Slab-pull and ridge-push acting together
It is involved in the Mantle because heat Is used for the temepeter and pressure is for how close the mantle is
Subduction is part of the geological process of plate tectonics. A subduction zone is a place where the oceanic plate is sinking back in to the mantle (usually at the edge of a continental plate.
Decompression melting of extremely hot mantle rock as it rises toward the surface.
The flow of mantle effects convection currents in the mantle. This process happens as hot material within the mantle begins to rise. As it rises, it begins to cool and then sinks. This process repeats as a cycle of convection currents.
CONVECTION
"subduction"
It is called subduction.
Convergent.
It is involved in the Mantle because heat Is used for the temepeter and pressure is for how close the mantle is
Subduction is part of the geological process of plate tectonics. A subduction zone is a place where the oceanic plate is sinking back in to the mantle (usually at the edge of a continental plate.
Decompression melting of extremely hot mantle rock as it rises toward the surface.
Sinking of oceanic lithosphere into the mantle at a subduction zone.
slab-pull and ridge-push
Because they "float" on the mantle and the mantle undergoes a process of convection.
The flow of mantle effects convection currents in the mantle. This process happens as hot material within the mantle begins to rise. As it rises, it begins to cool and then sinks. This process repeats as a cycle of convection currents.
Convection. It consists of heated magma rising, then cooling, sinking, and reheating constantly in the mantle.
usually from lava sinking to ocean floor and cooling.