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Cette carte conceptuelle, cree avec IHMC CmapTools, contient des informations liees a : Ancient Groundwater, Origin of Crust Material that can be Igneous Material, State can be Solid, Ancient Groundwater had variable Distribution, State depended on Crust Thermal Characteristics, State can be Liquid, Ancient Groundwater defines both Underground Water Circulation, State depended on Crust Permeability, Ancient Groundwater was drained through Emergence of Flows at the Surface, Ancient Surface Water through Percolation of Water from Channels & Basins, Cold Upper Regolith lies above Hydrosphere, Crust Porosity varies with Origin of Crust Material, Particle Size of Crustal Rocks depends on Origin of Crust Material, Underground Water Circulation through Pore Space, Distribution depended on Crust Thermal Characteristics, Ancient Groundwater may have been recharged by Ancient Surface Water, Origin of Crust Material that can be Brecciated Impact Material, Crust Thermal Characteristics depends on Degree of Pore Saturation, Underground Water Circulation through Underground Conduits, Solid is stable in Cold Upper Regolith, Pore Space define Crust Porosity