The asthenosphere.
The asthenosphere consists of many varieties of rock which is mostly in a semi molten condition. The temperatures in the asthenosphere reach levels high enough for most of the rock to become soft and plastic, capable of slowly moving while remaining in a solid state, while only about 10 percent is totally molten. The soft, plastic, but solid quality of the asthenosphere allows lithospheric plates to slide on top, resulting in the many earthquakes which occur in this region.
Solid
The Lithosphere, Asthenosphere, Mesosphere, outer core and Inner core.
Asthenosphere
The asthenosphere allows tectonic plates to move
The asthenosphere.
The asthenosphere allows tectonic plates to move
The asthenosphere allows tectonic plates to move
The two densest physical layers of the earth are the lithosphere and the asthenosphere.
The two densest physical layers of the earth are the lithosphere and the asthenosphere.
The asthenosphere consists of many varieties of rock which is mostly in a semi molten condition. The temperatures in the asthenosphere reach levels high enough for most of the rock to become soft and plastic, capable of slowly moving while remaining in a solid state, while only about 10 percent is totally molten. The soft, plastic, but solid quality of the asthenosphere allows lithospheric plates to slide on top, resulting in the many earthquakes which occur in this region.
Solid
The lithosphere is rigid and commonly deforms in a brittle manner; the asthenosphere tends to flow slowly and deform in a plastic manner.
Inner core, outer core, asthenosphere, lithosphere, and crust.
The Lithosphere, Asthenosphere, Mesosphere, outer core and Inner core.
The two densest physical layers of the earth are the lithosphere and the asthenosphere.