The heat that drives mantle convection comes from the colling of Earth's interior and the decay of radioactive isotopes
The heat comes from the outer core, which provides the heat.
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.
Radioactive decay, specifically the decay of elements like uranium, thorium, and potassium, occurs in the mantle. This decay releases heat energy, which drives convection currents in the mantle. This movement of material helps transfer heat from the Earth's interior to the surface.
The heat inside Earth primarily comes from two sources: residual heat from its formation, and the decay of radioactive elements in the mantle and core. This heat drives the movement of material in the Earth's interior, creating processes like mantle convection and the generation of Earth's magnetic field.
The ultimate source of heat that drives plate tectonics is believed to be the Earth's internal heat from radioactive decay in the mantle. This heat causes convection currents in the mantle, which in turn drive the movement of the tectonic plates.
The heat comes from the outer core, which provides the heat.
The heat that drives convection currents in the mantle primarily comes from the radioactive decay of elements such as uranium, thorium, and potassium. This heat causes the mantle material to become less dense, rise towards the surface, cool down, then sink back towards the core in a continuous cycle of convection.
uneven temperatures
Thermal convection that drives plate motion is caused by the movement of heat within the Earth's mantle. As the Earth's interior heat is transferred towards the surface, it generates convective currents in the mantle, leading to the movement of tectonic plates. This process is known as mantle convection and is a key driver of plate tectonics.
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.
Radioactive decay, specifically the decay of elements like uranium, thorium, and potassium, occurs in the mantle. This decay releases heat energy, which drives convection currents in the mantle. This movement of material helps transfer heat from the Earth's interior to the surface.
The energy that drives Earth's rock cycle comes from the Earth's internal heat, which originates from the decay of radioactive isotopes in the Earth's core and mantle. This heat causes convection currents in the mantle, leading to plate tectonics, volcanic activity, and the movement of rocks through the rock cycle.
The heat inside Earth primarily comes from two sources: residual heat from its formation, and the decay of radioactive elements in the mantle and core. This heat drives the movement of material in the Earth's interior, creating processes like mantle convection and the generation of Earth's magnetic field.
The thermal convection that drives plate motion is caused by the movement of molten rock in the mantle. Heat from Earth's core causes the mantle to circulate in a convection current, which in turn drags the overlying tectonic plates along with it, driving plate motion.
The energy that drives Earth's rock cycle primarily comes from Earth's interior, specifically from the heat generated by radioactive decay in the mantle and core. This heat drives processes like convection currents in the mantle, which in turn contribute to the movement of tectonic plates and the formation of new rocks through processes like melting and solidification.
Convection occurs in the mantle layer of the Earth. This process involves the movement of molten rock and heat within the mantle, which drives plate tectonics and other geologic phenomena.
The heat source that drives convection currents inside the Earth is primarily from the decay of radioactive elements within the Earth's core. This heat causes the material in the mantle to become less dense and rise, creating convection currents that drive the movement of tectonic plates.