Report on Langila (Papua New Guinea) — 10 October-16 October 2007
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 10 October-16 October 2007
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2007. Report on Langila (Papua New Guinea). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 10 October-16 October 2007. Smithsonian Institution and US Geological Survey.
Papua New Guinea
5.525°S, 148.42°E; summit elev. 1330 m
All times are local (unless otherwise noted)
RVO reported that emission of ash and white vapor plumes from Langila's Crater 2 continued during 1-16 October. Plumes rose to altitudes of 1.8-2.8 km (5,900-9,200 ft) a.s.l. and drifted WNW. The emissions were occasionally accompanied by roaring noises. Crater 3 was quiet.
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.
Source: Rabaul Volcano Observatory (RVO)