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Earth's crust and brittle upper mantle is called the lithosphere.
It is called the lithosphere.
Large segments of the crust and upper mantle known as the Lithospheric plates.
The upper mantle is located beneath the Earth's crust, extending from about 30 to 400 kilometers deep. It is part of the Earth's mantle layer, which lies between the crust and the core.
lithenosphere
P waves travel faster through the upper mantle because it is composed of denser rock materials compared to the crust. The higher density allows the seismic waves to propagate more efficiently through the upper mantle, resulting in higher velocity. Additionally, the upper mantle is composed of more solid rock material, while the crust may contain more heterogeneous and less dense materials that can slow down the waves.
Crust and the upper mantle
The crust and upper mantle make up the earth.
Earth's crust and brittle upper mantle is called the lithosphere.
It is called the lithosphere.
Large segments of the crust and upper mantle known as the Lithospheric plates.
The crust and uppermost brittle mantle are referred to as the lithosphere.
The layer of the Earth that contains both the crust and upper mantle is called the Lithosphere.
a mantle is something between the crust
The The crust and the uppermost layer of the mantle form the lithosphere. The asthenosphere, which is still in the upper mantle, is the next layer down.
Together the crust and upper mantle make the lithosphere.
The lithosphere is the crust Moho and upper mantle. It floats on a plasticity zone called the asthenosphere.