Dobličica
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Dobličica
The Dobličica is a stream in White Carniola. It is part of a karst aquifer. Due to its geological and hydrological characteristics and urbanization of the area, it is considered sensitive and subject to pollution. Geography The Dobličica has its source in the eastern foothills of Mount Poljane ( sl, Poljanska gora) at Lake Dobliče ( sl, Dobličko jezero), which is across and up to deep. The bed of the lake is covered with large boulders, among which karst water flows from two depressions. A karst spring with a constant flow feeds the lake, with an outflow in a broad but shallow channel. The upper part of the stream bed is rocky mixed with sand, and the banks are loamy. Soon after the source, another spring adds its water to the flow from the lake. The channel is bordered by typical riverside vegetation and meanders through meadows before being joined by another stream, the Potok, and emptying into the Lahinja River at Črnomelj. The Dobličica and the Lahinja surround the old ...
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Lahinja
The Lahinja is a river in White Carniola, the extreme southeastern part of Slovenia. It is long and originates from several karst springs at the end of a steephead valley between the villages of Knežina, Belčji Vrh, and Mali Nerajec. In its upper course the river flows towards the north in a narrow bed with a very shallow gradient, resulting in the fact that it meanders significantly. All of its major affluents join it from the west and all of them start from karst springs. At Dragatuš it is joined by its major tributary Podturnščica Creek, and at Črnomelj by Dobličica Creek. From the outflow of Podturnščica Creek the bed of the Lahinja is narrow and up to 20 m deep, with numerous bends. At the vicinity of one of them stands Gradac Castle. From Črnomelj to Gradac the river has no surface affluents, but below Gradac it is joined by the high-volume and faster-flowing Krupa. After its confluence with the Krupa, the Lahinja turns towards the east. It joins the Kolp ...
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Črnomelj
Črnomelj (; in older sources also ''Černomelj'', german: Tschernembl''Leksikon občin kraljestev in dežel zastopanih v državnem zboru,'' vol. 6: ''Kranjsko''. 1906. Vienna: C. Kr. Dvorna in Državna Tiskarna, p. 4.) is a town in southeastern Slovenia. It is the seat of the Municipality of Črnomelj. It lies on the left bank of the Lahinja and Dobličica rivers. The municipality is at the heart of the area of White Carniola, the southeastern part of the traditional region of Lower Carniola. It is now included in the Southeast Slovenia Statistical Region. It includes the hamlets of Čardak, Kočevje, Kozji Plac, Loka, and Nova Loka. Name Črnomelj was first attested in written sources in 1228 as ''Schirnomel'' (and as ''Zernomel'' in 1263, ''Zermenli'' in 1277, and ''Tscherneml'' in 1490). The name is derived from ''*Čьrnomľь'', based on the hypocorism ''*Čьrnomъ'', thus originally meaning 'Črnom's settlement'. In the modern German the name was ''Tschernembl''. Until 19 ...
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List Of Rivers Of Slovenia
300px, Map of river systems in Slovenia This is a list of rivers of Slovenia. There are 59 major rivers in Slovenia, altogether measuring about in length. The total length of all rivers in Slovenia is , which gives a river density of 1,33 km/km2. The territory of Slovenia mainly (, i.e. 81%) belongs to the Black Sea basin, and a smaller part (, i.e. 19%) belongs to the Adriatic Sea basin. These two parts are divided into smaller units in regard to their central rivers, the Mura River basin, the Drava River basin, the Sava River basin with Kolpa River basin, and the basin of the Adriatic rivers. p. 27 By drainage basin This list is arranged by drainage basin, with respective tributaries, arranged in the order of their confluence from mouth to source, indented under each larger stream's name. Draining into the Mediterranean Sea *Soča River ** Nadiža River *** Jamjak Creek *** Lerada Creek *** White Creek (''Bela'') **Vipava River *** Vrtojbica Creek *** Lijak Creek *** Br ...
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White Carniola
White Carniola ( sl, Bela krajina; german: Weißkrain or ''Weiße Mark'') is a traditional region in southeastern Slovenia on the border with Croatia. Due to its smallness, it is often considered a subunit of the broader Lower Carniola region, although with distinctive cultural, linguistic, and historical features. Due to its proximity with Croatia, White Carniola shares many cultural and linguistic features with the neighboring Kajkavian Croatian areas. It is generally considered the Slovenian region with the closest cultural affinity with other South Slavic territories. It was part of Slavonia until the 12th century, after which it shared the historical fate with the Windic March and Lower Carniola to the north. During the 19th century, it was one of the regions with the highest emigration rate in the Slovene Lands, and the Austrian Empire in general. During World War II, it was an important center of anti-Fascist resistance in Slovenia. Geography The area is confined by the ...
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Slovenia
Slovenia ( ; sl, Slovenija ), officially the Republic of Slovenia (Slovene: , abbr.: ''RS''), is a country in Central Europe. It is bordered by Italy to the west, Austria to the north, Hungary to the northeast, Croatia to the southeast, and the Adriatic Sea to the southwest. Slovenia is mostly mountainous and forested, covers , and has a population of 2.1 million (2,108,708 people). Slovenes constitute over 80% of the country's population. Slovene, a South Slavic language, is the official language. Slovenia has a predominantly temperate continental climate, with the exception of the Slovene Littoral and the Julian Alps. A sub-mediterranean climate reaches to the northern extensions of the Dinaric Alps that traverse the country in a northwest–southeast direction. The Julian Alps in the northwest have an alpine climate. Toward the northeastern Pannonian Basin, a continental climate is more pronounced. Ljubljana, the capital and largest city of Slovenia, is geogr ...
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Karst Spring
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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Catchwater
A catchwater device is a large-scale man-made device for catching surface runoff from hills and the sky from precipitation by channeling it to reservoirs for commercial and domestic use later. Freshwater is a scarce natural resource due to pollution, droughts, and overpopulation. Catchwater is a sustainable mechanism to increase freshwater in areas facing droughts or polluted waterways. Types Catchwater drains Catchwater drains may take the form of concrete canals, such as in Hong Kong, where there are many. Alternatively, they may take the form of a large concrete sheet, smothering a hill, and preventing rainfall from entering the rock strata, with a smaller channeling system for transport of the water to the storage tank - this latter system is in operation in Gibraltar. In Hong Kong there are approximately 120 km of concrete channels, used as gutters built along hillsides in order to direct freshwater runoff into reservoirs for local water consumption. These catchwate ...
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