The statement that best describes how paleomagnetic evidence supports the theory of plate tectonics is:
"Paleomagnetic evidence reveals that the distribution of magnetic minerals in rocks on Earth's surface corresponds to the positions of tectonic plates, providing evidence for continental drift."
This statement accurately reflects how the patterns of magnetic minerals in rocks, which record the Earth's magnetic field at the time the rocks were formed, provide insight into the historical movement of tectonic plates.