Page "Geography of Mars" Paragraph 27
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The giant impact hypothesis, originally proposed in the early 1980s, was met with skepticism due to the impact area's non-radial ( elliptical ) shape, where a circular pattern would be stronger support for impact by larger object ( s ).
Using geologic data, researchers found support for the single impact of a large object hitting Mars at approximately a 45-degree angle.
Additional evidence analyzing Martian rock chemistry for post-impact upwelling of mantle material would further support the giant impact theory.
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