Report on Langila (Papua New Guinea) — October 1986
Scientific Event Alert Network Bulletin, vol. 11, no. 10 (October 1986)
Managing Editor: Lindsay McClelland.
Langila (Papua New Guinea) Low-level seismicity; weak vapor emissions
Please cite this report as:
Global Volcanism Program, 1986. Report on Langila (Papua New Guinea). In: McClelland, L. (ed.), Scientific Event Alert Network Bulletin, 11:10. Smithsonian Institution. https://doi.org/10.5479/si.GVP.SEAN198610-252010.
Papua New Guinea
5.525°S, 148.42°E; summit elev. 1330 m
All times are local (unless otherwise noted)
"Langila remained at non-eruptive levels of activity with emissions restricted to weak white vapour. There were no reports of incandescence or audible sounds from the summits, and seismicity was at a very low level."
Geologic Background. Langila, one of the most active volcanoes of New Britain, consists of a group of four small overlapping composite basaltic-andesitic cones on the lower eastern flank of the extinct Talawe volcano. Talawe is the highest volcano in the Cape Gloucester area of NW New Britain. A rectangular, 2.5-km-long crater is breached widely to the SE; Langila volcano was constructed NE of the breached crater of Talawe. An extensive lava field reaches the coast on the north and NE sides of Langila. Frequent mild-to-moderate explosive eruptions, sometimes accompanied by lava flows, have been recorded since the 19th century from three active craters at the summit of Langila. The youngest and smallest crater (no. 3 crater) was formed in 1960 and has a diameter of 150 m.
Information Contacts: P. Lowenstein and P. de Saint-Ours, RVO.