Laurasia oor Nederlands
Laurasia
en
A supercontinent including most of the landmasses which make up today's continents of the northern hemisphere.
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Laurazië
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At the end of the Carboniferous period (300 Ma), the Hercynian or Variscan orogeny, in which the supercontinent Pangaea formed from Gondwana and Laurasia, was ended.
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The second one was Laurasia, which included Europe, North America and Asia, except for India.
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Reno's team arrives in Laurasia six years after the 1949 team arrived, to find only a few survivors.
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The northern part was called Laurasia, whereas the southern part was called Gondwana.
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The Tethys Ocean formed between Laurasia (Eurasia and North America) and Gondwana (Africa, India, Antarctica, Australia and South America) when the supercontinent Pangea broke up during the Triassic (200 million years ago).
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In 1893, the Austrian geologist Eduard Suess proposed the theory that an ancient and extinct inland sea had once existed between Laurasia and the continents which formed Gondwana II.
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Laurasia finally divided into the continents after which it is named: Laurentia (now North America) and Eurasia (excluding the Indian subcontinent).
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As it moved north, the floor of the Paleo-Tethys subducted under Laurasia and Cimmeria eventually collided with Laurasia, first at its western end c. 220 Ma, and Paleo-Tethys began to disappear altogether, closing from west to east.
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The Cimmeridian Superterrane has accreted to Mega Laurasia, the oceanic crust of the Neotethys is subducted to the north along the Dras volcanic arc, the Shigatze Ocean opens as a consequence of back-arc spreading, India is separated from Africa and E. Gondwana and the Indian Ocean opens.
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