Short description
This project aims at developing a physics-based tool to forecast scenarios for the location and time of a fissure eruption following magma propagation below the surface. Often magma avoids the central conduit and propagates through tortuous pathways, eventually opening a new fissure on the volcano flank or within a caldera. Similar old eruptive fissures are found in many areas now densely populated. The related hazard has so-far been estimated purely based on the spatial distribution of (...)
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