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This study utilizes GIS and digital elevation models (DEMs) to identify fluvial knickzones in mountain rivers of central Japan, focusing on stream gradients and their classification into local and trend types. The research reveals that knickzones are prevalent in steep upstream river segments, suggesting a hydraulic origin influenced by erosion and tectonic activity, while also noting the limited impact of regional lithology. The methodology provides a systematic approach for knickzone identification, enabl

Author

alejandra

Language

EN