Report on Langila (Papua New Guinea) — October 1979
Scientific Event Alert Network Bulletin, vol. 4, no. 10 (October 1979)
Managing Editor: David Squires.
Langila (Papua New Guinea) Occasional ash emission
Please cite this report as:
Global Volcanism Program, 1979. Report on Langila (Papua New Guinea) (Squires, D., ed.). Scientific Event Alert Network Bulletin, 4:10. Smithsonian Institution. https://doi.org/10.5479/si.GVP.SEAN197910-252010.
Papua New Guinea
5.525°S, 148.42°E; summit elev. 1330 m
All times are local (unless otherwise noted)
"No further strong explosions have been observed since those of 27 September. The ash deposit from the 27 September explosions was several millimeters thick 10 km from the source. Grey ash clouds were seen on a few days at the beginning and end of October, and white vapour emissions were observed occasionally. 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 E flank of the extinct Talawe volcano in the Cape Gloucester area of NW New Britain. A rectangular, 2.5-km-long crater is breached widely to the SE; Langila was constructed NE of the breached crater of Talawe. An extensive lava field reaches the coast on the N 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. The youngest and smallest crater (no. 3 crater) was formed in 1960 and has a diameter of 150 m.
Information Contacts: C. McKee, RVO.