Prilikom terenske nastave na Velebitu, na području Baških Oštarija, izmjereni su nagibi slojeva i azimuti tih slojeva. Područje Velebita dio je Jadranske karbonatne platforme koja je nastala početkom donje jure i postojala sve do kraja gornje krede kada je zbog tektonskih aktivnosti došlo do njezine dezintegracije. Za vrijeme njezina postojanja istaložio se veoma debeo sloj naslaga, ponajviše karbonatnog sastava. Na temelju izmjerenih nagiba slojeva, u radu se pokušala utvrditi prostorna ovisnost tih nagiba slojeva te na temelju dobivenih rezultata pokušalo se pojasniti te geološki interpretirati zašto prostorna ovisnost nije dokazana ili se pokazala izuzetno malih vrijednosti.

Abstract: During fieldwork at the Baške Oštarije location on the Velebit mountain, layer inclinations and their azimuths were measured. The Velebit area is the part of the Adriatic Carbonate Platform, which was created at the beginning of the Lower Jurassic and had existed until the end of the Upper Cretaceous. In the Upper Cretaceous, tectonic activities smashed the Adriatic Carbonate Platform. During its existence, a very thick layer of sediments was deposited, mostly of carbonate structure. Based on the measured layers’ slope, this thesis is trying to define spatial dependence of those layers’ inclination. On the basis of the results of the research, the thesis is trying to define and give a geological explanation as to why the spatial dependence has not been proven or has presented itself in very small values.