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  2. Pangaea Proxima - Wikipedia

    en.wikipedia.org/wiki/Pangaea_Proxima

    The formation of Pangaea Proxima will probably dramatically affect the environment. The collision of plates will result in mountain building, thereby shifting weather patterns. The sea level may drop because of increased glaciation. The rate of surface weathering may rise, increasing the rate at which organic material is buried. Pangaea Proxima ...

  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. 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.

  5. 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 cycle ...

  6. Chronology of continents - Wikipedia

    en.wikipedia.org/wiki/Chronology_of_continents

    Pangaea Proxima ~250 myf [3] Novopangaea ~250 myf [26] Aurica ~250 myf [26] Amasia ~250 myf [26] References This page was last edited on 17 December 2024, at 21: ...

  7. Central Pangean Mountains - Wikipedia

    en.wikipedia.org/wiki/Central_Pangean_Mountains

    Map of Earth during the Early Permian, around 285 million years ago, showing Central Pangean mountain range at equator. The Central Pangean Mountains were formed during the collision of Euramerica and northern Gondwana as part of the Variscan and Alleghanian orogenies, which began during the Carboniferous approximately 340 million years ago, and complete by the beginning of the Permian around ...

  8. Continental fragment - Wikipedia

    en.wikipedia.org/wiki/Continental_fragment

    Continental fragments and microcontinent crustal compositions are very similar to those of regular continental crust.The rifting process that caused the continental fragments to form most likely impacts their layers and overall thickness along with the addition of mafic intrusions to the crust.

  9. Timeline of the far future - Wikipedia

    en.wikipedia.org/wiki/Timeline_of_the_far_future

    According to the Pangaea Proxima model created by Christopher R. Scotese, a new subduction zone will open in the Atlantic Ocean, and the Americas will begin to converge back toward Africa. [58] [failed verification] Upper estimate for the lifespan of Saturn's rings in their current state. [68] 110 million