Gondwanaland was a supercontinent that existed around 510 to 180 million years ago and comprised what is now South America, Africa, Antarctica, India, and Australia. It covered an area of roughly 100 million square kilometers.
Pangaea broke into Gondwanaland and Laurasia.
The supercontinent Gondwanaland was named by the Austrian geologist Eduard Suess in 1885. He derived the name from the Gondwana region of central India, where rocks that were part of the ancient supercontinent were found.
When Pangaea split in two, there where two island landmasses. The Northern landmass was Laurasia. The Southern landmass was Gondwanaland.
Mountain Range, example is the Himalayas Mountains in ASIA, formed from collision of Indian with Asia during its northward migration from Gondwanaland.
Gondwanaland was a supercontinent that included what are now South America, Africa, the Arabian Peninsula, the Indian subcontinent, Madagascar, Australia, and Antarctica. These landmasses were joined together before breaking apart over millions of years to form the continents we know today.
Laurasia and Gondwanaland
The theory that Pangaea broke up into Laurasia and Gondwanaland was proposed by Alfred Wegener in the early 20th century as part of his theory of continental drift. Wegener suggested that these two supercontinents eventually drifted apart to form the continents we see today.
The five continents of Gondwanaland were Africa, South America, Antarctica, Australia, and the Indian subcontinent. These landmasses were part of the ancient supercontinent Gondwana before they eventually drifted apart to their current positions.
Then about 200 million years ago the land began to drift apart. It broke into two pieces, and scientists have called the continent in the north Laurasia and the continent in the south Gondwanaland. Gondwanaland included what we know as Antarctica, which was joined to South America, Africa, India, and Australia.The two large continents continued to break apart into the smaller continents that exist today. Scientists call this movement 'continental drift'
Gondwanaland includes continents such as South America, Africa, Antarctica, Australia, and the Indian subcontinent. Laurasia includes continents such as North America, Europe, and Asia.
The modern continents derived from Gondwanaland are South America, Africa, Antarctica, Australia, the Indian subcontinent, and the Arabian Peninsula. These landmasses were once part of the supercontinent Gondwana before they started drifting apart due to the movement of tectonic plates.
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.
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.
Pangea split into two continents: Laurasia and Gondwanaland.
Gondwanaland
Laurasia and Gondwanaland were part of the supercontinent Pangaea, which formed around 335 million years ago through the collision and joining of several smaller landmasses. As tectonic plates shifted and moved over millions of years, Laurasia drifted northward and Gondwanaland moved southwards to eventually break apart and form the continents we know today.