It happens when heat is transferred from the core to the crust.
Mantle Convection
The transfer of heat through a fluid of motion
Convection
It is a type of model where the lithosphere sinks to a great depth, which stirs the mantle. This model is what most researchers prefer.
Whole-mantle convection model or plume model
This model suggests that the mantle has two zones of convection. Specifically, the upper mantle's thin layer and the thicker mantle below the upper part.
layercakemodel
Rising mantle material at mid-ocean ridges creates the potential for plate to move away from the ridge with a force
ridgepush
As a slab sink, it pulls on the rest of the plate with a force