Tectonic plates are large, rigid pieces of the Earth's lithosphere that float on the semi-fluid asthenosphere.
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Tectonic plate movement is responsible for various geological phenomena, including earthquakes, volcanic eruptions, and the formation of mountain ranges.
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These plates move slowly, driven by the movement of the molten rock beneath them.
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The theory of plate tectonics has helped scientists understand the distribution of earthquakes, volcanoes, and other geological features around the world.
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The movement of tectonic plates has played a crucial role in the evolution of the Earth's continents and oceans over millions of years.
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The theory of plate tectonics was first proposed in the early 20th century and has since become a fundamental concept in geology.
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The boundaries between tectonic plates are known as plate boundaries, and there are three main types: divergent, convergent, and transform boundaries.
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The study of tectonic plates continues to provide valuable insights into the dynamic processes shaping the Earth's surface and deep interior.
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