The term "tectonic plate" refers to a large, rigid segment of the Earth's lithosphere, which is the outermost shell of the Earth. These plates are responsible for the movement and geological activity on the Earth's surface. Tectonic plates vary in size but can be enormous, covering vast areas of the Earth's surface. They float on the semi-fluid asthenosphere beneath them.
The theory of plate tectonics explains how these plates interact with each other. It suggests that the Earth's lithosphere is divided into several major plates and numerous smaller ones, and these plates are in constant motion. The interactions between tectonic plates give rise to various geological phenomena, such as earthquakes, volcanic eruptions, mountain formation, and the creation of ocean basins. The boundaries between these plates are where a lot of these geological activities occur, and they are classified into different types, including divergent boundaries (where plates move apart), convergent boundaries (where plates move toward each other), and transform boundaries (where plates slide past each other horizontally).
In essence, tectonic plates play a fundamental role in shaping the Earth's surface and are central to our understanding of Earth's geology and the processes that have shaped the planet over millions of years.
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