Geophysics
Conduction is the process by which heat is transferred through a material without the movement of the material itself. This transfer occurs at the atomic level, where faster-moving particles collide with slower-moving ones, passing on energy. In the context of Earth's heat budget, conduction plays a critical role in how heat moves from the interior of the Earth to its surface and affects geothermal gradients, which measure how temperature changes with depth.
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