The solid plastic layer upon which tectonic plates move is called the asthenosphere. It is located beneath the lithosphere and consists of partially molten rock that allows for the slow flow and movement of tectonic plates. This movement is driven by convection currents in the underlying mantle, facilitating the dynamic processes of plate tectonics.
The solid plastic layer of the Earth upon which tectonic plates move is called the asthenosphere. It lies beneath the rigid lithosphere and is characterized by its semi-fluid properties, allowing the tectonic plates to drift and interact. This movement is driven by convection currents within the underlying mantle.
The lithosphere, which includes the uppermost portion of the mantle, forms the solid tectonic plates along with the crust. This layer is divided into massive plates that float on the semi-fluid asthenosphere beneath them.
The layer that fits this description is the lithosphere. The lithosphere is comprised of the uppermost part of the mantle and the crust, and it is broken into tectonic plates that move on the Earth's surface.
The lithosphere, which includes the rigid outermost layer of the Earth's mantle, is responsible for the movement and formation of tectonic plates. These plates float on the semi-fluid asthenosphere below and interact with each other at plate boundaries, leading to processes like subduction and spreading.
The plastic solid layer of slowly flowing rock within the Earth is known as the asthenosphere. Located beneath the rigid lithosphere, the asthenosphere allows for the movement of tectonic plates due to its semi-fluid properties. This layer plays a crucial role in geological processes, such as plate tectonics and volcanic activity, contributing to the dynamic nature of the Earth's surface.
The asthenosphere.
The solid plastic layer of the mantle is called the asthenosphere. This region is partially molten and allows for the movement of tectonic plates.
The solid plastic layer of the Earth upon which tectonic plates move is called the asthenosphere. It lies beneath the rigid lithosphere and is characterized by its semi-fluid properties, allowing the tectonic plates to drift and interact. This movement is driven by convection currents within the underlying mantle.
The solid plastic layer of the mantle is called the asthenosphere. It is a semi-fluid layer below the lithosphere that allows the tectonic plates to move over it. The asthenosphere is responsible for the movement of the Earth's crustal plates.
Yes. Tectonic plates are in fact mostly solid.
The lithosphere, which includes the uppermost portion of the mantle, forms the solid tectonic plates along with the crust. This layer is divided into massive plates that float on the semi-fluid asthenosphere beneath them.
The lithosphere is the layer along the crust that forms the solid tectonic plates. It consists of the crust and the upper part of the mantle and is broken into several pieces that move and interact with each other due to tectonic forces.
The layer that fits this description is the lithosphere. The lithosphere is comprised of the uppermost part of the mantle and the crust, and it is broken into tectonic plates that move on the Earth's surface.
The lithosphere (which is composed of the crust and solid brittle upper mantle) makes up the Earth's tectonic plates.
the answer is the solid , but plastic layer found in the upper mantle ................hope this helps bye bye .
The lithosphere, which includes the rigid outermost layer of the Earth's mantle, is responsible for the movement and formation of tectonic plates. These plates float on the semi-fluid asthenosphere below and interact with each other at plate boundaries, leading to processes like subduction and spreading.
The plastic solid layer of slowly flowing rock within the Earth is known as the asthenosphere. Located beneath the rigid lithosphere, the asthenosphere allows for the movement of tectonic plates due to its semi-fluid properties. This layer plays a crucial role in geological processes, such as plate tectonics and volcanic activity, contributing to the dynamic nature of the Earth's surface.