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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
253:. 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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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.),
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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.
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slopes, especially on the sunny sides, where animal husbandry is practiced. The wood and metal industry has developed in Stari Trg pri Ložu.
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that disappears on the north edge of the karst field into 850-meter (2,790 ft) Golobina Cave west of
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The settlements in the Lož Karst Field are relatively large and have a clustered or linear layout.
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The Lož Karst Field lies between the Bloke
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and is fed by water from Mount Snežnik. Big Obrh Spring (
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area. The streams from the two springs join west of
345:Komac, Blaž, Karel Natek, & Matija Zorn. 2008.
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377:Foreign Travellers in the Slovene Karst: 1486–1900
265:is the economic and cultural center of the area.
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117:Learn how and when to remove this message
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364:Encyclopedia of Caves and Karst Science
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133:Southwest part of the Lož Karst Field
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299:Slovenija: geografski opis
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362:Gunn, John (ed.). 2004.
317:Slovenija in njeni kraji
330:Neodgovorna odgovornost
315:Planina, Francè. 1963.
375:Shaw, Trevor R. 2008.
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263:Stari Trg pri Ložu
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269:Economic activity
223:Izvir Veliki Obrh
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278:References
239:Obrh Creek
237:to create
192:Racna gora
160:Lož Valley
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