Earth and Environment Atlas

How The Planet Works
Concepts

Mantle Plume

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A proposed mechanism of convection within Earth's mantle, hypothesized to explain anomalous volcanism: super-heated material forming at the core-mantle boundary and rising through the mantle. Plumes are invoked as the cause of volcanic hotspots such as Hawaii and Iceland and of large igneous provinces such as the Deccan and Siberian Traps, though the hypothesis remains contested against plate-based explanations, and some of the volcanic regions it would explain lie far from any tectonic plate boundary.

Facts
Origin Year
1963 1
Mantle plumes were first proposed by J. Tuzo Wilson in 1963 and further developed by W. Jason Morgan in 1971 and 1972.
Cross-Tradition Connections

Associated With

A plume is posited to nucleate at the core-mantle boundary and rise through the mantle.

Volcanism, Processes

Hypothesized to explain anomalous volcanism such as hotspots and large igneous provinces.

In Discipline

Proposed By

Mantle plumes were first proposed by J. Tuzo Wilson in 1963.

Further developed by W. Jason Morgan in 1971 and 1972.

Sources
1. Mantle Plume (Wikipedia)
Wikimedia FoundationLead section; Concepts section
Quote, Lead section; Concepts section
Mantle plumes were first proposed by J. Tuzo Wilson in 1963 and further developed by W. Jason Morgan in 1971 and 1972.
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Open Questions (2 open questions)
Do deep mantle plumes feed volcanic hotspots such as Hawaii, or do shallower plate processes explain them?

Since its introduction the plume hypothesis has been repeatedly adapted to fit observed hotspots rather than making firm predictions, and critics have developed a rival plate hypothesis; with the growing number of models the plume concept has been criticized as a weakly defined hypothesis that as a general term is currently neither provable nor refutable. Seismic tomography has produced evidence read as favoring a plume beneath Hawaii and, since 2011, beneath Yellowstone, but the general question stays contested.

What would resolve this Seismic imaging of plume conduits from the core-mantle boundary to the surface at multiple hotspots, with resolution good enough that plume and plate explanations make distinguishably different predictions.
Geophysics, SeismologyMantle Plume (Wikipedia)
Do Deep Mantle Plumes Explain Hotspot Volcanism, or Is the Plate Hypothesis Right?

Whether anomalous volcanic hotspots such as Hawaii and Yellowstone are fed by narrow plumes rising from the core-mantle boundary, or are instead explained by shallow, plate-tectonic-driven processes, is contested as the Great Plume Debate; critics led by Don Anderson, Gillian Foulger and Warren Hamilton argue the plume hypothesis has not reliably predicted new hotspots since its 1971 introduction, while the rival plate hypothesis attributes the same volcanism to near-surface plate processes rather than a deep-mantle source.

What would resolve this Direct seismic tomographic imaging that resolves a continuous, narrow, deep-sourced conduit beneath a disputed hotspot, or a plume-model prediction of a previously unknown hotspot later confirmed by observation, would settle the debate in the plume hypothesis's favor; a demonstrated shallow, plate-driven mechanism sufficient to explain the same hotspots without invoking a deep source would settle it the other way.
GeophysicsMantle Plume (Wikipedia)
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