No, it is hotter because it is closer to the inner core
The Earth's mantle consists mainly of the upper mantle and the lower mantle. The upper mantle is made up of solid rock, while the lower mantle is composed of more solid and dense rock. The mantle plays a crucial role in the movement of tectonic plates and the convection currents that drive plate tectonics.
The upper mantle
The sinking process in the lower mantle convection cell occurs when cooler, denser material from the upper mantle descends into the lower mantle. As this material sinks, it displaces the hotter, less dense material in the lower mantle, which then rises toward the upper mantle. This movement creates a continuous cycle of convection, facilitating heat transfer within the Earth and influencing geological processes such as plate tectonics. The sinking process is driven by thermal and compositional differences within the mantle.
The mantle is composed of the upper mantle and the lower mantle. The upper mantle is known for its plasticity and convective movement, while the lower mantle is more rigid and is characterized by high-pressure conditions.
The density of the upper mantle is generally estimated to be around 3.3-3.4 grams per cubic centimeter. It is denser than the Earth's crust but less dense than the lower mantle. This density variation plays a significant role in the movement of tectonic plates.
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.
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 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 Earth's mantle consists mainly of the upper mantle and the lower mantle. The upper mantle is made up of solid rock, while the lower mantle is composed of more solid and dense rock. The mantle plays a crucial role in the movement of tectonic plates and the convection currents that drive plate tectonics.
The upper mantle is harder than the lower mantle
upper mantle
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.
the upper-mantle rocks are heavier while the lower mantle rocks are semisolid like melted plastic
The upper mantle