The asthenosphere.
A zone of the earth's mantle that lies beneath the lithosphere and consists of several hundred kilometers of deformable rock.
The asthenosphere is the weaker, hotter zone beneath the lithosphere that allows for the motion of Earth's rigid outer shell. Its semi-fluid properties enable the lithospheric plates to move and interact with each other.
The weaker, hotter zone beneath the lithosphere is called the asthenosphere. It is semi-fluid and allows for the motion of the Earth's rigid outer shell, or lithosphere, due to its high temperature and partial melting that makes it more ductile compared to the overlying lithosphere.
The asthenosphere.
Asthenosphere is directly before the lithosphere.
The pressure in the transition zone is typically around 15,000 to 30,000 psi. This zone is located between the lithosphere and asthenosphere, where the pressure gradually increases due to the increasing depth beneath the Earth's surface.
The weaker, hotter zone beneath the lithosphere is known as the asthenosphere. This semi-fluid layer is located in the upper mantle and allows for the movement of tectonic plates, which are part of the rigid lithosphere above it. The asthenosphere's ability to flow, due to its higher temperatures and pressures, facilitates the tectonic processes such as continental drift and plate tectonics.
ATM in the lithosphere stands for Asthenosphere (A) and Transition zone (T) to the mantle (M). The asthenosphere is a semi-fluid layer beneath the lithosphere that allows tectonic plates to move, while the transition zone refers to the region between the upper and lower mantle in the Earth's interior.
The lithosphere is thicker than the Earth's crust. The lithosphere includes the crust and the upper part of the mantle, typically ranging in thickness from about 100 to 200 kilometers beneath the oceanic crust and up to 250 kilometers beneath continental crust.
The transition zone between the asthenosphere and the crust is called the lithosphere. It is the rigid outer layer of the Earth that consists of the crust and the uppermost part of the mantle. The lithosphere is broken into tectonic plates that float and move on the semi-fluid asthenosphere beneath it.
The zone of rigid, brittle rock that makes up the outermost layer of Earth is called the lithosphere. It includes the crust and the uppermost part of the mantle, and is divided into tectonic plates that move and interact with each other. Beneath the lithosphere lies the asthenosphere, which is a more ductile and deformable region of the upper mantle.
The zone below the lithosphere is called the asthenosphere. It is a semi-solid layer of the Earth's mantle where the rock is partially molten, allowing for tectonic plate movement. The asthenosphere is located between 100 to 200 kilometers beneath the Earth's surface.