The convection currents will eventaully stop because there is no heat to keep them moving.
"Convention"? I think you mean "convection" currents, and they will die away quite rapidly as the fluid and its container cool.
The convection currents running through the asthenosphere are widely believed to be the source of movement of the tectonic plates.
The heat in the Earth's interior comes from two main sources: the radiogenic heat produced by the radioactive decay of isotopes in the mantle and crust and the primordial heat left over from the formation of the Earth.
Asthenosphere
Radioactive decay of long-lived isotopes in the Earth's deep interior is the source of heat which causes convection currents in the magma which causes tectonic plates to move.
"Convention"? I think you mean "convection" currents, and they will die away quite rapidly as the fluid and its container cool.
The difference in temperature and density is the cause of convection currents in the earths mantle. Convection currents are the flow that transfers heat within a fluid.
The difference in temperature and density is the cause of convection currents in the earths mantle. Convection currents are the flow that transfers heat within a fluid.
The convection currents running through the asthenosphere are widely believed to be the source of movement of the tectonic plates.
The convection currents running through the asthenosphere are widely believed to be the source of movement of the tectonic plates.
convection currents
The difference in temperature and density is the cause of convection currents in the earths mantle. Convection currents are the flow that transfers heat within a fluid.
Bad grammar.
Vertical convection in both the ocean and atmosphere is caused by uneven HEATing.The source of energy for convection in the ocean and atmosphere is heating from the sun.
Vertical convection in both the ocean and atmosphere is caused by uneven HEATing.The source of energy for convection in the ocean and atmosphere is heating from the sun.
yes. because the sun brings heat
The heat in the Earth's interior comes from two main sources: the radiogenic heat produced by the radioactive decay of isotopes in the mantle and crust and the primordial heat left over from the formation of the Earth.