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  2. Pangaea - Wikipedia

    en.wikipedia.org/wiki/Pangaea

    Pangaea or Pangea (/ p æ n ˈ dʒ iː ə / 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 million years ago, and began to break apart about 200 million years ...

  3. Panthalassa - Wikipedia

    en.wikipedia.org/wiki/Panthalassa

    Because of the large size of Panthalassa, a hundred million years could separate the accretion of different groups of fusulines. Assuming a minimum accretion rate of 3 centimetres per year (1.2 in/year), the seamount chains on which those groups evolved would be separated by at least 3,000 km (1,900 mi).

  4. Laurasia - Wikipedia

    en.wikipedia.org/wiki/Laurasia

    They split in two groups, with one returning to Gondwana (and stayed there after Pangaea split) while the other staying in Laurasia (until further descendants switched to Gondwana starting from the Jurassic). In the early Eocene, a peak in global warming led to a pan-Arctic fauna with alligators and amphibians present north of the Arctic Circle.

  5. Geophysicists just debunked a key assumption about how ... - AOL

    www.aol.com/article/2016/07/25/geophysicists...

    Before it split into the continents we know today, Earth was home to just a single landmass, or "supercontinent," called Pangea. Over tens of millions of years, as the familiar story goes, these ...

  6. Gondwana - Wikipedia

    en.wikipedia.org/wiki/Gondwana

    Gondwana formed part of Pangaea for c. 150 Ma [31] 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 Paleo-Tethys oceans.

  7. 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 ]

  8. Geological history of North America - Wikipedia

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

    As the Triassic ended, Pangaea was breaking up into separate continents again. Rift valleys formed along the east coast as the North American, European and African plates diverged. [58] This process created rifts down the east coast to Florida. [47] One of these rift valleys was inundated with ocean water and became the young Atlantic Ocean.

  9. Rare rock structures could provide a glimpse into possible ...

    www.aol.com/rare-rock-structures-could-glimpse...

    This week, uncover a hidden lagoon filled with living fossils, wake up early with Neanderthals, peer inside an exploded star, and more.