Gondwana was an ancient supercontinent that broke up about 180 million years ago. The continent eventually split into landmasses we recognize today: Africa, South America, Australia, Antarctica, the Indian subcontinent and the Arabian Peninsula.

Yes.. gondwana land broke into a number of pieces about 180 million years ago and formed landmasses which today ewe recognize as INDIA, AUSTRALIA, SOUTH AFRICA, SOUTH AMERICA and ANTARCTICA.

India and Australia during the Breaking of Gondwana Land

India and Australia were indeed part of a larger landmass known as Gondwana during the Mesozoic era, approximately 180 million years ago. Gondwana was a supercontinent that included present-day continents such as South America, Africa, Antarctica, India, and Australia.

Formation of Gondwana Land
Gondwana Land was formed through the amalgamation of several smaller landmasses. The breakup of the supercontinent Pangea led to the formation of two major landmasses - Laurasia in the north and Gondwana in the south. India and Australia were part of the Gondwana supercontinent.

India's Position within Gondwana
India was located on the eastern side of Gondwana, near the equator. It was primarily attached to Antarctica, Madagascar, and Australia. Over millions of years, the Indian subcontinent slowly drifted northward due to tectonic plate movements.

Breaking of Gondwana and Indian-Australian Separation
During the Late Jurassic and Early Cretaceous periods, Gondwana started to break apart. This breakup led to the separation of India from Australia and Antarctica, resulting in the opening of the Indian Ocean. The separation of India from Australia occurred around 136 million years ago.

Evidence of Indian-Australian Connection
Several lines of evidence support the connection between India and Australia during the Gondwana breakup:

1. Geological and paleontological similarities: Rocks and fossils found in India and Australia show remarkable similarities, suggesting a shared geological history.

2. Similarities in flora and fauna: The fossil record of plants and animals from both regions exhibits similarities, including certain species that were once widespread across Gondwana.

3. Geophysical studies: Geophysical data, such as magnetic anomalies and gravity surveys, provide evidence of the ancient connection between India and Australia.

4. Crustal fragments: The discovery of crustal fragments, known as ophiolites, in both India and Australia further supports their previous connection.

Conclusion
India and Australia were indeed part of the Gondwana supercontinent before its breakup. The separation of these landmasses resulted in the formation of the Indian Ocean and the Indian subcontinent's gradual northward drift. Geological, paleontological, and geophysical evidence strongly support the connection between India and Australia during the breaking of Gondwana Land.