India became a part of Asia through geological processes and historical movements. The Indian subcontinent was once part of the ancient supercontinent Gondwana, which began to break apart around 180 million years ago. The Indian Plate then drifted northward, eventually colliding with the Eurasian Plate about 50 million years ago, leading to the formation of the Himalayas and integrating India into the Asian landmass. This tectonic activity shaped India's geography and positioned it as a significant part of Asia.
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