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Report on Manam (Papua New Guinea) — 24 November-30 November 2010

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 24 November-30 November 2010
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2010. Report on Manam (Papua New Guinea). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 24 November-30 November 2010. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (24 November-30 November 2010)


Manam

Papua New Guinea

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

All times are local (unless otherwise noted)


RVO reported that during 19-25 November light brown to dark gray ash plumes were seen rising 400-500 m above Manam's South Crater. People living on the island reported occasional roaring and rumbling noises. Incandescent material ejected from the crater mainly fell back in and around the crater, but occasionally spilled into the SE and SW valleys. White vapor rose from Main Crater and incandescence from the crater was visible on most nights from 21 November onward.

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.

Source: Rabaul Volcano Observatory (RVO)