Report on Langila (Papua New Guinea) — June 1990
Bulletin of the Global Volcanism Network, vol. 15, no. 6 (June 1990)
Managing Editor: Lindsay McClelland.
Langila (Papua New Guinea) Vulcanian explosion earthquakes; weak red glow
Please cite this report as:
Global Volcanism Program, 1990. Report on Langila (Papua New Guinea) (McClelland, L., ed.). Bulletin of the Global Volcanism Network, 15:6. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199006-252010.
Papua New Guinea
5.525°S, 148.42°E; summit elev. 1330 m
All times are local (unless otherwise noted)
"A low level of activity prevailed . . . although there was an increase toward the end of the month. Crater 2 released a weak to moderate vapour and ash cloud while Crater 3 remained virtually inactive. Vulcanian explosion earthquakes were recorded occasionally. A weak red glow was observed over Crater 2 on most nights after 23 June."
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. de Saint-Ours and C. McKee, RVO.