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Report on Manam (Papua New Guinea) — 14 March-20 March 2007

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 14 March-20 March 2007
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2007. Report on Manam (Papua New Guinea). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 14 March-20 March 2007. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (14 March-20 March 2007)


Manam

Papua New Guinea

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

All times are local (unless otherwise noted)


RVO reported that Manam's Main Crater emitted gray ash plumes during 11-19 March. The plumes rose to altitudes of 2.3 km (7,500 ft) a.s.l. and drifted SE. Incandescence was visible the evenings of 11, 12, 16, and 18 March. Vapor clouds and occasional diffuse ash clouds were emitted from South Crater during 11-20 March.

According to a news article, four people were killed and one injured from an "ash-and-mud" avalanche in a valley on the northern part of the island. RVO received the report on 15 March, but had not yet confirmed whether it was a mudflow.

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.

Sources: Rabaul Volcano Observatory (RVO), Reuters