Report on Witori (Papua New Guinea) — October 1990
Bulletin of the Global Volcanism Network, vol. 15, no. 10 (October 1990)
Managing Editor: Lindsay McClelland.
Witori (Papua New Guinea) Mild summit and flank fumarolic activity
Please cite this report as:
Global Volcanism Program, 1990. Report on Witori (Papua New Guinea) (McClelland, L., ed.). Bulletin of the Global Volcanism Network, 15:10. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199010-252080
Papua New Guinea
5.5745°S, 150.5161°E; summit elev. 724 m
All times are local (unless otherwise noted)
"Emissions from the summit crater were very weak during an overflight in early September. Mild fumarolic emissions were noted from the NW flank of Pago."
Geological Summary. The active Pago cone has grown within the Witori caldera (5.5 x 7.5 km) on the northern coast of central New Britain contains the active Pago cone. The gently sloping outer caldera flanks consist primarily of dacitic pyroclastic-flow and airfall deposits produced during a series of five major explosive eruptions from about 5,600 to 1,200 years ago, many of which may have been associated with caldera formation. Pago cone may have formed less than 350 years ago; it has grown to a height above the 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. The Buru caldera cuts the SW flank.
Information Contacts: C. McKee and I. Itikarai, RVO.