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 transition zone at the base of the Earth's crust is known as the Mohorovicic discontinuity or Moho. This zone separates the Earth's crust from the underlying mantle and is characterized by a sudden increase in seismic wave velocity. It is typically found around 5 to 10 kilometers deep beneath the ocean floor and 20 to 70 kilometers deep beneath the continents.
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 the crust Moho and upper mantle. It floats on a plasticity zone called the asthenosphere.
The asthenosphere.
The zone you are referring to is the mesosphere, which lies between the base of the asthenosphere and the boundary separating the mantle from the core. It is characterized by high pressure and temperature conditions, as well as the gradual increase in density from the bottom of the mantle to the core-mantle boundary.
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 transition zone at the base of the Earth's crust is known as the Mohorovicic discontinuity or Moho. This zone separates the Earth's crust from the underlying mantle and is characterized by a sudden increase in seismic wave velocity. It is typically found around 5 to 10 kilometers deep beneath the ocean floor and 20 to 70 kilometers deep beneath the continents.
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.
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 the crust Moho and upper mantle. It floats on a plasticity zone called the asthenosphere.
In the crust the weak spot we have is the Magma Chamber. But, deep down to the mantle such weak zone is the Asthenosphere.
The 3 main layers are - Crust Mantle Core The 5 sublayers are lithosphere, asthenosphere, mesosphere, outer core, inner core
The asthenosphere.
This region is known as the mesosphere. The base of the mesosphere includes the D'' (D double prime) layer which is sometimes considered to be a transition zone between the mantle and the core-mantle boundary zone.
Savanna is the grassland transition zone between a desert and a more humid region.
It is called a savanna, a transition between a desert and a grassland or forest.
The transition zone between a desert and a forest is a savanna.