By the late Paleozoic, continental collisions formed the supercontinent of Pangaea and resulted in some of the great mountain chains, including the Appalachians, Ural Mountains, and mountains of Tasmania.
Pada Paleozoikum akhir, tabrakan antar benua membentuk benua raksasa Pangaea dan menghasilkan berbagai rangkaian gunung besar, termasuk pegunungan Appalachia, pegunungan Ural, dan pegunungan Tasmania.WikiMatrix WikiMatrix