The Earth's lithosphere is broken into separate sections called plates. These plates float on the semi-fluid asthenosphere and move due to the heat-driven convection currents below them.
The layer of the Earth that is broken into separate sections called plates is the lithosphere. These plates move due to the flow of the underlying asthenosphere, causing phenomena like earthquakes and volcanic activity at plate boundaries.
The Earth's outer layer, or lithosphere, is broken into sections called tectonic plates. These plates float on top of the semi-fluid asthenosphere beneath them and interact with each other at plate boundaries, causing movements such as earthquakes and volcanic activity.
The idea that Earth's lithosphere is divided into large moving sections is called the theory of plate tectonics. This theory explains how the Earth's lithosphere is broken into several plates that shift and interact with each other, resulting in various geological phenomena like earthquakes, volcanoes, and mountain formation.
The large sections of lithosphere that float on the asthenosphere are called tectonic plates. These plates are rigid sections of Earth's lithosphere that move and interact with each other at plate boundaries, causing geological phenomena like earthquakes and volcanic eruptions.
It is called plates.
Tectonic platea.
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tectonic plates
The lithosphere is made up of the "upper mantle" and earth's crust.The lithosphere is broken into separate sections called plate tectonics or tectonic plates.
Earths lithosphere is made up of upper mantle. The earths lithosphere is broken into separate sections and it is called as tectonic plates or plate tectonics.
They are called plates!
Plate tectonics
Earth's crust and upper mantle are broken into sections called tectonic plates. These plates float on the semi-fluid asthenosphere below them and interact with each other at plate boundaries, leading to geological processes like earthquakes and volcanic activity.
tectonic plates or you could say plate tectonics
The Earth's lithosphere is broken into separate sections called plates. These plates float on the semi-fluid asthenosphere and move due to the heat-driven convection currents below them.
That would be the lithosphere. This is broken into sections known as lithospheric (or tectonic) plates.