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).
The mantle of the Earth can reach temperatures between 1,292°F to 7,652°F, depending on the depth and location within the mantle.
The mantle is divided into two main layers: the upper mantle and the lower mantle. The upper mantle is closer to the Earth's crust and is more rigid, while the lower mantle is hotter and flows more easily due to higher temperatures and pressures.
H'm, i think it is either mantle of mantle and the crust of earth combined .so it is probably mantle
The hottest part of the mantle is believed to be near the core-mantle boundary, where temperatures can reach up to 4000 degrees Celsius. This intense heat is due to the heat generated by the Earth's core and the slow heat conduction through the solid rock of the mantle.
Me because I am so hot
The temperature of the Earth's mantle is higher than the temperatures of the outer layers, such as the crust, but lower than the core.
The mantle of the Earth can reach temperatures between 1,292°F to 7,652°F, depending on the depth and location within the mantle.
No. The temperatures are too hot sustain life.
uneven temperatures
The mantle is divided into two main layers: the upper mantle and the lower mantle. The upper mantle is closer to the Earth's crust and is more rigid, while the lower mantle is hotter and flows more easily due to higher temperatures and pressures.
H'm, i think it is either mantle of mantle and the crust of earth combined .so it is probably mantle
The mantle is hotter than the crust, with temperatures ranging from about 500°C to 900°C (932°F to 1652°F) at the upper boundary with the crust, and increasing with depth. The core-mantle boundary can reach temperatures exceeding 4000°C (7232°F).
A convection cell.
convection currents
The mantle is primarily composed of silicate minerals such as olivine, pyroxene, and feldspar. These minerals form the bulk of the Earth's mantle due to their abundance and ability to withstand high temperatures and pressures.
The hottest part of the mantle is believed to be near the core-mantle boundary, where temperatures can reach up to 4000 degrees Celsius. This intense heat is due to the heat generated by the Earth's core and the slow heat conduction through the solid rock of the mantle.
The density of the mantle increases with depth due to the increase in pressure and temperature. The lower mantle, in particular the part known as the D'' layer, is where the density of the material is greater due to the higher pressure and temperatures compared to the upper mantle.