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The age of a planet can often be inferred from the characteristics of its surface, such as the density and number of impact craters. A heavily cratered surface suggests greater age, as it indicates a longer exposure to impacts, while a smoother surface with fewer craters may indicate more recent geological activity or resurfacing. Additionally, the presence of certain geological features, like volcanoes or tectonic formations, can imply a younger age if they are still active or have recently formed. Radiometric dating of surface materials can also provide precise age estimates.

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1d ago

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