Analysis of seismic activity associated with the eruptions of 2007, which led to the collapse
of the Dolomieu crater on April 5th, reveals the link between the seismicity and the magma …

In the present episode of eruptive activity, evidence from seismicity for sustained magma
inflow from depth into the edifice of Piton de la Fournaise is lacking. Pre-eruptive main …

Seismic data have been used to catalog the location and volume of most of the rockfalls that
occurred at the Piton de la Fournaise volcano from May 2007, just after the major collapse of …

Arrival times of seismic waves from local earthquakes are inverted for both locating the
source and defining the 3-D velocity heterogeneity of Piton de la Fournaise. The lateral …

Piton de la Fournaise volcano (La Réunion Island) is one of the most active basaltic
volcanoes, with an average of one eruption every 10months. This study provides the first …

On April 5th 2007, a major collapse of the Dolomieu summit crater occurred at Piton de La
Fournaise volcano (La Réunion Island). To constrain the origin and the dynamics of the …

Peripheral diffuse degassing of CO 2 from the soil occurs across the western flank of Piton
de la Fournaise volcano (La Réunion Island, Indian Ocean) along a narrow zone. In this …

We explore the possible relationships between a structural heterogeneity, the hydrothermal
system, and the intrusive activity at Piton de la Fournaise volcano. Geological and …

Volcano‐tectonic seismicity has been recorded for decades on various volcanoes and is
linked with the magma transport and reservoir pressurization. Yet earthquakes often appear …

The short eruption of June 14–15 1985 was the beginning of an important cycle of activity of
Piton de la Fournaise that lasted more than two years and comprised twenty or so eruptive …