Steven Dutch, Natural and Applied Sciences, University
of Wisconsin - Green Bay
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Tycho is 53 miles (85 kilometers) in diameter. Like most medium-sized craters on the Moon, Tycho has a prominent central peak and terraces along the inner walls. These features formed as the compressed lunar crust rebounded after the impact. The compressed floor rebounded to throw up a central peak, and the overly steep crater walls collapsed along curving faults to form the terraces.
The surroundings of Tycho are ancient, heavily cratered crust more than 4 billion years old. This area is crater saturated, meaning every point on it has been cratered at least once. The craters here formed from the final impacts during the accretion of the moon.

(NASA
image)

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Created 17 December 2007, Last Update 13 February 2008
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