<?xml version="1.0"?><rdf: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-XN9TEZ1K/194e7246-a0d8-4b74-8abc-1f2f2dcd4f43/HTML"><dcterms:extent>96 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:doc-XN9TEZ1K/38970af0-c0e8-47a2-b8f5-f4a99b57ebeb/PDF"><dcterms:extent>566 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:doc-XN9TEZ1K/e4055eb9-a9b5-4a5f-ac76-a21470f4a108/TEXT"><dcterms:extent>67 KB</dcterms:extent></edm:WebResource><edm:TimeSpan rdf:about="1952-2002"><edm:begin xml:lang="en">1952</edm:begin><edm:end xml:lang="en">2002</edm:end></edm:TimeSpan><edm:ProvidedCHO rdf:about="URN:NBN:SI:doc-XN9TEZ1K"><dcterms:isPartOf rdf:resource="https://www.dlib.si/details/URN:NBN:SI:spr-TPZVJGGM" /><dcterms:issued>2001</dcterms:issued><dc:creator>Hrvatin, Mauro</dc:creator><dc:creator>Hrvatin, Mojca</dc:creator><dc:format xml:lang="sl">27 strani</dc:format><dc:format xml:lang="sl">številka:41</dc:format><dc:format xml:lang="sl">str. 91-117</dc:format><dc:identifier>ISSN:0373-4498</dc:identifier><dc:identifier>ISSN:1581-6613</dc:identifier><dc:identifier>COBISSID:19326509</dc:identifier><dc:identifier>URN:URN:NBN:SI:doc-XN9TEZ1K</dc:identifier><dc:language>en</dc:language><dc:publisher xml:lang="sl">Znanstvenoraziskovalni center SAZU, Geografski inštitut</dc:publisher><dcterms:isPartOf xml:lang="sl">Geografski zbornik</dcterms:isPartOf><dc:subject xml:lang="sl">Dinarski kras</dc:subject><dc:subject xml:lang="sl">Dobrepolje</dc:subject><dc:subject xml:lang="en">Dobrepolje Municipality</dc:subject><dc:subject xml:lang="sl">kras (geologija)</dc:subject><dc:subject xml:lang="sl">kraška polja</dc:subject><dc:subject xml:lang="sl">pokrajinska ekologija</dc:subject><dc:subject xml:lang="en">regional geography</dc:subject><dc:subject xml:lang="sl">regionalna geografija</dc:subject><dc:subject xml:lang="sl">Struge</dc:subject><dc:subject rdf:resource="http://www.wikidata.org/entity/Q817121" /><dcterms:temporal rdf:resource="1952-2002" /><dc:title xml:lang="sl">Ecological landscape units of the Dobrepolje-Struge karst| Naravne enote Dobrepoljsko-Struškega krasa|</dc:title><dc:description xml:lang="sl">Dobrepoljsko-Struško polje pada med tipična kraška polja Dinarskega krasa Slovenije. Močno razpotegnjeno v dinarski smeri lezi v globoki kotanji med Malo goro in Suho krajino. Dno Dobrepoljsko-Struškega polja, kraški ravnik v okolici Ponikev ter okoliška pobočja Male gore, Suhe krajine in Čušperške planote oblikujejo pokrajino, ki smo jo po osrednji reliefni enoti poimenovali Dobrepoljsko-Struški kras. Med naravnimi prvinami, ki sooblikujejo Dobrepoljsko-Struški kras, smo kot najbolj pomembne izpostavili kamnine, relief, prsti in rastje. Naravne prvine so med seboj tesno povezane in medsebojno odvisne. Najbolj tipične in najpomembnejše kombinacije posameznih kategorij naravnih prvin tvorijo naravne enote. Te smo poskušali ugotoviti s prekrivanjem posameznih vsebinskih slojev v okviru geografskega informacijskega sistema. Od 648 teoretično možnih kombinacij kategorij naravnih prvin, se jih dejansko pojavlja 19. Na temelju kriterijev tipičnosti in pomembnosti smo ugotovljene kombinacije kategorij združili v šest naravnih enot</dc:description><dc:description xml:lang="sl">The Dobrepolje-Struge polje is a typical karst polje of Slovenia's Dinaric karst region. Distinctly prolonged in the direction of the Dinaric Alps, it lies in a deep trough between the Mala gora and Suha krajina plateaus. The bottom of the Dobrepolje-Struge polje, the karst corrosion plain around Ponikve, and the neighbouring hillslopes of Mala gora, Suha krajina, and the Čušperk plateau comprise the Dobrepolje-Struge karst, so named after its central relief unit. Among the natural elements that form the Dobrepolje-Struge karst, rock, relief, soil, and vegetation were found to be of greatest importance. The natural elements of the Dobrepolje-Struge karst are closely connected and interdependent. The most typical and most significant combination of natural elements form ecological landscape units. We determined these units by overlapping content layers of rock, relief, soil and vegetation employing the Geographical Information System</dc:description><edm:type>TEXT</edm:type><dc:type xml:lang="sl">znanstveno časopisje</dc:type><dc:type xml:lang="en">journals</dc:type><dc:type rdf:resource="http://www.wikidata.org/entity/Q361785" /></edm:ProvidedCHO><ore:Aggregation rdf:about="http://www.dlib.si/?URN=URN:NBN:SI:doc-XN9TEZ1K"><edm:aggregatedCHO rdf:resource="URN:NBN:SI:doc-XN9TEZ1K" /><edm:isShownBy rdf:resource="http://www.dlib.si/stream/URN:NBN:SI:doc-XN9TEZ1K/38970af0-c0e8-47a2-b8f5-f4a99b57ebeb/PDF" /><edm:rights rdf:resource="http://rightsstatements.org/vocab/InC/1.0/" /><edm:provider>Slovenian National E-content Aggregator</edm:provider><edm:intermediateProvider xml:lang="en">National and University Library of Slovenia</edm:intermediateProvider><edm:dataProvider xml:lang="sl">ZRC SAZU, Geografski inštitut Antona Melika</edm:dataProvider><edm:object rdf:resource="http://www.dlib.si/streamdb/URN:NBN:SI:doc-XN9TEZ1K/maxi/edm" /><edm:isShownAt rdf:resource="http://www.dlib.si/details/URN:NBN:SI:doc-XN9TEZ1K" /></ore:Aggregation></rdf:RDF>