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Continental drift

Adapted from Wikipedia · Explorer experience

An old illustration showing how the Atlantic Ocean formed over millions of years.

What Is Continental Drift?

Continental drift is a fun idea about how the Earth works. It tells us that the big continents we see today—like Africa and South America—move very slowly. They move so slowly that you can’t feel it happening! This movement takes millions and millions of years.

A Clever Idea

A long time ago, in the year 1596, a mapmaker named Abraham Ortelius noticed something cool. He saw that some continents looked like puzzle pieces that could fit together. Then, in 1912, a scientist named Alfred Wegener thought up the idea of continental drift. He guessed that all the continents were once stuck together in one big land called Pangaea. Later, they broke apart and moved to new places.

How Do We Know Now?

Today, scientists know that something deep inside the Earth helps move the continents. This idea is part of a bigger science called plate tectonics. It helps us learn many cool things about our planet.

Images

Illustration of Mesosaurus, an ancient aquatic reptile from the early Permian period found in South America and Africa.
Portrait of Alfred Wegener, the scientist who proposed the theory of continental drift.

Related articles

This article is a child-friendly adaptation of the Wikipedia article on Continental drift, available under CC BY-SA 4.0.

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