The asthenosphere.
The lithosphere lies on top of the asthenosphere. The lithosphere is the rigid outer layer of the Earth, consisting of the crust and upper part of the mantle, while the asthenosphere is a semi-fluid layer beneath the lithosphere that allows for tectonic plate movement.
Actually, the uppermost mantle is part of the lithosphere. The lithosphere consists of the crust and attached uppermost rigid mantle.
The asthenosphere lies below the lithosphere.
The soft layer of rock in the mantle is called the asthenosphere. It is partially molten and enables the movement of tectonic plates. This layer lies beneath the lithosphere and contributes to the process of plate tectonics.
The asthenosphere is part of the upper mantle, which lies beneath the Earth's lithosphere. It is a semi-fluid layer of the mantle that allows the lithospheric plates to move and float on top of it.
The lithosphere lies on top of the asthenosphere. The lithosphere is the rigid outer layer of the Earth, consisting of the crust and upper part of the mantle, while the asthenosphere is a semi-fluid layer beneath the lithosphere that allows for tectonic plate movement.
The layer beneath the lithosphere is much softer and flows very slowly.
Actually, the uppermost mantle is part of the lithosphere. The lithosphere consists of the crust and attached uppermost rigid mantle.
Asthenosphere is directly before the lithosphere.
The asthenosphere lies below the lithosphere.
The layer beneath the lithosphere is much softer and flows very slowly.
Directly beneath the lithosphere lies the asthenosphere, which extends from the base of the lithosphere to about 700 km deep. The asthenosphere is characterized by its semi-fluid, ductile properties, allowing for the movement of tectonic plates above it. This layer plays a crucial role in plate tectonics and the dynamics of the Earth's interior.
The Mesosphere lies below the Asthenosphere.Above the Asthenosphere is the Lithosphere.
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.
The soft layer of rock in the mantle is called the asthenosphere. It is partially molten and enables the movement of tectonic plates. This layer lies beneath the lithosphere and contributes to the process of plate tectonics.
Oceans are primarily found on the Earth's surface, which is part of the outermost layer known as the lithosphere. Beneath the lithosphere lies the asthenosphere, but the oceans themselves rest directly on the lithosphere. The water in the oceans also interacts with the atmosphere above and the hydrosphere, which encompasses all water on Earth.