what is the source of heat in mantle convection current
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The primary sources of thermal energy for mantle convection are three: (1) internal heating due to the decay of the radioactive isotopes of uranium, thorium, and potassium; (2) the long-term secular cooling of the earth; and (3) heat from the core.
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The source of heat in mantle convection current is mentioned as follows:
- Internal heating caused by the decay of radioactive uranium isotopes is the principal source of thermal energy for mantle circulation.
- It can also be caused by the heat of the inner core.
- The heat energy from the core is transferred to the mantle, forcing it to rise towards the cooler Earth's surface.
- The heated mantle distributes its heat energy to the lithosphere.
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