Retovje Springs
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Retovje Springs
Retovje Springs is a group of springs that join to form the Big Ljubljanica River ( sl, Velika Ljubljanica). Name The name ''Retovje'' and names like it (e.g., ''Retje'', ''Dolnje Retje'') are derived from the Slovene common noun ''retje'' 'powerful karst spring' from the root ''*vrětje'' 'springing, gushing'.Pavlovec, Rajko. 2006. "Domači kraški izrazi z Ljubljanskega barja." ''Geografski vestnik'' 78(1):61–64. The generic term ''okence'' in the Slovene name of two springs at the site is a diminutive of the common noun ''okno'' (literally, 'window') in the secondary meaning 'spring, place where groundwater surfaces'.Bezlaj, France. 1982. ''Etimološki slovar slovenskega jezika'', vol. 2. Ljubljana: Slovenska akademija znanosti in umetnosti, p. 245. Geography The springs are located in the Retovje Valley, a steephead valley near Verd south of Vrhnika. The springs include: * Walnut Spring () * Cliff Spring (, ) * Big Spring () * Little Spring () Big Spring and Little Spring ...
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Retje
Retje () is a village in the Municipality of Loški Potok in southern Slovenia. The area is part of the traditional region of Lower Carniola and is now included in the Southeast Slovenia Statistical Region. Mass graves Retje is the site of two known mass graves associated with the Second World War. The Bezelj 1 Mass Grave ( sl, Grobišče pri Bezlju 1) is located in the woods northeast of the village, east of the road to Sodražica. It contains the remains of five German prisoners of war that were brought from Mali Log and murdered here. The Bezelj 2 Mass Grave () lies east of the first grave. It contains the remains of two Home Guard soldiers and three Russian Liberation Army soldiers. Church The local church, built on an isolated spot further up the valley northwest of the main settlement, is dedicated to Saint Florian and belongs to the parish of Loški Potok. It is a Baroque building dating to the late 17th or early 18th century. It has an octagonal floor plan In architec ...
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Dolnje Retje
Dolnje Retje (; in older sources also ''Dolenje Retje'',''Leksikon občin kraljestev in dežel zastopanih v državnem zboru,'' vol. 6: ''Kranjsko''. 1906. Vienna: C. Kr. Dvorna in Državna Tiskarna, p. 40. german: link=no, Unterretje) is a small village southeast of Velike Lašče in central Slovenia. The area is part of the traditional region of Lower Carniola and is now included in the Central Slovenia Statistical Region. Name The name ''Dolnje Retje'' literally means 'lower Retje', distinguishing the village from neighboring Gornje Retje (literally, 'upper Retje'). The name ''Retje'' (like the related name '' Retnje'') is derived from the plural demonym *''Vrětьjane'', based on the common noun *''vertьje'', referring to a higher dry area in a damp or swampy area. Cultural heritage A small 18th-century chapel-shrine at the crossroads in the centre of the settlement is dedicated to Saint Roch. Notable people The Slovene writer, political activist, playwright, and critic Fr ...
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Mirke Slovenia - Little Spring
Mirke () is a small settlement immediately south of Vrhnika in the Inner Carniola region of Slovenia. References External links *Mirke on Geopedia Populated places in the Municipality of Vrhnika {{Vrhnika-geo-stub ...
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Steephead Valley
A steephead valley, steephead or blind valley is a deep, narrow, flat bottomed valley with an abrupt ending. Such closed valleys may arise in limestone or karst landscapes, where a layer of permeable rock lies above an impermeable substract such as marl. Water flowing through a steephead valley leaves via one or more ponors or sinkholes. Blind valleys are typically dry at their lower ends. If the ponor cannot contain the high runoff during a flood event an intermittent flow may continue through the valley beyond the sink. Such a landform is called a semi-blind or half-blind valley. Development They are created by a stream flowing within the permeable rock and eroding it from within, until the rock above collapses opening up a steep narrow valley which is then further eroded by the stream running across the impermeable valley floor. At the head of the valley the stream emerges from the rock as a spring. Notable examples can be found in the Jura region of France, for example ...
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Verd
Verd (; in older sources also ''Vrd'',''Leksikon občin kraljestev in dežel zastopanih v državnem zboru,'' vol. 6: ''Kranjsko''. 1906. Vienna: C. Kr. Dvorna in Državna Tiskarna, p. 120. german: Werd) is a settlement south of Vrhnika in the Inner Carniola region of Slovenia. The Verd Viaduct on the A1 motorway from Ljubljana to Koper runs above the settlement. Geography Verd is a ribbon village between the foot of Ljubljana Peak ( sl, Ljubljanski vrh, ) and Retovje Springs. It includes the hamlets of Janezova Vas, Pritiska, Podgora, and Gradar. The soil in the lower part of the settlement is composed of marsh humus, and in the higher parts is brown loam. There is a large quarry on the slope of Javorč Hill () where limestone is extracted and crushed for use by the railroad. The nearby hills, with a predominantly limestone composition, are heavily forested. There are many karst sinkholes in the area. Name Verd was attested in written sources in 1260 as ''Werde'' (and as ''Werd'' ...
