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Evidence for periodic resurfacing on Venus includes the planet's relatively young surface age, estimated to be around 300 to 500 million years, which is inferred from crater counting. Additionally, radar mapping from missions like Magellan shows a lack of impact craters in certain regions, suggesting recent volcanic activity. The presence of large volcanic features and extensive lava flows supports the idea that Venus experiences resurfacing events, possibly caused by tectonic and volcanic processes.

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