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Report on Rabaul (Papua New Guinea) — May 1989

Scientific Event Alert Network Bulletin, vol. 14, no. 5 (May 1989)
Managing Editor: Lindsay McClelland.

Rabaul (Papua New Guinea) Seismicity increases slightly; inflation slows

Please cite this report as:

Global Volcanism Program, 1989. Report on Rabaul (Papua New Guinea). In: McClelland, L. (ed.), Scientific Event Alert Network Bulletin, 14:5. Smithsonian Institution. https://doi.org/10.5479/si.GVP.SEAN198905-252140.

Volcano Profile |  Complete Bulletin


Rabaul

Papua New Guinea

4.271°S, 152.203°E; summit elev. 688 m

All times are local (unless otherwise noted)


"In general, activity remained at background level in May. Seismicity increased slightly, with a total of 164 small caldera earthquakes. The daily earthquake count fluctuated between 0 and 19. The 7 events that could be located occurred in the NW part of the caldera seismic zone.

"Levelling measurements on 26 May showed that the S and SE parts of Matupit Island had risen by ~25 mm since the previous measurements on 30 March. Over the past 1.5 years, uplift has been approximately linear at a rate of ~40 mm/year, considerably less than the 1973-83 (pre-seismo-deformational crisis) rate of ~100 mm/year. No significant tilt changes were recorded in May, and EDM data showed no clear trends."

Geologic Background. The low-lying Rabaul caldera on the tip of the Gazelle Peninsula at the NE end of New Britain forms a broad sheltered harbor utilized by what was the island's largest city prior to a major eruption in 1994. The outer flanks of the 688-m-high asymmetrical pyroclastic shield volcano are formed by thick pyroclastic-flow deposits. The 8 x 14 km caldera is widely breached on the east, where its floor is flooded by Blanche Bay and was formed about 1400 years ago. An earlier caldera-forming eruption about 7100 years ago is now considered to have originated from Tavui caldera, offshore to the north. Three small stratovolcanoes lie outside the northern and NE caldera rims. Post-caldera eruptions built basaltic-to-dacitic pyroclastic cones on the caldera floor near the NE and western caldera walls. Several of these, including Vulcan cone, which was formed during a large eruption in 1878, have produced major explosive activity during historical time. A powerful explosive eruption in 1994 occurred simultaneously from Vulcan and Tavurvur volcanoes and forced the temporary abandonment of Rabaul city.

Information Contacts: H. Patia and C. McKee, RVO.