Mount Balbi
Balbi
Stratovolcano · Papua New Guinea · 2715m

- Type
- Stratovolcano
- Country
- Papua New Guinea
- Region
- Southwestern Pacific Volcanic Regions / Bougainville Volcanic Arc
- Elevation
- 2715m
- Coordinates
- -5.916, 155.001
- Last eruption
- Unknown
- Tectonic setting
- Subduction zone / Crustal thickness unknown
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
The complex andesitic Balbi stratovolcano on Bougainville Island includes a large number of coalesced cones and lava domes. Five well-preserved craters occupy a NW-SE-trending ridge north of the summit cone, which also contains a crater. Three large valleys with steep headwalls dissect the flanks. The age of the most recent eruption is not known precisely. An oral tradition of a major eruption during the 19th century is thought to be in error, but could refer to minor eruptive activity. Fumaroles are located within 600-m-wide Crater B and on its W flank.
From Wikipedia
Mount Balbi is a Holocene stratovolcano located in the northern portion of the island of Bougainville, Papua New Guinea. A gentle prominence at 05°54′09″S 154°59′28″E is the highest point of the island. There are five volcanic craters east of the summit, one of which contains a crater lake. The summit is composed of coalesced cones and lava domes which host a large solfatara field. There are numerous fumaroles near the craters, though Balbi has not erupted in historic time.
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Eruption history
Detailed timeline
- 1825 (±25 yrs)VEI ?Geological estimate1825 – OngoingCrater B ?
External links
⚠ For reference only. Not for emergency response.