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 · 266 words

Deep source
Seismic tomography, such as French and Romanowicz's 2015 imaging, shows broad plume conduits rooted near the core-mantle boundary.
Head and tail
The head melts by decompression under the lithosphere, while the tail feeds a stationary hotspot for millions of years.
Flood basalts
Plume heads produce large igneous provinces, such as the Deccan Traps from the Reunion plume about 66 million years ago.
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.
Initiator of rifting
Plume heads crack continents, as the Afar plume opened the Red Sea, Gulf of Aden and East African Rift.
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.
Explains the exceptions
Plumes explain volcanism far from boundaries, as at Hawaii and Yellowstone.
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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.