How were the hill ranges in the peninsular plateau formed?

The hill ranges in the peninsular plateau were formed through various geological processes over millions of years. During the Precambrian period, intense volcanic activity and tectonic movements gave rise to huge lava flows, which formed several layers of solidified rocks. These rocks were then uplifted and folded due to the collision of the Indian and Eurasian plates, resulting in the formation of fold mountains such as the Western Ghats and the Eastern Ghats. Additionally, weathering and erosion by rivers played a significant role in shaping these hill ranges, carving out valleys and creating distinct features within the plateau. Overall, the formation of the hill ranges in the peninsular plateau is a complex combination of volcanic activity, tectonic movements, and the erosive forces of nature.
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