Report on Witori (Papua New Guinea) — July 2004
Bulletin of the Global Volcanism Network, vol. 29, no. 7 (July 2004)
Managing Editor: Richard Wunderman.
Witori (Papua New Guinea) Mostly quiet except for thin white vapor emissions in July
Please cite this report as:
Global Volcanism Program, 2004. Report on Witori (Papua New Guinea) (Wunderman, R., ed.). Bulletin of the Global Volcanism Network, 29:7. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN200407-252080.
Papua New Guinea
5.576°S, 150.516°E; summit elev. 724 m
All times are local (unless otherwise noted)
Pago was quiet during July. The upper vents released thin white vapor throughout the month. No emission was observed from the lower vents. Seismic activity was at a low level.
Geologic Background. The 5.5 x 7.5 km Witori caldera on the northern coast of central New Britain contains the young historically active cone of Pago. The Buru caldera cuts the SW flank of Witori volcano. The gently sloping outer flanks of Witori volcano consist primarily of dacitic pyroclastic-flow and airfall deposits produced during a series of five major explosive eruptions from about 5600 to 1200 years ago, many of which may have been associated with caldera formation. The post-caldera Pago cone may have formed less than 350 years ago. Pago has grown to a height above that of the Witori caldera rim, and a series of ten dacitic lava flows from it covers much of the caldera floor. The youngest of these was erupted during 2002-2003 from vents extending from the summit nearly to the NW caldera wall.
Information Contacts: Ima Itikarai and Herman Patia, Rabaul Volcano Observatory (RVO), P. O. Box 386, Rabaul, Papua New Guinea.