The asthenosphere is typically around 100-200 kilometers thick beneath the Earth's crust. It is a semi-fluid layer of the upper mantle that allows for the movement of tectonic plates.
180 km
lithosphere
It is about 1200 km thick
the mantle, which contains the lithosphere, asthenosphere and the mesosphere
The Moho discontinuity is 31 miles/50KM thick.
180 km
The asthenosphere is approximately 100-200 kilometers thick beneath the Earth's crust. It is a semi-plastic layer of the mantle that lies below the lithosphere and plays a key role in plate tectonics and mantle convection.
The asthenosphere (or low-velocity zone) is believed to be about 200 kilometers (120 miles) thick. The layers of rock that make up the asthenosphere are thought to be partially melted and hotter than those in the lithosphere. If this were true, it would explain why the asthenosphere might also have less surface integrity, making it a possible source for the generation of new magma.
The asthenosphere is variously estimated as being from fifty to several hundred miles (eighty-five to several hundred kilometers) thick and consists of deformable rock.It is a zone of the Earth's mantle that lies beneath the lithosphere.For more information see the answer to the Related Questionshown below.
The asthenosphere is estimated to be approximately 100-200 kilometers thick. It is a semi-fluid layer in the upper mantle of the Earth that lies below the lithosphere and plays a crucial role in the movement of tectonic plates.
lithosphere
The asthenosphere is approximately 250 km to 400 km thick beneath the Earth's crust. However, its exact thickness can vary in different regions and can reach up to 700 km in some areas.
100,000,000,000 kilometers thick.
5 to 8 KM thick.
It is about 1200 km thick
Thick thousand of miles/kilometers thick
The asthenosphere is typically around 60 to 250 miles thick. The thickness can vary depending on the location and other geological factors. It is a semi-plastic layer beneath the Earth's lithosphere where convection currents occur.