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Ozren (Bosnia And Herzegovina)
Ozren is a mountain in northern Bosnia and Herzegovina. It lies between cities of Doboj and Zavidovići, partly in the Federation of Bosnia and Herzegovina, Federation and partly in the Republika Srpska entity. Ozren is rich in natural resources. It abounds in drinkable water springs surrounded by clean nature, hot spring, thermal wells with healing effects, ore and mineral resources. Its highest peak, Ostravica, is 918 meters high. References

{{Authority control Mountains of the Federation of Bosnia and Herzegovina Mountains of Republika Srpska Mountains of Bosnia and Herzegovina ...
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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 Herzegovina borders Serbia to the east, Montenegro to the southeast, and Croatia to the north and southwest. In the south it has a narrow coast on the Adriatic Sea within the Mediterranean, which is about long and surrounds the town of Neum. Bosnia, which is the inland region of the country, has a moderate continental climate with hot summers and cold, snowy winters. In the central and eastern regions of the country, the geography is mountainous, in the northwest it is moderately hilly, and in the northeast it is predominantly flat. Herzegovina, which is the smaller, southern region of the country, has a Mediterranean climate and is mostly mountainous. Sarajevo is the capital and the largest city of the country followed by Banja Luka, Tu ...
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Doboj
Doboj ( sr-cyrl, Добој, ) is a city located in Republika Srpska, an entity of Bosnia and Herzegovina. It is situated on the banks of Bosna river, in the northern region of the Republika Srpska. As of 2013, it has a population of 71,441 inhabitants. Doboj is the largest national railway junction and the operational base of the Railways Corporation of Bosnia and Herzegovina is located in Doboj. It is one of the oldest cities in Bosnia and Herzegovina and the most important urban center in northern Republika Srpska. Geography Prior to the war in Bosnia the municipality of the same name had a larger surface area. The largest part of the pre-war municipality is part of the Republika Srpska, including the city itself, (the Doboj Region). The southern rural areas are part of the Zenica-Doboj Canton of the Federation of Bosnia and Herzegovina, and the eastern rural part of the municipality is part of the Tuzla Canton, also in the Federation of Bosnia and Herzegovina. The parts ...
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Zavidovići
Zavidovići ( sr-cyrl, Завидовићи) is a town and municipality located in Zenica-Doboj Canton of the Federation of Bosnia and Herzegovina, an entity of Bosnia and Herzegovina. It is situated in central Bosnia and Herzegovina, located between Doboj and Zenica on the confluence of rivers Bosna, Krivaja and Gostović. It sits in a valley surrounded by many mountains of which the largest is Klek. As of 2013, the municipality had a population of 35,988 inhabitants and the town itself 8,174. History Zavidovići was home to two neolithic cultures: Butmir and Kakanj. Significant Kakanj culture site is located in Tuk. Zavidovići was developed by the Austrians during the 19th century Austro-Hungarian reign in Bosnia, mostly because of the "wood industry". After World War II, Krivaja, the company that was founded in 1884 and named after the Krivaja river, expanded. The company focused on furniture manufacturing, which it began to export to the United States under the name "K ...
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Federation Of Bosnia And Herzegovina
The Federation of Bosnia and Herzegovina is one of the two Political divisions of Bosnia and Herzegovina, entities within the State of Bosnia and Herzegovina, the other being Republika Srpska. The Federation of Bosnia and Herzegovina consists of 10 autonomous Cantons of the Federation of Bosnia and Herzegovina, cantons with their own governments and legislatures. The Federation was created by the 1994 Washington Agreement (1994), Washington Agreement, which ended the Croat–Bosniak War within the Bosnian War, and established a constituent assembly that continued its work until October 1996. The Federation has a Sarajevo, capital, Government of Bosnia and Herzegovina, government, president, parliament, customs and police departments and two postal systems. It occupies about half of the land of Bosnia and Herzegovina. From 1996 until 2005 it had its own army, the Army of the Federation of Bosnia and Herzegovina, later merged in the Armed Forces of Bosnia and Herzegovina. The ca ...
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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 Federation of Bosnia and Herzegovina. It is located in the north and east of the country. Its largest city and administrative centre is Banja Luka, lying on the Vrbas (river), Vrbas river. Republika Srpska was formed in 1992 at the outset of the Bosnian War with the stated intent to safeguard the interests of the Serbs of Bosnia and Herzegovina. The war saw the Ethnic cleansing in the Bosnian War, expulsion of the vast majority of Croats of Bosnia and Herzegovina, Croats and Bosniaks from the territory claimed by Republika Srpska and an inflow of Serbs expelled from Federation of Bosnia and Herzegovina. Following the Dayton Agreement of 1995, Republika Srpska achieved international recognition as an entity within Bosnia and Herzegovina. ...
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Hot Spring
A hot spring, hydrothermal spring, or geothermal spring is a spring produced by the emergence of geothermally heated groundwater onto the surface of the Earth. The groundwater is heated either by shallow bodies of magma (molten rock) or by circulation through faults to hot rock deep in the Earth's crust. In either case, the ultimate source of the heat is radioactive decay of naturally occurring radioactive elements in the Earth's mantle, the layer beneath the crust. Hot spring water often contains large amounts of dissolved minerals. The chemistry of hot springs ranges from acid sulfate springs with a pH as low as 0.8, to alkaline chloride springs saturated with silica, to bicarbonate springs saturated with carbon dioxide and carbonate minerals. Some springs also contain abundant dissolved iron. The minerals brought to the surface in hot springs often feed communities of extremophiles, microorganisms adapted to extreme conditions, and it is possible that life on Earth had its ...
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Mountains Of The Federation Of Bosnia And Herzegovina
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Mountains Of Republika Srpska
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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