Cryovolcanic emplacement of domes on Europa
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We model the emplacement of putative cryovolcanic domes on Europa. Erupted lava will be warm enough to relax and advance to form domes in Europa's frigid environment. Cryovolcanic domes may form from low viscosity H2O or briny solutions that undergo rapid cooling. Cryovolcanic domes may have rheologies that are consistent with terrestrial basalt.
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