it is located in the upper mantle.........
Tectonic plates that are located above mantle plumes are called hotspots. These hotspots are areas of volcanic activity that can create volcanic islands or seamounts as the tectonic plate moves over the stationary plume.
It is the mantle that is inferred to have convection currents that cause tectonic plates to move. Heat from the Earth's core creates these currents, which drive the movement of the rigid plates on the Earth's surface.
The upper mantle is a part of the Earth's mantle that is located just below the lithosphere. It plays a key role in the movement of tectonic plates that make up the lithosphere. Convection currents in the upper mantle drive the movement of tectonic plates, leading to processes such as plate tectonics, earthquakes, and volcanic activity.
No tectonic plates are in or even near the earth's core! The tectonic plates are fragments of the earth's crust. At subduction zones the edge of the subducting tectonic plate descends as much as a few hundred miles down into the earth's mantle before melting and becoming part of the mantle.
The asthenosphere is located in the upper part of the Earth's mantle, below the lithosphere. It is composed of partially molten rock that is ductile and flows slowly, allowing tectonic plates to move on top of it.
Tectonic plates that are located above mantle plumes are called hotspots. These hotspots are areas of volcanic activity that can create volcanic islands or seamounts as the tectonic plate moves over the stationary plume.
The solid portion of the upper mantle which behaves as a brittle solid is known as the lithospheric mantle. This part of the upper mantle along with the crust forms tectonic plates.
The lithosphere.
It is the mantle that is inferred to have convection currents that cause tectonic plates to move. Heat from the Earth's core creates these currents, which drive the movement of the rigid plates on the Earth's surface.
The upper mantle is a part of the Earth's mantle that is located just below the lithosphere. It plays a key role in the movement of tectonic plates that make up the lithosphere. Convection currents in the upper mantle drive the movement of tectonic plates, leading to processes such as plate tectonics, earthquakes, and volcanic activity.
No tectonic plates are in or even near the earth's core! The tectonic plates are fragments of the earth's crust. At subduction zones the edge of the subducting tectonic plate descends as much as a few hundred miles down into the earth's mantle before melting and becoming part of the mantle.
The upper level of the mantle is called the asthenosphere. It is a semi-fluid layer of the Earth's mantle located just below the lithosphere. The asthenosphere plays a key role in the movement of tectonic plates.
The asthenosphere is located in the upper mantle, just below the lithosphere. The lithosphere is the outermost layer of the Earth's crust that includes the rigid upper part of the mantle, while the asthenosphere is a semi-molten layer below the lithosphere that allows tectonic plates to move.
The asthenosphere is located in the upper part of the Earth's mantle, below the lithosphere. It is composed of partially molten rock that is ductile and flows slowly, allowing tectonic plates to move on top of it.
The lithosphere is the rigid outer layer of Earth made up of the crust and the upper part of the mantle. It is located on top of the asthenosphere, a partially molten layer of the mantle. The lithosphere is divided into large tectonic plates that move on the asthenosphere.
The plastic-like part of the mantle is known as the asthenosphere. It is a semi-fluid layer located beneath the lithosphere, composed of partially molten rock material that allows for the movement of tectonic plates.
The uppermost part of the mantle with liquid and plastic properties is called the asthenosphere. It is a semi-fluid layer located beneath the rigid lithosphere that allows for the movement of tectonic plates.