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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. 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 ...

  4. Naming of the Americas - Wikipedia

    en.wikipedia.org/wiki/Naming_of_the_Americas

    The naming of the Americas, or America, occurred shortly after Christopher Columbus 's death in 1506. The earliest known use of the name America dates to April 25, 1507, when it was applied to what is now known as South America. [1] It is generally accepted that the name derives from Amerigo Vespucci, the Italian explorer, who explored the new ...

  5. 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]

  6. 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.

  7. Geological history of North America - Wikipedia

    en.wikipedia.org/wiki/Geological_history_of...

    Up to half of the continent's modern surface area may have been submerged by this sea. [72] This is called the Western Interior Seaway. [73] It covered the majority of states like Texas, New Mexico, Oklahoma, Colorado, Kansas, Nebraska, the Dakotas, and Wyoming. [74] The seafloor was smooth and probably never submerged by more than 600 feet of ...

  8. Supercontinent - Wikipedia

    en.wikipedia.org/wiki/Supercontinent

    In geology, a supercontinent is the assembly of most or all of Earth 's continental blocks or cratons to form a single large landmass. [1][2][3] However, some geologists use a different definition, "a grouping of formerly dispersed continents", which leaves room for interpretation and is easier to apply to Precambrian times. [4]

  9. Tethys Ocean - Wikipedia

    en.wikipedia.org/wiki/Tethys_Ocean

    Tethys Ocean. First phase of the Tethys Ocean's forming: the (first) Tethys Sea starts dividing Pangaea into two supercontinents, Laurasia and Gondwana. The Tethys Ocean (/ ˈtiːθɪs, ˈtɛ -/ TEETH-iss, TETH-; Greek: ΤηθύςTēthús), also called the Tethys Sea or the Neo-Tethys, was a prehistoric ocean during much of the Mesozoic Era and ...