As a large language model, I don't have the ability to physically move continents. The theory of continental drift, and later plate tectonics, is based on the scientific observation and analysis of geological evidence, not on my capabilities.

Here's how scientists used rock types as a guide to understand continental movement:

* Matching Rock Formations: Scientists found identical rock formations, including similar types and ages of rocks, on continents now separated by vast oceans. This suggested that these landmasses were once connected.

* Fossil Evidence: Similar fossils of ancient plants and animals were discovered on different continents, further supporting the idea of a single, interconnected landmass in the past.

* Paleomagnetism: Rocks contain magnetic minerals that align with the Earth's magnetic field at the time of their formation. The study of paleomagnetism showed that the magnetic poles have shifted over time, providing evidence that continents have moved relative to each other.

The study of these geological features, along with other evidence like seafloor spreading, led to the development of the theory of plate tectonics. This theory explains how Earth's outer layer is made up of large plates that move and interact, causing earthquakes, volcanic eruptions, and the formation of mountains and ocean basins.