Report on Langila (Papua New Guinea) — June 1984

Scientific Event Alert Network Bulletin, vol. 9, no. 6 (June 1984)
Managing Editor: Lindsay McClelland

Langila (Papua New Guinea) Occasional ash emission; seismicity weak

Please cite this report as:

Global Volcanism Program, 1984. Report on Langila (Papua New Guinea). In: McClelland, L (ed.), Scientific Event Alert Network Bulletin, 9:6. Smithsonian Institution. http://dx.doi.org/10.5479/si.GVP.SEAN198406-252010.

Volcano Profile |  Complete Bulletin |  Download PDF [future] |  Export Citation [future]


Langila

Papua New Guinea

5.525°S, 148.42°E; summit elev. 1330 m

All times are local (unless otherwise noted)


"Activity was generally very weak at both craters in June. The emissions were usually white or occasionally blue vapours. However, lightly ash-laden clouds were emitted from Crater 2 on 16-18 and 21 June. Seismicity was at a very low level throughout, with occasional low-amplitude volcanic earthquakes."

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: C. McKee, RVO.