How and why the escape of interior heat becomes concentrated in particular regions to form convection cells remains unresolved.
Evidence support: Supported by the cited evidence one source
Evidence: Kious 1996 Primary authority
Geological process
Slow circulation of the solid mantle driven by internal heat, in which hot material rises and cooler, denser material sinks. The geometry of that circulation is far less well constrained than the fact of it.
4 of 4 claims on this page cite at least one registered source. Counts describe how each statement is known, not how likely it is to be true.
Each claim states how it is known and cites its evidence.
How and why the escape of interior heat becomes concentrated in particular regions to form convection cells remains unresolved.
Evidence support: Supported by the cited evidence one source
Evidence: Kious 1996 Primary authority
Convection carries Earth’s internal heat outward: hotter, less dense material rises, spreads and cools, and cooler, denser material sinks to be reheated. Convection cannot take place without a source of heat.
Evidence support: Supported by the cited evidence one source
Evidence: Kious 1996 Primary authority
The vertical orientation of the imaged conduits suggests very sluggish background circulation in the mantle below about 1,000 kilometres depth.
Evidence support: Supported by the cited evidence one source
Evidence: French 2015 Peer-reviewed
How many convection cells exist in the mantle, where and how they originate, and what structure they take are open questions.
Evidence support: Supported by the cited evidence one source
Evidence: Kious 1996 Primary authority
Record last updated 2026-09-06. Corrections follow the published corrections policy; superseded claims are retained, never silently edited.