Pangega

Pangaea, also spelled Pangea, was a supercontinent that existed during the late Paleozoic and early Mesozoic eras, approximately 335 to 175 million years ago. It was the first supercontinent to form after the breakup of the previous supercontinent, Rodinia. Pangaea was surrounded by the superocean Panthalassa, which covered most of the Earth's surface.

The formation of Pangaea began with the collision of the continents Laurasia and Gondwana around 300 million years ago. This collision resulted in the formation of the supercontinent, which was characterized by a single landmass and a single ocean. The interior of Pangaea was dominated by the vast interior seaway, known as the Tethys Sea, which separated the continents of Laurasia and Gondwana.

Pangaea began to break apart around 200 million years ago, leading to the formation of the modern continents. The breakup of Pangaea was a complex process that involved the opening of new ocean basins and the formation of new mountain ranges. The breakup of Pangaea is often associated with the Mesozoic era, which was marked by the rise of the dinosaurs and the formation of the Atlantic Ocean.

The breakup of Pangaea had a significant impact on the Earth's climate and the evolution of life. The opening of new ocean basins allowed for the exchange of water and nutrients between the oceans, which in turn influenced the global climate. The breakup of Pangaea also led to the formation of new mountain ranges, which influenced the distribution of plants and animals.

In summary, Pangaea was a supercontinent that existed during the late Paleozoic and early Mesozoic eras. Its formation and breakup had a significant impact on the Earth's climate and the evolution of life. The breakup of Pangaea led to the formation of the modern continents and the opening of new ocean basins.