Billy Mitchell
Caldera · Papua New Guinea · 1544m

- Type
- Caldera
- Country
- Papua New Guinea
- Region
- Southwestern Pacific Volcanic Regions / Bougainville Volcanic Arc
- Elevation
- 1544m
- Coordinates
- -6.090, 155.225
- Last eruption
- 1580
- Tectonic setting
- Subduction zone / Crustal thickness unknown
- Landform
- Caldera
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
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.
Eruption history
Detailed timeline
- 1580 (±19 yrs)VEI 6Geological estimate1580 – Ongoing
- 1032 (±23 yrs)VEI 5Geological estimate1032 – Ongoing
External links
⚠ For reference only. Not for emergency response.