The process of 'earth plates moving' is Alfred Wageners theory of continental drift. This theory proposes that convenction currents in the earths mantle provides a 'cushion' on which the plates can move.
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The movement of Earth's tectonic plates is caused by the motion of convection currents in the mantle. These currents are driven by the heat generated from the decay of radioactive isotopes and by the heat leftover from the formation of the Earth. As the mantle material moves, it drags the overlying tectonic plates along with it, causing them to spread apart, collide, or slide past each other.
Most geologists believe that the movement of the Earth's plates is caused by the process of convection currents in the mantle. These currents are driven by the heat generated from the core of the Earth, which causes the molten rock in the mantle to move in circular patterns, leading to the movement of the tectonic plates.
Continental plates move due to the process of plate tectonics, where the plates float on the semi-fluid asthenosphere layer beneath them. This movement is driven by convection currents in the mantle, caused by heat from the Earth's core. When these currents push or pull on the plates, they cause them to move, leading to phenomena like earthquakes, volcanic activity, and the formation of mountains.
The process is called plate tectonics. It involves the movement of Earth's lithosphere in separate pieces called tectonic plates, driven by forces such as mantle convection. These plates interact at plate boundaries, leading to various geological phenomena like earthquakes and mountain formation.
As Earth's plates move away from each other at divergent boundaries, new crust is created as magma rises to the surface and solidifies. This process can result in the formation of features such as mid-ocean ridges and rift valleys.
The lithospheric plates move around on the asthenosphere, which is a partially molten layer of the Earth's upper mantle. This semi-fluid layer allows the plates to slide and interact with each other.