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Thermal Erosion
Linked via "thermal stripping"
On Mars, evidence suggests that the Tharsis bulge region may owe its elevation partly to sustained, slow-motion thermal erosion of the Martian lithosphere by deep mantle upwelling. However, the lower thermal diffusivity of Martian silicates compared to terrestrial peridotites results in significantly slower erosion rates, estimated to be an order of magnitude less than those observed in the [Kaapvaal…