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Cratering rates serve as a useful estimate of surface age. Surface features can be reworked primarily through water erosion, but also by wind erosion and faulting (earthquakes), volcanoes, and crustal movement.

Mars and Jupiter being closer to the asteroid belt, the rate of cratering may be slightly higher there. Our moon's surface appears to be quite old, judging by the number of impact craters it has. Earth would have even more, being a bigger target, but earth impacts have been largely eroded and subducted over the course of hundreds of millions of years.

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