Billy Mitchell
Kaldera · Papua New Guinea · 1544 m

- Tipe
- Kaldera
- Negara
- Papua New Guinea
- Wilayah
- Pasifik Barat Daya / Bougainville Volcanic Arc
- Ketinggian
- 1544 m
- Koordinat
- -6.090, 155.225
- Letusan terakhir
- 1580
- Kondisi tektonik
- Subduction zone / Crustal thickness unknown
- Bentuk lahan
- Caldera
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
Billy Mitchell, a small pyroclastic shield immediately NE of Bagana volcano, has produced some of the largest Holocene eruptions in Papua New Guinea. The andesitic-to-dacitic volcano is truncated by a 2-km-wide caldera containing a shallow lake with a small island near its S shore. Two major explosive eruptions, one about 900 years ago and the other about 370 years ago, produced dacitic pyroclastic-fall deposits that cover most of the northern half of Bougainville Island. The younger eruption may have been responsible for formation of the nearly vertical, steep-walled summit caldera. Pyroclastic-flow and -surge deposits extend 25 km to the E coast of Bougainville Island.
Ringkasan Wikipedia
Ringkasan InggrisBilly Mitchell is a dormant pyroclastic shield volcano in central Bougainville, just north-east of the Bagana Volcano in Papua New Guinea. It is a small pyroclastic shield truncated by a 2 km wide caldera filled by a crater lake. It is named after Billy Mitchell, a 20th-century United States Army general who is sometimes regarded as the father of the United States Air Force.
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Riwayat letusan
Garis waktu rinci
- 1580 (±19 tahun)VEI 6Perkiraan geologi1580 – Berlangsung
- 1032 (±23 tahun)VEI 5Perkiraan geologi1032 – Berlangsung
Tautan eksternal
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