face very dense Fiordland bush, a narrow ridge with extreme exposure, and the challenge of carrying all their own water. Many creators highlight the boat ride to Sinbad Bay, the importance of a rare dry-weather window, and the dramatic Milford Sound views from the ridge. Other recurring themes are its status as one of New Zealand's most iconic yet rarely climbed mountains, with some choosing a guided ascent.
References
The summary above is compiled from the following sources. Click to explore them yourself.