Report on Langila (Papua New Guinea) — December 1986
Scientific Event Alert Network Bulletin, vol. 11, no. 12 (December 1986)
Managing Editor: Lindsay McClelland
Langila (Papua New Guinea) Light ashfall; weak seismicity
Please cite this report as:
Global Volcanism Program, 1986. Report on Langila (Papua New Guinea). In: McClelland, L (ed.), Scientific Event Alert Network Bulletin, 11:12. Smithsonian Institution. http://dx.doi.org/10.5479/si.GVP.SEAN198612-252010.
Papua New Guinea
5.525°S, 148.42°E; summit elev. 1330 m
All times are local (unless otherwise noted)
Weak to moderate amounts of white vapor issued from Crater 2 during December, but no sounds or summit incandescence were reported. Small quantities of ash fell at the observation post . . . on 15 December. A pilot described a black plume rising to 1,500 m on 3 January but the report could not be confirmed by the local observer. Seismic activity remained at a 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: J. Mori and P. Lowenstein, RVO.