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Report on Karkar (Papua New Guinea) — November 1979

Scientific Event Alert Network Bulletin, vol. 4, no. 11 (November 1979)
Managing Editor: David Squires.

Karkar (Papua New Guinea) No strong explosions; crater morphology described

Please cite this report as:

Global Volcanism Program, 1979. Report on Karkar (Papua New Guinea). In: Squires, D. (ed.), Scientific Event Alert Network Bulletin, 4:11. Smithsonian Institution.

Volcano Profile |  Complete Bulletin


Karkar

Papua New Guinea

4.649°S, 145.964°E; summit elev. 1839 m

All times are local (unless otherwise noted)


"As observed from the Kinim Observatory, no strong explosive activity occurred during November. During inspections of the summit and the crater lake floor on 17 and 18 November, it was found that fountaining of dark muddy water has virtually ceased and that several islands have been formed. The main island was [at the end of a peninsula] joined to the base of the S wall of the crater, and the other island was near the E edge of the lake. Several large boulders were present on the main island and it was bordered by narrow, smooth shores. Orange-brown discolouration was present over the central part of the island. At its N edge a vigorous geyser continuously jetted yellow-tinged water to heights of several tens of meters. The E half of the lake was green and the W half retained the same grey-brown colour seen previously."

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.

Information Contacts: C. McKee, RVO.