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Rabaul caldera, Papua New Guinea

Following a 27-hour period of intense earthquake activity, Tavurvur and Vulcan volcanoes on opposite sides of the Rabaul caldera erupted on September 19, 1994, at 6:05 a.m. and 7:17 a.m. respectively. The eruption column from Vulcan sent ash to at least 18 kilometers above sea level, and nearby Rabaul Town was quickly covered with ash between 25 and 80 centimeters thick. Activity stopped at Vulcan within about two weeks, but intermittent eruptive activity still continues at Tavurvur.

Small explosions at Tavurvur continued through December 1994. A short quiet period was followed by mild explosive activity between February and April 1995, which sent ash columns a few kilometers into the air. After another pause lasting about 6 months, frequent small explosions and ash emission resumed at Tavurvur in November 1995. Noteworthy activity since then includes intermittent strong strombolian activity, lava flows, and a small pyroclastic flow. On May 11, 1996, strombolian activity ejected slabs of lava 10 to 15 meters in diameter hundreds of meters above the vent and meter-sized blocks about 1 kilometer from the vent. On October 5, Tavurvur began erupting it's largest lava flow (4-5 million cubic meters) of the past 200 years. Another lava flow was erupted from Tavurvur in March 1997, and a strong explosion generated a small pyroclastic flow on April 12. Minor explosions and ash emission continue at Tavurvur and ash continues to fall intermittently on Rabaul Town and other areas around the caldera.

The Smithsonian Institution's Bulletin of the Global Volcanism Network provides online summaries of Rabaul caldera since 1996.

Rabaul Caldera, Papua New Guinea
Latitude and longitude 4.271 S., 152.203 E.

Globe: Location of Rabaul Caldera

Summit elevation 688 meters
Type of volcano caldera complex
Main hazards pyroclastic flows, tsunamis, ashfall, lahars
Date of last known eruption intermittent since 1994
Style of eruption explosive, effusive
Notes: Rabaul Caldera (14 x 9 km) is located on the north end of New Britain Island. The caldera forms a sheltered harbor whose north end was occupied by Rabaul Town before the 1994 eruption. Beginning as early as 1971 and increasing in 1983, a long period of unrest beneath the caldera (earthquakes and ground deformation) alerted scientists and residents alike of the possibility of renewed eruptive activity. Tavurvur and Vulcan also erupted together in 1878 and 1937-43; an eruption between May 29 and June 2, 1937, killed more than 500 people. Huge explosive eruptions 1,400 and 3,500 years ago significantly altered the caldera.

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U.S. Department of the Interior, U.S. Geological Survey, Menlo Park, California, USA
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Last modification: Wednesday, 10-Oct-2001 16:55:48 EDT (SRB)