Convection Currents - GCSE Geography Definition

Reviewed by: Bridgette Barrett

Last updated

Convection currents are the circular movements of fluid, such as air or liquid, caused by the heating and cooling process, which results in the transfer of heat energy. In the context of plate tectonics when the mantle beneath the Earth's crust is heated by the core, it becomes less dense and rises, creating upward currents. As it moves away from the heat source, it cools down, becomes denser, and sinks back towards the core, creating a continuous loop. Tectonic theory once stated the movement of the plates was the result of convection currents in the mantle. The current theory is called slab pull theory which suggests that the movement is the result of the weight of the denser oceanic plates subducting and dragging the rest of the plate along


Examiner-written GCSE Geography revision resources that improve your grades 2x

  • Written by expert teachers and examiners
  • Aligned to exam specifications
  • Everything you need to know, and nothing you don’t
GCSE Geography revision resources

Share this article

Bridgette Barrett

Reviewer: Bridgette Barrett

Expertise: Geography Lead

After graduating with a degree in Geography, Bridgette completed a PGCE over 25 years ago. She later gained an MA Learning, Technology and Education from the University of Nottingham focussing on online learning. At a time when the study of geography has never been more important, Bridgette is passionate about creating content which supports students in achieving their potential in geography and builds their confidence.

The examiner written revision resources that improve your grades 2x.

Join now