Cooler, older, oceanic lithosphere sink into the mantle at
A) sites of long-lived, hot spot volcanism in the ocean basins
B) rift zones along mid-ocean ridges
C) subduction zones along convergent plate boundaries
D) transform fault zones along divergent plate boundaries
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Cooler, older, oceanic lithosphere sinks into the mantle at subduction zones along convergent plate boundaries.
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Hello mate
here's your answer
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Option C✔✔
Subduction zones along convergent plate boundaries.
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here's your answer
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Option C✔✔
Subduction zones along convergent plate boundaries.
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Hope it helps you
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