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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

    Panthalassa, also known as the Panthalassic Ocean or Panthalassan Ocean (from Greek πᾶν "all" and θάλασσα "sea"), [1] was the vast superocean that encompassed planet Earth and surrounded the supercontinent Pangaea, the latest in a series of supercontinents in the history of Earth

  4. 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.

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

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

    Over tens of millions of years, as the familiar story goes, these giant hunks of rock slowly split apart, breaking up at a rate of just a millimeter — a little more than the thickness of a ...

  6. Tethys Ocean - Wikipedia

    en.wikipedia.org/wiki/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 (/ ˈ t iː θ ɪ s, ˈ t ɛ-/ TEETH-iss, TETH-; Greek: Τηθύς Tēthús), also called the Tethys Sea or the Neo-Tethys, was a prehistoric ocean during much of the Mesozoic Era and early-mid Cenozoic Era.

  7. Rodinia - Wikipedia

    en.wikipedia.org/wiki/Rodinia

    Rodinia (from the Russian родина, rodina, meaning "motherland, birthplace" [1] [2] [3]) was a Mesoproterozoic and Neoproterozoic supercontinent that assembled 1.26–0.90 billion years ago (Ga) [4] and broke up 750–633 million years ago (Ma). [5]

  8. Unknown God - Wikipedia

    en.wikipedia.org/wiki/Unknown_God

    The Unknown God or Agnostos Theos (Ancient Greek: Ἄγνωστος Θεός) is a theory by Eduard Norden first published in 1913 that proposes, based on the Christian Apostle Paul's Areopagus speech in Acts 17:23, that in addition to the twelve main gods and the innumerable lesser deities, ancient Greeks worshipped a deity they called "Agnostos Theos"; that is: "Unknown God", which Norden ...

  9. Classical Greece - Wikipedia

    en.wikipedia.org/wiki/Classical_Greece

    The Parthenon, in Athens, a temple to Athena. Classical Greece was a period of around 200 years (the 5th and 4th centuries BC) in Ancient Greece, [1] marked by much of the eastern Aegean and northern regions of Greek culture (such as Ionia and Macedonia) gaining increased autonomy from the Persian Empire; the peak flourishing of democratic Athens; the First and Second Peloponnesian Wars; the ...