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  2. Supercontinent - Wikipedia

    en.wikipedia.org/wiki/Supercontinent

    Contributing to Pangaea's popularity in the classroom, its reconstruction is almost as simple as fitting together the present continents bordering the Atlantic ocean like puzzle pieces. [4] For the period before Pangaea, there are two contrasting models for supercontinent evolution through geological time.

  3. 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.

  4. Pangaea - Wikipedia

    en.wikipedia.org/wiki/Pangaea

    Map of Pangea around 250 million years ago, at the beginning of the Triassic. 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]

  5. Chronology of continents - Wikipedia

    en.wikipedia.org/wiki/Chronology_of_continents

    A continent is a large geographical region defined by the continental shelves and the cultures on the continent. [1] In the modern day, there are seven continents. However, there have been more continents throughout history. Vaalbara was the first supercontinent. [2] Europe is the newest continent. [3]

  6. Gondwana - Wikipedia

    en.wikipedia.org/wiki/Gondwana

    The continent of Gondwana was named by the Austrian scientist Eduard Suess, after the region in central India of the same name, which is derived from Sanskrit for "forest of the Gonds". [6] The name had been previously used in a geological context, first by H. B. Medlicott in 1872, [ 7 ] from which the Gondwana sedimentary sequences ( Permian ...

  7. List of paleocontinents - Wikipedia

    en.wikipedia.org/wiki/List_of_paleocontinents

    The degree of certainty to which the identified landmasses can be regarded as independent entities reduces as geologists look further back in time. The list includes cratons, supercratons, microcontinents, continents and supercontinents. For the Archean to Paleoproterozoic cores of most of the continents see also list of shields and cratons.

  8. Scientists Found Ancient Tectonic Plates in the Middle of ...

    www.aol.com/scientists-found-ancient-tectonic...

    The model displayed remnants of submerged plates located under oceans and in the middle of continents, which—according to our current understanding of the plate tectonic cycle—are all too far ...

  9. Geological history of Earth - Wikipedia

    en.wikipedia.org/wiki/Geological_history_of_Earth

    The Carboniferous was a time of active mountain building, as the supercontinent Pangea came together. The southern continents remained tied together in the supercontinent Gondwana, which collided with North America-Europe along the present line of eastern North America.

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