Pangaea and Continental Drift

Scrub through 240 million years of plate motion using local GPlates-derived reconstruction frames. Between scientific snapshots, the lesson blends nearby frames so the breakup of Pangaea feels smooth while keeping the big tectonic story clear.

240 million years ago Pangaea assembled
Most major landmasses are locked together in a single supercontinent. The Atlantic Ocean has not opened yet, and the southern continents still travel as a connected group.
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Use the slider or play button to follow the breakup of Pangaea from 240 million years ago to today.
Guided Timelapse 240 Ma
240 Ma Today

Concept 01

Pangaea was not permanent.

The supercontinent formed and later broke apart because tectonic plates keep moving. Continents are passengers on those plates, so the map of Earth changes over millions of years.

Concept 02

Oceans can open.

When crust stretches and splits, magma rises and forms new ocean floor. That is how the Atlantic opened between North America, Eurasia, South America, and Africa.

Concept 03

Continents can collide.

India did not stay isolated. It moved north and collided with Asia, helping raise the Himalayas. Continental drift is not just about breaking apart. It is also about crashing together.

Concept 04

The motion is still happening now.

The continents have not "arrived" forever. The Atlantic is still widening, Africa is moving north, and Australia continues drifting. Today's map is one frame in a much longer tectonic movie.

Evidence

Matching coastlines and rock layers

The fit between eastern South America and western Africa is not the only clue. Rock belts and mountain structures also line up across oceans when the continents are reassembled.

Evidence

Fossils on separate continents

Identical fossils of plants and animals appear on continents now far apart. That makes sense if those continents used to be connected and later drifted away from each other.

Evidence

Magnetic stripes on the seafloor

Ocean crust records Earth's magnetic field as it forms. Symmetrical magnetic stripes on either side of mid-ocean ridges helped confirm seafloor spreading and plate tectonics.