<P> Gondwana (/ ɡɒndˈwɑːnə /), or Gondwanaland, was a supercontinent that existed from the Neoproterozoic (about 550 million years ago) until the Carboniferous (about 320 million years ago). It was formed by the accretion of several cratons . Eventually, Gondwana became the largest piece of continental crust of the Paleozoic Era, covering an area of about 100,000,000 km (39,000,000 sq mi). During the Carboniferous, it merged with Euramerica to form a larger supercontinent called Pangaea . Gondwana (and Pangaea) gradually broke up during the Mesozoic Era . The remnants of Gondwana make up about two - thirds of today's continental area . </P> <P> The formation of Gondwana began c. 800 to 650 Ma with the East African Orogeny--the collision of India, Madagascar, and Sri Lanka with East Africa--and was completed c. 600 to 530 Ma with the overlapping Brasiliano and Kuunga orogenies--the collision of South America with Africa and the addition of Australia and Antarctica, respectively . </P> <P> The continent of Gondwana was named by Austrian scientist Eduard Suess, after the Gondwana region of central northern India which is derived from Sanskrit for "forest of the Gonds". The name had been previously used in a geological context, first by H.B. Medlicott in 1872, from which the Gondwana sedimentary sequences (Permian - Triassic) are also described . The term "Gondwanaland" is preferred by some scientists in order to make a clear distinction between the region and the supercontinent . </P>

Which continent of today were part of gondwana land