20.500.12556/RUL-174714 Geomorfološka analiza kanjona Socke Geomorphological analysis of Socka canyon Socka je manjše naselje v občini Vojnik, isto ime pa ima tudi globoko vrezana dolina reke Hudinje v Vitanjskih Karavankah. Območje spada med osamljeni kras, k enoti Paškokonjiškega krasa, kjer še kraške oblike niso bile podrobneje opisane. Namen diplomskega dela je bilo opraviti geomorfološko analizo kanjona Socke. Za dosego le tega smo opravili pregled strokovne literature o obravnavanem območju ter literature na temo krasa, s poudarkom na kanjonih in fluviokraških dolinah, izdelali geomorfološko karto na podlagi terenskega dela in dalje izvedli morfografsko, morfometrično, morfogenetsko ter morfostrukturno analizo in sintezo ugotovitev. Kanjon Socka spada med tipične kanjone, nastale s procesom antecedence. Na preučevanem območju se prepletata kraški in fluvialni relief. Kraško površje prevladuje, vendar se med seboj tudi razlikuje, saj so se razvili različni tipi krasa, in sicer globoki, plitvi in fluviokras. Na pobočjih se je razvil fluviokras, ki se mestoma prepleta z globokim krasom. Na posameznem tipu krasa so se razvile tipične kraške oblike, v največji meri pa so se razvili erozijski jarki. Socka is a smaller settlement in the municipality of Vojnik, sharing its name with deeply incised valley of the Hudinja river in the Vitanje Karavanke. The area is part of the isolated karst, belonging to the Paško-Konjiško karst unit, where karst landforms have not yet been described in detail. The aim of this thesis was to perform a geomorphological analysis of the Socka canyon. To achieve this, we reviewed the professional literature on the area in question and literature on karst, with a focus on canyons and fluviokarst valleys, created a geomorphological map based on fieldwork, and then conducted a morphographic, morphometric, morphogenetic, and morphostructural analysis and synthesis of results. The Socka canyon was identified as a typical canyon formed with antecedence. Within the study area, karst and fluvial relief is intertwined. Karst terrain is predominant, but it also varies, as different types of karst have developed, namely deep, shallow, and fluviokarst. On the slopes, fluviokarst has developed, which in some places intertwines with deep karst. Each type of karst is characterized by its typical karst landforms, with erosional gullies being the most common. osamljen kras geomorfološka analiza kraške reliefne oblike kanjon Socka isolated carst geomorphological analysis karst landforms Socka canyon true false false Slovenski jezik Angleški jezik Diplomsko delo/naloga 2025-10-09 07:18:45 2025-10-09 07:18:47 2025-11-27 03:55:50 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 599282 58753.pdf 58753.pdf 1 E8C42365B77FDDF6FDE11AE4C8494998 de5b046aade9733aa685f6f5db4639c1a3c6862ac8ad5d3df929f7291501089c 322de0d4-a4cf-11f0-9328-0050569b8976 https://repozitorij.uni-lj.si/Dokument.php?lang=slv&id=219590 Filozofska fakulteta 0 0 0