{"?xml":{"@version":"1.0"},"edm:RDF":{"@xmlns:dc":"http://purl.org/dc/elements/1.1/","@xmlns:edm":"http://www.europeana.eu/schemas/edm/","@xmlns:wgs84_pos":"http://www.w3.org/2003/01/geo/wgs84_pos","@xmlns:foaf":"http://xmlns.com/foaf/0.1/","@xmlns:rdaGr2":"http://rdvocab.info/ElementsGr2","@xmlns:oai":"http://www.openarchives.org/OAI/2.0/","@xmlns:owl":"http://www.w3.org/2002/07/owl#","@xmlns:rdf":"http://www.w3.org/1999/02/22-rdf-syntax-ns#","@xmlns:ore":"http://www.openarchives.org/ore/terms/","@xmlns:skos":"http://www.w3.org/2004/02/skos/core#","@xmlns:dcterms":"http://purl.org/dc/terms/","edm:WebResource":[{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:DOC-H6YMPCTL/58aad8b3-3a34-4ab2-a8d6-125f4e8659ef/PDF","dcterms:extent":"21625 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:DOC-H6YMPCTL/3eeba967-dee2-44ca-891e-ab2d76c2891a/TEXT","dcterms:extent":"85 KB"}],"edm:TimeSpan":{"@rdf:about":"1974-2025","edm:begin":{"@xml:lang":"en","#text":"1974"},"edm:end":{"@xml:lang":"en","#text":"2025"}},"edm:ProvidedCHO":{"@rdf:about":"URN:NBN:SI:DOC-H6YMPCTL","dcterms:isPartOf":[{"@rdf:resource":"https://www.dlib.si/details/URN:NBN:SI:spr-MWCGR4RQ"},{"@xml:lang":"sl","#text":"Acta carsologica"}],"dcterms:issued":"1996","dc:creator":"Slabe, Tadej","dc:format":[{"@xml:lang":"sl","#text":"letnik:25"},{"@xml:lang":"sl","#text":"str. 391-434"}],"dc:identifier":["ISSN:0583-6050","COBISSID:4135725","URN:URN:NBN:SI:doc-H6YMPCTL"],"dc:language":"sl","dc:publisher":{"@xml:lang":"sl","#text":"Slovenska akademija znanosti in umetnosti"},"dc:subject":[{"@xml:lang":"sl","#text":"kras (geologija)"},{"@xml:lang":"sl","#text":"kraške jame"},{"@xml:lang":"en","#text":"List of caves in Slovenia"},{"@xml:lang":"sl","#text":"reke"},{"@xml:lang":"sl","#text":"speleogeneza"},{"@xml:lang":"sl","#text":"speleomorfologija"}],"dcterms:temporal":{"@rdf:resource":"1974-2025"},"dc:title":{"@xml:lang":"sl","#text":"Jamski skalni relief, ki ga dolbe vodni tok| Cave rocky relief hollowed out by a turbulent water flow|"},"dc:description":[{"@xml:lang":"sl","#text":"The most important factor that shapes the karst caverns is water flow that leaves important speleomorphological evidence on a cave rocky relief. The origin and development of most typical rocky features of a kind are presented. The study is completed by laboratory tests in plaster of Paris. Single rocky features compose a rocky relief which is typical of the passages shaped in different hydrological zones of karst"},{"@xml:lang":"sl","#text":"Najbolj izraziti dejavniki oblikovanja kraških votlin so vodni tokovi, ki zapuščajo speleomorfogenetsko pomembne sledi tudi v skalnem reliefu. Predstavljen je nastanek in razvoj najbolj značilnih tovrstnih skalnih oblik. Študij je dopolnjen z laboratorijskimi poskusi z mavcem. Posamezne skalne oblike so povezane v skalni relief, značilen za rove, ki se oblikujejo v različnih hidroloških conah krasa"}],"edm:type":"TEXT","dc:type":[{"@xml:lang":"sl","#text":"znanstveno časopisje"},{"@xml:lang":"en","#text":"journals"},{"@rdf:resource":"http://www.wikidata.org/entity/Q361785"}]},"ore:Aggregation":{"@rdf:about":"http://www.dlib.si/?URN=URN:NBN:SI:DOC-H6YMPCTL","edm:aggregatedCHO":{"@rdf:resource":"URN:NBN:SI:DOC-H6YMPCTL"},"edm:isShownBy":{"@rdf:resource":"http://www.dlib.si/stream/URN:NBN:SI:DOC-H6YMPCTL/58aad8b3-3a34-4ab2-a8d6-125f4e8659ef/PDF"},"edm:rights":{"@rdf:resource":"http://rightsstatements.org/vocab/InC/1.0/"},"edm:provider":"Slovenian National E-content Aggregator","edm:intermediateProvider":{"@xml:lang":"en","#text":"National and University Library of Slovenia"},"edm:dataProvider":{"@xml:lang":"sl","#text":"ZRC SAZU"},"edm:object":{"@rdf:resource":"http://www.dlib.si/streamdb/URN:NBN:SI:DOC-H6YMPCTL/maxi/edm"},"edm:isShownAt":{"@rdf:resource":"http://www.dlib.si/details/URN:NBN:SI:DOC-H6YMPCTL"}}}}