Why the Deccan Plateau Has Numerous Waterfalls

The Deccan Plateau's abundant waterfalls arise from a confluence of geological and climatic factors:

1. Elevation & Topography: Average 500–600 m elevation with rugged escarpments and valleys provides hydraulic head.
2. Monsoon Rainfall: Intense June–September rains generate high seasonal discharge.
3. Geology: Basalt (Deccan Traps), sandstone, limestone vary in erosion resistance, creating cliffs and ledges.
4. River Systems: Major rivers (Godavari, Krishna, Kaveri) cross elevation drops.
5. Faults & Rifts: Crustal weaknesses disrupt drainage, forming knickpoints.
6. Conservation: Protected areas preserve natural waterfall landscapes.

Together, these create ideal conditions for waterfall formation and persistence.