The temperature ranges from 932 to 1,652-degrees F, at the top, where it meets the crust, to 7,230-degrees F at the lower mantle. Temperature and pressure increase with depth.
The temperature in the Earth's mantle can be anywhere from 500 to 900 degrees Celsius. Closer to the core of the Earth, the temperature can reach 4,000 degrees Celsius.
Temperature Density and Pressure
1000-1500 degrees Celsius
Inner Mantle: The average temperature is about 3000ºC Outer Mantle: The average temperature is about 2200ºC
They would differ in temperature, mineralogy, density, and pressure.
5600c
the average temperature for the Earth's lower mantle is 5400 degrees
The asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.
The temperature in the Earth's mantle can be anywhere from 500 to 900 degrees Celsius. Closer to the core of the Earth, the temperature can reach 4,000 degrees Celsius.
The lithosphere is the upper portion of the mantle. Its temperature is around 300 to 500 degrees Celsius. The lower portion of the mantle, which is the asthenosphere, has a temperature of around 4500 degrees Celsius.
Temperature Density and Pressure
Temperature is about 2000 to 3000 degrees celsius maybe less.The mantle is hot but not the hottest layer.It is is the second layer of the Earth. The mantle is the thickest layer of the earth, it is the layer of the earth beneath the crust.Upper mantle and Lower mantle are the two parts of the mantle, The lower mantle is deeper and denser than the upper mantle .
The mesosphere
1000-1500 degrees Celsius
The middle mantle is just above the lower mantle.
The Lower Mantle
The asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.