Billy Mitchell
Caldera · Papua New Guinea · 1544 m

- 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
Línea de tiempo detallada
- 1580 (±19 años)VEI 6Estimación geológica1580 – En curso
- 1032 (±23 años)VEI 5Estimación geológica1032 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.