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  • Während das Oberflächenmaterial unseres Heimatplaneten aus der chemischen Verwitterung der darunter liegenden Gesteinsschichten oder der eiszeitlichen Geröllmassen entstanden ist, bedeckt den Mars eine dicke Schicht aus feinkörnigem Staub. (de)
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  • spektrum.de: Planetologie: Die unirdischen Landschaften des Mars. 1. Juli 2003, abgerufen am 1. Juni 2024. (de)
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