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Gondwana ( / ɡɒndˈwɑːnə /) [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. Gondwana was formed by the accretion of several cratons ...
The Gondwana Rainforests of Australia, ... the largest Gondwanan rainforest in Australia is located in Tasmania's Tarkine wilderness. The number of visitors to the ...
Gondwana, also known as Gondaranya, the land of Gondwana, is a region of India named after the Gondi people who live there (though they can also be found in other parts of India). The name of the ancient continent of Gondwanaland was derived from Gondwana, because some of the earliest rock formations of this continent were first investigated in ...
The Gondwana Kingdoms were the ruling kingdoms in the Gondwana region of India. The Gondwana region includes the core region of the eastern part of the Vidarbha of Maharashtra, Garha Kingdom, the parts of Madhya Pradesh immediately to the north of it, and parts of western Chhattisgarh. The wider region extends beyond these, also including parts ...
The name is a portmanteau of Laurentia and Asia. [2] Laurentia, Avalonia, Baltica, and a series of smaller terranes, collided in the Caledonian orogeny c. 400 Ma to form Laurussia/Euramerica. Laurussia/Euramerica then collided with Gondwana to form Pangaea. Kazakhstania and Siberia were then added to Pangaea 290–300 Ma to form Laurasia.
The southwestern sector (now South America) was located to the far south, with Brazil situated near the South Pole. The northwestern edge of Gondwana was an active margin for much of the Devonian, and saw the accretion of many smaller land masses and island arcs.
First phase of the Tethys Ocean's forming: the (first) Tethys Sea starts dividing Pangaea into two supercontinents, Laurasia and Gondwana.. The Tethys Ocean (/ ˈ t iː θ ɪ s, ˈ t ɛ-/ TEETH-iss, TETH-; Greek: Τηθύς Tēthús), also called the Tethys Sea or the Neo-Tethys, was a prehistoric ocean during much of the Mesozoic Era and early-mid Cenozoic Era.
In geology, a supercontinent is the assembly of most or all of Earth 's continental blocks or cratons to form a single large landmass. [1][2][3] However, some geologists use a different definition, "a grouping of formerly dispersed continents", which leaves room for interpretation and is easier to apply to Precambrian times. [4]