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 rigid zone above the asthenosphere that includes the crust and upper mantle is called the lithosphere. This layer is divided into tectonic plates that float on the semi-fluid asthenosphere and move due to the convection currents beneath them.
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 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 Athenosophere is the layer below the lithosphere in the mantle. It can bend like plastic, but if you kicked it, you would stub your toe.
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 asthenosphere.
The asthenosphere.
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 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 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.
The asthenosphere.
I dont think there is a solid layer between the Lowwer Mantle and the Lithosphere. The only layer which lies in this region is the Asthenosphere, which is a Weak Zone and in Molten State.
The rigid zone above the asthenosphere that includes the crust and upper mantle is called the lithosphere. This layer is divided into tectonic plates that float on the semi-fluid asthenosphere and move due to the convection currents beneath them.
Lithosphere, Asthenosphere, Mesosphere, outer core, inner core
One characteristic of the asthenosphere is that it is a semi-fluid layer beneath the lithosphere where the material can flow slowly over time. This property allows for the movement of tectonic plates.
The lithosphere is the crust Moho and upper mantle. It floats on a plasticity zone called the asthenosphere.