the upper-mantle rocks are heavier while the lower mantle rocks are semisolid like melted plastic
the upper-mantle rocks are heavier while the lower mantle rocks are semisolid like melted plastic
The lower mantle is more rigid and dense than the asthenosphere in the upper mantle because of higher pressure and temperature conditions. The increased pressure in the lower mantle prevents rocks from flowing as easily as in the asthenosphere. This leads to higher density and rigidity in the lower mantle region.
The lower part of the mantle is called the "lower mantle" or "mesosphere", while the upper part of the mantle is referred to as the "upper mantle" or "asthenosphere".
The upper mantle is harder than the lower mantle
upper mantle
The Earth's upper mantle is composed of solid rock that flows through liquid rock, also known as lava.
The upper mantle and the lower mantle.
The mantle is divided into the upper mantle, transition zone, and lower mantle. The upper mantle is beneath the lithosphere, the transition zone lies between the upper and lower mantle, and the lower mantle extends to the outer core.
under the upper mantle
The lower mantle is under greater pressure than the upper mantle, compressing the rock into a denser form.
Temperature: The upper mantle is cooler than the lower mantle. Composition: The upper mantle is more silicate-rich and less dense compared to the lower mantle. Physical properties: The upper mantle is more rigid and brittle, while the lower mantle is more ductile and capable of flow.
The upper mantle