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Dynamic Crustal Uplift Due to Plume Activity

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Mantle Plumes and Their Effects

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Abstract

Plume ascent is driven by buoyancy due to density difference from the surrounding material.

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Choudhuri, M., NemĨok, M. (2017). Dynamic Crustal Uplift Due to Plume Activity. In: Mantle Plumes and Their Effects. SpringerBriefs in Earth System Sciences. Springer, Cham. https://doi.org/10.1007/978-3-319-44239-6_3

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