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Papua New Guinea · Caldera

Billy Mitchell

Type
Caldera
Elevation
1544m
Last eruption
1580
Billy Mitchell
Photo: NASA Space Shuttle image ISS001-358-32, http://eol.jsc.nasa.gov/ · Public domain · Wikimedia Commons
Type
Caldera
Country
Papua New Guinea
Region
Southwestern Pacific / 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

2 recordedGlossary
Summary (VEI over time)
Click a bar to see individual eruptions · Use arrow keys to move between bars, Enter to open
1032~1087 · 1 eruptions · max VEI 51525~1580 · 1 eruptions · max VEI 610321142130614161525

Detailed timeline

  1. 1580 (±19 yrs)VEI 6Geological estimate
    1580 – end unknown
  2. 1032 (±23 yrs)VEI 5Geological estimate
    1032 – end unknown

Nearby volcanoes

External links

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