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Geomorfološke značilnosti območja Živega muzeja Krasa
ID Mahne, Jan (Author), ID Stepišnik, Uroš (Mentor) More about this mentor... This link opens in a new window, ID Breg Valjavec, Mateja (Co-mentor)

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Abstract
V diplomskem delu sem proučil in opisal geomorfološke značilnosti območja Živega muzeja Krasa, ki se razteza med Sežano, Lipico in slovensko-italijansko mejo. Za cilje sem si postavil pregled literature in kartografskega gradiva, zamejitev proučevanega območja, izvedbo morfografske analize in sintezo ugotovitev. Na celotnem območju, ki ga uvrščamo v matični Kras, se pojavljajo značilne kraške reliefne oblike, ki so posledica apnenčaste matične podlage, na katero ima bistven vpliv korozija padavinske vode. Prisotni so vsi trije značilni procesi, kjer je prevladujoč proces raztapljanje, vode se pretakajo pretežno v podzemlju, zato na površju ni vodotokov, akumulacija materiala pa je zanemarljiva. Osrednji rezultat diplomskega dela je morfografska karta, ki prikazuje prepoznane reliefne oblike na proučevanem območju. V sodelovanju z Osnovno šolo Sežana sem pripravil poučno ekskurzijo po delu območja, ki je z vidika kraških pojavov najbolj zanimiv.

Language:Slovenian
Keywords:Geomorfologija, kras, matični Kras, Živi muzej Krasa
Work type:Bachelor thesis/paper
Organization:FF - Faculty of Arts
Year:2023
PID:20.500.12556/RUL-149813 This link opens in a new window
Publication date in RUL:10.09.2023
Views:488
Downloads:56
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Secondary language

Language:English
Title:Geomorphological features of the living karst museum
Abstract:
In my thesis I studied and described the geomorphological characteristics of the area of the Living karst Museum, which stretches between Sežana, Lipica and the Slovenian-Italian border. My objectives were to review the literature and cartographic material, delineate the study area, carry out a morphographic analysis and synthesise the findings. The entire area classified as Karst of origin is characterised by distinctive karst landforms, which are the result of a limestone bedrock that has been significantly affected by corrosion from rainwater. All three characteristic processes are present, with dissolution being the dominant process, with water flowing mainly underground, so there are no surface watercourses and negligible accumulation of material. The main result of the thesis is a morphographic map showing the identified landforms in the study area. In cooperation with the Sežana Primary School, I organised an educational excursion to the part of the area that is the most interesting in terms of karst phenomena.

Keywords:Geomorphology, Karst, Karst of origin, Living karst Museum

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