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Geomorfološka analiza Babnega polja
Guzelj, Sara (Author), Stepišnik, Uroš (Mentor) More about this mentor... This link opens in a new window

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Abstract
Babno polje je najvišje ležeče polje Notranjskega podolja. Polje je na sredini zoženo in razdeljeno na manjši hrvaški in večji slovenski del. Glede na obliko, lego, gospodarsko izrabo in hidrološke razmere se močno loči od ostalih polj omenjenega podolja. Polje se raztega v značilni dinarski smeri ob Idrijskem prelomu, ki poteka preko polja. Dno polja na slovenski in hrvaški strani prekrivajo sedimenti. Vzpeti, robni del polja gradijo apnenci in dolomiti jurske in kredne starosti ter triasni dolomit. Babno polje še nikoli ni bilo predstavljeno v celoti iz geomorfološkega vidika. Za proučevano območje so bile narejene morfografska, morfometrična, morfogenetska in morfostrukturna analiza, pridobljeni podatki pa so bili digitalizirani. Stik dolomita in apnenca je vplival na razvoj kraških oblik (jama, vrtača) ter fluviokraških oblik (erozijski jarek, dolec, izvir, ponikev). V pokrajini so zaradi človekovih posegov, prisotne antropogene oblike (kanal za regulacijo struge).

Language:Slovenian
Keywords:Babno polje, Notranjsko podolje, kras, geomorfologija, kraško polje.
Work type:Bachelor thesis/paper (mb11)
Organization:FF - Faculty of Arts
Year:2020
Views:335
Downloads:185
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Secondary language

Language:English
Title:Geomorphological analysis of the Babno polje
Abstract:
The Babno Polje is the most highly lying field in set of Notranjsko podolje. Field is narrowed in the middle. It's distributed to smaller Croatian and larger Slovene field. In terms of its shape, location, economic use and hydrological conditions and the Babno polje significantly differs from other fields of the mentioned river basin. The Babno Polje has shaped in a typical Dinaric direction, along the Idrija Fault running across the field. The central part of Slovenian and Croatian field is covered by sediments. The higher, edge part of the field is made of limestone and dolomite from the Jurassic period and Cretaceous age and Triassic dolomite. An area is well soaked, which is quickening the geomorphological processes. The Babno polje has never been comprehensively presented from the geomorphologic perspectives. The morphological, morphometric, morphogenetic and morphostructural analyses has been done for the study area. Gained data were digitised. The contact of dolomite and limestone, have had an impact on the development of typical karst features (cave, doline) and fluviokarst land forms (erosion gullies, dell, spring, swallowholes). Due to human activities in the area, other anthropogenic forms are also present in Babno polje (channel for regulation of water).

Keywords:Babno polje, Notranjsko podolje, karst, geomorphology, karst field.

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