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Bunica
The Bunica ( sr-cyrl, Буница) is a short river in Bosnia and Herzegovina and a left bank tributary of the Buna. Its source (Vrelo Bunice), located in a place called Parila under sharp cliffs between the two villages of Hodbina and Malo Polje, is 14 km south from Mostar. It is a very deep and strong karstic spring and difficult to access. Together with the Buna river, it flows west for approximately 10 km and joins the Neretva river near Buna village. The Bunica is a main tributary of the Buna. See also * Blagaj Blagaj is a village in the south-eastern region of the Mostar basin, in the Herzegovina-Neretva Canton of Bosnia and Herzegovina. It stands at the edge of Bišće plain and is one of the most valuable mixed urban and rural built environments in ... * Krupa (Neretva) * Hutovo Blato * Vrelo Bune Rivers of Bosnia and Herzegovina Karst springs of Bosnia and Herzegovina Landforms of the Federation of Bosnia and Herzegovina b Upper Horizons Hydroel ...
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Buna Village
Buna (Serbian Cyrillic: Буна) is a populated settlement at the confluence of the Buna river and Neretva river some 10 km downstream the Neretva and south of Mostar, Herzegovina-Neretva Canton, Bosnia and Herzegovina. The famous source of the Buna river ('' Vrelo Bune'') is a strong karstic spring. The Buna river flows west from its source for approximately 9 kilometres and joins the Neretva near the village Buna. Demographics According to the 2013 census, its population was 1,291. See also * Blagaj * Bunica * Vrelo Bunice * Bregava * Stolac Stolac is an ancient city located in Herzegovina-Neretva Canton of the Federation of Bosnia and Herzegovina, an entity of Bosnia and Herzegovina. It is located in the region of Herzegovina. Stolac is one of the oldest cities in Bosnia and Herzego ... * Trebižat * Hutovo Blato References Populated places in Mostar Villages in the Federation of Bosnia and Herzegovina {{HerzegovinaNeretvaCanton-geo-stub ...
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Rivers Of Bosnia And Herzegovina
This is a list of rivers of Bosnia and Herzegovina ordered alphabetically. Draining into the Black Sea * Glina ( right tributary to Kupa) ** Glinica (right tributary) *** Bojna *** Bužimica ** Kladušnica ( right tributary in Velika Kladuša) * Korana (right tributary to Kupa) ** Mutnica (Korana) (right tributary) * Sava (right tributary of the Danube) ** Bosna (right tributary) *** Babina rijeka (right tributary near/in Zenica) *** Fojnička rijeka ( left tributary) **** Lepenica (Fojnička rijeka) (left tributary) ***** Bijela rijeka (Lepenica) (right tributary near Kreševo) ***** Crna rijeka (Lepenica) (right tributary near Kreševo) ***** Kreševka (right tributary in Kreševo) **** Željeznica (Fojnička rijeka) (right tributary) ***** Dragača (left tributary in Fojnica) *** Goruša (right tributary in Visoko) *** Krivaja (right tributary in Zavidovići) **** Stupčanica (source of the Krivaja (in confluence with the Bioštica) and right tributary in Olo ...
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Buna (Neretva)
The Buna ( sr-Cyrl, Буна) is a short river in Bosnia and Herzegovina; it is a left bank tributary of the Neretva. Its source (Vrelo Bune), a strong karstic spring, is near the village of Blagaj, southeast of Mostar. It is best known for the ''Buna Spring'' (Vrelo Bune), one of the strongest springs in Europe and extremely cold water. The Buna flows west for approximately 9 km, starts at Blagaj and meandering through the villages of Blagaj, Kosor, Malo Polje, Hodbina and joins the Neretva at settlement Buna. The Bunica river is main left bank tributary of the Buna. See also * Vrelo Bunice * Mostarska Bijela * Hutovo Blato * Daorson * List of Illyrian cities This is a list of settlements in Illyria founded by Illyrians (southern Illyrians, Dardanians, Pannonians), Liburni, Ancient Greeks and the Roman Empire. A number of cities in Illyria and later Illyricum were built on the sites or close to the ... Rivers of Bosnia and Herzegovina Springs of Bosnia ...
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Blagaj
Blagaj is a village in the south-eastern region of the Mostar basin, in the Herzegovina-Neretva Canton of Bosnia and Herzegovina. It stands at the edge of Bišće plain and is one of the most valuable mixed urban and rural built environments in Bosnia and Herzegovina, distinguished from other similar built environments in its urban layout. Blagaj was most likely named for its mild weather patterns since ''blaga'' in Bosnian means "mild". Blagaj is situated at the spring of the Buna river and a historical tekke (''tekija'' or Dervish monastery). The Blagaj Tekija was built around 1520, with elements of Ottoman architecture and Mediterranean style and is considered a national monument. Blagaj Tekke is a monastery built for the Dervish. Sources Vrelo Bune, the source of the Buna river, is a strong karstic spring. The river flows west for approximately and joins the Neretva near the village Buna. The historic site of the Blagaj Fort (also ''Stjepan-grad'' or ''Stipan-grad''), o ...
