The decay of radioactive isotopes.
The decay of radioactive isotopes.
The decay of radioactive isotopes.
The decay of radioactive isotopes.
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The main sources of heat in the Earth's interior are residual heat from the planet's formation, radioactive decay of elements like uranium, thorium, and potassium, and heat generated by ongoing processes like mantle convection and core formation. This heat leads to processes like plate tectonics, volcanic activity, and the Earth's magnetic field.
The primary source of heat in Earth's interior is residual heat left over from the planet's formation, along with heat generated by the decay of radioactive isotopes. This heat drives mantle convection and plate tectonics, resulting in geological processes such as volcanic activity and earthquakes.
The major heat source of Earth's crust is residual heat from the planet's formation and radioactive decay of elements like uranium, thorium, and potassium within the Earth's interior. This heat is responsible for driving processes like mantle convection, plate tectonics, and volcanic activity on the Earth's surface.
Geothermal energy is powered by the heat stored below the Earth's surface. This energy is harnessed using geothermal power plants to produce electricity and heat for various applications like heating buildings and spas. The natural heat from the Earth's interior is a renewable energy source that provides a constant and sustainable energy supply.
asthenosphere
geothermal