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Kanjonska dolina reke Rakitnice je ena izmed najglobljih in najdaljsih na Dinarskem krasu. Prispevek obravnava osnovne morfoloske in morfostrukturne znacilnosti kanjonske doline in njeno geomorfolosko regionalizacijo. Poudarjena je zlasti mocna povezava med litologijo, tektoniko in reliefom, saj so znatno vlogo pri razvoju te reliefne oblike odigrali zlasti neotektonski procesi v kvartarju. The canyon valley of the Rakitnica river is one of the deepest and longest in the Dinaric karst. The paper states the basic morphological and morphostructural characteristics of the canyon, and gives its geomorphological regionalization. High level of correlation between lithology, tectonics and relief of the researched area has been determined. Genesis and development of this relief form have been considerably guided by neotectonic processes during the Quaternary.

Basic Morphological and Morphostructural Characteristics of the Rakitnica Canyon (Dinaric Karst, Bosnia and Herzegovina)