Piton de la Fournaise Update

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Piton de la Fournaise eruption
From: Thomas Staudacher <staud@xxxxxxxxxxxxxxx>
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The April 2, 2007 eruption at Piton de la Fournaise started at about 650 m 
altitude after a short summit eruption within Dolomieu crater on February 18, 
followed by an other short flank eruption at 1900 m altitude close to 
the ?Deuxième Formica Leo? crater on March 30.

Since the beginning, the eruption was accompanied by a very strong seismic 
activity beneath the summit, which let us fear a collapse of the Dolomieu 
crater floor.

The eruption formed a very large cone of lapilies, lava fountains of up to 200 
m have been observed and lava debit of the eruption is extremely high. First 
volume estimations give us about 40x10^6 m^3 within the first 10 days, without 
the material which went to the sea.

In the night of April 5 to 6 and over the whole following day, the Dolomieu 
crater floor in fact collapsed, dragging along about 30 to 40 m of 
the ?Dolomieu sud? plateau and the remaining separation between Bory and 
Dolomieu craters. These collapses formed large dust clouds above Piton de la 
Fournaise and the seismic events were felt by habitants at the 4 km far ?gite 
du volcan?. On Friday a new collapse again formed such a dust cloud.

New estimations of the depth of Dolomieu are about 300 m or even more over an 
area of 1000 to 800 m, with an estimated volume of about 50x x10^6 m^3 .

Presently the eruption goes on with lava fountains about 100 m high and a lava 
flow of up to 200 m long going to the sea.

During this eruption, enhanced SO2 were measured by the local ORA and SO2 and 
dust clouds were observed from space over the Indian Ocean.

Thomas Staudacher

OVPF/IPGP

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Thomas Staudacher
Observatoire volcanologique du Piton de la Fournaise
 14 RN3 le 27ème km
F-97418 La Plaine des Cafres
 La Réunion
tél +262(0)262 27 52 92
fax +262(0)262 59 12 04
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