Pannotia

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A topic known well beyond its field, found in many languages.

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Pannotia (from Greek: pan-, "all", -nótos, "south"; meaning "all southern land"), also known as the Vendian supercontinent, Greater Gondwana, and the Pan-African supercontinent, is a proposed relatively short-lived Neoproterozoic supercontinent that may have formed at the end of the Precambrian during the Pan-African orogeny (650–500 Ma), during the Cryogenian period, and broke apart 560 Ma with the opening of the Iapetus Ocean, in the late Ediacaran and early Cambrian.

Excerpt from the Wikipedia article “Pannotia”, under the CC BY-SA 4.0 license. Read the article on Wikipedia

Image: Original uploader was Jcwf at nl.wikipedia, Public domain, via Wikimedia Commons.