because of deep current
The asthenosphere allows tectonic plates to move
The soft layer of the mantle on which the tectonic plates move is called the asthenosphere. It is a semi-fluid layer beneath the lithosphere that allows for the movement of the tectonic plates due to convection currents in the mantle.
Because the Asthenosphere is malleable, divergent boundaries and convergent boundaries are formed. The plasticity of the Asthenosphere allows the plates to move through sea floor spreading and subduction zones.
The asthenosphere allows tectonic plates to move
The asthenosphere allows tectonic plates to move
The asthenosphere is the region of the Earth that is soft and putty-like, located beneath the lithosphere. The asthenosphere allows for the movement of tectonic plates due to its semi-fluid state, which allows the plates to slide and move over it.
It's where the plates of the lithosphere move around on, the plastic like layer of the asthenosphere. the plates move around on these
The asthenoshere acts like jello and allows the lithosphere, containing the plate, to move. Tectonic plates could not move without the asthenoshere.
The asthenoshere acts like jello and allows the lithosphere, containing the plate, to move. Tectonic plates could not move without the asthenoshere.
The asthenosphere is a partially molten layer in Earth's mantle that allows the lithospheric plates to move on top of it. The heat and pressure in the asthenosphere weakens the rocks, making them more flexible and able to flow slowly. This flow in the asthenosphere causes the plates to move and interact with each other, leading to phenomena like earthquakes and volcanic activity.
The plates of lithosphere float on top of the semi-fluid asthenosphere, which is located beneath the lithosphere in the Earth's upper mantle. The asthenosphere allows the plates to move and interact with each other due to its partially molten and more ductile nature compared to the lithosphere above it.
Tectonic plates float on the asthenosphere, which is a semi-fluid layer of the Earth's mantle. This allows the plates to move and interact with each other, causing geological phenomena such as earthquakes and volcanic activity.