Billy Mitchell
Caldera · Papua New Guinea · 1544 m

- Tipo
- Caldera
- Paese
- Papua New Guinea
- Regione
- Pacifico sud-occidentale / 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.
Sintesi da Wikipedia
Riassunto in ingleseBilly 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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Storia delle eruzioni
Cronologia dettagliata
- 1580 (±19 anni)VEI 6Stima geologica1580 – In corso
- 1032 (±23 anni)VEI 5Stima geologica1032 – In corso
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.