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2018 GS Paper I

UPSC CSE (Main) 2018 · GS Paper I · Question 6

Define mantle plume and explain its role in plate tectonics.

UPSC Civil Services (Main) Examination 2018, General Studies Paper I (GS 1), Question 6 — 10 marks, 150 words.

Syllabus line: World physical geography — “Salient features of world’s physical geography.”

GS Paper I 2018 · Q6

10 marks · 150 words World physical geography X-Ray · Core #27

Define mantle plume and explain its role in plate tectonics.

Approach · directive: “define / explain”

What it asks · Define a mantle plume and show how it relates to hotspots, volcanism, continental break-up and plate motion.

It asks 2 things — answer each

  1. Define: what a mantle plume is, where it rises from and how it makes a hotspot
  2. Explain its role in plate tectonics: recording plate motion, rifting and break-up, flood basalts, ridge and intraplate volcanism, driving force and the debate

Open with · A mantle plume is a narrow column of hot, buoyant rock rising from the deep mantle; where it meets the plate it creates a hotspot, linking deep-Earth heat to plate behaviour.

Cover

  • Definition: hot, buoyant rock rising from deep in the mantle, possibly near the core–mantle boundary; its head spreads and melts under the lithosphere.
  • Fixed source: plumes stay roughly stationary while plates drift over them, the hotspot idea J. Tuzo Wilson proposed in 1963.
  • Plate motion: the Hawaiian Islands–Emperor Seamounts chain ages away from the active vent, tracing the Pacific Plate's path.
  • Break-up: plumes dome and weaken the lithosphere, opening rifts that can split continents.
  • Flood basalts: plume heads pour out vast lava, as in the Deccan Traps linked to the Réunion plume.
  • Ridge and intraplate volcanism: Iceland on a ridge, Yellowstone far from plate edges; plume push is minor beside slab pull, and the model is still debated.

Close with · Plate boundaries explain most volcanism and rifting; plumes explain the exceptions, from mid-plate volcanic chains to flood basalts and new oceans.

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  • J. Tuzo Wilson proposed the hotspot theory in 1963 to explain the Hawaiian Islands–Emperor Seamounts chain as the Pacific Plate moving over a fixed heat source.Hotspots: Mantle thermal plumes — USGS, This Dynamic Earth ↗“In 1963, J. Tuzo Wilson, the Canadian geophysicist who discovered transform faults, came up with an ingenious idea that became known as the "hotspot" theory.”
  • Some hotspots lie near diverging plate boundaries such as beneath Iceland; others lie under continental crust, as at Yellowstone.Hotspots: Mantle thermal plumes — USGS, This Dynamic Earth ↗“Some are concentrated near the mid-oceanic ridge system, such as beneath Iceland, the Azores, and the Galapagos Islands.”

Question: UPSC's CS (Main) 2018, GS Paper I — paper ↗. Approach: Minimalist IAS, checked 16 Oct 2026 (how we verify) — UPSC publishes no model answers. ·

Model answer· 223words · Minimalist IAS

A mantle plume is a narrow column of unusually hot, buoyant rock rising from deep in the mantle, possibly near the core–mantle boundary. Where it meets the plate above, it creates a hotspot, linking deep-Earth heat to plate behaviour.

What a mantle plume is

  • Mechanism: the plume head spreads beneath the lithosphere and partly melts, feeding volcanoes above.
  • Fixed source: plumes stay roughly stationary while plates drift over them, the hotspot idea J. Tuzo Wilson proposed in 1963.
Plume riseshead spreads and meltshotspot volcanoplate moves onvolcanic chain
  1. Plume rises
  2. head spreads and melts
  3. hotspot volcano
  4. plate moves on
  5. volcanic chain

Role in plate tectonics

  • Recording plate motion: the Hawaiian–Emperor chain ages away from the active vent, tracing the Pacific Plate's path.
  • Continental break-up: a plume domes and weakens the lithosphere, opening rifts that can split continents.
  • Flood basalts: plume heads pour out vast lava; the Deccan Traps of the Maharashtra plateau are linked to the Réunion plume.
  • Ridge and intraplate volcanism: plumes explain extra volcanism on ridges (Iceland) and volcanoes far from plate edges (Yellowstone).
  • Driving force: plume push is minor beside slab pull and ridge push, but plumes can shift plate boundaries.
  • Debate: some hotspots may have shallow, non-plume origins, so the model remains under study.

Plate boundaries explain most of the Earth's restlessness; plumes explain the exceptions: mid-plate volcanic chains, flood basalts like the Deccan, and rifts that open oceans.

Prepared by Minimalist IAS to the answer standard of Shivam Singh (mentor, 7 years) · facts checked against official sources (how we verify) · updated 16 Oct 2026. UPSC publishes no model answers: compare your structure and coverage with this, then write your own.

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