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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. Supercontinent - Wikipedia

    en.wikipedia.org/wiki/Supercontinent

    Pangaea's supercontinent cycle is a good example of the efficiency of using the presence or lack of these entities to record the development, tenure, and break-up of supercontinents. There is a sharp decrease in passive margins between 500 and 350 Ma during the timing of Pangaea's assembly.

  4. Newark Basin - Wikipedia

    en.wikipedia.org/wiki/Newark_Basin

    Approximately 220 million years ago, during the late Triassic Period, the supercontinent Pangaea began to break apart. The focus of the rifting began somewhere between where present-day eastern North America and north-western Africa were joined. As in all rifting environments, grabens formed. Many of these grabens were created, but for some of ...

  5. Paleocontinent - Wikipedia

    en.wikipedia.org/wiki/Paleocontinent

    Pangea broke apart after 70 million years. The supercontinent was torn apart through fragmentation, which is where parts of the main landmass would break off in stages. There were two main events that led to the dispersal of Pangea. The first was a passive rifting event that occurred in the Triassic period.

  6. 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 ...

  7. Supercontinent cycle - Wikipedia

    en.wikipedia.org/wiki/Supercontinent_cycle

    Map of Pangaea with modern continental outlines. The supercontinent cycle is the quasi-periodic aggregation and dispersal of Earth's continental crust.There are varying opinions as to whether the amount of continental crust is increasing, decreasing, or staying about the same, but it is agreed that the Earth's crust is constantly being reconfigured.

  8. Depiction of Jesus - Wikipedia

    en.wikipedia.org/wiki/Depiction_of_Jesus

    The face that Neave constructed suggested that Jesus would have had a broad face and large nose, and differed significantly from the traditional depictions of Jesus in renaissance art. [82] Additional information about Jesus' skin color and hair was provided by Mark Goodacre , a New Testament scholar and professor at Duke University.

  9. Geology of the Appalachians - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Appalachians

    Pangea began to break up about 220 million years ago, in the early Mesozoic (late Triassic period). As Pangea rifted apart a new passive tectonic margin was born, and the forces that created the Appalachian, Ouachita, and Marathon Mountains were stilled. Weathering and erosion prevailed, and the mountains began to wear away.