The region of India that is part of Gondwanaland primarily includes the southern states, particularly the Deccan Plateau, which encompasses parts of Karnataka, Andhra pradesh, Telangana, Tamil Nadu, and Maharashtra. This area features ancient geological formations that date back to the time when Gondwanaland existed. Additionally, the northeastern states, like Arunachal Pradesh and parts of Assam, also share geological ties to this ancient supercontinent.
India belonged to the southern part (Gondwanaland) of a super continent that once existed millions of years ago. India is called a subcontinent because it is separated from rest of asia by the Himalayas and the climate of India is also very different.
The peninsular plateau of India is considered part of Gondwanaland because it is composed of ancient crystalline rocks that are geologically similar to those found in other regions that were once part of this supercontinent. Gondwanaland included present-day continents such as Africa, South America, Australia, and Antarctica, and the geological features of the Indian plateau, including its age and rock formations, align with those found in these regions. Additionally, fossil evidence and the alignment of tectonic features support the idea of a shared geological history before the continents drifted apart. This connection highlights the ancient unity of landmasses and the subsequent geological evolution of the Indian subcontinent.
Yes. India was once part of the Gondwanaland which consisted of the whole of Africa. Throughout most of geologic time there were only two primordial continents: Laurasia in the north and Gondwanaland in the south, separated by the Sea of Tethys. Gondwanaland consisted of Africa, peninsular India, Australia, South America, Antarctica and Eurasian regions south of the Alpine-Himalayan chain. About 265 million years ago, this continental togetherness began to split. For 200 million years, India, Arabia, and Apulia (consisting of parts of Italy, the Balkan states, Greece, and Turkey) drifted across the ocean, and finally collided with the rest of Eurasia 65 million years ago. The collision uplifted the Alpine-Himalayan mountain ranges extending from Spain (the Pyrenees) and northwest Africa (the Atlas) along the northern margin of the Mediterranean Sea (the Alps, Carpathians) into southern Asia (the Himalayas) to reach Indonesia.
Sikkim is part of India.
the eastern part of india
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.
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GONDWANALAND
Australia is a continent in its own right. It was once part of the supercontinent Pangaea, which broke up into Laurasia and Gondwanaland. Australia was part of Gondwanaland.
India belonged to the southern part (Gondwanaland) of a super continent that once existed millions of years ago. India is called a subcontinent because it is separated from rest of asia by the Himalayas and the climate of India is also very different.
The continents of South America, Africa, Antarctica, Australia, the Indian subcontinent, and the Arabian Peninsula were all part of Gondwanaland. Today, these landmasses have drifted apart and now form separate continents.
Pangaea was the original super-continent which broke up into Gondwanaland and Laurasia. Gondwanaland consisted of present day Africa, Antarctica, Australia, India and South America and began to break up about 250 million years ago. Australia was completely free of the other land masses by 30 million years ago.
Australia was once part of a large landmass. That large landmass was called Gondwanaland. Australia broke apart from Gondwanaland over 65 million years ago.
India is known as the subcontinent. Many millions of years ago, after the super continent Gondwanaland broke up, India gradually moved north and crashed into Asia forming the Himalayan mountain range and became a part of Asia in the process.
Pangaea was the original super-continent which broke up into Gondwanaland and Laurasia. Gondwanaland consisted of present day Africa, Antarctica, Australia, India and South America.
After Pangaea, the supercontinent split into two main landmasses: Laurasia in the northern hemisphere and Gondwanaland in the southern hemisphere. Laurasia eventually broke up into North America, Europe, and Asia, while Gondwanaland split into South America, Africa, India, Antarctica, and Australia.
The peninsular plateau of India is considered part of Gondwanaland because it is composed of ancient crystalline rocks that are geologically similar to those found in other regions that were once part of this supercontinent. Gondwanaland included present-day continents such as Africa, South America, Australia, and Antarctica, and the geological features of the Indian plateau, including its age and rock formations, align with those found in these regions. Additionally, fossil evidence and the alignment of tectonic features support the idea of a shared geological history before the continents drifted apart. This connection highlights the ancient unity of landmasses and the subsequent geological evolution of the Indian subcontinent.