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Report on Ulawun (Papua New Guinea) — 4 September-10 September 2002

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 4 September-10 September 2002
Managing Editor: Gari Mayberry

Please cite this report as:

Global Volcanism Program, 2002. Report on Ulawun (Papua New Guinea). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 4 September-10 September 2002. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (4 September-10 September 2002)


Ulawun

Papua New Guinea

5.05°S, 151.33°E; summit elev. 2334 m

All times are local (unless otherwise noted)


On 7 September a low-level (less than ~3.6 km a.s.l.) ash plume was visible on satellite imagery, extending to the NW.

Geologic Background. The symmetrical basaltic-to-andesitic Ulawun stratovolcano is the highest volcano of the Bismarck arc, and one of Papua New Guinea's most frequently active. The volcano, also known as the Father, rises above the N coast of the island of New Britain across a low saddle NE of Bamus volcano, the South Son. The upper 1,000 m is unvegetated. A prominent E-W escarpment on the south may be the result of large-scale slumping. Satellitic cones occupy the NW and E flanks. A steep-walled valley cuts the NW side, and a flank lava-flow complex lies to the south of this valley. Historical eruptions date back to the beginning of the 18th century. Twentieth-century eruptions were mildly explosive until 1967, but after 1970 several larger eruptions produced lava flows and basaltic pyroclastic flows, greatly modifying the summit crater.

Source: Darwin Volcanic Ash Advisory Centre (VAAC)