The solid layer found between the lithosphere and the outer core is called the asthenosphere. It is a semi-plastic layer that allows the lithospheric plates to move over it.
The plastic-like layer below the lithosphere is called the asthenosphere. It is partially molten and allows the rigid lithosphere above it to move and drift on the flowing asthenosphere, causing tectonic plate movement.
The deepest layer of the lithosphere is called the asthenosphere. It is located just below the lithosphere and is made up of partially molten rock that allows the lithosphere to move and float on top of it. The asthenosphere plays a crucial role in plate tectonics and the movement of Earth's crustal plates.
The lithosphere is defined as the crust plus the brittle, uppermost mantle to which it is attached. The part of the upper mantle called the asthenosphere is ductile, and is the portion of the mantle on which the lithosphere 'floats'. Essentially, it is a difference in the degree of ductility. The lithosphere is brittle; the mantle is ductile.
The solid outer crust layer of the Earth is called the lithosphere. The top portion of the mantle layer, just beneath the lithosphere, is called the asthenosphere.
The lithosphere floats on a layer of the Earth's mantle called the asthenosphere. The asthenosphere is a semi-fluid layer beneath the lithosphere that allows the movement of tectonic plates.
The part of the mantle below the lithosphere is called the Asthenosphere.
Upper Mantle
Because of something called Isostacy-the gravitational equilibrium between lithosphere and asthenosphere, such that plates "float" at an elevation that dependes on the thickness and density. EX. Think floating ice cubes
The large sections of lithosphere that float on the asthenosphere are called tectonic plates. These plates are rigid sections of Earth's lithosphere that move and interact with each other at plate boundaries, causing geological phenomena like earthquakes and volcanic eruptions.
The asthenosphere.
The solid plastic layer of the mantle beneath the lithosphere is called the asthenosphere. It is characterized by its semi-fluid nature, allowing for the movement of tectonic plates over time. The asthenosphere plays a crucial role in the process of plate tectonics.
The lithosphere associates mainly with the weak molten layer of the mantle called the asthenosphere.
The lithosphere is the crust Moho and upper mantle. It floats on a plasticity zone called the asthenosphere.
It's called the asthenosphere.
The upper mantle is divided into two main sections: the lithosphere and the asthenosphere. The lithosphere is rigid and includes the crust, while the asthenosphere is a semi-fluid layer beneath the lithosphere where convection currents occur.
The solid outer crust layer is called the lithosphere, and the top portion of the mantle layer is called the asthenosphere. The lithosphere is rigid and consists of the crust and the uppermost part of the mantle, while the asthenosphere is a ductile layer beneath the lithosphere where convection currents occur.