Report on Manam (Papua New Guinea) — June 2001
Bulletin of the Global Volcanism Network, vol. 26, no. 6 (June 2001)
Managing Editor: Richard Wunderman.
Manam (Papua New Guinea) False report of 25 June lava flows; low-level ash emissions continue
Please cite this report as:
Global Volcanism Program, 2001. Report on Manam (Papua New Guinea) (Wunderman, R., ed.). Bulletin of the Global Volcanism Network, 26:6. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN200106-251020.
Papua New Guinea
4.08°S, 145.037°E; summit elev. 1807 m
All times are local (unless otherwise noted)
Activity remained low following the 4 June 2000 eruption of Southern Crater. A pilot's report of multiple lava flows traveling from Manam on 25 June along with an ash cloud to 4.5 km was determined to be false. The Rabaul Volcano Observatory reported that the volcano had been quiet for many months and that the only observed activity occurred on 14 June when fine ash was produced from a small emission, and on 26 June when weak roaring/rumbling noises were heard. After 26 June only occasional low-level ash emissions took place. There have been no instrumental recordings since 16 January 2001.
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: Ima Itikarai, Rabaul Volcano Observatory (RVO), P.O. Box 386, Rabaul, Papua New Guinea; Washington Volcanic Ash Advisory Center (VAAC), Satellite Analysis Branch, NOAA/NESDIS/E/SP23, NOAA Science Center Room 401, Camp Springs, MD 20746, USA (URL: http://www.ssd.noaa.gov/).