The lithosphere, which includes the Earth's crust and part of the upper mantle, is about 100 km thick. This rigid outer layer is divided into tectonic plates that float on the semi-fluid asthenosphere beneath them.
Earth's mantle is a rocky shell about 2,890 km (1,800 mi) thick that constitutes about 84 percent of Earth's volume. Two main zones are distinguished in the upper mantle: the inner asthenosphere composed of flowing rock in the state of plasticity, about 200 km thick, and the lowermost part of the lithosphere, composed of rigid rock, about 50 to 120 km thick. A thin crust, the upper part of the lithosphere, surrounds the mantle and is about 5 to 75 km thick. The mantle is divided into sections which are based upon results from seismology. These layers (and their depths) are the following: the upper mantle (starting at the Moho, or base of the crust around 7 to 35 km, downward to 410 km), the transition zone (410-660 km), the lower mantle (660-2891 km), and in the bottom of the latter region there is the anomalous D" layer with a variable thickness (on average ~200 km thick)
The Earth's layers vary in thickness. The crust is thinnest under the oceans, around 5-10 km thick, and thicker under continents, around 20-70 km thick. The mantle extends from the crust to about 2,900 km below the surface, while the outer core is about 2,300 km thick and the inner core is about 1,200 km thick.
The deep mantle is the region in Earth's interior located between the lower mantle and the core. It extends from about 660 km to 2,900 km below the Earth's surface. This region is thought to consist mainly of solid rock undergoing high pressures and temperatures.
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.
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 Earth's crust is about 40 km thick on average. It consists of the outermost solid shell of the Earth and is divided into tectonic plates that float on the semi-fluid asthenosphere below.
The asthenosphere is a layer in the Earth's mantle that lies between 100 km to 200 km beneath the Earth's surface. It is characterized by its semi-fluid or ductile behavior due to high temperatures and pressures.
180 km
The asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.
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 a semi-fluid layer of the Earth's mantle located beneath the lithosphere. It is responsible for plate tectonics and the movement of tectonic plates. The asthenosphere is composed of hot, solid rock that can flow slowly over long periods of time.
The asthenosphere is a semi-fluid layer located beneath the lithosphere of the Earth's crust. It is responsible for the movement of tectonic plates due to its plasticity. The asthenosphere is composed of hot, partially molten rock that allows for convection currents to occur, driving plate tectonics.
5 to 8 KM thick.
300 km
300 km
The lithosphere, which includes the Earth's crust and part of the upper mantle, is about 100 km thick. This rigid outer layer is divided into tectonic plates that float on the semi-fluid asthenosphere beneath them.