The southern part of Pangaea was called Gondwana. It was a supercontinent that existed during the late Paleozoic and Mesozoic eras, before breaking apart into the continents we recognize today.
The top part of Pangaea was called Laurasia. It comprised the northern portion of the supercontinent, while Gondwana made up the southern portion. Laurasia eventually split into North America, Europe, and Asia.
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.
The two continents that Pangaea separated into are Laurasia in the northern hemisphere and Gondwana in the southern hemisphere.
When all the continents were joined together as one supercontinent, it was called Pangaea.
When all continents were connected, they were part of the supercontinent called Pangaea. Pangaea existed during the late Paleozoic and early Mesozoic eras, before breaking apart into 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.
Gondwana
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.
Gondwana was a supercontinent that existed around 500 million years ago and included landmasses that would later split and form the continents we know today. Evidence for the Gondwana supercontinent includes geological similarities, rock formations, and fossil evidence found across separate continents. For instance, the fit of the continents along their coastlines, matching mountain ranges, and similar plant and animal species provide strong support for the theory. Additionally, the presence of unique flora and fauna on different continents that were once part of Gondwana further confirms this ancient landmass's existence.
Gondwana
Hypothesis sunken Between Continents
During the Triassic, there was one supercontinent called Pangaea. There was a large sea between what is now southern Asia and eastern Africa, called the Tethys. In the early Jurassic, however, Pangaea began to split into a northern and southern half, the former called Laurasia and the latter called Gondwana.
The theory of Pangaea is called the continental drift theory. It proposes that Earth's continents were once joined together in a single large landmass that later broke apart and drifted into their current positions.
Antartica was located at the southernmost part of Gondwana. Gondwana was the southern landmass of Pangaea. It consisted of the modern day continents Africa, South America, Australia, India, Arabia, Antarctica, and the European Balkans.
africa
in Asia
The term "Pangaea" comes from the Greek words "pan" meaning "all" and "gaea" meaning "Earth." It is used to refer to the supercontinent that existed around 300 million years ago when all the landmasses were joined together.