Abstract
Karst in the research area is characterized by fluviokarst surface morphology with developed underground karst. Karstification here has been active for quite long period, with the geological and geomorphological evolution of the area in Neogene and Quaternary having biggest influence on its intensity and distribution.
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Temovski, M. (2016). General Conclusions. In: Evolution of Karst in the Lower Part of Crna Reka River Basin. Springer Theses. Springer, Cham. https://doi.org/10.1007/978-3-319-24547-8_7
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DOI: https://doi.org/10.1007/978-3-319-24547-8_7
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