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Question
- a hot, rising mantle plume is most likely to be found beneath which type of boundary?
continental - continental divergent boundaries
oceanic - oceanic divergent boundaries
oceanic - oceanic convergent boundaries
continental - continental convergent boundaries
Mantle plumes are hot upwellings from deep in the mantle. Continental-continental divergent boundaries (e.g., the East African Rift) involve thinning continental crust, allowing mantle plumes to rise and drive rifting. Divergent boundaries pull plates apart, creating a pathway for plumes, while convergent boundaries involve subduction (not plume rise). Oceanic divergent boundaries (mid-ocean ridges) are driven by asthenospheric flow, not deep plumes as commonly as continental divergent settings.
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continental-continental divergent boundaries