<?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-P37QPT2D/0d0bcdc2-c45b-4d58-af81-bfcf852e8e94/PDF"><dcterms:extent>1699 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:doc-P37QPT2D/3ebb3176-2930-427d-91e2-b18f56afd581/TEXT"><dcterms:extent>16 KB</dcterms:extent></edm:WebResource><edm:TimeSpan rdf:about="1954-2025"><edm:begin xml:lang="en">1954</edm:begin><edm:end xml:lang="en">2025</edm:end></edm:TimeSpan><edm:ProvidedCHO rdf:about="URN:NBN:SI:doc-P37QPT2D"><dcterms:isPartOf rdf:resource="https://www.dlib.si/details/URN:NBN:SI:spr-B4L2ESHC" /><dcterms:issued>2002</dcterms:issued><dc:creator>Ravbar, Nataša</dc:creator><dc:format xml:lang="sl">številka:4</dc:format><dc:format xml:lang="sl">letnik:49</dc:format><dc:format xml:lang="sl">str. 3-8</dc:format><dc:identifier>ISSN:0016-7274</dc:identifier><dc:identifier>COBISSID:20370274</dc:identifier><dc:identifier>URN:URN:NBN:SI:doc-P37QPT2D</dc:identifier><dc:language>sl</dc:language><dc:publisher xml:lang="sl">Zveza geografskih društev Slovenije</dc:publisher><dcterms:isPartOf xml:lang="sl">Geografski obzornik</dcterms:isPartOf><dc:subject xml:lang="sl">Kitajska</dc:subject><dc:subject xml:lang="sl">kras (geologija)</dc:subject><dc:subject xml:lang="sl">krasoslovje</dc:subject><dc:subject xml:lang="sl">kraški pojavi</dc:subject><dcterms:temporal rdf:resource="1954-2025" /><dc:title xml:lang="sl">Fengcong, fenglin in shilin|</dc:title><dc:description xml:lang="sl">Although karst researches in China are carried out separately from the karst-sciences of western countries, terms such as fengcong, fenglin and shilin are enforcing gradually into international and Slovene karst terminology. Instead of cone and tower karst Chinese karstologists distinguish two types of tower karst: fengcong and fenglin. Shilin is a type of the subjacent karst. Karren have been transformated into the high pillars and reshaped by rain corrosion. Among them there are deep vertical fractures and trenches</dc:description><dc:description xml:lang="sl">Čeprav se kraško raziskovanje na Kitajskem razvija ločeno od krasoslovja na Zahodu, se v mednarodni in slovenski kraški terminologiji postopoma uveljavljajo izrazi fengcong, fenglin, shilin in drugi. Namesto stolpastega in stožčastega krasa kitajski krasoslovci ločujejo dva tipa stolpastega krasa: fengcong in fenglin. Shilin pa označuje pokrajino večjih skalnih gmot, visokih 20 do 50 metrov, ki so tesno skupaj, a dajejo videz, kot da so samostoječe, ker so med njimi globoke vertikalne razpoke in jarki</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-P37QPT2D"><edm:aggregatedCHO rdf:resource="URN:NBN:SI:doc-P37QPT2D" /><edm:isShownBy rdf:resource="http://www.dlib.si/stream/URN:NBN:SI:doc-P37QPT2D/0d0bcdc2-c45b-4d58-af81-bfcf852e8e94/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">Zveza geografov Slovenije</edm:dataProvider><edm:object rdf:resource="http://www.dlib.si/streamdb/URN:NBN:SI:doc-P37QPT2D/maxi/edm" /><edm:isShownAt rdf:resource="http://www.dlib.si/details/URN:NBN:SI:doc-P37QPT2D" /></ore:Aggregation></rdf:RDF>