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Vrhnika
Vrhnika (; german: Oberlaibach;''Leksikon občin kraljestev in dežel zastopanih v državnem zboru,'' vol. 6: ''Kranjsko''. 1906. Vienna: C. Kr. Dvorna in Državna Tiskarna, p. 120. la, Nauportus) is a town in Slovenia. It is the seat of the Municipality of Vrhnika. It is located on the Ljubljanica River, 21 km from Ljubljana along the A1 motorway. Geography Vrhnika lies at the southwest end of the Ljubljana Marsh near the sources of the Ljubljanica River, where the Ljubljana Basin opens up between the foot of Ljubljana Peak ( sl, Ljubljanski vrh, ) and Ulovka Hill (). The territory of the town extends south onto the Logatec Plateau ( sl, Logaška planota), where the Big and Little Drnovica Collapse Sinkholes ( sl, Velika Drnovica, Mala Drnovica) are found. A rich network of springs and streams originates and joins near the town to form the source of the Ljubljanica. Name The settlement at the location of today's Vrhnika was attested in antiquity as ''Nauportus'' in Latin, ...
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Ljubljanica
The Ljubljanica (), known in the Middle Ages as the ''Sava'', is a river in the southern part of the Ljubljana Basin in Slovenia. The capital of Slovenia, Ljubljana, lies on the river. The Ljubljanica rises south of the town of Vrhnika and flows into the Sava River about downstream from Ljubljana. Its largest affluent is the Mali Graben Canal. Including its source affluent the Little Ljubljanica ( sl, Mala Ljubljanica), the river is in length. The Little Ljubljanica joins the Big Ljubljanica ( sl, Velika Ljubljanica) after and the river continues its course as the Ljubljanica. The Ljubljanica is the continuation of several karst rivers that flow from the Prezid Karst Field ( sl, Prezidsko polje) to Vrhnika on the surface and underground in caves, and so the river is poetically said to have seven names (six name changes): Trbuhovica, Obrh, Stržen, Rak, Pivka, Unica, and Ljubljanica. Archaeological significance The Ljubljanica has become a popular site for archaeologists ...
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Sump (cave)
A sump, or siphon, is a passage in a cave that is submerged under water. A sump may be static, with no inward or outward flow, or active, with continuous through-flow. Static sumps may also be connected underwater to active stream passage. When short in length, a sump may be called a duck, however this can also refer to a section or passage with some (minimal) airspace above the water. Depending on hydrological factors specific to a cave – such as the sea tide, changes in river flow, or the relationship with the local water table – sumps and ducks may fluctuate in water level and depth (and sometimes in length, due to the shape of adjacent passage). Exploration past a sump Diving Short sumps may be passed simply by holding one's breath while ducking through the submerged section (for example, Sump 1 in Swildon's Hole). This is known as "free diving" and can only be attempted if the sump is known to be short and not technically difficult (e.g. constricted or requiring nav ...
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Municipality Of Vrhnika
The Municipality of Vrhnika (; sl, Občina Vrhnika) is a municipality in Slovenia. The administrative seat of the municipality is the town of Vrhnika.Municipality of Vrhnika website


Settlements

In addition to the municipal seat of Vrhnika, the municipality also includes the following settlements: * Bevke * Bistra * Blatna Brezovica * Drenov Grič * Jamnik *
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Springs Of Slovenia
Spring(s) may refer to: Common uses * Spring (season), a season of the year * Spring (device), a mechanical device that stores energy * Spring (hydrology), a natural source of water * Spring (mathematics), a geometric surface in the shape of a helically coiled tube * Spring (political terminology), often used to name periods of political liberalization * Springs (tide), in oceanography, the maximum tide, occurs twice a month during the full and new moon Places * Spring (Milz), a river in Thuringia, Germany * Spring, Alabel, a barangay unit in Alabel, Sarangani Province, Philippines * Șpring, a commune in Alba County, Romania * Șpring (river), a river in Alba County, Romania * Springs, Gauteng, South Africa * Springs, the location of Dubai British School, Dubai United States * Springs, New York, a part of East Hampton, New York * Springs, Pennsylvania, an unincorporated community * Spring, Texas, a census-designated place * Spring District, neighborhood in Bellevue, Washington ...
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Karst Springs
A karst spring or karstic spring is a spring (outflow of groundwater) that is part of a karst hydrological system. Description Because of their often conical or inverted bowl shape, karst springs are also known in German-speaking lands as a ''Topf'' ("pot") which is reflected in names such as Aachtopf (the source of the Radolfzeller Aach) or Blautopf (the source of the Blau river in Blaubeuren). Karst springs often have a very high yield or discharge rate, because they are often fed by underground drainage from a large catchment basin. Because the springs are usually the terminus of a cave drainage system at the place where a river cave reaches the Earth's surface, it is often possible to enter the caves from karst springs for exploration. Large karst springs are located in many parts of the world; the largest ones are believed to be in Papua New Guinea, with others located in Mediterranean countries such as Bosnia and Herzegovina, Croatia, Turkey, Slovenia, and Italy. Types ...
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