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Obrh
Obrh Creek () is a losing stream that originates and terminates in the Lož Karst Field in the Municipality of Loška Dolina. It is a watercourse in the Ljubljanica watershed. It is created by the confluence of Little Obrh Creek ((スロベニア語:Mali Obrh)) and Big Obrh Creek ((スロベニア語:Veliki Obrh)); the latter is fed by two tributaries: Brežiček Creek and Viševek Brežiček Creek ((スロベニア語:Viševski Brežiček)). The confluence, at which point it is simply named ''Obrh'', lies west of the village of Pudob.〔Komac, Blaž, Karel Natek, & Matija Zorn. 2008. ''Geografski vidiki poplav v Sloveniji'' (= ''Geografija Slovenije'' 20). Ljubljana: ZRC, p. 85.〕 In the northwest, limestone part of the karst field, Obrh Creek starts to drain into many sinkholes, and higher water flows into Golobina Cave. The stream re-emerges at a spring to the northwest on the southeast edge of the Cerknica Karst Field.〔Gunn, John (ed.). 2004. ''Encyclopedia of Caves and Karst Science''. New York: Fitzroy Dearborn, p. 430.〕〔Shaw, Trevor R. 2008. ''Foreign Travellers in the Slovene Karst: 1486–1900''. Ljubljana: ZRC, p. 32.〕 == Name == The name ''Obrh'' comes from the Slovene common noun ''obrh'', referring to a powerful karst spring that usually surfaces below a cliff, creating a small deep lake that flows into a valley. The noun is originally a fused prepositional phrase, *''ob vьrxъ'' 'at the summit' (i.e., at the highest point of the watercourse).〔Snoj, Marko. 2009. ''Etimološki slovar slovenskih zemljepisnih imen''. Ljubljana: Modrijan and Založba ZRC, p. 287.〕
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