Plate tectonics is the scientific theory that describes the large-scale motion of the Earth'slithosphere. The lithosphere is divided into several large and small tectonic plates that float on the semi-fluid asthenosphere beneath them. These plates are constantly moving, and interactions at their boundaries cause many geological phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges.
Key Concepts
Here are the key concepts that you should understand about plate tectonics:
Plate Boundaries: There are three main types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where plates move towards each other, and transform boundaries where plates slide past each other.
By mastering these key concepts and studying the driving forces behind plate tectonics, you will gain a solid understanding of this fundamental geological theory.
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