Final answer:
There are four types of evidence that support continental drift: fitting together of continents, matching fossils, matching mountain ranges, and paleoclimate evidence.
Step-by-step explanation:
There are four types of evidence that support continental drift:
- Fitting together of continents: The continents appear to fit together like pieces of a puzzle. For example, the eastern coast of South America fits perfectly into the western coast of Africa.
- Matching fossils: Fossils of the same plants and animals have been found on different continents that are now separated by oceans. This suggests that the continents were once connected.
- Matching mountain ranges: Mountain ranges on different continents, such as the Appalachian Mountains in North America and the Caledonian Mountains in Europe, have similar rock formations, indicating that they were once part of the same mountain range.
- Paleoclimate evidence: Evidence from ancient climates, such as the presence of glaciers in places like Africa and India, suggest that these areas were once located closer to the poles.