Application of Dimensionless Hypsometric Curves in Evaluation of Erosion and Sedimentation Areas in Baneh Watershed

Among the most important features of basins, which are very effective in the process of erosion, are physical properties. In this regard, elevation and topographic properties directly and indirectly influence the erosion process and affect other parameters such as climatic conditions of the basins (amount and type of precipitation) and soil that are very important in the state of erosion at the surface of basins. Therefore, for assessing the erosion and sedimentation status at the Baneh basin, the real and theoretical hypsometric tables and curves are calculated and displayed. According to them, we find that the Baneh basin, while undergoing erosion and sedimentation, is relatively further away from the state of equilibrium, and is younger.