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The newest geological interval, the Amazonian, is marked by a thinner environment and speedy water evaporation. Late-stage volcanism, together with Olympus Mons eruptions, together with Aeolian erosion, formed Mars’ panorama, revealing indicators of glaciation and ice-related processes. That is when the purple hue of Mars began appearing on account of floor adjustments from anhydrous ferric oxides. Mars life seemingly grew to become extinct by this level.
