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Pangaea or Pangea (/ pænˈdʒiːə / pan-JEE-ə) [1] was a supercontinent that existed during the late Paleozoic and early Mesozoic eras. [2] It assembled from the earlier continental units of Gondwana, Euramerica and Siberia during the Carboniferous period approximately 335 million years ago, and began to break apart about 200 million years ...
Pangea, supercontinent that incorporated almost all of Earth's landmasses in early geologic time. Fully assembled by the Early Permian Epoch (some 299 million to about 273 million years ago), it began to break apart about 200 million years ago, eventually forming the modern continents and the Atlantic and Indian oceans.
Learn how Pangea, a single continent that existed 300-200 million years ago, broke apart to form the Atlantic Ocean and the continents we know today. Explore the geology, volcanism, and plate tectonics behind this epic event.
Pangea was a supercontinent that existed about 336 million years ago and broke up into the present-day continents. Learn about the origin, formation, and breakup of Pangea, as well as the ancient supercontinents that preceded it.
Learn how the supercontinent Pangaea was fragmented into current continents by plate movements. See the time sequence of maps and the history of continental drift theory.
Learn about Pangaea, the ancient supercontinent that existed 320 to 195 million years ago and how it formed and broke up due to plate tectonics. Discover the evidence for Pangaea's existence from fossils, coal deposits, magnetic minerals and more.
Pangaea was the global supercontinent that formed in the Palaeozoic era and broke up in the Mesozoic and Cenozoic eras. Learn about the formation, break-up and sources of Pangaea from this simple and concise article.
Pangaea was a hypothetical supercontinent that existed before plate tectonics broke it apart into the current continents. Learn about its formation, breakup, geography, and evidence from this online encyclopedia article.
Learn how scientists discovered the ancient supercontinent Pangaea and how plate tectonics broke it apart into the continents we know today. Explore the evidence from fossils, rocks, magnetic fields and seafloor spreading that reveals the history of Earth's crust.
Pangea was a supercontinent that existed during the late Paleozoic and early Mesozoic eras, incorporating nearly all of Earth's continents into a single, C-shaped landmass. The formation of Pangea was a gradual process of continental collision that took place over millions of years. It began to break apart approximately 200 million years ago, a process that resulted in the continental ...