Its about .1 to 1.5 million atmosheres.
Its about .1 to 1.5 million atmosheres.
The density of Earth's mantle varies depending on its depth. The part right below the crust has a density of about 3.4 grams per cubic centimeter while the lowest part of the mantle is 5.6 grams per cubic centimeter.
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.
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) near the boundary with the core.
Its about .1 to 1.5 million atmosheres.
Its about .1 to 1.5 million atmosheres.
The stiffer mantle (upper) is one of the layers of the earth's crust and composed of hot liquid rock. The range of density is between 3-100 or 3.4g/cm and 4.3g/cm.
The stiffer mantle (upper) is one of the layers of the earth's crust and composed of hot liquid rock. The range of density is between 3-100 or 3.4g/cm and 4.3g/cm.
The stiffer mantle (upper) is one of the layers of the earth's crust and composed of hot liquid rock. The range of density is between 3-100 or 3.4g/cm and 4.3g/cm.
The density of Earth's mantle varies depending on its depth. The part right below the crust has a density of about 3.4 grams per cubic centimeter while the lowest part of the mantle is 5.6 grams per cubic centimeter.
Not if it is within the normal range
It is the state in which the arterial blood pressure is within the normal range.
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.
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.
Read the tyre wall, it should have the pressure envelope there. Any pressure within that range should be okay. If you want less rolling resistance inflate the tyre to the higher end of the range.
The asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.