Peninsular Rivers

The Narmada and Tapi are the two major west-flowing peninsular rivers. Unlike the perennial Himalayan rivers, they are rain-fed and experience significantly reduced flow channels during dry seasons.

The Godavari is the largest peninsular river system in India, stretching over 1,465 km. Because of its massive scale and religious importance, it is traditionally called the Dakshin Ganga or Vridha Ganga.

Narmada and Tapi flow through hard rock rift valleys, which limits their sediment load. Additionally, their high-velocity entry into the steep gradient of the Arabian Sea creates estuaries rather than deltas.

The Shivanasamudra Falls is formed by the Cauvery River in Karnataka and is home to one of India's oldest operational hydroelectric power stations, commissioned in 1902.

The Jog Falls is created by the Sharavati River dropping vertically from a height of 253 meters in the Western Ghats region of Shimoga district, Karnataka.

The Damodar River flows through a distinct structural rift valley formed by down-faulting along the Chota Nagpur Plateau margin, mirroring the structural setups of the Narmada and Tapi rift tracks.

The Pranhita River is the largest tributary of the Godavari River, formed by the structural convergence of the Wardha, Wainganga, and Penganga rivers, draining a massive interior section of Central India.

The Krishna Water Disputes Tribunal (KWDT) manages water allocations among the riparian states of Maharashtra, Karnataka, Telangana, and Andhra Pradesh.

The Amarkantak Plateau is a classic example of a radial drainage pattern. Rivers like the Narmada (flowing west), Son (flowing north), and Mahanadi/Johilla originate from a central high point and flow outward in divergent directions.

The Vedavati (also known as Hagari in its lower course) is a major tributary of the Tungabhadra River, which itself is the primary right-bank tributary of the Krishna river system.