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Ribnik (river)
The Ribnik ( cyrl, Рибник, ) is a river in western Bosnia and Herzegovina. It is a headwater tributary of the Sana, which it meat at Strane and Velije hamlets of the Gornji Ribnik village, 17 km below the Sana's own source springs, bringing in a large amounts of water to the still young Sana. It is among shortest of the Sana tributaries but at the same time among largest by the volume it discharges into the receiving Sana. The Ribnik is well known as a prime fly fishing fishery and is popular among anglers throughout the world. __TOC__ Name The name of the river derives from the Slavic word for fish, ''riba'', from which derives ''ribnjak'' or '' ribnik'', a fish pond, a river, or a pool, or a body of water stocked with fish. Geography and hydrology The Ribnik river, just like the Sana in its upper course, is classified mountain river with upland freshwater ecology, with its very clear and cold waters, classified as the Class I (or A) purity. Gushing out of the kars ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gornji Ribnik
Gornji Ribnik ( sr-cyrl, Горњи Рибник) is a village in the municipality of Ribnik, Republika Srpska, Bosnia and Herzegovina Bosnia and Herzegovina ( sh, / , ), abbreviated BiH () or B&H, sometimes called Bosnia–Herzegovina and often known informally as Bosnia, is a country at the crossroads of south and southeast Europe, located in the Balkans. Bosnia and H ....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. The river Ribnik runs through the settlement. References {{Ribnik municipality Populated places in Ribnik Villages in Republika Srpska ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Riba
The Royal Institute of British Architects (RIBA) is a professional body for architects primarily in the United Kingdom, but also internationally, founded for the advancement of architecture under its royal charter granted in 1837, three supplemental charters and a new charter granted in 1971. Founded as the Institute of British Architects in London in 1834, the RIBA retains a central London headquarters at 66 Portland Place as well as a network of regional offices. Its members played a leading part in promotion of architectural education in the United Kingdom; the RIBA Library, also established in 1834, is one of the three largest architectural libraries in the world and the largest in Europe. The RIBA also played a prominent role in the development of UK architects' registration bodies. The institute administers some of the oldest architectural awards in the world, including RIBA President's Medals Students Award, the Royal Gold Medal, and the Stirling Prize. It also manages ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Srnetica
Srnetica ( sr-cyrl, Срнетица) is a village in the municipality of Istočni Drvar (East Drvar), Bosnia and Herzegovina. It lies in western Bosnia, in the part of municipality of Drvar awarded to Republika Srpska Republika Srpska ( sr-Cyrl, Република Српска, lit=Serb Republic, also known as Republic of Srpska, ) is one of the two Political divisions of Bosnia and Herzegovina, entities of Bosnia and Herzegovina, the other being the Feder ..., at a mountain saddle about 1050 metres above sea. From the beginning of 20th century to 1975, there was a main junction of forest narrow-gauge railways built by AG Otto Steinbeis. The tracks are now dismantled and transformed into paths. Demographics According to the 2013 census, its population was nil. References {{coord, 44, 27, 11, N, 16, 35, 52, E, type:city_source:kolossus-frwiki, display=title Populated places in Istočni Drvar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karstic 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Donji Vrbljani
Donji Vrbljani ( sr-cyrl, Доњи Врбљани) is a village in the municipality of Ribnik, Republika Srpska, Bosnia and Herzegovina Bosnia and Herzegovina ( sh, / , ), abbreviated BiH () or B&H, sometimes called Bosnia–Herzegovina and often known informally as Bosnia, is a country at the crossroads of south and southeast Europe, located in the Balkans. Bosnia and H ....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 {{Ribnik municipality Populated places in Ribnik Villages in Republika Srpska ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vitorog
Vitorog ( sr-cyrl, Виторог) is a mountain in the municipality of Glamoč, Bosnia and Herzegovina. It has an altitude of . See also *List of mountains in Bosnia and Herzegovina List of mountains in Bosnia and Herzegovina: References * {{DEFAULTSORT:List Of Mountains In Bosnia and Herzegovina Mountains in Bosnia and Herzegovina Bosnia and Herzegovina Mountains Bos ''Bos'' (from Latin '' bōs'': cow, ... References Mountains of Bosnia and Herzegovina {{Canton10-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Klekovača
Klekovača ( sr-cyrl, Клековача) is a mountain in the Dinaric Alps of western Bosnia and Herzegovina, located near Drvar and Bosanski Petrovac Bosanski Petrovac ( sr-cyrl, Босански Петровац) is a town and municipality located in the Una-Sana Canton of the Federation of Bosnia and Herzegovina, an entity of Bosnia and Herzegovina. As of 2013 census, the municipality has a .... The highest peak is the Velika Klekovača at . References Mountains of Bosnia and Herzegovina {{BosniaHerzegovina-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upland And Lowland
Upland and lowland are conditional descriptions of a plain based on elevation above sea level. In studies of the ecology of freshwater rivers, habitats are classified as upland or lowland. Definitions Upland and lowland are portions of plain that are conditionally categorized by their elevation above the sea level. Lowlands are usually no higher than , while uplands are somewhere around to . On unusual occasions, certain lowlands such as the Caspian Depression lie below sea level. Upland habitats are cold, clear and rocky whose rivers are fast-flowing in mountainous areas; lowland habitats are warm with slow-flowing rivers found in relatively flat lowland areas, with water that is frequently colored by sediment and organic matter. These classifications overlap with the geological definitions of "upland" and "lowland". In geology an "upland" is generally considered to be land that is at a higher elevation than the alluvial plain or stream terrace, which are considered t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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