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Report on Manam (Papua New Guinea) — September 1997

Bulletin of the Global Volcanism Network, vol. 22, no. 9 (September 1997)
Managing Editor: Richard Wunderman.

Manam (Papua New Guinea) Few earthquakes, gentle steaming, and nighttime crater glow

Please cite this report as:

Global Volcanism Program, 1997. Report on Manam (Papua New Guinea). In: Wunderman, R (ed.), Bulletin of the Global Volcanism Network, 22:9. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199709-251020.

Volcano Profile |  Complete Bulletin


Manam

Papua New Guinea

4.08°S, 145.037°E; summit elev. 1807 m

All times are local (unless otherwise noted)


Seismicity remained low throughout September with 700-1,500 low-amplitude events measured per day. A water-tube tiltmeter 4 km SW of the summit showed no significant deformation. South Crater was quiet with continual gentle white-to-blue vapor emissions. A steady, dull glow was observed at nights. This glow ceased sometime between the 25th and 30th of the month (the summit was obscured by cloud between these dates). Main Crater emitted varying amounts of white vapor with an occasional gray tinge. No noise or glow was discernable.

Geologic Background. The 10-km-wide island of Manam, lying 13 km off the northern coast of mainland Papua New Guinea, is one of the country's most active volcanoes. Four large radial valleys extend from the unvegetated summit of the conical 1807-m-high basaltic-andesitic stratovolcano to its lower flanks. These "avalanche valleys" channel lava flows and pyroclastic avalanches that have sometimes reached the coast. Five small satellitic centers are located near the island's shoreline on the northern, southern, and western sides. Two summit craters are present; both are active, although most historical eruptions have originated from the southern crater, concentrating eruptive products during much of the past century into the SE valley. Frequent historical eruptions, typically of mild-to-moderate scale, have been recorded since 1616. Occasional larger eruptions have produced pyroclastic flows and lava flows that reached flat-lying coastal areas and entered the sea, sometimes impacting populated areas.

Information Contacts: B. Talai and H. Patia, RVO.