20.500.12556/RUL-174340 Geomorfološko kartiranje kvartarnih pobočnih sedimentov na območju Skrilj v Vipavski dolini raziskovalna naloga Geomorphological mapping of quaternary slope deposits in Skrilj aren in Vipava valley research paper Raziskava obravnava geomorfološko kartiranje kvartarnih pobočnih sedimentov na območju Skrilj v Vipavski dolini. Namen naloge je bil preučiti prostorsko razporeditev sedimentov in geomorfoloških oblik ter ugotoviti povezave med litološko sestavo, tektonsko zgradbo in dinamiko pobočnih procesov. Metodološki pristop je vključeval pregled obstoječih geoloških in geomorfoloških študij, analizo lidar podatkov ter podrobno terensko kartiranje z digitalnimi orodji (FieldMove in QGIS). Na terenu so bile dokumentirane litostratigrafske enote (apnenec, fliš, grušč, karbonatna breča) ter prepoznane geomorfološke oblike, kot so kalciturbiditne megaplasti, melišča, plazovine in gravitacijski karbonatni bloki. Rezultati raziskave kažejo, da narivanje karbonatov na fliš ustvarja ostro litološko mejo, ki pogojuje premike sedimentov. Flišna podlaga deluje kot drsna ploskev, po kateri se premikajo gruščni nanosi in večji karbonatni bloki. Prepoznani so bili večfazni gravitacijski premiki, vključno z rotacijskimi in translacijskimi procesi, ki jih dodatno spodbuja kombinacija intenzivnega preperevanja in hidrogeološke razmere. Sklepna ugotovitev je, da je geomorfološka zgradba območja Skrilj rezultat tesne povezanosti tektonskih, litoloških in hidrogeoloških dejavnikov, ki skupaj oblikujejo kompleksno dinamiko kvartarnih pobočnih sedimentov. The study addresses the geomorphological mapping of Quaternary slope deposits in the Skrilje area of the Vipava Valley, SW Slovenia. The aim of the research was to examine the spatial distribution of sediments and geomorphological features, and to identify the relationships between lithological composition, tectonic structure, and slope dynamics. The methodological approach included a review of existing geological and geomorphological studies, analysis of lidar data, and detailed field mapping using digital tools (FieldMove and QGIS). Lithostratigraphic units (limestone, flysch, scree, and carbonate breccia) were documented in the field and geomorphological features such as calciturbidite megabeds, scree deposit (talus slopes), landslide deposits, and gravitational carbonate blocks were identified. The results show that the overthrust of carbonates onto flysch creates a distinct lithological boundary that controls sediment displacement. The flysch bedrock represents a sliding surface for scree accumulations and large carbonate blocks. Several phases of gravitational movements were recognized, including rotational and translational slides, further enhanced by intense weathering and hydrogeological conditions. The study concludes that the geomorphological structure of the Skrilje area is the result of a close interplay of tectonic, lithological, and hydrogeological factors, which together determine the complex dynamics of the Quaternary slope deposits. Vipavska dolina Skrilje geomorfološko kartiranje pobočni procesi Vipava Valley Skrilje geomorphological mapping slope processes true false false M. Kos Slovenski jezik Angleški jezik Zaključna naloga 2025-10-01 09:00:33 2025-10-01 09:00:37 2025-11-21 03:32:24 0000-00-00 00:00:00 2025 0 Ljubljana 0 Ljubljana X, 35 f. 0000-00-00 NiDoloceno NiDoloceno NiDoloceno 0000-00-00 0000-00-00 0000-00-00 55 109256 257746691 27981.pdf 27981.pdf 1 7EDFA316FCD6D80DA1BA0A3C6B2A6F9E aa01471ba7158c5dd4b6af7f324e7afc5bb333d5a9bb172075f2d421ed8a8478 217c5c25-9e94-11f0-9328-0050569b8976 https://repozitorij.uni-lj.si/Dokument.php?lang=slv&id=219130 27982.JPG 27982.JPG 1 C44EB454F9DD00EE9846E4A69D1FBDBE 281209a1a01a1105d282d8a02003a2cc628ce0c6ff41e2846c0e7f3b745aadeb 217cb6aa-9e94-11f0-9328-0050569b8976 https://repozitorij.uni-lj.si/Dokument.php?lang=slv&id=219131 Naravoslovnotehniška fakulteta 0 0 0