How do distinctive rock strata support the continental drift?

Distinctive rock strata provide evidence for continental drift by showing similar geological formations, ages, and fossil types across continents that are now widely separated. For instance, identical sedimentary layers and mountain ranges found on different continents suggest they were once connected. This correlation in rock strata supports the idea that continents have moved apart over time, consistent with the theory of plate tectonics. Additionally, matching fossil records in these strata reinforce the notion of a shared geological history.