Simulations conducted by researchers at ETH Zurich suggest a strong likelihood that Venuss rift valleys are still geologically active rather than being mere relics of a bygone era, as had been previously believed. This finding reshapes our understanding of Earths sister planet and will influence future missions to Venus.
Simulations conducted by researchers at ETH Zurich suggest a strong likelihood that Venuss rift valleys are still geologically active rather than being mere relics of a bygone era, as had been previously believed. This finding reshapes our understanding of Earths sister planet and will influence future missions to Venus.
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