The correct answer is "all of the above." Each of the listed options provides evidence for the theory of continental drift:
- Fossil evidence - Similar fossils found on different continents suggest that these landmasses were once joined.
- Glacial deposits - Glacial marks and deposits found in currently warm regions indicate that those continents were once located closer to the poles and connected.
- Match up of landforms, rocks, and other resources - Similar geological features and rock formations on different continents support the idea that they were once part of a single massive landmass.
Thus, "all of the above" is the best choice.