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Which process influences the final slope stability of basaltic lava flows post-eruption?

A)Differential cooling induced thermal contraction.
B)Progressive sedimentation over flow surfaces.
C)Localized aeolian deposit accumulation rates.
D)Vegetative root wedging weakening integrity.

💡 Explanation

Differential cooling causes thermal contraction, initiating fracturing and potential slope failure because diverse cooling rates affect internal stresses. Therefore, answer A is correct rather than options B, C, and D, which involve external processes.

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