The physics of hypervelocity impacts causes impact craters to be radially symmetric
The physics of hypervelocity and high-energy impacts generally produces centrally symmetric or quasicircular craters, provided the impact is perpendicular rather than oblique.
The retrieved literature supports the idea that impact cratering processes tend to be centrally or bilaterally symmetric under standard (perpendicular) conditions, creating circular or quasicircular depressions, whereas oblique impacts introduce asymmetry.
Campbell O, Blenkinsop T, Gilbert O, Mol L. Surface damage from perpendicular and oblique bullet impacts in stone.. 2022. https://doi.org/10.1098/rsos.220029
Paper 6 discusses how perpendicular impacts create symmetric craters, contrasting them with asymmetric oblique impacts.
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Hörz F, Basilevsky AT, Head JW, Cintala MJ. Erosion of lunar surface rocks by impact processes: A synthesis.. 2020. https://doi.org/10.1016/j.pss.2020.105105
Paper 9 notes that impact processes in rocks are centrally to bilaterally symmetric, producing quasicircular depressions.
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