Factors influencing the eruption of water-based magmas through Europa's ice crust

Physics

Scientific paper

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Icy Satellites, Europa, Satellite Surfaces, Planetary Crusts, Magma, Ground Water, Silicates, Volcanoes, Density Measurement, Ejecta

Scientific paper

We explore the factors which control the melting of ice by silicate magmas at the base of the ice crust of Europa and the ability of the resulting fluids, which may contain some proportion of fragmented silicate material, to reach the surface through dikes. We find that fluids carrying significant proportions of silicate clasts can only reach the surface if the ice layer is less than about 15 km. Fluid discharge rates up to 2 x 10 exp 4 cu m/s from fissure vents up to about 15 km long are likely.

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