Pangaea
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Pangaea or Pangea was a supercontinent that existed during the late Paleozoic and early Mesozoic eras. It assembled from the earlier continental units of Gondwana, Euramerica and Siberia during the Ca
The supercontinent Pangaea in the early Mesozoic (at 200 Ma)
Alfred Wegener c. 1924–1930
Appalachian orogeny
Fossil Dicroidium zuberi leaf from the Early Triassic of Argentina. Dicroidium was a ubiquitous tree across much of southern Pangaea during the Triassic period.
Gondwana
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Gondwana was a large landmass, sometimes referred to as a supercontinent. The remnants of Gondwana make up around two-thirds of today's continental area, including South America, Africa, Antarctica, A
Reconstruction showing final stages of assembly of Gondwana, 550 Mya
Geology of Asia 450.Ma
Geology of Asia 350Ma
Geology of Asia 300Ma