The mantle under the crust it is made of molten rock material
A glacier is an example of a solid that flows, albeit very slowly.
The layer you are referring to is the asthenosphere, which is composed of solid rock that flows slowly due to high heat and pressure. This layer is located beneath the lithosphere and is responsible for the movement of tectonic plates.
The rock layer beneath the Earth's surface that slowly flows is the mantle. (Given enough time, all rocks, even the most solid, will flow through molecular motion.)The mantle is a slowly convecting layer of rock which flows in order to transfer heat from the core to the Earth's surface. It is this convection that drives the movements of the continents and can cause volcanic mountains to form.The athenosphere is the highly viscous, mechanically-weak and ductilely-deforming upper mantle of the Earth. It is the zone upon which the great rigid and brittle lithospheric plates of the Earth's crust move about. However, the whole mantle is flowing, albeit very slowly.
soler system
The layer of solid rock that flows very slowly is called the asthenosphere. It is located beneath the lithosphere and is responsible for the movement of tectonic plates. The asthenosphere has the ability to flow due to high temperatures and pressures, allowing it to deform over long periods of time.
No, the asthenosphere is a semi-solid layer of the Earth's mantle that flows slowly over time due to high temperatures and pressure. It is not a cool solid rock.
A glacier is an example of a solid that flows, albeit very slowly.
molden
Anywhere from 5 to 70 miles, roughly, the range of thickness of the lithosphere.
Anywhere from 5 to 70 miles, roughly, the range of thickness of the lithosphere.
The layer you are referring to is the asthenosphere, which is composed of solid rock that flows slowly due to high heat and pressure. This layer is located beneath the lithosphere and is responsible for the movement of tectonic plates.
The rock layer beneath the Earth's surface that slowly flows is the mantle. (Given enough time, all rocks, even the most solid, will flow through molecular motion.)The mantle is a slowly convecting layer of rock which flows in order to transfer heat from the core to the Earth's surface. It is this convection that drives the movements of the continents and can cause volcanic mountains to form.The athenosphere is the highly viscous, mechanically-weak and ductilely-deforming upper mantle of the Earth. It is the zone upon which the great rigid and brittle lithospheric plates of the Earth's crust move about. However, the whole mantle is flowing, albeit very slowly.
The mantle layer of the Earth is approximately 2,900 km thick. It lies between the Earth's crust and core and is composed of solid rock that flows slowly over time due to heat and pressure.
The mantle is the thickest layer of the Earth, extending from the crust to the outer core. It makes up approximately 84% of Earth's volume and is composed of solid rock material that flows slowly over geological timescales.
soler system
The layer of solid rock that flows very slowly is called the asthenosphere. It is located beneath the lithosphere and is responsible for the movement of tectonic plates. The asthenosphere has the ability to flow due to high temperatures and pressures, allowing it to deform over long periods of time.
The thickest layer of the Earth is the mantle, which extends from the crust to the outer core. The mantle is approximately 2,900 kilometers (1,800 miles) thick and is made up of solid rock that flows slowly over long periods of time.