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Lož Karst Field
The Lož Karst Field (; (スロベニア語:Loško polje)), also known as the Lož Valley ((スロベニア語:Loška dolina)),〔Melik, Anton. 1959. ''Slovenija: geografski opis'', vol. 2, part 3. Ljubljana: Slovenska matica, p. 541.〕〔Planina, Francè. 1963. ''Slovenija in njeni kraji''. Ljubljana: Prešernova družba, p. 104.〕 is a karst field in Inner Carniola〔Kovačič, Gregor & Nataša Ravbar. 2011. Dinamika poplavljanja Planinmskega polja v obdobju oktober 2008–april 2009. In: Matija Zorn, Blaž Komac, Rok Ciglič, & Miha Pavšek (eds.), ''Neodgovorna odgovornost'' (= ''Naravne nesreče'' 2), pp. 91–101. Ljubljana: ZRC, p. 93.〕 in southwest Slovenia. It is the smallest karst field in Inner Carniola.〔
==Geography==
The Lož Karst Field lies between the Bloke Plateau to the north, Mount Race ((スロベニア語:Racna gora), ) to the east, and Mount Snežnik to the west. It is about long and wide, and lies on Triassic dolomite oriented in the Dinaric direction.
Little Obrh Spring ((スロベニア語:Izvir Mali Obrh)) lies on the south edge of the karst field in Kozarišče near Snežnik Castle and is fed by water from Mount Snežnik.〔〔 Big Obrh Spring ((スロベニア語:Izvir Veliki Obrh)) lies on the east side of the karst field, near Vrhnika pri Ložu, and is fed by water from Mount Race and the Potok Plateau in the Loški Potok area.〔〔 The streams from the two springs join west of Pudob〔Komac, Blaž, Karel Natek, & Matija Zorn. 2008. ''Geografski vidiki poplav v Sloveniji'' (= ''Geografija Slovenije'' 20). Ljubljana: ZRC, p. 85.〕 to create Obrh Creek, a losing stream that disappears on the north edge of the karst field into Golobina Cave west of Dane, emerging to the west at Lake Cerknica.〔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.〕 Flooding affects only the western part of the karst field, below Dane, which is uninhabited. In the past, more of the karst field used to flood, and so at the end of the 19th century a lower entrance was cut into the cave, which reduced the depth and duration of flooding.
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