Matching Coastlines: The coastlines of certain continents, like Africa and South America, appear to fit together like pieces of a puzzle. This suggests that they were once connected before splitting apart.

Fossils: The presence of fossils of the same species on different continents indicates that these landmasses were once part of the same larger continent. For example, the fossil of the fern Glossopteris has been found in Africa, South America, Antarctica, India, and Australia, suggesting that these continents were all once connected as part of the supercontinent Gondwana.

Rock Formations: The discovery of similar rock formations on different continents provides further evidence of continental drift. For instance, the Karoo Basin in South Africa and the Paraná Basin in South America are both composed of similar rock sequences that were formed at the same time.

Magnetic Studies: Magnetic studies of the ocean floor have shown patterns of magnetic reversals that correspond to changes in the Earth's magnetic field. By analyzing these patterns, scientists have been able to determine the direction and rate at which the continents have moved over time.

Continental Reconstruction: By combining evidence from various sources, scientists have been able to reconstruct how the continents have moved over millions of years. These reconstructions show the progressive breakup of supercontinents like Pangea and Gondwana into the continents we see today.