Gondwana

Neoproterozoic to Cretaceous landmass

Gondwana ( gon-DWAHN-ə; Sanskrit: गोण्डवन, romanized: Gōṇḍavana, lit. 'forest of the Gonds', pronounced [goːɳɖɐʋɐnɐ]) 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. Gondwana was formed by the accretion of several cratons (large stable blocks of the Earth's crust), beginning c.

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