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  2. Supercontinent - Wikipedia

    en.wikipedia.org/wiki/Supercontinent

    According to modern definitions, a supercontinent does not exist today; [1] the closest is the current Afro-Eurasian landmass, which covers approximately 57% of Earth's total land area. The last period in which the continental landmasses were near to one another was 336 to 175 million years ago, forming the supercontinent Pangaea .

  3. 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 ...

  4. Variscan orogeny - Wikipedia

    en.wikipedia.org/wiki/Variscan_orogeny

    Location of the Hercynian-Alleghenian mountain belts in the middle of the Carboniferous period.Present day coastlines are indicated in grey for reference. [1]The Variscan orogeny, or Hercynian orogeny, was a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea.

  5. Continental drift - Wikipedia

    en.wikipedia.org/wiki/Continental_drift

    He proposed that the continents had once formed a single landmass, called Pangaea, before breaking apart and drifting to their present locations. [32] Wegener was the first to use the phrase "continental drift" (1912, 1915) [5] [18] (German: "die Verschiebung der Kontinente") and to publish the hypothesis that the continents had somehow ...

  6. Argentina vs. Peru highlights: Lionel Messi's assist leads to ...

    www.aol.com/argentina-vs-peru-live-updates...

    The odds are stacked in Argentina’s favor for Tuesday’s match vs. Peru. Argentina is a -650 favorite to win, while Peru has +1600 odds in the match. A tie has +625 odds.

  7. Geology of the Pacific Ocean - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Pacific_Ocean

    Birth of the Pacific plate 180 million years ago. In the Early Jurassic, the supercontinent Pangaea was surrounded by the superocean Panthalassa, the ocean floor of which was composed of the Izanagi, Farallon, and Phoenix plates. [6]

  8. 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.

  9. Aurica (supercontinent) - Wikipedia

    en.wikipedia.org/wiki/Aurica_(supercontinent)

    It is one of the four proposed supercontinents that are speculated to form within 200 million years, the others being Pangaea Proxima, Amasia, and Novopangaea. The Aurica hypothesis was created by scholars at the Geological Magazine [ 1 ] following an American Geophysical Union study linking the strength of ocean tides to the supercontinent ...