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The 44 pages that link to Mantle convection, each with the reason it gives.

• Plate tectonicsRelated: The traditional engine proposed for plate motion, now paired with slab pull and ridge push.

• Seafloor spreadingRelated: One proposed driving force behind ridge push and the motion of plates.

• PangaeaRelated: The engine that gathered the continents and later pulled them apart.

• Mantle plumeRelated: Plumes and plates are the two proposed modes of mantle convection; how they coexist is unsettled.

• Continental driftRelated: Holmes's 1920s proposal supplied the mechanism Wegener lacked.

• Eurasian PlateRelated: Mantle dynamics contribute to the forces that move tectonic plates.

• Planetary differentiationRelated: Differentiated layers exchange heat and shape the mantle’s long-term circulation.

• EarthRelated: It helps power the motion of tectonic plates above the mantle.

• Earth's mantleRelated: Convection transports heat through the mantle and contributes to plate motion.

• GeologyRelated: Its patterns and links to plate motion remain difficult to observe directly.

• Tectonic plateRelated: Its thermal circulation contributes to forces that move plates.

• Hotspot (geology)Related: Convection transports heat and may shape the mantle flow feeding hotspot volcanism.

• AsthenosphereRelated: The convecting asthenosphere carries the plates riding on top of it.

• Harry HessRelated: Hess invoked mantle circulation as a possible driver of ocean-floor movement.

• Arthur HolmesRelated: Holmes proposed this circulation as the force capable of moving continents.

• Lord RayleighRelated: Rayleigh-number scaling helps characterize whether mantle heat transfer is conductive or convective.

• Earth's crustRelated: Its circulation contributes to the forces that move plates and reshape crust.

• GeoneutrinoRelated: Radiogenic heat estimates help constrain the thermal energy available to drive mantle motion.

• Mantle viscosityRelated: Viscous creep lets hot mantle rise and cooler mantle sink over millions of years.

• Radiogenic heatRelated: Radiogenic heating contributes to the temperature differences that drive mantle motion.

• Harold JeffreysRelated: Convection became Holmes’s proposed engine for continental motion, but Jeffreys disputed its ability to drive drift.

• Mineral physicsRelated: Mineral viscosity and phase changes influence the pattern and speed of mantle flow.

• Upper mantleRelated: Convection transports heat through the upper mantle and helps drive plate motion.

• Internal structure of EarthRelated: It transfers heat through the mantle and contributes to surface tectonic activity.

• Rheology of the mantleRelated: Convection models solve the mantle flow laws to predict plate speeds and patterns.

• EoarcheanRelated: It supplied heat and helped drive early crust formation and recycling.

• Seafloor spreading hypothesisRelated: Hess explicitly tied spreading to convection cells rising under ridges and descending at trenches.

• Geological history of EarthRelated: Its flow helps drive plate motion and long-term surface change.

• Lower mantleRelated: Convection carries heat and may transport material across the lower mantle.

• Tectonics of VenusRelated: On Venus, convection loads the crust vertically instead of dragging plate-sized rafts.

• Earth's internal heat budgetRelated: Convection transports internal heat toward the surface and helps power plate tectonics.

• GeodynamicsRelated: It transports internal heat and helps drive the movement of tectonic plates.

• Geology of VenusRelated: It can drive Venus’s volcanism, crustal deformation, and long-term heat loss.