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The term "Kerbtal" refers to a type of valley characterized by steep, knife-edge ridges and valley slopes that meet in a V-shape. This geomorphic feature develops in areas with rapid uplift and intense fluvial action, such as tropical mountains. The formation of Kerbtal valleys is influenced by groundwater flow and is a result of both modern and ancient geological processes. These valleys are distinct from glacially carved valleys, which often exhibit U-shaped cross profiles.12

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