The crust moves on a plastic like layer of the mantle.
The crust moves on a plastic like layer of the mantle.
The lithosphere, which includes the crust and uppermost part of the mantle, moves on a plastic-like layer of the mantle called the asthenosphere. This layer is partially molten and allows the lithospheric plates to move slowly over time due to convection currents.
The layer 100km below the surface is known as the asthenosphere. It is a semi-fluid layer within the upper mantle of the Earth where rock is ductile and able to flow slowly over time.
The plasticlike layer of Earth is the asthenosphere. It is a zone of the upper mantle where rock is soft and capable of gradual flow. The lithospheric plates float and move on top of the asthenosphere, contributing to the movement of tectonic plates.
First of all, there is no location of plate techtonics! Plate techtonics is the theory that Earth's crust and part of the upper mantle are broken into sections. These sections (plates) move on a plasticlike layer of the mantle.
Earth's thick plastic-like layer is the mantle. The mantle is a dense, semi-solid layer of the Earth's interior that lies beneath the crust and extends down to the outer core. It is composed of solid rock that can flow slowly over long periods of time.
The answer is Lithosphere!!!
The Earth's plastic-like layer is the asthenosphere, which is a semi-fluid layer of the upper mantle. It is composed of partially molten rock that allows tectonic plates to move slowly over it. The asthenosphere plays a key role in the process of plate tectonics.
the lithosphere.
Anthensophere
The lithosphere is the layer that moves with the tectonic plates. The lithosphere is made up of the crust and the upper part of the mantle, and it is broken into tectonic plates that move and interact with each other.
Moho barrier: Top of mantleOceanic crust: Thinnest layerUpper mantle: Moves the crustLower mantle: Borders liquid core