2018 · GS Paper 1 · Q6 · 10 marks

Define mantle plume and explain its role in plate tectonics.

In short

A mantle plume is a hot, buoyant column rising from the deep mantle that forms hotspots, records plate motion, splits continents and builds flood basalts. The Reunion plume formed the Deccan Traps about 66 million years ago and is argued to have sped India's northward drift.

Model answer

Ghissu Editorial · Verified 4 Oct 2026

Introduction
A mantle plume is a column of abnormally hot, buoyant rock rising from deep in the mantle, possibly the core-mantle boundary, with a broad head and narrow tail; at the surface it forms a hotspot. Wilson (1963) and Morgan (1971) built the idea into plate tectonics.
How a Mantle Plume Works
Hot Spot and Mantle Plume Formation
Hot Spot and Mantle Plume Formation
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Deep source

Seismic tomography, such as French and Romanowicz's 2015 imaging, shows broad plume conduits rooted near the core-mantle boundary.

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Head and tail

The head melts by decompression under the lithosphere, while the tail feeds a stationary hotspot for millions of years.

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Flood basalts

Plume heads produce large igneous provinces, such as the Deccan Traps from the Reunion plume about 66 million years ago.

Role of Mantle Plumes in Plate Tectonics
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Recorder of plate motion

A plate sliding over a fixed plume leaves an age-progressive chain, as in the Hawaiian-Emperor chain, whose bend records a change in Pacific plate motion.

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Initiator of rifting

Plume heads crack continents, as the Afar plume opened the Red Sea, Gulf of Aden and East African Rift.

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Driver of plate speed

Cande and Stegman (2011) argued the Reunion plume pushed India to its fastest northward drift, leaving the Lakshadweep-Chagos ridge as its track.

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Explains the exceptions

Plumes explain volcanism far from boundaries, as at Hawaii and Yellowstone.

Conclusion
Mantle plumes add a deep, vertical engine to plate tectonics, though their depth of origin is still debated. For India they explain the Deccan Traps and, arguably, the fast drift that preceded the Himalayan collision.

This model answer is indicative and the model can make mistakes; please verify key facts independently.

Hand-drawn diagram: Rise of a Mantle Plume. Rise of a Mantle Plume. Flow: Heat at core-mantle boundary → Hot buoyant column rises → Head flattens under lithosphere → Decompression melting, flood basalts → Plate drifts, hotspot track
Diagram: Rise of a Mantle Plume

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Question from the official UPSC Civil Services (Main) Examination 2018 paper. Answer written by Ghissu's engine and checked against our editorial standards. Found an error? Tell us and we correct it within 48 hours.

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