<?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-0I6ESB4T/6b830910-74de-4789-8d75-33e65887aa8c/HTML"><dcterms:extent>127 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:doc-0I6ESB4T/a9a7e424-b26e-42a0-b5ca-36ff461983ce/PDF"><dcterms:extent>2880 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:doc-0I6ESB4T/ca8a22fd-7ae8-496c-8244-24baba606e7c/TEXT"><dcterms:extent>86 KB</dcterms:extent></edm:WebResource><edm:TimeSpan rdf:about="2003-2025"><edm:begin xml:lang="en">2003</edm:begin><edm:end xml:lang="en">2025</edm:end></edm:TimeSpan><edm:ProvidedCHO rdf:about="URN:NBN:SI:doc-0I6ESB4T"><dcterms:isPartOf rdf:resource="https://www.dlib.si/details/URN:NBN:SI:spr-EEHMIXWQ" /><dcterms:issued>2007</dcterms:issued><dc:creator>Komac, Blaž</dc:creator><dc:creator>Zorn, Matija</dc:creator><dc:format xml:lang="sl">številka:2</dc:format><dc:format xml:lang="sl">letnik:47</dc:format><dc:format xml:lang="sl">str. 139-169</dc:format><dc:identifier>ISSN:1581-6613</dc:identifier><dc:identifier>COBISSID:27574317</dc:identifier><dc:identifier>URN:URN:NBN:SI:doc-0I6ESB4T</dc:identifier><dc:language>en</dc:language><dc:language>sl</dc:language><dc:publisher xml:lang="sl">Slovenska akademija znanosti in umetnosti</dc:publisher><dc:publisher xml:lang="sl">Založba ZRC</dc:publisher><dcterms:isPartOf xml:lang="sl">Acta geographica Slovenica</dcterms:isPartOf><dc:subject xml:lang="sl">geomorfologija</dc:subject><dc:subject xml:lang="en">geomorphology</dc:subject><dc:subject xml:lang="sl">kartografija</dc:subject><dc:subject xml:lang="sl">metodologija</dc:subject><dc:subject xml:lang="sl">modeliranje</dc:subject><dc:subject xml:lang="sl">ogroženost</dc:subject><dc:subject xml:lang="sl">podori</dc:subject><dc:subject xml:lang="sl">relief</dc:subject><dc:subject xml:lang="en">Slovenia</dc:subject><dc:subject xml:lang="sl">Slovenija</dc:subject><dc:subject xml:lang="en">topography</dc:subject><dc:subject xml:lang="sl">zemeljski plazovi</dc:subject><dc:subject rdf:resource="http://www.wikidata.org/entity/Q52109" /><dcterms:temporal rdf:resource="2003-2025" /><dc:title xml:lang="sl">Probability modelling of landslide hazard| Probabilistično modeliranje plazovitosti|</dc:title><dc:description xml:lang="sl">In this journal, the authors (Zorn, Komac 2004) previously described the use of two deterministic methods for establishing the possibility of landsliding. This time, they take a step forward and using the example of the flysch Goriška Brda hills present the probability modelling of landslide hazard. In probability methods, the intensity and distribution of the processes are established by comparing indirectly determined landscape elements and the actual situation, while in deterministic methods, subjective decisions have animpact on the result. Authors have elaborated a probability map for landslides with a fixed return period using the Dempster-Shafer method on the basis of the data on 800 landslides that occurred with intensive precipitationin the fall of 1998</dc:description><dc:description xml:lang="sl">V reviji sta avtorja (Zorn, Komac 2004) opisala uporabo dveh determinističnih metod za ugotavljanje plazovitosti. Tokrat gresta korak naprej in na primeru flišnih Goriških brd predstavljata probabilistično metodo za ugotavljanje plazovitosti. Pri probabilističnih metodah intenzivnost in razširjenost procesov ugotavljamo s primerjavo posredno določenih pokrajinskih prvin in dejanskega stanja, medtem ko pri deterministričnih na rezultat vplivajo tudi subjektivne odločitve. Probabilistični zemljevid plazovitosti z določeno povratno dobo je bil izdelan z Dempster-Shaferjevo metodo na podlagi podatkov o 800 zemeljskih plazovih, ki so nastali ob intenzivnih padavinah jeseni 1998</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-0I6ESB4T"><edm:aggregatedCHO rdf:resource="URN:NBN:SI:doc-0I6ESB4T" /><edm:isShownBy rdf:resource="http://www.dlib.si/stream/URN:NBN:SI:doc-0I6ESB4T/a9a7e424-b26e-42a0-b5ca-36ff461983ce/PDF" /><edm:rights rdf:resource="http://creativecommons.org/licenses/by-nc-nd/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-0I6ESB4T/maxi/edm" /><edm:isShownAt rdf:resource="http://www.dlib.si/details/URN:NBN:SI:doc-0I6ESB4T" /></ore:Aggregation></rdf:RDF>