asthenosphere
The mechanical layer that lies below the lithosphere is the asthenosphere. It is a partially molten layer of the Earth's upper mantle that allows the lithospheric plates to move and interact.
The tectonic plates are contained within the lithosphere, which is the outermost mechanical layer of the Earth. The lithosphere comprises the crust and the uppermost part of the mantle and is rigid and brittle, allowing the tectonic plates to move and interact at their boundaries. Beneath the lithosphere lies the asthenosphere, a more ductile layer that facilitates the movement of the tectonic plates above it.
The D" layer (pronounced D double prime layer) forms the base of the Earth's lower mantle. Below this lies the outer core. This boundary zone is marked by a seismic discontinuity known as the Gutenberg discontinuity.
The Earth's crust lies above the mantle.
asthenosphere
The mechanical layer that lies below the lithosphere is the asthenosphere. It is a partially molten layer of the Earth's upper mantle that allows the lithospheric plates to move and interact.
The asthenosphere lies below the lithosphere.
The mechanical layer below the lithosphere is the asthenosphere. This layer is partially molten and allows the lithosphere to move and float on top of it. The asthenosphere plays a crucial role in plate tectonics by facilitating the movement of tectonic plates.
Mesosphere lies above the core.
Spongy Layer
thermosphere
solid rock baby
The asthenosphere and the mantle.
The layer below the corona is the chromosphere. It lies just below the corona and is characterized by a reddish glow during solar eclipses.
The mechanical layer above the core is the mantle. It is a thick layer of rock that sits between the core and the Earth's crust. The mantle is responsible for convection currents that drive plate tectonics and other geological processes.
The Asthenosphere is the upper layer of Earth's mantle. It lies below the Lithosphere.