The primeval supercontinent that split into Gondwanaland and Laurasia between 250 and 300 million years ago is known as Pangaea. Pangaea was a massive landmass that existed during the late Paleozoic and early Mesozoic eras, before it began to break apart due to the movement of tectonic plates.
During the breakup of Pangaea, two new supercontinents emerged: Gondwanaland, which consisted of the southern landmasses including South America, Africa, Antarctica, Australia, and the Indian subcontinent, and Laurasia, which comprised the northern landmasses such as North America, Europe, and Asia.
This separation of Pangaea had a significant impact on the Earth's geology and climate, leading to the formation of new oceans and mountain ranges, as well as changes in plant and animal life. The split of Pangaea also played a crucial role in shaping the continents as we know them today.
The process of continental drift and the breakup of Pangaea are essential concepts in the field of plate tectonics, which studies the movement and interactions of the Earth's lithosphere. Understanding the history of Pangaea helps scientists to piece together the puzzle of how the Earth's landmasses have shifted and changed over millions of years.
In conclusion, Pangaea was the primeval supercontinent that split into Gondwanaland and Laurasia between 250 and 300 million years ago, setting the stage for the formation of the continents as we see them today. The breakup of Pangaea had a profound impact on the Earth's geology and climate, shaping the planet's landscapes and ecosystems in ways that continue to influence our world to this day.
7000
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