Piton de la Fournaise

Magma interactions, crystal mush formation, timescales, and unrest during caldera collapse and lateral eruption at ocean island basaltic volcanoes (Piton de la Fournaise, La Reunion)

Petrological studies can inform of the processes and time scales of magma movement and ascent, and thus allow associating them with monitoring unrest signals, and thus better mitigate volcano hazar

Left hand side: Inversion results for n = 1, Q = 170, f = 10 Hz and b = 1 km s−1 .

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