Pangaea existed from about 250 to 175 million years ago.
The two landmasses that split from Pangaea are Laurasia and Gondwana. Laurasia eventually formed North America, Europe, and Asia, while Gondwana formed South America, Africa, Antarctica, Australia, and the Indian subcontinent.
Pangaea split into two main pieces: Laurasia in the north and Gondwana in the south. Over time, these landmasses further fragmented into the continents we recognize today.
Pangaea began to break apart around 175 million years ago during the Jurassic period. This breakup eventually led to the formation of two separate landmasses known as Laurasia (in the north) and Gondwana (in the south).
The two halves of Pangaea are Laurasia, which was located in the northern hemisphere, and Gondwana, which was located in the southern hemisphere. These two landmasses eventually broke apart to form the continents we know today.
When Pangaea split in two, there where two island landmasses. The Northern landmass was Laurasia. The Southern landmass was Gondwanaland.
The northern part of Pangaea was known as Laurasia. It formed from the breakup of the Pangea supercontinent during the Mesozoic era, about 200 million years ago. Laurasia eventually split into North America, Europe, and Asia.
One example is the landmasses that used to be part of Pangaea, which eventually split into the continents we have today. Another example is the landmasses of North America and Europe, which were once connected by the supercontinent Laurasia but separated due to continental drift.
When Pangaea first started to separate, two large landmasses formed: Laurasia in the north and Gondwana in the south.
The supercontinent Pangaea was formed about 335 million years ago and split into two large landmasses, Laurasia and Gondwana, around 180 million years ago. The modern countries we know today did not exist during Pangaea's time, as landmasses were still connected.
The single continent that split into two continents called Gondwana and Laurasia is Pangaea. Pangaea was a supercontinent that existed about 335-175 million years ago, before eventually breaking apart into these two landmasses which later drifted to form the continents we know today.
Pangaea split into two supercontinents, Laurasia and Gondwana, during the Mesozoic Era due to the movement of tectonic plates. The splitting process, called continental drift, was driven by the forces caused by mantle convection beneath the Earth's crust. Over millions of years, these forces gradually separated the landmasses that formed Pangaea.
One of the two supercontinents that Pangaea split into is Laurasia.