The lithospheric plates.
One example of a structure on Earth that moves on the asthenosphere is a tectonic plate. These plates are huge sections of Earth's lithosphere that float and move on the semi-fluid asthenosphere. The movement of these plates is responsible for phenomena such as earthquakes, volcanic activity, and the formation of mountains.
The tectonic plates are the structures that move on the asthenosphere. The plates are found on the lithosphere which lies over the asthenosphere.
Asthenosphere
Asthenosphere
The asthenosphere is located in the upper mantle. The asthenosphere is below the lithosphere, the brittle outer shell of the Earth.
The rigid layer of earth surrounding the asthenosphere is the lithosphere.
The tectonic plates are the structures that move on the asthenosphere. The plates are found on the lithosphere which lies over the asthenosphere.
The lithosphere over lies the asthenosphere and is broken up into discrete sections known as tectonic plates which move.
The asthenosphere.
Asthenosphere
Asthenosphere
asthenosphere
Asthenosphere
No. The asthenosphere is plastic in texture.
The asthenosphere is located in the upper mantle. The asthenosphere is below the lithosphere, the brittle outer shell of the Earth.
The asthenosphere is located in the upper mantle. The asthenosphere is below the lithosphere, the brittle outer shell of the Earth.
It is called the asthenosphere.
The grinding of tectonic plates. This caused by the outer core sending heat to the asthenosphere. The heat creates convection cells (aka convection currents), which move the asthenosphere. The tectonic, or lithospheric, plates are floating on the asthenosphere. When the asthenosphere moves, the tectonic plates move, and they gring together. The grinding will eventually cause a tectonic plate to fracture, which releases energy through the earth as seismic waves, and an earthquake occurs.