Steady state topography

Steady state topography refers to a theoretical state of landforms where the rate of erosion and the rate of uplift or sediment deposition are balanced over time. In this context, the landscape reaches a dynamic equilibrium such that the overall shape and characteristics of the topography remain relatively constant despite ongoing geological processes. In practice, steady state topography is achieved when the forces that shape the landscape (such as tectonic uplift, erosion by wind or water, and sediment transport) are in equilibrium.