The continents formed at the break-up of Pannotia and Rodinia at the end of the Proterozoic slowly moved together again, forming the supercontinent Pangaea in the late Paleozoic.
The continents formed at the break-up of Pannotia and Rodinia at the end of the Proterozoic slowly moved together again during the Paleozoic. This eventually resulted in phases of mountain building that created the supercontinent Pangaea in the late Paleozoic.