plate tectonic theory
The upper mantle is divided into two main sections: the lithosphere and the asthenosphere. The lithosphere is rigid and includes the crust, while the asthenosphere is a semi-fluid layer beneath the lithosphere where convection currents occur.
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.
The activity of the Earth's moving plates is called plate tectonics. It involves the movement and interaction of large sections of the Earth's lithosphere, resulting in phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges.
crust
plate tectionics theory......................:-)
plate tectonic theory
plate tectonic theory
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.
Plate tectonics
The upper mantle is divided into two main sections: the lithosphere and the asthenosphere. The lithosphere is rigid and includes the crust, while the asthenosphere is a semi-fluid layer beneath the lithosphere where convection currents occur.
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.
It is called plates.
These are known as tectonic plates.
Tectonic platea.
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.
The theory that Earth's crust is divided into sections that interact with each other over time is called plate tectonics. This theory explains how the Earth's lithosphere is divided into several large and small plates that float and move on the semi-fluid asthenosphere beneath them. The interactions between these plates cause phenomena such as earthquakes, volcanic eruptions, and mountain formation.