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  2. Gondwana - Wikipedia

    en.wikipedia.org/wiki/Gondwana

    Gondwana ( / ɡɒndˈwɑːnə /) [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. Gondwana was formed by the accretion of several cratons ...

  3. List of paleocontinents - Wikipedia

    en.wikipedia.org/wiki/List_of_paleocontinents

    Continent Fused with the Yangtze block to form the South China Craton during the Early Paleozoic. [11] Cimmeria: 300 Late Carboniferous–Early Permian Continent Rifted off margin of Gondwana, opening up Neotethys, collided with Laurasia about 150 Ma in the Cimmerian Orogeny. Regarded as being made up of many separate continental fragments. [12]

  4. Pangaea - Wikipedia

    en.wikipedia.org/wiki/Pangaea

    Pangaea. The supercontinent Pangaea in the early Mesozoic (at 200 Ma) 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 approximately 335 ...

  5. Laurasia - Wikipedia

    en.wikipedia.org/wiki/Laurasia

    The name is a portmanteau of Laurentia and Asia. [2] Laurentia, Avalonia, Baltica, and a series of smaller terranes, collided in the Caledonian orogeny c. 400 Ma to form Laurussia/Euramerica. Laurussia/Euramerica then collided with Gondwana to form Pangaea. Kazakhstania and Siberia were then added to Pangaea 290–300 Ma to form Laurasia.

  6. Natural history of Australia - Wikipedia

    en.wikipedia.org/wiki/Natural_history_of_Australia

    Australia was created by the junction of three early pieces of continental crust (cratons). Three areas of the Australian landmass that are made of Archaean rocks are more than 2.5 billion years old, among the oldest known rocks. These igneous and metamorphic rocks are found in the Yilgarn (West) and Pilbara (North) cratons in today's Western ...

  7. Karoo-Ferrar - Wikipedia

    en.wikipedia.org/wiki/Karoo-Ferrar

    The Karoo and Ferrar Large Igneous Provinces (LIPs) are two large igneous provinces in Southern Africa and Antarctica respectively, collectively known as the Karoo-Ferrar, Gondwana, [1] or Southeast African LIP, [2] associated with the initial break-up of the Gondwana supercontinent at c. 183 Ma. Its flood basalt mostly covers South Africa and ...

  8. Gondwana (India) - Wikipedia

    en.wikipedia.org/wiki/Gondwana_(India)

    Gondwana, also known as Gondaranya, the land of Gondwana, is a region of India named after the Gond people who live there (though they can also be found in other parts of India). The name of the ancient continent of Gondwanaland was derived from Gondwana, because some of the earliest rock formations of this continent were first investigated in ...

  9. Seychelles microcontinent - Wikipedia

    en.wikipedia.org/wiki/Seychelles_microcontinent

    The Gondwana supercontinent began to break up in the Middle Jurassic, about 167 million years ago. At that time, East Gondwana, comprising Antarctica, Madagascar, India, and Australia, began to separate from Africa. East Gondwana then began to separate about 115–120 million years ago when India began to move northward. [5]