The boundary between the asthenosphere and the lithosphere is normally below the Moho (which marks the boundary between the crust and the mantle).
The exception to this is below mid-ocean ridges where the moho and the lithosphere / asthenosphere boundary are at the same depth.
The lithosphere lies above the asthenosphere. The asthenosphere is where isostatic adjustments take place and it is a very ductile region. Seismic waves pass slower through this region of the earth than they do through the overlying lithosphere.
It is the asthenosphere.
asthenosphere
The asthenosphere is a part of the upper mantle of the Earth. It is below the lithosphere and can be over 400 miles thick in areas.
The Mesosphere lies below the Asthenosphere.Above the Asthenosphere is the Lithosphere.
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.
The asthenosphere lies below the lithosphere.
The lithosphere lies above the asthenosphere. The asthenosphere is where isostatic adjustments take place and it is a very ductile region. Seismic waves pass slower through this region of the earth than they do through the overlying lithosphere.
The asthenosphere
The Asthenosphere.
Asthenosphere
It is the asthenosphere.
The part of the mantle below the lithosphere is called the Asthenosphere.
The asthenosphere is located in the upper mantle. The asthenosphere is below the lithosphere, the brittle outer shell of the Earth.
A place where the crust of the lithosphere has fractured is known as the asthenosphere. The asthenosphere is located below the lithosphere and is where plate tectonic movement occurs.
A place where the crust of the lithosphere has fractured is known as the asthenosphere. The asthenosphere is located below the lithosphere and is where plate tectonic movement occurs.
Asthenosphere.