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Bagana
EntityQ799827· pop 14· linked from 9 articles

Also known as Mount Bagana

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 sections
Contents
  • 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

Connections

Categories