Queen Mary's Peak
| Queen Mary's Peak | |
|---|---|
| Tristan da Cunha | |
 Gambar satelit dari Tristan da Cunha | |
| Titik tertinggi | |
| Ketinggian | 2.062 m (6.765 ft) |
| Puncak | 2.062 m (6.765 ft) |
| Masuk dalam daftar | Sangat tinggi |
| Koordinat | 37°06′40″S 12°17′18″W / 37.11111°S 12.28833°W |
| Geografi | |
 Lokasi di Tristan da Cunha | |
| Letak | Tristan da Cunha |
| Geologi | |
| Usia batuan | 148 ± 8 ka[1] |
| Jenis gunung | Gunung berapi perisai |
| Letusan terakhir | Oktober 1961–Maret 1962[2] |
| Pendakian | |
| Pendakian pertama | Sekitar 1 Januari 1817[3] |
Queen Mary's Peak adalah gunung di pulau Tristan da Cunha, di Samudra Atlantik Selatan. Gunung ini memiliki ketinggian 2.062 meter (6.765 ft) di atas permukaan laut. Gunung ini dinamakan berdasarkan Mary dari Teck, Permaisuri dari Raja George V. Ini merupakan titik tertinggi di wilayah seberang laut Britania Raya bernama Saint Helena, Ascension dan Tristan da Cunha, dan di semua wilayah seberang laut Britania Raya dengan populasi permanen. Queen Mary's Peak berada di peringkat ke-17 menurut isolasi topografis.
Referensi
- ^ Dunkley, Peter N. (2002). Volcanic Hazard Assessment of Tristan da Cunha, South Atlantic (PDF). British Geological Survey.
- ^ "Tristan da Cunha". Global Volcanism Program. Institusi Smithsonian.
- ^ Carmichael, Dugald (1817), "Some Account of the Island of Tristan da Cunha and of its Natural Productions", The Transactions of the Linnean Society of London, 12: 483–513
Proyek lainnya
Media terkait Queen Mary's Peak di Wikimedia Commons
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