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The lithosphere come from two Greek words which means sphere and rocky. The lithosphere is the rigid and the outermost shell of a rocky planet that is defined on the basis of the mechanical properties.
The lithosphere is the outermost shell of a rocky planet defined on the basis of the mechanical properties. On Earth, it comprises the crust and the portion of the upper mantle that behaves elastically on time scales of thousands of years or greater. The outermost shell of a rocky planet defined on the basis of the chemistry and mineralogy is a crust.
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.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
Oceanic lithosphere is dense enough to be forced down into the mantle. Continental lithosphere is not.
The lithosphere come from two Greek words which means sphere and rocky. The lithosphere is the rigid and the outermost shell of a rocky planet that is defined on the basis of the mechanical properties.
The lithosphere is the outermost shell of a rocky planet defined on the basis of the mechanical properties. On Earth, it comprises the crust and the portion of the upper mantle that behaves elastically on time scales of thousands of years or greater. The outermost shell of a rocky planet defined on the basis of the chemistry and mineralogy is a crust.
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.
The lower boundary of the asthenosphere is not well defined. It lies below the lithosphere and above the lower mantle and outer core. It usually lies at depths of 80-200 km but can range as deep as 700 km.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
The uppermost mantle and the crust makes the lithosphere.
The difference between the core and the lithosphere is the core is on the top of the lithosphere and the lithosphere is on the bottom of the core
An avalanche is sometimes defined as a cascade of snow.
The lithosphere is composed of the crust and uppermost hard, brittle mantle.
lithosphere.
division of lithosphere
Lithosphere (apex)