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Vrelo Bunice
The Bunica ( sr-cyrl, Буница) is a short river in Bosnia and Herzegovina and a left-bank tributary of the Neretva. It is also a main tributary of the Buna. Its source, Vrelo Bunice, is located under sharp cliffs between the villages of Hodbina and Malo Polje, 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 the village of Buna. The Bunica is inhabited by endemic trout species known under its vernacular name as Softmouth trout. References See also * Blagaj, Mostar * 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 ... * Hutovo Blato * Vrelo Bune Rivers of Bosnia and Herzegovina Karst springs of Bo ...
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Karst Spring
A karst spring or karstic spring is a Spring (hydrology), spring (exsurgence, 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), Blau river in Blaubeuren). Karst springs often have a very high yield (hydrology), yield or Discharge (hydrology), 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 ...
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Buna, Mostar
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 this village that has taken its name from the river. Demographics According to the 2013 census, its population was 1,291. See also * Blagaj, Mostar * Vrelo Bunice * Bregava * Stolac * Trebižat Trebižat is a village in Bosnia and Herzegovina. According to the 1991 census, the village is located in the municipality of Čapljina Čapljina ( cyrl, Чапљина, ) is a city located in Herzegovina-Neretva Canton of the Federation of Bosn ... * Hutovo Blato References Populated places in Mostar Villages in the Federation of Bosnia and Herzegovina {{Herzegov ...
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Karst Springs Of Bosnia And Herzegovina
Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some evidence that karst may occur in more weathering-resistant rocks such as quartzite given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. 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 Oil and gas reserves and resource quantification, hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology ...
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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 tri ...
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Vrelo Bune
''Vrelo Bune'' (; ) is a natural and architectural ensemble located at the spring of the Buna River near Blagaj, a village-town, and is part of the wider "Townscape ensemble of the town of Blagaj — Historical and Natural Heritage of Bosnia and Herzegovina" (featuring Ottoman Mediterranean architecture dating back to 1520), situated southeast of Mostar, Bosnia and Herzegovina. The primary rationale behind the decision of the KONS to designate the site as protected and thus include it in the protected area of Blagaj as a historic urban area, lies in the harmonious coexistence of natural and architectural, cultural, and historical elements, as evidenced by the "distinctive quality of the coexistence of the natural and the man-made" and the "integration of the physical structure into the landscape". Vrelo Bune The Buna river, a short waterway in Bosnia and Herzegovina, serves as a left-bank tributary of the Neretva River. Originating from the Vrelo Bune (), a robust karsti ...
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Hutovo Blato
Hutovo Blato is a nature reserve and bird reserve A bird reserve (also called ornithological reserve) is a wildlife refuge designed to protect bird species. Like other wildlife refuges, the main goal of a reserve is to prevent species from becoming endangered or extinct. Typically, bird species in ... 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 Bird migration, 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 alo ...
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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 is an extension and outlet 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. The river has rich biodiversity, with numerous fish species endemic to the Neretva basin inhabiting Krupa and its lakes. It is observed that important '' Salmo marmoratus'', known under its vernacular name as ''glavatica'' and/or ''gonjavac'', and endemic to the handful of rivers of the Adriatic watershed, enters these waters to spawn. See a ...
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Blagaj, Mostar
Blagaj is a historic village and protected heritage site in Bosnia and Herzegovina. It is located in the south-eastern region of the Mostar basin, in the Herzegovina-Neretva Canton. 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 '' tekija'' (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 ( ...
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Softmouth Trout
''Salmo obtusirostris'', commonly known as the softmouth trout, also known as the Adriatic trout, or Adriatic salmon, is a species of salmonid fish endemic to a handful rivers spilling into Adriatic in the Western Balkans, in southeastern Europe, namely in Bosnia and Herzegovina, Croatia and Montenegro. The scientific name has changed several times through history; synonyms include ''Thymallus microlepis'', ''Salmothymus obtusirostris'' and ''Salar obtusirostris''. This species spawns in the early spring and is an obligatory freshwater fish. They are an important game fish in the region. Distribution and subspecies ''Salmo obtusirostris'' is found naturally in four drainages of the Adriatic Sea, in Croatia, Bosnia and Herzegovina and Montenegro: the Neretva-Vrljika system, the Jadro, the Morača-Zeta system, and possibly the Krka river drainage around Knin although it is presumed extinct for some time now. In addition, sometimes during 1960's, it has been introduced from the Ja ...
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Spring (hydrosphere)
A spring is a natural exit point at which groundwater emerges from an aquifer and flows across the ground surface as surface water. It is a component of the hydrosphere, as well as a part of the water cycle. 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 Hydrostatics#Hydrostatic pressure, hydrostatic pressure. A spring produced by the emergence of Geothermal activity, geothermally heated groundwater is known as a hot spring. The yield (hydrology), yield of spring water 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 water table reaches above the surface level, or if the terrain depression (geology), depresses sharply. Springs may also be formed ...
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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 (''Buna Spring''), is a strong karstic spring located near the village of Blagaj, southeast of Mostar. Vrelo Bune is one of the strongest springs in Europe and has extremely cold water. The Buna flows west for approximately 9 km, starts at Blagaj and, meandering through the villages of Blagaj, Kosor, Malo Polje and Hodbina, joins the Neretva near the settlement Buna. The site of confluence is called Buna Canals. The Bunica river is the main left-bank tributary of the Buna. The Buna is major habitat for an endemic trout species known under its vernacular name as Softmouth trout. See also * Vrelo Bunice * Mostarska Bijela * Hutovo Blato * Daorson Daorson was the capital of the Illyrian tribe of the Daorsi (Ancient Greek Δαόριζοι, Δαούρσιοι; Latin ''Daorsei''). The Daorsi lived in the valley of the Neretva Riv ...
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Karst
Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some evidence that karst may occur in more weathering-resistant rocks such as quartzite given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. 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 Oil and gas reserves and resource quantification, hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology ...
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