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impact theory

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impact theory [′im‚pakt ‚thē·ə·rē]
(astronomy)
A theory which holds that most features of the moon's surface were formed by the impact of meteorites. Also known as meteoric theory; meteoritic theory.


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That theory was greeted with great skepticism when first proposed in 1984, and the Younger Dryas impact theory is facing the same reception.
The impact theory gets even more support from additional findings from other scientists.
Another group, led by Francis Nimmo at the University of California at Santa Cruz, ran a different set of computer simulations that support the impact theory.
 
 
 
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