Cooler older oceanic lithosphere sinks

Cooler older oceanic lithosphere sinks

A) subduction zones along convergent plate boundaries

B) sites of long-lived, hot spot volcanism in the ocean basins

C) transform fault zones along divergent plate boundaries

D) rift zones along mid-ocean ridges

Correct Answer :

Option (A) – subduction zones along convergent plate boundaries

 

Cooler older oceanic lithosphere sinks

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