Report on Lopevi (Vanuatu) — 5 July-11 July 2006
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 5 July-11 July 2006
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2006. Report on Lopevi (Vanuatu). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 5 July-11 July 2006. Smithsonian Institution and US Geological Survey.
16.507°S, 168.346°E; summit elev. 1413 m
All times are local (unless otherwise noted)
Based on pilot reports, the Wellington VAAC reported that an eruption plume from Lopevi on 5 July reached an unknown altitude and smoke-and-ash plumes on 8 and 9 July reached altitudes of 3.7 km (12,000 ft) a.s.l. and drifted E and SE, respectively.
Geologic Background. The small 7-km-wide conical island of Lopevi, known locally as Vanei Vollohulu, is one of Vanuatu's most active volcanoes. A small summit crater containing a cinder cone is breached to the NW and tops an older cone that is rimmed by the remnant of a larger crater. The basaltic-to-andesitic volcano has been active during historical time at both summit and flank vents, primarily along a NW-SE-trending fissure that cuts across the island, producing moderate explosive eruptions and lava flows that reached the coast. Historical eruptions at the 1413-m-high volcano date back to the mid-19th century. The island was evacuated following major eruptions in 1939 and 1960. The latter eruption, from a NW-flank fissure vent, produced a pyroclastic flow that swept to the sea and a lava flow that formed a new peninsula on the western coast.