Counting the amount of impact craters on a surface can help determine how old it is.
Asteroids' surfaces and the rocky, ice-covered moons of the outer gas giants are both cratered. The craters left behind by striking objects can provide details on a planet's surface's nature and composition, as well as its age.
Therefore, it may be said that a crater's age is generally determined by its size. From oldest to newest, the history of crater formation can be loosely divided into three periods: the production of big and tiny craters. Only tiny craters were created.
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