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How Tectonic Plates Move

Understand that convection currents in the molten mantle drive the movement of rigid tectonic plates; distinguish between convergent (collision/subduction), divergent (spreading ridges), and transform (sliding) plate boundaries; explain why volcanoes, earthquakes, and mountain chains cluster at boundaries; introduce the Wilson cycle of supercontinent assembly and breakup

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The lesson

You already know Earth has layers, and that heat keeps moving inside the mantle. That movement is called a convection current: hot rock rises, cools, and sinks back down in a slow loop. These currents drag the rigid plates riding on top of the mantle, which is why the plates never stop moving, even though you cannot feel it.

Where two plates meet, they move in one of three ways. At a divergent boundary, like the Mid-Atlantic Ridge, plates pull apart and new crust rises to fill the gap. At a convergent boundary, plates crash together, and one often slides under the other. At a transform boundary, like the San Andreas Fault, plates grind past each other sideways without creating or destroying crust.

Try it together

Where the Nazca Plate meets the South American Plate, the thinner ocean plate is forced underneath the thicker continental plate. This sinking process is called subduction, and it happens at a convergent boundary. It explains why the Andes Mountains keep rising, why earthquakes shake the region, and why volcanoes erupt there: the sinking plate melts deep underground, and the melted rock pushes back up.

One landmassPulls apartOcean growsPlates meetReunites
You learned about Pangaea, the ancient supercontinent. Plates gather into one landmass, split apart, spread into oceans, then collide and reunite, over and over. This repeating pattern is called the Wilson cycle.
Good to know

Volcanoes, earthquakes, and mountain ranges are not scattered randomly across the globe. They trace the edges of the plates, forming patterns like the Pacific Ring of Fire. A pattern on a hazard map is really a map of plate boundaries.

Mantle convection drives plates together, apart, or past each other at convergent, divergent, and transform boundaries, which is why quakes, volcanoes, and mountains trace patterns like the Ring of Fire.

Watch it

Where it sits

Where this leads

Jobs that lean on this skill. Follow one to see everything it is built on.

Then practise

8 questions wait behind this lesson, each with its answer explained. Every answer feeds the sky: stars light as they are learned, and dim when it is time to come back.

How Tectonic Plates Move · Science, ages 11 to 12 · LightMySky