The geomorphic character of the Narmada Valley is defined by its unique topography and geological features. The valley is formed along a rift zone, characterized by a series of fault lines that have created deep, linear troughs. This allows the Narmada River to flow from east to west, which is unusual for Indian rivers. Surrounding the valley are the Vindhya and Satpura mountain ranges, providing a dramatic contrast in elevation. The valley is also marked by its varied landforms, including terraces, alluvial plains, and rugged hills. These geomorphic features play a crucial role in the region’s ecology and agriculture.