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  2. Gondwana - Wikipedia

    en.wikipedia.org/wiki/Gondwana

    Gondwana (/ ɡ ɒ n d ˈ w ɑː n ə /) [1] was a large landmass, sometimes referred to as a supercontinent. The remnants of Gondwana make up around two-thirds of today's continental area, including South America, Africa, Antarctica, Australia, Zealandia, Arabia, and the Indian subcontinent.

  3. Geology of Bangladesh - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Bangladesh

    In the Permian period, Bangladesh was part of the supercontinent Gondwana. The existence of Gondwana was first theorized by Rupert Jones, a European coal mine operator who in 1829 published a hypothesis about coal fields beneath Bangladesh. Gondwana came into use in the 1870s, named after the Gond people.

  4. Indian subcontinent - Wikipedia

    en.wikipedia.org/wiki/Indian_subcontinent

    The Indian subcontinent was formerly part of Gondwana, a supercontinent formed during the late Neoproterozoic and early Paleozoic. [7] Gondwana began to break up during the Mesozoic, with Insular India separating from Antarctica 130–120 million years ago [36] and Madagascar around 90 million years ago, [37] during the Cretaceous.

  5. Rodinia - Wikipedia

    en.wikipedia.org/wiki/Rodinia

    The result was the formation of Gondwana. The Rodinia hypothesis assumes that rifting did not start everywhere simultaneously. Extensive lava flows and volcanic eruptions of Neoproterozoic age are found on most continents, evidence for large scale rifting about 750 Ma. [1]

  6. Actually, All Bees Come From an Ancient Supercontinent ... - AOL

    www.aol.com/lifestyle/actually-bees-come-ancient...

    A new study claims that the origin of bees is tens of millions of years older than previously believed.

  7. Pannotia - Wikipedia

    en.wikipedia.org/wiki/Pannotia

    Pannotia was centred on the South Pole, hence its name. Pannotia (from Greek: pan-, "all", -nótos, "south"; meaning "all southern land"), also known as the Vendian supercontinent, Greater Gondwana, and the Pan-African supercontinent, was a relatively short-lived Neoproterozoic supercontinent that formed at the end of the Precambrian during the Pan-African orogeny (650–500 Ma), during the ...

  8. Pan-African orogeny - Wikipedia

    en.wikipedia.org/wiki/Pan-African_orogeny

    Because the formation of Gondwana encompassed several continents and extended from the Neoproterozoic to the early Palaeozoic, Pan-African could no longer be considered a single orogeny, [4] but rather an orogenic cycle that included the opening and closing of several large oceans and the collisions of several continental blocks.

  9. Gondwana Kingdoms - Wikipedia

    en.wikipedia.org/wiki/Gondwana_Kingdoms

    The Gondwana Kingdoms were ruled by Rajgonds. The Rajgonds are the ruling class among the Gond. The Gond is the dominating Community in Gondwana region. The name Gondwana named after Gondi people. Gonds are followers of the nature-based religion Gondi Religion/Koyapunem. [1] Gondwana means "Country inhabited by Gonds".