The evidence for continental drift includes:
1. Fossil Evidence: Similar fossils of plants and animals found on continents that are now separated by oceans suggest that these landmasses were once connected.
2. Rock and Mountain Evidence: Mountain ranges on different continents have similar rock formations and structures, indicating that they were once part of the same landmass.
3. Climate Evidence: Evidence of glaciers in regions that currently have a warm climate, such as glacial grooves in rocks in tropical areas, supports the theory of continental drift.
4. Puzzle-like Fit of Continents: The way continents like South America and Africa seem to fit together like pieces of a jigsaw puzzle provides further evidence for continental drift.