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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
País
Papua New Guinea
Región
Southwestern Pacific Volcanic Regions / Bougainville Volcanic Arc
Altitud
1544 m
Coordenadas
-6.090, 155.225
Última erupción
1580
Contexto tectónico
Subduction zone / Crustal thickness unknown
Forma volcánica
Caldera
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

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.

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1032~1087 · 1 erupciones · VEI máx. 51525~1580 · 1 erupciones · VEI máx. 610321142130614161525

Línea de tiempo detallada

  1. 1580 (±19 años)VEI 6Estimación geológica
    1580 – En curso
  2. 1032 (±23 años)VEI 5Estimación geológica
    1032 – En curso

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.