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Abstract: Potential for porous and discrete-fracture hydrothermal circulation below the seafloor of Europa, given low gravity and modest internal heating (AGU25)

Potential for porous and discrete-fracture hydrothermal circulation below the seafloor of Europa, given low gravity and modest internal heating

Kristin Dickerson1, Andrew T Fisher2, Jeffrey Hyman3, John P Ortiz4, Phil H Stauffer3 and Donna K Blackman2, (1)University of California Santa Cruz, Earth and Planetary Sciences, Santa Cruz, CA, United States, (2)University of California Santa Cruz, Earth and Planetary Sciences, Santa Cruz, United States, (3)Los Alamos National Laboratory, Los Alamos, United States, (4)Los Alamos National Laboratory, Hanover, United States