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  2. A supercontinent cycle is the break-up of one supercontinent and the development of another, which takes place on a global scale. [4] Supercontinent cycles are not the same as the Wilson cycle, which is the opening and closing of an individual oceanic basin. The Wilson cycle rarely synchronizes with the timing of a supercontinent cycle. [1]

  3. Global view centered on North America. North America is the third largest continent, and is also a portion of the third largest supercontinent if North and South America are combined into the Americas and Africa, Europe, and Asia are considered to be part of one supercontinent called Afro-Eurasia.

  4. Jan 13, 2024 · Researchers don't know exactly how big Rodinia was, but North America was likely the core of the landmass, according to Smithsonian Ocean. The continents we know today were unrecognizable...

    • Patrick Pester
  5. Authors. William L. Newman. From about 300-200 million years ago (late Paleozoic Era until the very late Triassic), the continent we now know as North America was contiguous with Africa, South America, and Europe. They all existed as a single continent called Pangea.

  6. Pangea, supercontinent that incorporated almost all of Earth’s landmasses in early geologic time. Fully assembled by the Early Permian Epoch (some 299 million to about 273 million years ago), it began to break apart about 200 million years ago, eventually forming the modern continents and the Atlantic and Indian oceans.

    • The Editors of Encyclopaedia Britannica
    • Is North America a supercontinent?1
    • Is North America a supercontinent?2
    • Is North America a supercontinent?3
    • Is North America a supercontinent?4
    • Is North America a supercontinent?5
  7. Jan 11, 2017 · Scientists have even predicted the formation of the next supercontinent — an amalgam of North America and Asia, evocatively named Amasia — some 250 million years from now. WAITING FOR AMASIA...

  8. Apr 20, 2021 · North America broke away (and, soon thereafter, South America as well) from elevated tensile stress beneath Africa (Box 2), where mantle upwelling from the African LLSVP is located today and...

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