How was the Peninsular Plateau formed?

The Peninsular Plateau, also known as the Deccan Plateau, was formed through a combination of geologic processes over millions of years. It mainly resulted from volcanic activity and tectonic forces. Around 65 million years ago, volcanic eruptions from the Deccan Traps deposited layers of lava and volcanic ash over a large area. As the lava cooled and solidified, it created a thick layer of basalt, forming the base of the plateau. Over time, tectonic forces pushed the Plateau upwards, creating a broad and elevated landmass. The region was also affected by weathering and erosion, which carved out valleys and caves, adding to the diverse topography of the plateau.

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