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Report on Piton de la Fournaise (France) — 13 May-19 May 2015

Piton de la Fournaise

Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
13 May-19 May 2015
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2015. Report on Piton de la Fournaise (France). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 13 May-19 May 2015. Smithsonian Institution and US Geological Survey.

Weekly Report (13 May-19 May 2015)

Piton de la Fournaise


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

All times are local (unless otherwise noted)

OVPDLF reported that during 4-16 May the number and magnitude of earthquakes at Piton de la Fournaise increased, and inflation was detected at the base of the summit cone. Gas emissions intensified; specifically hydrogen sulfide emissions increased on 5 May after a peak of sulfur dioxide values on 3 May. A seismic crisis was detected on 17 May. Between 1100 and 1230 the network detected 200 volcano-tectonic events, and then at 1250 a more intense seismic crisis began. Significant deformation at the crater rim was detected and a few minutes later, at 1345, an eruption started outside and SE of Dolomieu crater in the Castle crater area. Visual confirmation occurred 15 minutes later as clouds moved away. Volcanologists observed the area and noted lava fountains from three fissures, and two lava flows. A very large gas plume emitted during the first few hours of the eruption rose 3.6-4 km altitude and drifted NW. The fissure furthest W stopped issuing lava fountains before midnight. On 18 May only one fissure was active and the SSW-drifting gas plume was much smaller. Hydrogen sulfide emissions continued to be high, and carbon dioxide emissions increased. Lava fountains from a single vent along the second fissure, further E, rose 40-50 m. The lava flow had traveled 4 km, reaching an elevation of 1.1 km. Three field observations occurred on 19 May; scientists observed lava fountains 20-30 m high, and the advancing lava flow which had traveled 750 m in the previous day, reaching 1 km elevation.

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.

Source: Observatoire Volcanologique du Piton de la Fournaise (OVPF)