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Billy Mitchell

Kaldera · Papua New Guinea · 1544 m

Billy Mitchell truncated by a 2-km-wide caldera containing a lake. It is seen here from the north, with the eroded, forested Reini volcano on the center horizon and neighboring Bagana volcano at the top right. Billy Mitchell has been the source of some of the largest Holocene eruptions of Papua New Guinea. Two major explosive eruptions, one about 900 years ago and the other about 370 years ago, produced ashfall across most of the N half of Bougainville Island.
Billy Mitchell truncated by a 2-km-wide caldera containing a lake. It is seen here from the north, with the eroded, forested Reini volcano on the center horizon and neighboring Bagana volcano at the top right. Billy Mitchell has been the source of some of the largest Holocene eruptions of Papua New Guinea. Two major explosive eruptions, one about 900 years ago and the other about 370 years ago, produced ashfall across most of the N half of Bougainville Island. · Foto: Photo by Wally Johnson, 1989 (Australia Bureau of Mineral Resources). · Wikimedia Commons
Tipe
Kaldera
Negara
Papua New Guinea
Wilayah
Southwestern Pacific Volcanic Regions / 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.

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
1032~1087 · 1 letusan · VEI maks. 51525~1580 · 1 letusan · VEI maks. 610321142130614161525

Garis waktu rinci

  1. 1580 (±19 tahun)VEI 6Perkiraan geologi
    1580 – Berlangsung
  2. 1032 (±23 tahun)VEI 5Perkiraan geologi
    1032 – Berlangsung

Tautan eksternal

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