Piton de La Fournaise is in a period of intense volcanic activity since 1998. To constrain the
magma dynamics responsible for this activity, we combined GPS ground deformation …

Piton de La Fournaise (Réunion Island) had shown 8 months of high activity during 2003,
including four eruptions and one intrusion. The monitoring networks, provided by the …

After 15months of summit deflation, the unrest of Piton de La Fournaise renewed in August
2008 with several seismic crises and the re-pressurization of the plumbing system. The …

Since the middle of the 20th century, improvement in volcano monitoring techniques has
provided large data sets that can be used to evaluate the evolution of magma plumbing …

The relationship between shallow magma storage and flank injections in volcanic edifices is
rarely documented. We analyse the time series of geodetic and seismic data collected at …

During pre-eruptive periods and eruptions, Piton de la Fournaise volcano shows an
asymmetric magma-induced pattern of deformation. The origin of this asymmetry is not well …

Basaltic magma chambers are often characterized by emptying and refilling cycles that
influence their evolution in space and time, and the associated eruptive activity. During April …

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 …

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 …