Matches in DBpedia 2016-04 for { <http://wikidata.dbpedia.org/resource/Q1039805> ?p ?o }
Showing triples 1 to 81 of
81
with 100 triples per page.
- Q1039805 subject Q7037629.
- Q1039805 subject Q7239874.
- Q1039805 abstract "Uvala is originally a local toponym used by people in some regions in Croatia, Bosnia and Herzegovina, Montenegro and Serbia. In geosciences it denotes a closed karst depression, a terrain form usually of elongated or compound structure and of larger size than that of sinkholes (dolines). It is a morphological form frequently found in the “Outer Dinarides” anywhere between Slovenia and Greece. But large closed karst depressions are found on all continents in different landscapes and therefore uvala has become a globally established term, used also to distinguish such depressions from Poljes (size of many km). Definitions of uvalas are often poorly empirically supported. “The coalescence of dolines” is a most frequently found and still dominant explanation. Yet because of the ongoing dissatisfaction with this definition the term ‘uvala’ has often been belittled – occasionally it was even proposed that the term be given up altogether!However, recent empirical research (~2009) revised poor mainstream definitions, stating that “…uvalas are large (in km scale) karst closed depressions of irregular or elongated plan form resulting from accelerated corrosion along major tectonically broken zones.” This is arguing for the “re-introducing of uvalas into modern karstology” - distinguishing them from dolines and poljes in size (typically) and “also in morphology and combination of genetic factors”, which give them “a status of a particular karst relief form.”".
- Q1039805 thumbnail Uvala_Veliki-Lubenovac_NVelebit_Croatia.jpg?width=300.
- Q1039805 wikiPageExternalLink glossary.pdf.
- Q1039805 wikiPageExternalLink geol.htm.
- Q1039805 wikiPageExternalLink 1774538.
- Q1039805 wikiPageExternalLink 208252.
- Q1039805 wikiPageExternalLink ?issue=3.
- Q1039805 wikiPageWikiLink Q11081619.
- Q1039805 wikiPageWikiLink Q1152275.
- Q1039805 wikiPageWikiLink Q1286.
- Q1039805 wikiPageWikiLink Q1340510.
- Q1039805 wikiPageWikiLink Q134783.
- Q1039805 wikiPageWikiLink Q137056.
- Q1039805 wikiPageWikiLink Q1434835.
- Q1039805 wikiPageWikiLink Q15903.
- Q1039805 wikiPageWikiLink Q159589.
- Q1039805 wikiPageWikiLink Q163082.
- Q1039805 wikiPageWikiLink Q167466.
- Q1039805 wikiPageWikiLink Q16817.
- Q1039805 wikiPageWikiLink Q17073733.
- Q1039805 wikiPageWikiLink Q179132.
- Q1039805 wikiPageWikiLink Q179177.
- Q1039805 wikiPageWikiLink Q180184.
- Q1039805 wikiPageWikiLink Q183.
- Q1039805 wikiPageWikiLink Q186131.
- Q1039805 wikiPageWikiLink Q188645.
- Q1039805 wikiPageWikiLink Q188734.
- Q1039805 wikiPageWikiLink Q189915.
- Q1039805 wikiPageWikiLink Q190429.
- Q1039805 wikiPageWikiLink Q191250.
- Q1039805 wikiPageWikiLink Q193343.
- Q1039805 wikiPageWikiLink Q1979583.
- Q1039805 wikiPageWikiLink Q2110260.
- Q1039805 wikiPageWikiLink Q215.
- Q1039805 wikiPageWikiLink Q223275.
- Q1039805 wikiPageWikiLink Q224.
- Q1039805 wikiPageWikiLink Q225.
- Q1039805 wikiPageWikiLink Q236.
- Q1039805 wikiPageWikiLink Q23757.
- Q1039805 wikiPageWikiLink Q25276.
- Q1039805 wikiPageWikiLink Q254077.
- Q1039805 wikiPageWikiLink Q26185.
- Q1039805 wikiPageWikiLink Q263635.
- Q1039805 wikiPageWikiLink Q265619.
- Q1039805 wikiPageWikiLink Q2694749.
- Q1039805 wikiPageWikiLink Q403.
- Q1039805 wikiPageWikiLink Q40614.
- Q1039805 wikiPageWikiLink Q41.
- Q1039805 wikiPageWikiLink Q463896.
- Q1039805 wikiPageWikiLink Q491689.
- Q1039805 wikiPageWikiLink Q4935045.
- Q1039805 wikiPageWikiLink Q52139.
- Q1039805 wikiPageWikiLink Q531953.
- Q1039805 wikiPageWikiLink Q5413532.
- Q1039805 wikiPageWikiLink Q576413.
- Q1039805 wikiPageWikiLink Q609634.
- Q1039805 wikiPageWikiLink Q625139.
- Q1039805 wikiPageWikiLink Q6538759.
- Q1039805 wikiPageWikiLink Q6592057.
- Q1039805 wikiPageWikiLink Q6609084.
- Q1039805 wikiPageWikiLink Q668593.
- Q1039805 wikiPageWikiLink Q669883.
- Q1039805 wikiPageWikiLink Q679384.
- Q1039805 wikiPageWikiLink Q702489.
- Q1039805 wikiPageWikiLink Q7037629.
- Q1039805 wikiPageWikiLink Q7205.
- Q1039805 wikiPageWikiLink Q7239874.
- Q1039805 wikiPageWikiLink Q745430.
- Q1039805 wikiPageWikiLink Q76259.
- Q1039805 wikiPageWikiLink Q76267.
- Q1039805 wikiPageWikiLink Q76756.
- Q1039805 wikiPageWikiLink Q7918880.
- Q1039805 wikiPageWikiLink Q8039213.
- Q1039805 wikiPageWikiLink Q853364.
- Q1039805 wikiPageWikiLink Q853422.
- Q1039805 wikiPageWikiLink Q946033.
- Q1039805 comment "Uvala is originally a local toponym used by people in some regions in Croatia, Bosnia and Herzegovina, Montenegro and Serbia. In geosciences it denotes a closed karst depression, a terrain form usually of elongated or compound structure and of larger size than that of sinkholes (dolines). It is a morphological form frequently found in the “Outer Dinarides” anywhere between Slovenia and Greece.".
- Q1039805 label "Uvala (landform)".
- Q1039805 depiction Uvala_Veliki-Lubenovac_NVelebit_Croatia.jpg.