Report on Karkar (Papua New Guinea) — 2 January-8 January 2008
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 2 January-8 January 2008
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2008. Report on Karkar (Papua New Guinea). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 2 January-8 January 2008. Smithsonian Institution and US Geological Survey.
Papua New Guinea
4.649°S, 145.964°E; summit elev. 1839 m
All times are local (unless otherwise noted)
RVO reported that white vapor emissions from the Bagiai cone in Karkar's inner caldera were observed by a visiting field team during 27-31 December. The resultant white vapor plume was also visible from the mainland. Communities to the W and SW reported hearing roaring noises associated with gas emissions. Images sent to RVO on 11 December indicated that the vegetation on the SE flank was completely withered.
Geologic Background. Karkar is a 19 x 25 km wide, forest-covered island that is truncated by two nested summit calderas. The 5.5-km-wide outer caldera was formed during one or more eruptions, the last of which occurred 9000 years ago. The eccentric 3.2-km-wide inner caldera was formed sometime between 1500 and 800 years ago. Parasitic cones are present on the N and S flanks of this basaltic-to-andesitic volcano; a linear array of small cones extends from the northern rim of the outer caldera nearly to the coast. Most historical eruptions, which date back to 1643, have originated from Bagiai cone, a pyroclastic cone constructed within the steep-walled, 300-m-deep inner caldera. The floor of the caldera is covered by young, mostly unvegetated andesitic lava flows.
Source: Rabaul Volcano Observatory (RVO)