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  2. 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]

  3. Pangaea - Wikipedia

    en.wikipedia.org/wiki/Pangaea

    The fourth-last supercontinent, called Columbia or Nuna, appears to have assembled in the period 2.0–1.8 billion years ago . [ 26 ] [ 27 ] Columbia/Nuna broke up, and the next supercontinent, Rodinia , formed from the accretion and assembly of its fragments.

  4. Supercontinent - Wikipedia

    en.wikipedia.org/wiki/Supercontinent

    The last period in which the continental landmasses were near to one another was 336 to 175 million years ago, forming the supercontinent Pangaea. The positions of continents have been accurately determined back to the early Jurassic , shortly before the breakup of Pangaea. [ 6 ]

  5. Last Glacial Period - Wikipedia

    en.wikipedia.org/wiki/Last_Glacial_Period

    A chronology of climatic events of importance for the Last Glacial Period, about the last 120,000 years The Last Glacial Period caused a much lower global sea level.. The Last Glacial Period (LGP), also known as the Last glacial cycle, occurred from the end of the Last Interglacial to the beginning of the Holocene, c. 115,000 – c. 11,700 years ago, and thus corresponds to most of the ...

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

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

    Apparently, Pangea broke apart at about the speed fingernails grow.

  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. Geological history of North America - Wikipedia

    en.wikipedia.org/wiki/Geological_history_of...

    The Cannonball Sea near Minot, North Dakota was the last of the North American interior. [136] Cenozoic marine invertebrates are best known from deposits near the coasts and tend to resemble modern forms. Solitary corals became common, but coral reefs formed only around the Gulf of Mexico. [137] Sharks were common during the Cenozoic. [138]

  9. Rodinia - Wikipedia

    en.wikipedia.org/wiki/Rodinia

    The rifting of the continents created new oceans and seafloor spreading, which produces warmer, ... This page was last edited on 2 December 2024, at 19:47 (UTC).