Final answer:
The new evidence for continental drift included fossil records, mountain ranges, and ocean currents.
Step-by-step explanation:
Wegener's theory of continental drift was initially met with skepticism, but it gained acceptance as scientists provided further evidence. The new evidence included:
- Fossil records: Matching fossils were found on continents that were separated by oceans, suggesting that the continents were once connected.
- Mountain ranges: Matching mountain ranges were found on continents that were separated by oceans, indicating that they were once part of the same landmass.
- Ocean currents: The patterns of ocean currents were consistent with the movement of continents, supporting the idea of continental drift.
These pieces of evidence played a crucial role in confirming Wegener's theory and paved the way for the development of the plate tectonics theory.