How do distinctive rock strata support the theory of the cotinital drift?

Distinctive rock strata provide crucial evidence for the theory of continental drift by showing similarities in geological formations across distant continents. For instance, identical sequences of rock layers and fossilized remains found in South America and Africa suggest that these landmasses were once connected. Additionally, similar age and composition of rocks across continents support the idea that they were part of a single supercontinent, Pangaea, before drifting apart. This geological continuity underscores the concept that continents have moved over geological time, aligning with the principles of continental drift.