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Report on Matthew Island (France) — July 1977

Natural Science Event Bulletin, vol. 2, no. 7 (July 1977)
Managing Editor: David Squires.

Matthew Island (France) Photograph from 11 February showing the vent

Please cite this report as:

Global Volcanism Program, 1977. Report on Matthew Island (France). In: Squires, D. (ed.), Natural Science Event Bulletin, 2:7. Smithsonian Institution. https://doi.org/10.5479/si.GVP.NSEB197707-258010.

Volcano Profile |  Complete Bulletin


Matthew Island

France

22.33°S, 171.32°E; summit elev. 177 m

All times are local (unless otherwise noted)


[An RNZAF crew flew over Matthew Island on 11 February and photographed the volcano. The vent was weakly emitting vapor (figure 1).]

Figure (see Caption) Figure 1. Photograph taken from the N on 11 February 1977, showing the vent and about 2/3 of Matthew Island. Photograph taken by the Royal New Zealand Air Force (RNZAF).

Geologic Background. Isolated Matthew Island is composed of two low andesitic-to-dacitic cones separated by a narrow isthmus. Matthew Island was discovered in 1788 by a ship captain, who named the island after the owner of his vessel. Only the triangular eastern portion of the small, 0.6 x 1.2 km wide island was present prior to the 1940s, when construction of the larger western segment began; it consists primarily of lava flows. The 177-m-high western cone contains a crater that is breached to the NW and is filled by a lava flow whose terminus forms the NW coast.

Information Contacts: I. Nairn, NZGS, Rotorua.