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Buna (Neretva)
The Buna ( Serbian Cyrillic: Буна) is a short river in Bosnia and Herzegovina; it is a left bank tributary of the Neretva. Its source (Vrelo Bune), a strong karstic spring, is near the village Blagaj, southeast of Mostar. It is best known for the ''Buna Spring'' (Vrelo Bune), one of the strongest springs in Europe and extremely cold water. The Buna flows west for approximately 9 km, starts at Blagaj and meandering through villages Blagaj, Kosor, Malo Polje, Hodbina and joins the Neretva at settlement Buna. The Bunica river is main left bank tributary of the Buna. See also * Vrelo Bunice * Mostarska Bijela * Hutovo Blato * Daorson * List of Illyrian cities This is a list of settlements in Illyria founded by Illyrians (southern Illyrians, Dardanians, Pannonians), Liburni, Ancient Greeks and the Roman Empire. A number of cities in Illyria and later Illyricum were built on the sites or close to the s ... Rivers of Bosnia and Herzegovina Springs of Bosnia ...
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Neretva
The Neretva ( sr-cyrl, Неретва, ), also known as Narenta, is one of the largest rivers of the eastern part of the Adriatic basin. Four HE power-plants with large dams (higher than 150,5 metres) provide flood protection, power and water storage. It is recognized for its natural environment and diversity of its landscape. Freshwater ecosystems have suffered from an increasing population and the associated development pressures. One of the most valuable natural resources of Bosnia and Herzegovina and Croatia is its freshwater resource, contained by an abundant wellspring and clear rivers. Situated between the major regional rivers (Drina river on the east, Una river on the west and the Sava river) the Neretva basin contains the most significant source of drinking water. The Neretva is notable among rivers of the Dinaric Alps region, especially regarding its diverse ecosystems and habitats, flora and fauna, cultural and historic heritage. Its name has been suggested to c ...
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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. Type ...
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Karst Springs Of Bosnia And Herzegovina
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier. ...
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Vrelo Bune
'' means Good, fine;''(see also'' ''Latin names of rivers)'' , location = Blagaj, Herzegovina-Neretva Canton, Bosnia and Herzegovina , spring_source = , elevation = 140 , coordinates = , coords_ref = , hot_spring_type = , type = Karst spring , provides = Buna river , magnitude = , height = , duration = , frequency = , discharge = 30 , temperature = , depth = , child = , embedded= Footnotes UNESCO WHC Tentative List Since 11/12/2007 ''Ref.'': 5280 ''Region'': Europe and North America ''Criteria'': ii, iii, iv, v, vi, vii ''iucn Category'': Mixed - natural and architectural ensemblBosnia and Herzegovina - UNESCO World Heritage CentreWebsiteCommission to Preserve National Monuments of Bosnia and Herzegovina Vrelo Bune (Serbian Cyrillic: Врело Буне; ) is the natural and architectural ensemble at the Buna river spring near Blagaj ''kasaba'' (village-town) and a part of the wider ''"Townscape ensemble of the town of Blagaj — Historical and Natura ...
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Hutovo Blato
Hutovo Blato ( sr-cyrl, Хутово Блато) is a nature reserve and bird reserve located in Bosnia and Herzegovina. It is primarily composed of marshlands that were created by the underground aquifer system of the Krupa River. It is fed from the limestone massif of Ostrvo that divides the Deransko Lake and Svitavsko Lake. The reserve is on the list of BirdLife International's Important Bird Areas. It is the largest reserve of its kind in the region, in terms of both size and diversity. It is home to over 240 types of migratory birds and dozens that make their permanent home in the sub-Mediterranean wetlands surrounding Deransko Lake. In the migration season, tens of thousands of birds fill the lake and its surroundings. Wetlands The valley along the last 30 km of the Neretva River, and the river itself, comprise a remarkable landscape. Downstream from the confluence of its tributaries, the Trebižat and Bregava rivers, the valley spreads into an alluvial fan coveri ...
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Krupa (Neretva)
The Krupa ( sr-cyrl, Крупа) river is a left tributary of the river Neretva and the main water current of Hutovo Blato, which leads the waters from Gornje Blato and Svitavsko Lake into the Neretva river near Dračevo. The length of Krupa is 9 km with an average depth of 5 meters. The Krupa does not have an actual source, but is actually an extension of Deransko Lake. Also, the Krupa is a unique river in Europe, because the river flows both ways. It flows normally from the source to the mouth and from the mouth to the source. This happens when, due to high water levels and large quantities of water, the Neretva pushes the Krupa river in the opposite direction. See also * Bregava The Bregava ( sr-cyrl, Брегава) is a sinking river in Bosnia and Herzegovina that passes through the town of Stolac. It is a left tributary of the Neretva river. The river Bregava and its buildings - bridges, mills and stamping mills over ... * Hutovo Blato References External ...
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Spring (hydrosphere)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust ( pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels throu ...
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