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the claim

Central peaks in lunar craters are formed by crustal rebound after impact

the verdict

SUPPORTED

the evidence backs this

confidence 87/100

Central peaks in complex lunar craters expose deep-seated mantle and crustal materials, supporting the model that these elevated structures are formed by the rebound of the lunar crust following a large impact event.

Evidence for · 2

Copernicus Crater Central Peak: Lunar Mountain of Unique Composition

1982 · cited by 94

Identifies deep-seated olivine and unique mafic mineral assemblages exposed at the central peak of Copernicus crater, supporting the mechanism of deep crustal material uplift.

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More for · 1

Volcanic processes within the Petavius crater, nearside of the Moon.

2025 · cited by 1

Confirms that central peaks in craters like Petavius expose deep crustal and mantle-derived mineral compositions consistent with uplift during impact crater formation.

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first checked02 Aug 2026

judged → SUPPORTED · 8702 Aug 2026

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