The upper mantel is the part of the mantel nearest to the Earth's surface. It is a little cooler than the lower mantel therefore more viscous, or pasty, than the lower mantel. Temperatures range between 932 °F-1,652 °F. at the upper boundary with the crust to over 7,200 °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 periditute), 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.
The temperature of a mantel can vary depending on the type of fuel being used (wood, gas, electric) and how long it has been burning. Typically, a wood-burning mantel can reach temperatures of 500-900°F (260-480°C) when in use.
The lithosphere includes the uppermost part of the mantle and it also includes all of the crust.
Both the lithosphere and asthenosphere are parts of Earth's uppermost layer, known as the Earth's crust. The lithosphere is the rigid outer layer made up of the crust and a part of the upper mantle, while the asthenosphere is a semi-fluid layer beneath the lithosphere. They are both involved in the movement of Earth's tectonic plates.
The asthenosphere is a semi-fluid layer of the Earth's upper mantle beneath the lithosphere. It is responsible for the movement of tectonic plates due to its semi-fluid nature, allowing them to slide and shift over the asthenosphere. The asthenosphere plays a crucial role in plate tectonics and the dynamics of the Earth's surface.
Mikey Mantel played for the NEW YORK YANKEES.
The upper mantle is also known as the asthenosphere.
It is the upper and lower mantle. It has the consistency of warm asphalt.
lithosphere
Melted, plasticlike rocks
I.am not sure but i think it is bc i believe the upper mantel is extremely hot
CRUST (lithosphere)
upper mantle.
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Mantle, is the homophone of Mantel ;)
Mantle is a homophone for mantel.
The depth of the upper mantle ranges from about 30 to 400 kilometers below the Earth's surface. This layer is predominantly composed of solid rock materials and plays a significant role in the movement of tectonic plates.
The Mantel is 2876 km. thick.