Report on Bagana (Papua New Guinea) — 2 March-8 March 2016
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
2 March-8 March 2016
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2016. Report on Bagana (Papua New Guinea). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 2 March-8 March 2016. Smithsonian Institution and US Geological Survey.
Papua New Guinea
6.137°S, 155.196°E; summit elev. 1855 m
All times are local (unless otherwise noted)
Based on analyses of satellite imagery and model data, the Darwin VAAC reported that on 3 March a plume from Bagana possibly containing ash rose to an altitude of 2.1 km (7,000 ft) a.s.l. and drifted 110 km NE; ash was not discernible in images and RVO stated that ash was not seen by ground observers. The next day an ash plume rose to an altitude of 2.1 km (7,000 ft) a.s.l. and drifted 45-55 km NE and E.
Geological Summary. Bagana volcano, occupying a remote portion of central Bougainville Island, is one of Melanesia's youngest and most active volcanoes. This massive symmetrical cone was largely constructed by an accumulation of viscous andesitic lava flows. The entire edifice could have been constructed in about 300 years at its present rate of lava production. Eruptive activity is frequent and 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 flanks on all sides.