The continental drift theory came to fruition in 1912 by a man named Alfred Wegener, who was a geophysicist and meteorologist. The four pieces of evidence for the continental drift include continents fitting together like a puzzle, scattering ancient fossils, rocks, mountain ranges, and the old climatic zones' locations.
Fossils of remarkably similar plants and animals have been discovered on opposite sides of the Atlantic Ocean. The fossils look like one another, and it can be concluded that the organisms must have lived in close proximity to one another. Fossils have been uncovered where the animal or plant was fossilized, suggesting that these organisms could not withstand the current climate.
This scenario means that the continents must have once lived in different climates. This situation reinforces the notion that they were once in other locations. There are landforms on various continents that match one another.