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Introduction to plate tectonics

Review your understanding of plate tectonics in this free article aligned to NGSS standards.

Key points:

  • Earth’s lithosphere, or outermost shell, is broken up into large pieces called tectonic plates.
  • These plates move slowly over the asthenosphere, a layer of softer rock below the lithosphere. On average, tectonic plates move a few centimeters per year.
  • The place where two plates meet is called a plate boundary. There are three main types of plate boundaries.
    • Divergent boundaries occur where two plates are moving away from each other. Along these boundaries, rift valleys and mid-ocean ridges are common.
    • Convergent boundaries occur where two plates are moving toward each other. Along these boundaries, mountains and trenches are common.
    • Transform boundaries occur where two plates are moving past each other. Along these boundaries, earthquakes are common.
  • Evidence for plate motion can be seen in various features on Earth. For example, some of the continents have complementary coastlines. This suggests that the continents were once joined together.
A map showing the boundaries of Earth’s major and minor tectonic plates. Image credit: U.S. Geological Survey on Wikimedia Commons, public domain.

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