lithosphere
lithosphere
Together the crust and upper mantle make the lithosphere.
Earth's crust and brittle upper mantle is called the lithosphere.
Together the crust and upper mantle make the lithosphere.
plat techtonce
The crust and upper mantle make up the earth.
The lithosphere consists of the crust and the upper part of the mantle. The crust is the outermost layer of the Earth, while the upper mantle is the solid rock layer beneath the crust. Together, they form the rigid outer shell of the Earth.
The lithosphere is made up of two layers: the crust and the uppermost part of the mantle. The crust is the outermost layer of the lithosphere and is composed of solid rock, while the upper mantle beneath it is also solid but more ductile.
The crust and the solid upper mantle are referred to as one layer because they collectively make up the Earth's lithosphere, which is the rigid outermost layer of the Earth. This layer is divided into tectonic plates that float on the semi-fluid asthenosphere below. The lithosphere includes both the crust and the uppermost part of the mantle, which behave as a single mechanical layer in plate tectonics.
The two layers that make up the lithosphere are the crust and the upper part of the mantle. The crust is the outermost layer of the Earth, while the upper mantle is the solid part of the mantle that lies just below the crust. These two layers together form the rigid outer shell of the Earth known as the lithosphere.
The lithosphere is the rigid outermost shell of a rocky planet. It comprises the crust and the portion of the upper mantle that behaves elastically on time scales of thousands of years or greater.In the Earth, the lithosphere includes the crust and the uppermost mantle, which constitute the hard and the crust.Also, in the Earth, the lithosphere is more in the crust, than in the uppermost mantle.
The crust and the hard uppermost mantle make up the lithosphere, which is the solid, rocky layer covering the entire surface of the planet and reacts to stresses as a brittle solid. The lithosphere ranges in thickness from 50 - 200 kmA and is fragmented into tectonic plates with boundaries where plates collide, diverge, or grind past each other.A Wilson, M. (2000) Igneous Petrogenesis - A Global Tectonic Approach, Chapman and Hall, London.