It is 500 to 900 Celsius at the upper boundary and 4000 Celsius at the boundary near the outer core. A2. The values range between 500 deg C at the crust boundary, to over 4 000 deg C at the outer Core boundary.
A1. between 100 to 1600 Celsius. The Mantle temperature varies to about 1600-4000 degrees.
The average temperature of the mantle is is 5400 ºF (3000ºC).
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) at the boundary with the core. Although the higher temperatures far exceed the melting points of the mantle rocks at the surface (about 1200 °C for representative peridotite), the mantle is almost exclusively solid. The enormous lithostatic pressure exerted on the mantle prevents melting, because the temperature at which melting begins (the solidus) increases with pressure.
Temperatures in the lower mantle are estimated to range from 1600-4000 oC.
The inner mantle of the Earth is so hot that the rock flows. It is about 932 to 1652 degrees Fahrenheit.
You have the inner core, outer core, mantle, upper mantle and crust. The mantle itself has a temperature of 500 to 900 degrees Celsius, which is 932 to 1,652 degrees Fahrenheit.
The temperatures in the mantle can be as 500-900 degrees C near the crust and 4000 degrees C near the core.
H'm, i think it is either mantle of mantle and the crust of earth combined .so it is probably mantle
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.
convection cell
Me because I am so hot
pressure.
H'm, i think it is either mantle of mantle and the crust of earth combined .so it is probably mantle
No. The temperatures are too hot sustain life.
uneven temperatures
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.
these nutz
A convection cell.
convection cell
convection currents
Me because I am so hot
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) at the boundary with the core. Although the higher temperatures far exceed the melting points of the mantle rocks at the surface (about 1200 °C for representative peridotite), the mantle is almost exclusively solid. The enormous lithostatic pressure exerted on the mantle prevents melting, because the temperature at which melting begins (the solidus) increases with pressure.
pressure.
The asthenosphere, part of the upper mantle.