20.500.12556/RUL-115944 Geomorfološke značilnosti Dobrepolja in porečja Rašice Geomorphological Features of Dobrepolje and Rašica River Basin Namen zaključne seminarske naloge je geomorfološka analiza Dobrepolja in porečja Rašice. Za dosego namena so bili zastavljeni vmesni cilji, ki vključujejo pregled in proučitev literature, zamejitev območja, geomorfološko analizo, ki je vključevala morfografsko, morfometrično in morfostrukturno analizo. Končni cilj naloge je opredeljen kot morfogenetska interpretacija, ki je temeljila na analitskem delu raziskave ter na izbrani literaturi. Cilj, ki obsega geomorfološko analizo, je bil dosežen na podlagi kombinacije geomorfoloških analitskih metod. Glavni rezultati geomorfološke analize so morfografska, morfometrična in morfostrukturna analiza Dobrepolja in porečja Rašice. Glavni zaključek tega dela je, da na vzhodnem delu proučevanega območja prevladuje kraški genetski tip reliefa, na zahodnem delu proučevanega območja pa je oblikovan fluviokraški tip reliefa. Le na manjšem delu porečja Rašice se razvija fluvialni relief. Iz hidrološkega vidika Dobrepolje v svojem severnem delu deluje izrazito dvojno. Ob normalnih vodostajih namreč deluje kot suho kraško polje brez površinskih vodotokov, ob ekstremno visokih vodah pa deluje kot pritočno-ponorniško kraško polje. The purpose of this thesis is geomorphological analysis of Dobrepolje and the Rašica river basin. Intermediate goals include reviewing and examining the literature, delimiting the area and geomorphological analysis, which will include morphographic, morphometric, and morphostructural analysis. The final goal of the assignment is defined as a morphogenetic interpretation based on the analytical part of the research and the selected literature. The objective of geomorphological analysis was achieved based on a combination of geomorphological analytical methods. The main result of the geomorphological analysis are morphography, morphometry, and morphostructure of the Dobrepolje and Rašica river basin. The main conclusion of the thesis is that the eastern part of the studied area is dominated by the karst genetic type of relief, while in the western part of the studied area a fluviokarst relief type is formed. Only a small part of the Rašica river basin is formed by fluvial relief type. From the hydrological point of view, Dobrepolje shows hydrological duality in its northern part. At normal water levels, it acts as a dry karst field without surface watercourses. Only at extreme high waters it acts as a border karst field. kras kontaktni kras fluviokras kraško polje dolci karst contact karst fluviokarst karst field dells true false false Slovenski jezik Angleški jezik Diplomsko delo/naloga 2020-05-01 07:45:04 2020-05-01 07:45:08 2022-08-28 03:46:29 0000-00-00 00:00:00 2020 0 0 0000-00-00 NiDoloceno NiDoloceno NiDoloceno 0000-00-00 0000-00-00 0000-00-00 1970-01-01 453053 4333.pdf 4333.pdf 1 3FAE4130B994293AF0A3BC940839C723 6bc42823304f4c91e87b1f722b35a1e07bfbb1a31b0973273a9436c542b1c255 c7ba7385-a1b8-11eb-a523-00155dcfd717 https://repozitorij.uni-lj.si/Dokument.php?lang=slv&id=129327 Filozofska fakulteta 0 0 0