Via currents of heated rock in the mantle which rise toward the surface. Very slowly.
Conduction augmented by convection-currents within the Mantle.
there are many reasons for heat in earths crust. like the friction between rock masses during movements of earths crust. there may also be heat left over from the original heat of earths interior. but the main reason for heat in earths crust is radioactive elements. they give off energy that can be absorbed as heat. some radioactive elements include uranium, thorium, and a form of potassium.
The heat transfer is moved to the crust. The earth's crust moves to the inner core
heat energy transferred by earths atmosphere by the sun
the inner core
Geothermal Energy
there are many reasons for heat in earths crust. like the friction between rock masses during movements of earths crust. there may also be heat left over from the original heat of earths interior. but the main reason for heat in earths crust is radioactive elements. they give off energy that can be absorbed as heat. some radioactive elements include uranium, thorium, and a form of potassium.
The heat transfer is moved to the crust. The earth's crust moves to the inner core
Beneath the surface of the earth temperature remains the same. Within the Earth, irregular convection cells within the mantle transfer heat from the core to the surface of the planet. Volcanoes and earthquakes are two examples of heat transferring from the interior to the surface.
Convection currents are agents of heat transfer within Earth's interior. And could also serve as mechnism for heat generation in the earth crust.
heat energy transferred by earths atmosphere by the sun
Geothermal Energy
the inner core
Earth's surface is free to radiate heat into space. The interior is not. The interior does transfer heat the the surface, but rather slowly. It is hot due to residual heat from Earth's formation and from the heat generated by the decay of radioactive elements.
it comes from earths interior heat
False.
False.
It's called the convection current.