The Lož Karst Field (pronounced[ˈloːʃ]; Slovene: Loško polje), also known as the Lož Valley (Slovene: Loška dolina),[1][2] is a karst field in Inner Carniola[3] in southwest Slovenia. It is the smallest karst field in Inner Carniola.[1]
The Lož Karst Field lies between the Bloke Plateau to the north, Mount Race (Slovene: Racna gora, 1,140 meters or 3,740 feet) to the east, and Mount Snežnik to the west. It is about 6 kilometers (3.7 mi) long and 4 kilometers (2.5 mi) wide, and lies on Triassic dolomite oriented in the Dinaric direction.
Little Obrh Spring (Slovene: 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.[1][2] Big Obrh Spring (Slovene: 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.[1][2] The streams from the two springs join west of Pudob[4] to create Obrh Creek, a losing stream that disappears on the north edge of the karst field into 850-meter (2,790 ft) Golobina Cave west of Dane, emerging to the west at Lake Cerknica.[5][6] 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.
Settlementsedit
The settlements in the Lož Karst Field are relatively large and have a clustered or linear layout. Stari Trg pri Ložu is the economic and cultural center of the area.
Economic activityedit
The karst field ranges between 570 meters (1,870 ft) and 590 meters (1,940 ft) in elevation and is surrounded by steep wooded slopes. The flat areas are used for tilled fields, and lower parts near the creeks for meadows. There are also meadows and pastures along the edges of the gentler slopes, especially on the sunny sides, where animal husbandry is practiced. The wood and metal industry has developed in Stari Trg pri Ložu.
Referencesedit
^ abcdMelik, Anton. 1959. Slovenija: geografski opis, vol. 2, part 3. Ljubljana: Slovenska matica, p. 541.
^ abcPlanina, Francè. 1963. Slovenija in njeni kraji. Ljubljana: Prešernova družba, p. 104.
^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.
^Komac, Blaž, Karel Natek, & Matija Zorn. 2008. Geografski vidiki poplav v Sloveniji (= Geografija Slovenije 20). Ljubljana: ZRC, p. 85.
^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.
lož, karst, field, this, article, needs, additional, citations, verification, please, help, improve, this, article, adding, citations, reliable, sources, unsourced, material, challenged, removed, find, sources, news, newspapers, books, scholar, jstor, march, 2. This article needs additional citations for verification Please help improve this article by adding citations to reliable sources Unsourced material may be challenged and removed Find sources Loz Karst Field news newspapers books scholar JSTOR March 2015 Learn how and when to remove this template message The Loz Karst Field pronounced ˈloːʃ Slovene Losko polje also known as the Loz Valley Slovene Loska dolina 1 2 is a karst field in Inner Carniola 3 in southwest Slovenia It is the smallest karst field in Inner Carniola 1 Southwest part of the Loz Karst Field Contents 1 Geography 2 Settlements 3 Economic activity 4 References 5 External linksGeography editThe Loz Karst Field lies between the Bloke Plateau to the north Mount Race Slovene Racna gora 1 140 meters or 3 740 feet to the east and Mount Sneznik to the west It is about 6 kilometers 3 7 mi long and 4 kilometers 2 5 mi wide and lies on Triassic dolomite oriented in the Dinaric direction Little Obrh Spring Slovene Izvir Mali Obrh lies on the south edge of the karst field in Kozarisce near Sneznik Castle and is fed by water from Mount Sneznik 1 2 Big Obrh Spring Slovene Izvir Veliki Obrh lies on the east side of the karst field near Vrhnika pri Lozu and is fed by water from Mount Race and the Potok Plateau in the Loski Potok area 1 2 The streams from the two springs join west of Pudob 4 to create Obrh Creek a losing stream that disappears on the north edge of the karst field into 850 meter 2 790 ft Golobina Cave west of Dane emerging to the west at Lake Cerknica 5 6 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 Settlements editThe settlements in the Loz Karst Field are relatively large and have a clustered or linear layout Stari Trg pri Lozu is the economic and cultural center of the area Economic activity editThe karst field ranges between 570 meters 1 870 ft and 590 meters 1 940 ft in elevation and is surrounded by steep wooded slopes The flat areas are used for tilled fields and lower parts near the creeks for meadows There are also meadows and pastures along the edges of the gentler slopes especially on the sunny sides where animal husbandry is practiced The wood and metal industry has developed in Stari Trg pri Lozu References edit a b c d Melik Anton 1959 Slovenija geografski opis vol 2 part 3 Ljubljana Slovenska matica p 541 a b c Planina France 1963 Slovenija in njeni kraji Ljubljana Presernova druzba p 104 Kovacic Gregor amp Natasa Ravbar 2011 Dinamika poplavljanja Planinmskega polja v obdobju oktober 2008 april 2009 In Matija Zorn Blaz Komac Rok Ciglic amp Miha Pavsek eds Neodgovorna odgovornost Naravne nesrece 2 pp 91 101 Ljubljana ZRC p 93 Komac Blaz Karel Natek amp Matija Zorn 2008 Geografski vidiki poplav v Sloveniji Geografija Slovenije 20 Ljubljana ZRC p 85 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 External links editLoz Karst Field on Geopedia45 41 56 N 14 28 42 E 45 69889 N 14 47833 E 45 69889 14 47833 Retrieved from https en wikipedia org w index php title Loz Karst Field amp oldid 1195589105, wikipedia, wiki, book, books, library,
