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Trebišnjica
The Trebišnjica ( sr-cyrl, Требишњица) is a river in Bosnia and Herzegovina, and the right tributary of the Neretva. Before it was utilized for hydro exploitation via various hydrotechnical interventions and systems with different purposes, Trebišnjica used to be a sinking river, rising and sinking through its course before resurfacing at various places from the Neretva river below the Čapljina to the Adriatic Sea, Adriatic coast, and along the coast from the Neretva Delta to Sutorina. With a total length of above the ground, and roughly another below the surface, the Trebšnjica river is one of the longest sinking rivers in the world with the total of above and under the ground. In hydrological terms, it represents a sub-basin within the Neretva river basin. In classical antiquity, the river was known as the Arion, Sources The Trebišnjica river originate near town of Bileća. The source of the river is a system of strong karst spring, karstic wellsprings distr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trebišnjica Wellsprings Group
Trebišnjica wellspring-group is a system of two geographically and hydrologically distinct principal groupings of strong karst spring, karstic springs, Trebišnjica and Čeplica, which together constitute source of the Trebišnjica river. Wellsprings are located just below town of Bileća in Bosnia and Herzegovina. The entire area where founts are situated is submerged under Bilećko Lake since 1967, formed after the construction of Trebinje-1 Hydroelectric Power Station and its large arch dam at Grnčarevo village. Springs The Trebišnjica river emerges under the karst, karstic plateau on which town of Bileća sits. There are two main spring-groups, first in immediate proximity of town itself, and second little more than 3 kilometers downstream at Čepelica village. Trebišnjica spring-group The Trebišnjica spring-group at Bileća, at a.s.l., is composed of three major wellspring outlets, "Dejanova Pećina", "Vrelo Oko", and "Nikšičko Vrelo". Čepelica spring-group Another ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neretva River
The Neretva (, sr-Cyrl, Неретва), also known as Narenta, is one of the largest rivers of the eastern part of the Adriatic basin. Four hydroelectric power plants with large dams (higher than 15 metres) provide flood protection, electricity and water storage. The Neretva is recognized for its natural environment and diverse landscapes. 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 bee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Hydroelectricity, hydroelectric power plants with Dam, large dams (higher than 15 metres) provide flood protection, electricity and water storage. The Neretva is recognized for its natural environment and diverse landscapes. 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 spring (hydrosphere), wellspring and clear rivers. Situated between the major regional rivers (Drina river on the east, Una (Sava), 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 faun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Vrutak
Lake Vrutak is artificial reservoir on the Trebišnjica river in Popovo Polje, near Hutovo village, Bosnia and Herzegovina. The lake serves as compensation and storage basin for Pump-Storage Hydroelectric Power Plant "Čapljina". Hydropower and irrigation system Lake Vrutak is the last and smallest of three artificial reservoirs in hydroelectric power plant system Trebišnjica - HES "Donji Horizonti", and serves as compensation basin for Pump-Storage Hydroelectric Power Plant "Čapljina". Other two being Bilećko Lake, the first and largest, and flow-regulation (compensation) basin Trebinjsko Lake just upstream of Trebinje. ''(pdf)''; Hidroenergetski sistem sliva Neretva-Trebišnjics: CHE "Čapljina" - JP "EP HZHB" ''(Bosanski/Hrvatski/Srpski)'' S ...
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Ombla
The Ombla is a short river in Croatia, northeast of Dubrovnik. Its course is approximately long, and it empties into the Rijeka Dubrovačka, ria formed by the Adriatic Sea near Komolac in Dubrovnik-Neretva County. Rijeka Dubrovačka is actually a ria, a flooded river valley formed through changes in sea surface elevation on a geologic time scale. The river rises as a karst spring fed by groundwater replenished by Trebišnjica, which is an influent stream flowing in Popovo Polje, in the immediate hinterland of the Ombla. The elevation difference between the river's source and its mouth is just over . The average discharge of the river is per second. The drainage basin of the Ombla encompasses and, besides the short surface course, includes only groundwater flow. The Ombla is used as a source of drinking water for Dubrovnik's water supply network, and construction of a hydroelectric power plant has been planned for the past two decades. , the plans entail construction of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sinking River
A losing stream, disappearing stream, influent stream or sinking river is a stream or river that loses water as it flows downstream. The water infiltrates into the ground recharging the local groundwater, because the water table is below the bottom of the stream channel. This is the opposite of a more common ''gaining stream'' (or ''effluent stream'') which increases in water volume farther downstream as it gains water from the local aquifer. Losing streams are common in arid areas due to the climate which results in huge amounts of water evaporating from the river generally towards the mouth. Losing streams are also common in regions of karst topography where the streamwater may be completely captured by a cavern system, becoming a subterranean river. Examples There are many natural examples of subterranean rivers including: Bosnia and Herzegovina * Unac; Mušnica-Trebišnjica- Krupa/Ombla (Trebišnjica is considered to be one of the largest sinking rivers in the world; ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Čepelica River
Čepelica ( sr-cyrl, Чепелица) is a village and the small river in the municipality of Bileća, Republika Srpska, Bosnia and Herzegovina Bosnia and Herzegovina, sometimes known as Bosnia-Herzegovina and informally as Bosnia, is a country in Southeast Europe. Situated on the Balkans, Balkan Peninsula, it borders Serbia to the east, Montenegro to the southeast, and Croatia to th ....Official results from the book: Ethnic composition of Bosnia-Herzegovina population, by municipalities and settlements, 1991. census, Zavod za statistiku Bosne i Hercegovine - Bilten no.234, Sarajevo 1991. References Villages in Republika Srpska Populated places in Bileća Lower Horizons Hydroelectric Power Stations System Trebišnjica {{Bileća-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Estavelles
In karst geology, estavelle or inversac is a ground orifice which, depending on weather conditions and season, can serve either as a sink or as a source of fresh water. It is a type of ponor or sinkhole A sinkhole is a depression or hole in the ground caused by some form of collapse of the surface layer. The term is sometimes used to refer to doline, enclosed depressions that are also known as shakeholes, and to openings where surface water .... References Karst Cave geology Dinaric karst formations Dinaric Alps {{geology-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vrelo Čepo
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Vrelo may refer to: Places Bosnia and Herzegovina * Vrelo (Cazin) Kosovo * Vrelo (Istok) Serbia * Vrelo (Aleksinac) * Vrelo (Babušnica) * Vrelo (Kuršumlija) * Vrelo (Niš) * Vrelo (Ub) Other * Vrelo (river) Vrelo ( sr-Cyrl, Врело) is a right tributary of the river Drina in the settlement of Perućac, Bajina Bašta Municipality in Serbia. The river is only 365 meters long and is probably one of the shortest rivers in the world. Course The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aquifer
An aquifer is an underground layer of water-bearing material, consisting of permeability (Earth sciences), permeable or fractured rock, or of unconsolidated materials (gravel, sand, or silt). Aquifers vary greatly in their characteristics. The study of water flow in aquifers and the characterization of aquifers is called ''hydrogeology''. Related concepts include aquitard, a bed (geology), bed of low permeability along an aquifer, and aquiclude (or ''aquifuge''), a solid and impermeable region underlying or overlying an aquifer, the pressure of which could lead to the formation of a confined aquifer. Aquifers can be classified as saturated versus unsaturated; aquifers versus aquitards; confined versus unconfined; isotropic versus anisotropic; porous, karst, or fractured; and transboundary aquifer. Groundwater from aquifers can be sustainably harvested by humans through the use of qanats leading to a well. This groundwater is a major source of fresh water for many regions, althoug ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
