20.500.12556/RUL-173478 Geomorfološke značilnosti in geodiverziteta Bele krajine Geomorphological characteristics and geodiversity of Bela krajina Območje preučevanja obsega uravnani nižinski del Bele krajine, ki ga na severu in zahodu omejujeta kraški planoti Gorjanci in Kočevski Rog, na jugu in vzhodu pa kanjon reke Kolpe. Namen magistrske naloge je opisati geomorfološke značilnosti in izračunati indeks geodiverzitete Bele krajine. Raziskava temelji na analizi literature in preteklih raziskav, ki so služile kot teoretska osnova. S prepletom kabinetnega in terenskega dela smo izvedli morfografsko in morfometrično analizo ter opisali značilne kraške pojave na proučevanem območju. Rezultati kažejo, da Belokranjski ravnik sestavljajo zelo raznolike kraške oblike, ki so posledica prepletanja tektonskih, litoloških in kraških procesov. Globoki kras se odraža z izrazito odsotnostjo površinskih voda in veliko gostoto vrtač, medtem ko plitvi kras zaznamujejo kanjoni in kraške kotline s površinsko vodo v dnu kotanj. Fluviokras se pojavlja tam, kjer so podlaga manj prepustne kamnine, kar omogoča nastanek stalnih ali občasnih vodotokov. Delo predstavlja pomemben prispevek k poznavanju kraških oblik na Belokranjskem ravniku in ponuja uporabno osnovo za nadaljnje geomorfološke, hidrološke in speleološke raziskave. The study area comprises the leveled lowland part of Bela krajina, bounded in the north and west by the karst plateaus of Gorjanci and Kočevski Rog, and in the south and east by the Kolpa River canyon. The aim of this master’s thesis is to describe the geomorphological characteristics and to calculate the geodiversity index of Bela krajina. The research is based on an analysis of the literature and previous studies, which served as the theoretical framework. By combining desk-based and fieldwork methods, a morphographic and morphometric analysis was carried out, along with a description of characteristic karst phenomena in the study area. The results show that the Bela krajina plain is composed of highly diverse karst forms, resulting from the interplay of tectonic, lithological, and karst processes. The deep karst is reflected in the pronounced absence of surface waters and a high density of dolines, whereas the shallow karst is characterized by canyons and karst depressions with surface water at their bottoms. Fluviokarst occurs where the substratum consists of less permeable rocks, which enable the formation of permanent or intermittent streams. This work represents an important contribution to the understanding of karst landforms in the Bela krajina plain and provides a useful basis for further geomorphological, hydrological, and speleological research. geomorfologija geodiverziteta kras kraški ravnik Bela krajina geomorphology geodiversity karst karst plain Bela Krajina true false false Slovenski jezik Angleški jezik Magistrsko delo/naloga 2025-09-18 07:15:15 2025-09-18 07:15:37 2025-11-09 03:57:25 0000-00-00 00:00:00 2025 0 0 0000-00-00 NiDoloceno NiDoloceno NiDoloceno 0000-00-00 0000-00-00 0000-00-00 1970-01-01 592055 57128.pdf 57128.pdf 1 D2825887F572AED7F363E5538CF7C3F4 dcd33cf31f74952070beaae8a906b236094b5df16f69051c052fba50dab07125 5a933a0b-944e-11f0-9328-0050569b8976 https://repozitorij.uni-lj.si/Dokument.php?lang=slv&id=217993 Filozofska fakulteta 0 0 0