Lake Cerknica

Lake Cerknica

Lake Cerknica after rain
Location Inner Carniola
Coordinates 45°44′59″N 14°22′20″E / 45.74972°N 14.37222°E / 45.74972; 14.37222Coordinates: 45°44′59″N 14°22′20″E / 45.74972°N 14.37222°E / 45.74972; 14.37222
Type intermittent
Basin countries Slovenia
Surface area 38 km² (max.)
Average depth 10 m (max.)
Surface elevation 546 m to 551 m
Settlements Cerknica, Dolenje Jezero, Gorenje Jezero, Grahovo
Lake Cerknica in winter, with the summit of Slivnica in the background
The Cerknica Polje after the lake has dried out

Lake Cerknica (pronounced [ˈtseːɾknitsa]; Slovene: Cerkniško jezero, German: Zirknitzer See) is an intermittent lake in the southern part of the Cerknica Polje, a karst polje in Inner Carniola, a region in southwestern Slovenia.[1] The lake, oriented in the Dinaric direction from northwest to southeast, is present for the most part of the year.[1] When full, it is the largest lake in the country. The plain is surrounded by the Javornik Hills (1,268 metres or 4,160 feet) to the south and Slivnica (1,022 m or 3,353 ft) to the north, both belonging to Dinaric Alps. The area of the lake mainly reaches 28 square kilometres (11 sq mi), but can reach up to 38 km2 (15 sq mi) and the surface level varies from 546 m (1,791 ft) to 551 m (1,808 ft) above sea level. The lake is an important wildlife resort, especially as a nesting place for many bird species. Botanically, it is distinguished by amphibious plants. It is therefore a part of two Natura 2000 areas of protection[2] and the focus of the Inner Carniola Regional Park, which covers additional Natura 2000 areas in the broader region.[3] The climate in the area is continental, with a mean temperature of 9.2 °C (48.6 °F) and the annual precipitation about 1,700 millimetres (67 in). The largest settlement at the border of the lake is Cerknica, located north of the lake. Various watersports, including windsurfing, are popular on the lake.

Intermittent behavior

The lake, which under ordinary conditions has an area of about 26 km2 (10 sq mi) and a mean depth of 6.1 m (20 ft), communicates through a number of openings with a series of subterranean reservoirs or caverns, some of which are above the lake level in the surrounding hills. In the autumn, when the rainfall is slight, the lake is completely drained into the reservoirs lying below its level, and its bed is speedily covered with rich vegetation. With the returning heavy rains, the surrounding higher reservoirs are filled and discharge suddenly through the subterranean passages into the lake, so that the latter very rapidly regains its ordinary volume and may even inundate the surrounding country. The changes in level are, however, very irregular. Sometimes the lake does not disappear for several years, and it can remain dry for over a year, as it did in 1834–35. It is rich in fish, which disappear and return with the water.[4]

Research history

Strabo in his Geography mentions a "marsh called Lugeon" (helos Lougeon kaloumenon) which has been identified with Lake Cerknica,[5] Lougeon being Strabo's Greek rendition of a local toponym, perhaps of Illyrian origin. It is Romanized as Lugeum. In November 1687 the Carniolan polymath Johann Weikhard von Valvasor described the lake in his letter to the Royal Society, an excerpt of which was published in the Society's Philosophical Transactions in December that year.[6] He proposed a model of filling and emptying the lake, based on Cartesian mechanics.[7] The first to accurately describe the functioning of Lake Cerknica was Tobias Gruber in 1781,[8] followed in 1784 by Belsazar Hacquet.[9]

References

  1. 1 2 Turk, Janez. "Cerkniško polje" [Cerknica Polje]. In Šmid Hribar; Golež, Gregor; Podjed, Dan; Kladnik, Drago; Erhartič, Bojan; Pavlin, Primož; Ines, Jerele. Enciklopedija naravne in kulturne dediščine na Slovenskem [Encyclopedia of Natural and Cultural Heritage in Slovenia] (in Slovenian). Retrieved 17 May 2012.
  2. ↑ Projektno območje. Project Life. Notranjska Regional Park. Accessed 2009-12-16. (in Slovene)
  3. ↑ Notranjska Regional Park - informative leaflet. Accessed 2009-12-16.
  4. ↑  Gilman, D. C.; Thurston, H. T.; Colby, F. M., eds. (1905). "Zirknitzer See". New International Encyclopedia (1st ed.). New York: Dodd, Mead.
  5. ↑ Strabo, Strabo, Geography, v. 7, ch. 5 at perseus.tufts.edu
  6. ↑ Reisp, Branko (1983). Kranjski polihistor Janez Vajkard Valvasor [The Carniolan Polymath Johann Weikhard von Valvasor] (in Slovenian). Mladinska knjiga. pp. 177–184. COBISS 13772033.
  7. ↑ Weichard, John (1686–1692). "An Extract of a Letter written to the Royal Society out of Carniola, by Mr. John Weichard Valvaſor, R. Soc. S. being a full and accurate deſcription of the wonderful Lake of Zirknitz in that Country". Philosophical Transactions (1683-1775). 16: 411–427. JSTOR 101905.
  8. ↑ Kranjc, Andrej (1984). "Raziskovanje vodnih jam na Slovenskem: pregled od antike do danes" [The Exploration of Water Caves in the Slovene Lands: An Overview from the Antiquity Until Today]. Kronika (in Slovenian). Section for the History of Places, Association of Historical Societies of Slovenia. 32 (1): 35–43. ISSN 0023-4923.
  9. ↑ Jerele, Ines. "Geologija alpskega sveta Slovenije" [The Geology of the Alpine Landscapes of Slovenia]. In Šmid Hribar, Mateja; Golež, Gregor; Podjed, Dan; Kladnik, Drago; Erhartič, Bojan; Pavlin, Primož; Ines, Jerele. Enciklopedija naravne in kulturne dediščine na Slovenskem – DEDI [Encyclopedia of Natural and Cultural Heritage in Slovenia] (in Slovenian). Retrieved 25 July 2012.
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