Very hot and although still solid able to flow in convection currents.
Decay of radioactive elements in the mantle heats it.
Decay of radioactive elements in the mantle heats it.
Source of heat in mantle come from radioactive decay of the radioactive elements inside the earth..
The heat that drives mantle convection primarily comes from the decay of radioactive elements within the Earth's mantle and core. This process releases heat that generates thermal gradients, causing material to move within the mantle. The heat may also originate from the residual heat left over from the Earth's formation.
The heat in Earth's mantle comes from the decay of radioactive elements, primarily uranium, thorium, and potassium. This radioactive decay releases heat energy that warms the mantle, driving convective currents and contributing to the movement of tectonic plates.
No. It's radioactive decay within the planet.
Radioactive decay - mainly of potassium.
Geothermal, originated from radioactive decay in the core and lower mantle.
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 source of heat in the mantle primarily comes from the decay of radioactive elements like uranium, thorium, and potassium. This process releases energy in the form of heat which contributes to the high temperatures within the Earth's mantle.
internal heating due to the decay of the radioactive isotopes of uranium, thorium, and potassium
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.