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  2. Pangaea - Wikipedia

    en.wikipedia.org/wiki/Pangaea

    Map of Earth around 85 million years ago, during the Late Cretaceous. The second major phase in the break-up of Pangaea began in the Early Cretaceous (150–140 Ma), when Gondwana separated into multiple continents (Africa, South America, India, Antarctica, and Australia).

  3. Gondwana - Wikipedia

    en.wikipedia.org/wiki/Gondwana

    Gondwana (/ ɡ ɒ n d ˈ w ɑː n ə /) [1] 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, Australia, Zealandia, Arabia, and the Indian Subcontinent.

  4. Central Pangean Mountains - Wikipedia

    en.wikipedia.org/wiki/Central_Pangean_Mountains

    Map of Earth during the Early Permian, around 285 million years ago, showing Central Pangean mountain range at equator. The Central Pangean Mountains were formed during the collision of Euramerica and northern Gondwana as part of the Variscan and Alleghanian orogenies, which began during the Carboniferous approximately 340 million years ago, and complete by the beginning of the Permian around ...

  5. Supercontinent - Wikipedia

    en.wikipedia.org/wiki/Supercontinent

    Pangaea's supercontinent cycle is a good example of the efficiency of using the presence or lack of these entities to record the development, tenure, and break-up of supercontinents. There is a sharp decrease in passive margins between 500 and 350 Ma during the timing of Pangaea's assembly.

  6. Laurasia - Wikipedia

    en.wikipedia.org/wiki/Laurasia

    Euramerica in the Devonian [citation needed] Map of Earth around 405 million years ago, during the Early Devonian, showing Euramerica (centre) and Gondwana (south and east) Laurentia remained almost static near the Equator throughout the early Palaeozoic, separated from Baltica by the up to 3,000 km (1,900 mi)-wide Iapetus Ocean . [ 20 ]

  7. File:Pangaea continents.svg - Wikipedia

    en.wikipedia.org/wiki/File:Pangaea_continents.svg

    Pangea map, with names of the continents. Image of pangaea made by en:User:Kieff. File: ... Geological history of North America;

  8. Opening of the North Atlantic Ocean - Wikipedia

    en.wikipedia.org/wiki/Opening_of_the_North...

    The opening of the North Atlantic Ocean is a geological event that has occurred over millions of years, during which the supercontinent Pangea broke up. As modern-day Europe (Eurasian Plate) and North America (North American Plate) separated during the final breakup of Pangea in the early Cenozoic Era, [1] they formed the North Atlantic Ocean.

  9. Paleocontinent - Wikipedia

    en.wikipedia.org/wiki/Paleocontinent

    The only land mass to not be a part of Pangea were the former North and South China plates, they created a much smaller land mass in the ocean. There was a massive ocean that encompassed the world called Panthalassa, because most of the continental crust was sutured together into one giant continent there was a giant ocean to match.