Glossopteris was a plant whose fossils have been found across South America, Africa, India, Antarctica, and Australia, suggesting that these continents were once connected as part of the supercontinent Gondwana. This supports the idea that these continents broke up around 180 million years ago during the Jurassic Period.
This suggests that these continents broke up around 200 million years ago during the Mesozoic era. This breakup eventually led to the formation of the Atlantic Ocean.
The two continents that formed when Pangaea broke apart are Laurasia in the north and Gondwana in the south. These two supercontinents eventually broke up further to form the continents we have today.
The single landmass before it broke apart into continents is known as Pangaea. This supercontinent existed during the late Paleozoic and early Mesozoic eras.
Before the continents broke apart, they were part of a single supercontinent called Pangaea. It is believed that Pangaea existed around 300 million years ago during the Paleozoic and Mesozoic eras.
No, Pangaea separated into two main supercontinents called Laurasia and Gondwana. These two supercontinents eventually broke apart to form the continents we have today.
This isn't the full answer sorry but The globetrotters plant
This isn't the full answer sorry but The globetrotters plant
This isn't the full answer sorry but The globetrotters plant
This isn't the full answer sorry but The globetrotters plant
The single mass which eventually broke into the continents is referred to as Pangaea.
When Pangaea broke apart we got continents which what we have today.
Pangea
No, they float on it.
Pangea
Pangea.
The two continents that formed when Pangaea broke apart are Laurasia in the north and Gondwana in the south. These two supercontinents eventually broke up further to form the continents we have today.
Continents and tectonic plates drifted to their present positions due to the process of plate tectonics. This movement is driven by the slow shifting of the Earth's lithosphere on the more fluid asthenosphere beneath it. The movement of these plates over millions of years has resulted in the present configuration of the continents and ocean basins.