Report on Manam (Papua New Guinea) — 15 May-21 May 2013

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 15 May-21 May 2013
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2013. Report on Manam (Papua New Guinea). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 15 May-21 May 2013. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (15 May-21 May 2013)


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 29 April-16 May activity at Manam was low, characterized by white, and sometimes blue, vapor plumes rising from Southern Crater. White vapor plumes also rose from Main Crater. Seismicity fluctuated but remained high until 1 May; seismicity then declined to a low on 4 May where it stayed for the rest of the period. RVO reminded people to stay away from the four main radial valleys, and especially the SE and SW ones where most products from the activity at Southern Crater were channeled.

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)