the mantel makes up the asthenosphere
The continents of the Earth are sliding through the asthenosphere. This is the viscous part of the mantle on which the plates of the lithosphere sit.
they sit on the asthenosphere
The mesosphere is made up of plenty of things. It is underneath the asthenosphere and the lower part of the mantle. The mesosphere extends from the bottom of the asthenosphere to the earth's core. give me a piture. The mesosphere also means middle.
The convection currents running through the asthenosphere are widely believed to be the source of movement of the tectonic plates.
The Asthenosphere.
the mantel makes up the asthenosphere
The middle and lower mantle makes up the asthenosphere.
the mantel makes up the asthenosphere
asthenosphere
The asthenosphere lies in, and is the upper ductile part of, the mantle. It is the layer directly underneath the lithosphere; the layer composed of the crust and uppermost rigid mantle.
Because of the asthenosphere.
The continents of the Earth are sliding through the asthenosphere. This is the viscous part of the mantle on which the plates of the lithosphere sit.
The differences and similarities between lithosphere and asthenosphere are as follows. Lithoshphere is made up of rigid rocks flowing above asthenosphere. Asthenosphere has rocks that are more plastic like because they can flow even tho they are still solid rock. The top part of asthenosphere is the same as the lower part of lithosphere, if the top part of asthenosphere cools it then becomes part of lithosphere. Lithosphere and asthenosphere are both made up of the upper part of the mantle on Earth but Lithosphere is also made up of the crust.
The asthenosphere has the ability to slow down seismic waves. Is not made up of earths plates that would be the lithosphere.
mesosphere, asthenosphere, ionosphere
Mountains don't sink because of buoyancy. The continental crust and the rest of the lithosphere float on the asthenosphere like a boat on the water. Mountains have roots that extend down into the asthenosphere that coordinate to the mass of the mountain.
The rock in the asthenosphere is partially molten, allowing it to flow and deform slowly under pressure. This unique property makes the asthenosphere capable of supporting the movement of tectonic plates on Earth's surface.