Planetary Science
A complex crater is a type of impact structure characterized by a central peak or peak ring, formed by the rebound of the Earth's crust after the impact of a large asteroid or comet. These craters typically have a larger diameter and more intricate structure compared to simple craters, featuring terraced walls and a flat floor. The formation of complex craters is influenced by the size of the impacting body, the velocity of the impact, and the geological characteristics of the target surface.
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