Want this question answered?
Laurasia and Gondwanaland were two supercontinents that existed hundreds of millions of years ago. Laurasia was mainly located in the Northern Hemisphere and Gondwanaland in the Southern Hemisphere. The breakup of these supercontinents ultimately led to the formation of the modern continents we have today.
Laurasia and Gondwanaland formed during the late Carboniferous period, around 300 million years ago, through the breakup of the supercontinent Pangaea. Laurasia was located in the northern hemisphere, while Gondwanaland was in the southern hemisphere.
Gondwana included most of the landmasses in today's Southern Hemisphere, including Antarctica, South America, Africa, Madagascar, and the Australian continent. The Arabian Peninsula and the Indian Subcontinent, which have now moved entirely into the Northern Hemisphere, were also included.
Gondwanaland was a supercontinent that gradually broke apart due to the movement of tectonic plates, forming the continents we have today. Antarctica drifted towards its current location at the South Pole as the breakup occurred. Today, Antarctica is mostly covered by ice, making it one of the coldest and most isolated places on Earth.
The breakup of Pangaea, in other words - the current theory.
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 breakup of the continents was primarily caused by the movement of tectonic plates in the Earth's crust. This movement led to the gradual separation of landmasses over millions of years, creating the continents as we know them today. This process is known as plate tectonics.
After the breakup of the supercontinent Laurasia, the continents formed include North America, Europe, and Asia. These continents continue to drift and change in shape due to plate tectonics.
The continents began to separate around 200 million years ago during the breakup of the supercontinent Pangaea. This process led to the formation of the current continents and their modern configurations.
Continents have evolved over billions of years through the process of plate tectonics. This involves the movement and interaction of large sections of the Earth's lithosphere, resulting in the formation, breakup, and reformation of continents. The continents we see today have been shaped by processes such as subduction, seafloor spreading, and continental collisions.
Pangea split into two supercontinents, Laurasia and Gondwana. Laurasia includes the core of the North America, Asia (without India) and Europe (without the Balkans) Gondwana composed most of Africa, South America, Australia, India, Arabia, Antarctica and the Balkans.
One major geographic event that took place during the Mesozoic Era was the breakup of the supercontinent Pangaea. This breakup led to the separation of landmasses that eventually formed the continents we recognize today.