
Bagana
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Bagana is an active volcanic cone located in the centre of the island of Bougainville, Papua New Guinea, the largest island of the Solomon group. It is the most active volcano in the country, occupying a remote portion of central Bougainville Island. It is one of Melanesia's youngest and most active volcanoes.
In the Vinony graph
Within Vinony's link graph, Bagana is referenced by 9 other articles, and connects out to Autonomous Region of Bougainville, Papua New Guinea and Solomon Islands.
The entry is geolocated on the map in mountain, across 2 mapped points.
It sits within the topics Active volcanoes, Mountains of Papua New Guinea and Stratovolcanoes of Papua New Guinea.
Its subject is documented across 13 Wikipedia language editions.
Key facts
- Mountain.name
- Mt Bagana
- Mountain.photo
- MtBalbiToreNASA.jpg
- Mountain.photo_caption
- An ash plume originating from Bagana at right, just below the dark-colored caldera lake of Billy Mitchell
- Mountain.map
- Papua New Guinea
- Mountain.elevation_m
- 1893
- Mountain.prominence_m
- 1010
- Mountain.listing
- Ribu
- Mountain.location
- Bougainville, Papua New Guinea
- Mountain.range
- Emperor Range
- Mountain.type
- Lava cone
- Mountain.last_eruption
- 2000 to 2025 (ongoing)
via Wikipedia infobox
Wikidata facts
- Elevation
- 1750
- Image
- Bagana Volcano.jpg
Show 1 more fact
- Commons category
- Bagana Volcano
Sources (1)
via Wikidata · CC0
~2 min read
Encyclopedic overview
2 sectionsContents
- See also
- References
Bagana is an active volcanic cone located in the centre of the island of Bougainville, Papua New Guinea, the largest island of the Solomon group. It is the most active volcano in the country, occupying a remote portion of central Bougainville Island. It is one of Melanesia's youngest and most active volcanoes.
Bagana is a massive symmetrical, roughly 1893m-high lava cone largely constructed by an accumulation of viscous andesitic lava flows. The entire lava cone could have been constructed in about 300 years at its present rate of lava production. Eruptive activity at Bagana is frequent and is characterized by non-explosive effusion of viscous lava that maintains a small lava dome in the summit crater, although explosive activity occasionally producing pyroclastic flows also occurs. Lava flows form dramatic, freshly preserved tongue-shaped lobes up to 50 m thick with prominent levees that descend the volcano's flanks on all sides.
Excerpted from Wikipedia’s “Bagana” article, available under the CC BY-SA 4.0 licence.
On the map
2 mapped locations