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Billy Mitchell

Caldera · 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
Tipo
Caldera
Paese
Papua New Guinea
Regione
Southwestern Pacific Volcanic Regions / Bougainville Volcanic Arc
Altitudine
1544 m
Coordinate
-6.090, 155.225
Ultima eruzione
1580
Contesto tettonico
Subduction zone / Crustal thickness unknown
Forma vulcanica
Caldera
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

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.

Storia delle eruzioni

Riepilogo (VEI nel tempo)
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1032~1087 · 1 eruzioni · VEI max. 51525~1580 · 1 eruzioni · VEI max. 610321142130614161525

Cronologia dettagliata

  1. 1580 (±19 anni)VEI 6Stima geologica
    1580 – In corso
  2. 1032 (±23 anni)VEI 5Stima geologica
    1032 – In corso

Link esterni

⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.