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  2. Gondwana - Wikipedia

    en.wikipedia.org/wiki/Gondwana

    Gondwana and Laurasia formed the Pangaea supercontinent during the Carboniferous. Pangaea began to break up in the Mid-Jurassic when the Central Atlantic opened. [32] In the western end of Pangaea, the collision between Gondwana and Laurasia closed the Rheic and Palaeo-Tethys oceans.

  3. Pangaea - Wikipedia

    en.wikipedia.org/wiki/Pangaea

    Break-up of Gondwana 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).

  4. List of paleocontinents - Wikipedia

    en.wikipedia.org/wiki/List_of_paleocontinents

    Animation of the break-up of the supercontinent Pangaea and the subsequent drift of its constituents, from the Early Triassic to recent (250 Ma to 0).. This is a list of paleocontinents, significant landmasses that have been proposed to exist in the geological past.

  5. Scientists Have Miraculously Located the Lost Continent of ...

    www.aol.com/scientists-miraculously-located-lost...

    Argoland, once part of the ancient supercontinent Gondwana, was long thought to be lost. ... And as Argoland started breaking off from Australia and drifting north, the break-up got even messier.

  6. Per USA Today, Gondwana, a former supercontinent, broke off from the landmass of Pangea about 180 million years ago and included multiple other continents including South America, Africa ...

  7. Matching dinosaur footprints discovered an ocean apart - AOL

    www.aol.com/matching-dinosaur-footprints-found...

    Gondwana is a former supercontinent that broke off from the landmass of Pangea about 180 million years ago. It included South America, Africa, Australia and Antarctica.

  8. Supercontinent - Wikipedia

    en.wikipedia.org/wiki/Supercontinent

    A supercontinent cycle is the break-up of one supercontinent and the development of another, which takes place on a global scale. [4] Supercontinent cycles are not the same as the Wilson cycle, which is the opening and closing of an individual oceanic basin. The Wilson cycle rarely synchronizes with the timing of a supercontinent cycle. [1]

  9. Karoo-Ferrar - Wikipedia

    en.wikipedia.org/wiki/Karoo-Ferrar

    The Karoo and Ferrar large igneous provinces (LIPs), in Southern Africa and Antarctica respectively, collectively known as the Karoo-Ferrar, Gondwana, [1] or Southeast African LIP, [2] are associated with the initial break-up of the Gondwana supercontinent at c..