Final answer:
Glacial evidence, paleontological similarities, and magnetic reversals support the theory of plate tectonics and the existence of a super-continent.
Step-by-step explanation:
The three pieces of evidence supporting the theory that plates were once part of a super-continent are:
- Glacial evidence: Glacial striations and till, which are found across multiple continents, suggest that these land masses were once connected and covered by a single ice sheet.
- Paleontological similarities: Matching fossils and similar species found on different continents provide evidence that these land masses were once joined.
- Magnetic reversals: The pattern of magnetic reversals recorded in rocks on either side of mid-oceanic ridges supports the idea that these ridges were once part of a single land mass.