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Which risk increases along strike-slip faults connecting seafloor spreading centers?

A)Widespread, sustained mantle plume volcanism
B)Intense, shallow-focus earthquake occurrences
C)Large, rapid continental ice sheet formation
D)Accelerated, global seafloor mineral deposition

💡 Explanation

High stress accumulates in the transform fault zone because lateral motion resists friction via elastic deformation and brittle failure. Therefore, there is a greater risk of intense earthquake occurrences, rather than diffuse volcanism or ice formation, which involve different geological processes.

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