20.500.12556/RUL-151426 Geomorfološke značilnosti Čepovanskega dola Geomorphological characteristics of Čepovan dol Območje proučevanja obsega Čepovanski dol, ki je na zahodu omejen z Banjšicami, na vzhodu pa s Trnovskim gozdom in grebenom Skopce. Namen magistrske naloge je geomorfološka analiza Čepovanskega dola ter njegova morfogenetska in morfodinamična interpretacija. Raziskava je bila izvedena na podlagi podrobne analize domačih in tujih virov znanstvene ter strokovne literature, ki so služili kot teoretska osnova za izvedbo nadaljnje terenske analize in analiz sedimenta. V sklopu analiz sedimenta so bile izvedene granulometrična analiza, analiza rentgenske fluorescence in analiza rentgenske difrakcije. Razvoj Čepovanskega dola je potekal v treh fazah. Najprej je na jugu delovala korozijska uravnava v plitvem krasu, medtem ko je severni del deloval kot kopast kras. Na to območje je s severa vtekal vodotok, ki se je kasneje zaradi tektonskega dvigovanja območja, antecedentno vrezal in oblikoval kanjon. Na območju Grgarja, kjer je kanjon prečil flišne kamnine je nastala kraška kotlina. V zadnji fazi je po aktivaciji Idrijskega preloma prišlo do obglavitve vodotoka, Čepovanski dol je s tem postal hidrološko neaktiven. The study area comprises of Čepovan dol, a canyon, that is limited by the Banjšice Plateau to the west, and the Trnovo Forest and the Skopca ridge to the east. The aim of this master's thesis is the geomorphological analysis of Čepovanski dol and its morphogenetic and morphodynamic interpretation. The research conducted was founded on the detailed analysis of scientific and professional literature, serving as the theoretical basis for further field and sediment analysis. The sediment analysis included granulometric analysis, X-ray fluorescence analysis, and X-ray diffraction analysis. The development of Čepovan dol occurred in three phases. Initially, the southern part functioned as a corrosion plain in shallow karst, while the northern part was characterized by cone karst. From the north, a watercourse flowed into the area. Later, due to the tectonic uplift of the area, the watercourse antecedently carved and formed the canyon. A karst basin was formed in the Grgar area where the canyon cut through flysch rocks. After the activation of the Idrija Fault in the final phase the watercourse was beheaded, causing Čepovanski dol to become hydrologically inactive. geomorfologija Dinarski kras Čepovanski dol suh kanjon granulometrična analiza XRF XRD geomorphology Dinaric karst Čepovan dol dry canyon granulometric analysis XRF XRD true false false Slovenski jezik Angleški jezik Magistrsko delo/naloga 2023-10-05 15:59:31 2023-10-05 15:59:32 2023-10-07 03:40:32 0000-00-00 00:00:00 2023 0 0 0000-00-00 NiDoloceno NiDoloceno NiDoloceno 0000-00-00 0000-00-00 0000-00-00 1970-01-01 535147 31572.pdf 31572.pdf 1 F1D348394D596E18AD324C473139BB6F ef573acd7e56c1b2842ca0400ae4e8eb4db119efa5f2e61125118ac520815d95 69a362f4-6387-11ee-aa25-0050569b8976 https://repozitorij.uni-lj.si/Dokument.php?lang=slv&id=176404 Filozofska fakulteta 0 0 0