Yes, it is believed that the movements of Plate Tectonics is generated by the convection currents in the mantle. The continents are made up of rocks somewhat lighter than the dense dark-coloured volcanic rocks of the interior. They therefore float on the denser rocks.
The same convection currents, or the net effect of them, is believed to generate the electric currents that produce the Earth's magnetic field.
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 currents and heat transfer
convection currents
Mantle convection causes the tectonic plates of the Earth to move slowly. Mantle convection is when heat moves from the mantle to the surface and causes the mantle, and the tectonic plates to move very slowly.
Convection currents in the mantle are streams of fluid produced by the process of heat transfer from one place to another. The earth gets very hot as you go nearer to the core. The mantle is thus heated up as it is right next to the core. As a result, convection currents are formed.*Core: It is a spherical zone that lies at the center of the earth.*Mantle: It is the layer surrounding the outer core of the earth.
Its more ov a movement really not a process. Tectonic plates move due to convection currents in the mantle.
It's the change (decrease) in density with heating that produces the currents that we refer to as convection currents.
convection
convection
convection currents
convection currents
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 currents and heat transfer
Convection is the process that causes warm air to rise and cold air to sink. As such, the winds caused by this process are called convection currents.
convection
convection currents