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It's called the convection current.

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βˆ™ 15y ago
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βˆ™ 6mo ago

The main mechanism for heat transfer in Earth's mantle is through convection currents. These currents are driven by the heat generated by the decay of radioactive elements in the mantle, causing hot material to rise and cooler material to sink. This convective motion helps drive the motion of tectonic plates and is a key process in the Earth's heat budget.

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Q: Current in earths mantle that transfers heat in earths interior?
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Related questions

Is the heat source for the convection current in the mantle in the sun?

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.


Which structural layer of earths interior have scientists concluded is liquid?

the mantle


Which layer makes up the majority of earths interior?

The mantle is the largest layer in the Earth's interior.


What are oceans current are formed by what?

Moving plates in the earths mantle.


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they are crust and the mantle and also the core


Name the thick layer of earths interior that lies between the crust and the core?

The mantle


What are the parts of earths interior?

There three basic part of earth are The crust The mantle The core


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the convection currents will stop


What would happend to the convection currents in the mantle if earths interior eventually cooled down?

They will stop.


Is the heat source for the convection currents in the mantle for the sun?

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.


Is heat source for the convection currents in the mantle the sun?

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.


What is the thick layer of earths interior that lies between the crust and the core?

the mantle, which contains the lithosphere, asthenosphere and the mesosphere