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The peninsular plateau extends further east beyond the rajmahal hills to from meghalaya or the shillong plateau. Garo-rajmahal gap separates this plateau from the main block. The peninsular plateau in india formed due to gondwanaland’s tectonic shifts, resulting in a triangular plateau.
Extent and location: The plateau extends roughly from the south of the indo-gangetic plains to the southern tip of india at kanyakumari. It stretches from the aravalis in the northwest to the rajmahal … Since then, it has been gradually filled by the sediments brought by the himalayan and peninsular rivers. Average depth of alluvial deposits in these plains ranges from 1,000-2,000 m.
Average depth of alluvial deposits in these plains ranges from 1,000-2,000 m.