In the mantle, temperatures range between 500 to 900 °C (932 to 1,652 °F) at the upper boundary with the crust; to over 4,000 °C (7,230 °F) near the boundary with the core.
Temperatures in the earth's mantle range from 932 to 1,652 degrees Fahrenheit.
Earths mantle is less dense and very hot. The mantle is 2885km thick.
its under the crust, its hot, its orange, its above the core, its in the earth
The mantle is the largest layer in the Earth's interior.
The flow of hot rock in earths mantle will stop and Earth's magnetic field will disappear
Yes the upper mantle is solid. The lower mantle however is not.
the earths mantle is very hot were cornstarch is not hot at all
the earths mantle is very hot were cornstarch is not hot at all
Decay of radioactive elements in the mantle heats it.
the earths mantle is very hot were cornstarch is not hot at all
the earths mantle is very hot were cornstarch is not hot at all
The flow of hot rock in earths mantle will stop and Earth's magnetic field will disappear
Earths mantle is less dense and very hot. The mantle is 2885km thick.
the average temperature for the Earth's lower mantle is 5400 degrees
It is the Mantle.
The earths mantle is less dense and it's very hot.
its under the crust, its hot, its orange, its above the core, its in the earth
The mantle is 82% of Earth's volume. It is composed of ultramafic rock called peridotite, which is hot enough to flow.