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Report on Piton de la Fournaise (France) — November 1976

Piton de la Fournaise

Natural Science Event Bulletin, vol. 1, no. 14 (November 1976)
Managing Editor: David Squires.

Piton de la Fournaise (France) Lava flow during 2-3 November from fissure N of Dolomieu Crater

Please cite this report as:

Global Volcanism Program, 1976. Report on Piton de la Fournaise (France) (Squires, D., ed.). Natural Science Event Bulletin, 1:14. Smithsonian Institution. https://doi.org/10.5479/si.GVP.NSEB197611-233020

Piton de la Fournaise


21.244°S, 55.708°E; summit elev. 2632 m

All times are local (unless otherwise noted)

An effusive eruption began at 1300 on 2 November from a 300-m-long fissure N of Dolomieu Crater. The eruption ended at 0400 the next day after producing a lava flow 1 km long. No casualties or damage were reported. Piton de la Fournaise had been dormant since the end of five months of activity on 6 April 1976 [Bulletin of Volcanic Eruptions (BVE), no. 16].

Geological Summary. The massive Piton de la Fournaise basaltic shield volcano on the French island of RĂ©union in the western Indian Ocean is one of the world's most active volcanoes. Much of its more than 530,000-year history overlapped with eruptions of the deeply dissected Piton des Neiges shield volcano to the NW. Three calderas formed at about 250,000, 65,000, and less than 5000 years ago by progressive eastward slumping of the volcano. Numerous pyroclastic cones dot the floor of the calderas and their outer flanks. Most historical eruptions have originated from the summit and flanks of Dolomieu, a 400-m-high lava shield that has grown within the youngest caldera, which is 8 km wide and breached to below sea level on the eastern side. More than 150 eruptions, most of which have produced fluid basaltic lava flows, have occurred since the 17th century. Only six eruptions, in 1708, 1774, 1776, 1800, 1977, and 1986, have originated from fissures on the outer flanks of the caldera. The Piton de la Fournaise Volcano Observatory, one of several operated by the Institut de Physique du Globe de Paris, monitors this very active volcano.

Information Contacts: M. Krafft, Ensisheim.