2025 · GS Paper 1 · Q16 · 15 marks

Discuss how the changes in shape and sizes of continents and ocean basins of the planet take place due to tectonic movements of the crustal masses.

In short

Tectonic movements reshape continents and ocean basins by creating crust at divergent ridges, consuming it at convergent trenches, crumpling it into mountains in collisions and shifting it along transform faults. The Atlantic widened after Pangaea broke up, while the Tethys closed as India collided with Eurasia.

Model answer

Ghissu Editorial · Verified 4 Oct 2026

Introduction
The Atlantic widens by a few centimetres a year while the Himalaya keeps rising as India presses into Asia. Plate tectonics, built on Wegener's drift and Hess's sea-floor spreading, explains how moving lithospheric plates keep reshaping continents and ocean basins.
Forces that Move the Crustal Plates
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Mantle convection

Arthur Holmes proposed that convection currents driven by radioactive heat drag the overlying plates.

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Ridge push and slab pull

New crust slides off mid-ocean ridges, and dense slabs sinking at trenches pull plates behind them.

How Plate Boundaries Reshape Continents and Oceans
Sea Floor Spreading (Mid-Oceanic Ridge to Trench Cross-Section)
Sea-floor spreading at the ridge and subduction at the trench
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Divergent boundaries widen oceans

Rifting opened the Atlantic after Pangaea broke up, and the Red Sea and East African Rift are forming the next ocean.

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Convergent boundaries shrink oceans

Subduction at trenches like the Mariana Trench shrinks the Pacific, and the Tethys vanished when India met Eurasia.

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Collision grows continents

Colliding crust thickens into the Himalaya and the Alps, while island arcs such as Japan add land.

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Transform boundaries shift shape

Along the San Andreas Fault, plates slide past each other and redraw coastlines.

Way Forward
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Hazard zoning

With about 59% of India's land prone to moderate or severe earthquakes (NDMA), IS 1893 seismic zoning must be enforced in building approvals.

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Monitoring

The INCOIS tsunami warning centre (2007) and the Deep Ocean Mission (2021) should expand seismic and seabed monitoring.

Conclusion
Ridges create crust, trenches consume it and collisions crumple it into mountains, so continents and ocean basins are always in motion. Understanding this helps India live safely on an active plate margin.

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

Hand-drawn diagram: Sea-floor Spreading and Subduction. Sea-floor Spreading and Subduction. Flow: Convection rises under ridge → New crust forms at ridge → Ocean floor spreads apart → Cold slab sinks at trench → Crust consumed in mantle → (back to start)
Diagram: Sea-floor Spreading and Subduction
Hand-drawn diagram: Boundaries that reshape the map. Boundaries that reshape the map. Diagram (tree): Boundaries that reshape the map; Plate boundaries; Divergent: Atlantic, Red Sea widen; Convergent: Pacific shrinks, Himalaya rises; Transform: San Andreas shifts coast
Diagram: Boundaries that reshape the map

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Question from the official UPSC Civil Services (Main) Examination 2025 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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