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 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.
asthenosphere
The Earth's mantle is a solid layer beneath the crust that moves and flows slowly over the long term, causing tectonic plate movements. This slow movement is due to the high temperatures and pressures within the mantle, which allow the solid rock to deform and flow over time.
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 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 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.
asthenosphere
The oceanic crust is primarily made of solid rock, primarily basalt. However, beneath the oceanic crust, there is a layer of partially molten rock called the mantle that flows slowly over time.
The layer of the mantle that is solid rock but flows like putty is called the asthenosphere. This layer is located beneath the lithosphere and allows tectonic plates to move due to its partially molten nature.
The Earth's mantle is a solid layer beneath the crust that moves and flows slowly over the long term, causing tectonic plate movements. This slow movement is due to the high temperatures and pressures within the mantle, which allow the solid rock to deform and flow over time.
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.
Under bedrock is the mantle, which is the layer of rock between Earth's crust and core. The mantle consists of solid rock that flows very slowly over time. It is much thicker than the crust and contains a significant portion of Earth's mass.
The solid layer of the earth that can still flow is called the asthenosphere. This layer is located in the mantle of the earth the layer below the upper crust and lithosphere, home of the tectonic plates.
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.
This layer of solid rock is called bedrock.