Report on Ulawun (Papua New Guinea) — April 1994
Bulletin of the Global Volcanism Network, vol. 19, no. 4 (April 1994)
Managing Editor: Richard Wunderman
Ulawun (Papua New Guinea) Sharp increase in seismicity followed by strong dark grey emissions
Please cite this report as:
Global Volcanism Program, 1994. Report on Ulawun (Papua New Guinea). In: Wunderman, R (ed.), Bulletin of the Global Volcanism Network, 19:4. Smithsonian Institution. http://dx.doi.org/10.5479/si.GVP.BGVN199404-252120.
Papua New Guinea
5.05°S, 151.33°E; summit elev. 2334 m
All times are local (unless otherwise noted)
"There was an increase in the level of activity in April. At the beginning of the month, emissions consisted of moderate white vapour. However, these emissions changed through the month to strong thick white vapour and there were occasional reports of grey and blue emissions. On 19 April, very strong, thick, dark grey emissions were reported. Very fine ashfall was reported on the NW side of the volcano on 28 April, and steady weak red glow was seen on the 30th.
"Seismic monitoring was affected by telemetry problems from mid-March until 12 April. When the system was restored, daily earthquake totals were ~400-500. On 18 April there was a sharp increase to ~540 earthquakes/day. The daily totals then increased steadily through the remainder of the month to ~630 at month's end. Earthquake amplitudes showed a progressive increase after 12 April."
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. Ulawun volcano, also known as the Father, rises above the north coast of the island of New Britain across a low saddle NE of Bamus volcano, the South Son. The upper 1000 m of the 2334-m-high Ulawun volcano is unvegetated. A prominent E-W-trending escarpment on the south may be the result of large-scale slumping. Satellitic cones occupy the NW and eastern flanks. A steep-walled valley cuts the NW side of Ulawun volcano, 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.
Information Contacts: I. Itikarai and C. McKee, RVO.