<?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-KYNKTD2J/5d8b5f9e-0fda-4bf6-936a-71189a342848/PDF"><dcterms:extent>32960 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:DOC-KYNKTD2J/4c467680-61c2-4ebc-9535-34496cc8749f/TEXT"><dcterms:extent>0 KB</dcterms:extent></edm:WebResource><edm:TimeSpan rdf:about="1974-2025"><edm:begin xml:lang="en">1974</edm:begin><edm:end xml:lang="en">2025</edm:end></edm:TimeSpan><edm:ProvidedCHO rdf:about="URN:NBN:SI:DOC-KYNKTD2J"><dcterms:isPartOf rdf:resource="https://www.dlib.si/details/URN:NBN:SI:spr-MWCGR4RQ" /><dcterms:issued>2025</dcterms:issued><dc:creator>Fayad, Noura Hamdy</dc:creator><dc:creator>Knez, Martin</dc:creator><dc:creator>Slabe, Tadej</dc:creator><dc:creator>Torab, Magdy</dc:creator><dc:format xml:lang="sl">številka:1</dc:format><dc:format xml:lang="sl">letnik:54</dc:format><dc:format xml:lang="sl">str. 11-37</dc:format><dc:identifier>ISSN:0583-6050</dc:identifier><dc:identifier>DOI:10.3986/ac.v54i1.14332</dc:identifier><dc:identifier>COBISSID_HOST:246889987</dc:identifier><dc:identifier>URN:URN:NBN:SI:doc-KYNKTD2J</dc:identifier><dc:language>en</dc:language><dc:publisher xml:lang="sl">Slovenska akademija znanosti in umetnosti</dc:publisher><dcterms:isPartOf xml:lang="sl">Acta carsologica</dcterms:isPartOf><dc:subject xml:lang="en">carbonate rocks</dc:subject><dc:subject xml:lang="en">complexometry</dc:subject><dc:subject xml:lang="sl">karbonatne kamnine</dc:subject><dc:subject xml:lang="sl">Keopsova piramida (Giza, Egipt)</dc:subject><dc:subject xml:lang="sl">kompleksometrija</dc:subject><dc:subject xml:lang="en">Pyramid of Cheops (Giza, Egypt)</dc:subject><dc:subject xml:lang="en">rock relief</dc:subject><dc:subject xml:lang="sl">skalni relief</dc:subject><dcterms:temporal rdf:resource="1974-2025" /><dc:title xml:lang="sl">Karst rock weathering of the Great Pyramid of Giza| Zakrasevanje Keopsove piramide|</dc:title><dc:description xml:lang="sl">The exposed stone blocks of soft carbonate rock, from which the pyramid is built, quickly develop a distinctive form and rock relief. The outer parts of the blocks are often undercut into overhangs. On their upper parts, a protective crust forms through rock dissolution and rapid recrystallization under the influence of occasional rain and seeping water, shielding the rock from wind erosion and dissolution. This crust, in turn, is dotted by small pits, whose bare surfaces remain exposed to wind erosion, allowing them to expand and grow deeper. In the lower sections, where the rock is fully exposed, wind erosion primarily carves out larger cups and channels. A thin crust may occasionally form over these sections, but tends to flake off quickly. This process suggests rapid karstification and the ongoing disintegration of the stone blocks</dc:description><dc:description xml:lang="sl">Izpostavljeni skalni bloki mehke karbonatne kamnine, iz katerih je piramida, razmeroma hitro pridobijo značilno obliko in skalni relief. Na zunanjih delih so bloki največkrat previsno spodjedeni. Njihov zgornji del, ki ga občasno dosegata dež in polzeča voda, prekriva skorja, ki nastane z raztapljanjem kamnine in hitro rekristalizacijo ter skalo ščiti pred vetrom in šibkim raztapljanjem. Razčlenjen je z vdolbinicami, katerih površina je pogosto gola in zato izpostavljena vetrni eroziji, kar omogoča njihovo rast. V spodnjem delu, kjer je skala gola, v večini primerov povsem prevladujejo skalne oblike, ki jih dolbe vetrna erozija, torej večje vdolbine in žlebovi. Tanka skorja, ki občasno prekrije njihovo površino, se hitro lušči. Sklepamo na hitro zakrasevanje in razpadanje skalnih blokov</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-KYNKTD2J"><edm:aggregatedCHO rdf:resource="URN:NBN:SI:DOC-KYNKTD2J" /><edm:isShownBy rdf:resource="http://www.dlib.si/stream/URN:NBN:SI:DOC-KYNKTD2J/5d8b5f9e-0fda-4bf6-936a-71189a342848/PDF" /><edm:rights rdf:resource="http://creativecommons.org/licenses/by/4.0/" /><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</edm:dataProvider><edm:object rdf:resource="http://www.dlib.si/streamdb/URN:NBN:SI:DOC-KYNKTD2J/maxi/edm" /><edm:isShownAt rdf:resource="http://www.dlib.si/details/URN:NBN:SI:DOC-KYNKTD2J" /></ore:Aggregation></rdf:RDF>