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 …

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 …

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 …

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

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 …

From 2003 to 2007, eruptive activity at Piton de la Fournaise was shown to follow cycles,
comprising many summit/proximal eruptions and finishing by a distal eruption. GPS …

Calderas are oval fault-bounded depressions in volcanic regions. The formation of a small
analog, a summit pit-crater, has followed a ten-month cycle of eruptive activity at Piton de la …

We present a study of the seismicity which preceded the 1998 March 9 eruption of the Piton
de la Fournaise volcano. The eruption was preceded by a seismic crisis unusually long for …

The aim of this work is to propose a general model of Piton de la Fournaise volcano using
information from geological and geophysical studies. Firstly, we make a graphical …

An eruption on the eastern flank of Piton de la Fournaise volcano started on 16 November,
2002 after 10 months of quiescence. After a relatively constant level of activity during the first …