enow.com Web Search

Search results

  1. Results from the WOW.Com Content Network
  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. Madagascar plate - Wikipedia

    en.wikipedia.org/wiki/Madagascar_Plate

    The initiation of Gondwana breakup, and transform faulting along the Davie Fracture Zone, occurred in the Toarcian (about 182 million years ago) following the eruption of the Bouvet (Karoo) mantle plume. At this time East Gondwana, comprising the Antarctic, Madagascar, Indian, and Australian plates, began to separate from the African plate.

  4. Seychelles microcontinent - Wikipedia

    en.wikipedia.org/wiki/Seychelles_microcontinent

    The Gondwana supercontinent began to break up in the Middle Jurassic, about 167 million years ago. At that time, East Gondwana, comprising Antarctica, Madagascar, India, and Australia, began to separate from Africa. East Gondwana then began to separate about 115–120 million years ago when India began to move northward. [5]

  5. Karoo-Ferrar - Wikipedia

    en.wikipedia.org/wiki/Karoo-Ferrar

    Karoo-Ferrar formed just prior to the breakup of Gondwana in the Lower Jurassic epoch, about 183 million years ago; [4] this timing corresponds to the early Toarcian anoxic event and the Pliensbachian-Toarcian extinction. [5] It covered about 3 x 10 6 km 2. [6]

  6. East Gondwana - Wikipedia

    en.wikipedia.org/wiki/East_Gondwana

    The South Polar region of the Cretaceous comprised the continent of East Gondwana–modern day Australia, Zealandia, and Antarctica–a product of the break-up of Gondwana in the Cretaceous Period. The southern region, during this time, was much warmer than it is today, ranging from perhaps 4–8 °C (39–46 °F) in the latest Cretaceous ...

  7. Pangaea - Wikipedia

    en.wikipedia.org/wiki/Pangaea

    Pangaea is the most recent supercontinent reconstructed from the geologic record and therefore is by far the best understood. The formation of supercontinents and their breakup appears to be cyclical through Earth's history. There may have been several others before Pangaea.

  8. big.assets.huffingtonpost.com

    big.assets.huffingtonpost.com/athena/files/2025/...

    big.assets.huffingtonpost.com

  9. Pan-African orogeny - Wikipedia

    en.wikipedia.org/wiki/Pan-African_orogeny

    "A review of the evolution of the Mozambique Belt and implications for the amalgamation and dispersal of Rodinia and Gondwana". Proterozoic East Gondwana: supercontinent assembly and breakup. Geological Society. ISBN 1-86239-125-4. van Hinsbergen, D. J. J. (2011). The Formation and Evolution of Africa: A Synopsis of 3.8 Ga of Earth History ...