The Asthenosphere is a layer of the upper mantle.
The asthenosphere is not a plate boundary. It is the layer of Earth's mantle on which tectonic plates float.
asthenosphere
The layer directly below the lithosphere is the asthenosphere. The asthenosphere is partially molten and allows for the movement of tectonic plates above it.
The lithosphere surrounds the asthenosphere.
The lithosphere sits on top of the asthenosphere.
The layer directly under the Lithosphere is the Asthenosphere. The Asthenosphere is a semi-fluid layer of the Earth's mantle that allows for the movement of the tectonic plates above it. It is hotter and more ductile compared to the rigid Lithosphere.
The lithosphere, asthenosphere, and mesosphere are all located within the Earth's upper mantle, which is part of the mantle layer. The lithosphere is the rigid outermost layer of the Earth, including the crust and uppermost mantle. The asthenosphere is a partially molten layer below the lithosphere, while the mesosphere is a solid layer beneath 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 rigid layer of Earth surrounding the asthenosphere is the lithosphere. It is composed of the crust and the upper portion of the mantle and is broken into tectonic plates that float on the semi-fluid asthenosphere below.
This is known as 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 partially molten layer of the mantle is called the asthenosphere. This zone is partially molten and allows tectonic plates to move on top of it.