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Faculty of Architecture, Civil Engineering and Geodesy, University of Banja Luka , Banja Luka , Bosnia and Herzegovina
University of Banja Luka , Banja Luka , Bosnia and Herzegovina
University of Banja Luka , Banja Luka , Bosnia and Herzegovina
University of Banja Luka , Banja Luka , Bosnia and Herzegovina
The term "Durmitor flysch" was first introduced into the geological literature in 1948 by [1].. Under this term, he refers to a powerful geological formation, formed at the transition from the Upper Cretaceous to the Paleogene. Its distribution begins from the northern Albanian table and the so-called Cukali zone in the south, through the central part of Montenegro and northeastern Herzegovina, and extends to central Bosnia and Mount Vlašić [1]. It is named after the highly noticeable and extensive development of the southwest slopes of Mount Durmitor, while the best gradation of this formation and all modern geodynamic processes can be most clearly observed in the area of the Čemerno mountain pass in northeastern Herzegovina. The specific characteristics of this part of the Durmitor flysch complex will be the subject of this paper.
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