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The scarce knowledge of bedrock channel morphology has limited our understanding of landscape formation. Bedrock channel's morphology is controlled by various factors like sediment properties, climatic conditions, rock strength and local topography. In this study, laboratory scale experiments were conducted to understand the relationship between sediment feed rate and lateral erosion. We also implemented a numerical model and tested it for reproducing the experiments. The numerical modeldoi:10.2208/jscejam.72.i_527 fatcat:yaypmjyeyrhs7p75d3hvjepc5q