The crust and uppermost part of the mantle (lithospheric mantle) are located in the lithosphere. The lithosphere is composed of the rigid outermost layer of Earth, including the crust and the solid upper part of the mantle.
Both the crust and the upper mantle are solid layers of the Earth's lithosphere. However, the crust is more brittle and less dense than the mantle. Additionally, the crust is composed primarily of oxygen and silicon (silicate minerals) whereas the mantle contains more iron and magnesium.
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 mantle is divided into two main layers: the upper mantle and the lower mantle. The upper mantle is further divided into the lithosphere and the asthenosphere. The lithosphere is rigid and made up of the crust and the upper part of the mantle, while the asthenosphere is semi-molten and capable of flowing.
The two layers of the lithosphere is made up of the oceanic lithosphere and continental lithosphere. The oceanic lithosphere is associated with oceanic crust and the ocean basins. The continental lithosphere is associated with the continental crust.
The lithosphere is the rigid outer layer of Earth made up of the crust and the upper part of the mantle. It is located on top of the asthenosphere, a partially molten layer of the mantle. The lithosphere is divided into large tectonic plates that move on the asthenosphere.
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.
Both the crust and the upper mantle are solid layers of the Earth's lithosphere. However, the crust is more brittle and less dense than the mantle. Additionally, the crust is composed primarily of oxygen and silicon (silicate minerals) whereas the mantle contains more iron and magnesium.
Crust and the upper mantle
The lithosphere is divided into two layers: the crust and the upper part of the mantle. The crust includes the Earth's outermost layer that is divided into continental and oceanic crust. The upper part of the mantle beneath the crust is known as the asthenosphere.
crust and upper mantle
crust and upper mantle
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 includes the crust and the very top of the mantle. The lithosphere is cool and brittle.
The mantle is divided into two main layers: the upper mantle and the lower mantle. The upper mantle is further divided into the lithosphere and the asthenosphere. The lithosphere is rigid and made up of the crust and the upper part of the mantle, while the asthenosphere is semi-molten and capable of flowing.
Yes. The simple layers are: crust, (lithosphere), mantle, and then crust. (Inner and outer)
It is located in the crust and upper mantle of the Earth.
The lithosphere is defined as the crust plus the brittle, uppermost mantle to which it is attached. The part of the upper mantle called the asthenosphere is ductile, and is the portion of the mantle on which the lithosphere 'floats'. Essentially, it is a difference in the degree of ductility. The lithosphere is brittle; the mantle is ductile.