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Cette carte conceptuelle, cree avec IHMC CmapTools, contient des informations liees a : Recent Volcanism on Mars, Reduced Cooling produce Broaded Sheet Flows, Thin Martian Atmosphere leads to Reduced Cooling, Lava Flow Characteristics includes Flow Velocity, Terrestrial Continental Flood Lavas are characterized by Tumuli, Young Lava Flows localized in Tharsis Buldge, Remarkably Young Age is suggested by Paucity of Impact Craters, Inflated Lava Flows produce Broaded Sheet Flows, Martian Gravity leads to Raised Crust, Flood "Breakouts" suggest Lava Flows like Terrestrial Basalts, Terrestrial Continental Flood Lavas recognized as Continental Flood Lavas, Theoretical Models are based on Qualitative Evidence, Continental Flood Lavas show differences because of Thin Martian Atmosphere, Insulated Sheets suggest Lava Flows like Terrestrial Basalts, Slower Crust Growth produce Broaded Sheet Flows, Lava Flow Characteristics includes Viscosity, Theoretical Models are based on Quantitative Evidence, Recent Volcanism on Mars show analogies with Terrestrial Continental Flood Lavas, Broaded Sheet Flows generated by Flood "Breakouts", Martian Gravity leads to Inflated Lava Flows, Plate-Rafted Morphologies identified by Ridges