When convection currents sink near the mantle, they create drag on the lithospheric plates above. This drag causes the plates to move in the direction of the sinking current. As the plates move, they can interact with other plates, leading to processes like subduction or mountain formation.
Convection is the transfer of heat through the movement of a fluid, such as a liquid or gas. In the Earth's mantle, hot magma rises near the core, is cooled near the surface, and then sinks back down. This continuous cycle of rising and sinking creates convection currents that drag tectonic plates along with them, causing the plates to move.
Convection cells in the mantle drive plate tectonics by creating currents that cause plates to move. As hot mantle material rises at mid-ocean ridges, it pushes plates apart. When the material cools and sinks back down at subduction zones, it pulls plates along with it. This continuous cycle of rising and sinking material creates convection currents that move the plates over geologic time scales.
No, convection currents in the upper mantle cause tectonic plates to move.
convection currents!
there is convection in the mantle. it causes the plates to move.
The upper mantle contains convection currents that move the tectonic plates.
They move apart.
because of convection currents in the mantle
They are the means by which plates of the lithoshpere move.
They are the means by which plates of the lithoshpere move.
convection currents