Linked from

The 11 pages that link to Core–mantle boundary, each with the reason it gives.

• Mantle convectionRelated: The hot lower boundary from which thermal buoyancy in the mantle arises.

• Earth's mantleRelated: Heat and material exchange across this boundary can influence deep mantle dynamics.

• Earth's coreBroader topic: Heat crossing this interface helps drive convection in the outer core.

• Beno GutenbergBroader topic: Gutenberg’s 1914 analysis placed this boundary at roughly 2,900 kilometers depth.

• GeodynamoRelated: Heat flow and magnetic coupling across this boundary influence the geodynamo’s operating conditions.

• Earth's outer coreBroader topic: Heat and chemical exchange across this boundary shape outer-core convection.

• Planetary coreBroader topic: Heat and chemical exchange across this boundary influence both core convection and mantle evolution.

• Internal structure of EarthRelated: Heat and material exchange across this interface influence both deep layers.

• Lower mantleRelated: It defines the lower mantle’s deepest boundary.

• Earth's internal heat budgetBroader topic: Heat crossing this boundary links core cooling to heat flow through the mantle.

• Iron planetRelated: Iron planets have a large core relative to this boundary's mantle side.