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Resava River
The Resava ( sr-Cyrl, Ресава) is a river in central Serbia, a 65 km-long right tributary to the Velika Morava. It also gives the name to the surrounding Resava region, the Resava Monastery, the coal mines in its valley and a popular tourist destination of Resava Cave. River The Resava originates from the Homolje region in eastern Serbia. It springs out at an altitude of 1,100 m and flows westward between the mountains of Beljanica (on the north) and Kučaj (on the south). In its upper course, the Resava runs parallel to its left tributary, the ''Kločanica'', and area around the villages of Strmosten, Vodna and Stenjevac is known for many caves ('' Resava Cave'', ''Sokolica'', ''Crystal'', etc.). The Resava carved a 25 km-long and 400 m-deep gorge, with a central part of it representing a typical canyon valley, the ''Sklop''. In the gorge, the river becomes a sinking river for a while and creates a 25 m-high waterfall, until recently, the highest one in cen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beljanica
Beljanica () is a mountain in the Homolje region in eastern Serbia, near the town of Žagubica Žagubica ( sr-cyr, Жагубица, ; ro, Jagubița or ) is a village and municipality located in the Braničevo District of the eastern Serbia. It is situated in the geographical region of Homolje. In 2011, the population of the village is 2 .... Its highest peak has an elevation of 1,339 meters above sea level. References Mountains of Serbia Serbian Carpathians {{Serbia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Despotovac
Despotovac ( sr-cyr, Деспотовац) is a town and municipality located in the Pomoravlje District of central Serbia. It is 130 kilometers southeast of Belgrade. Its name stems from Despot, a title of Serbian medieval prince Stefan Lazarević. As of 2011 census, the town has a total population of 4,212, while the municipality has a population of 22,995. History The Serb Orthodox monastery of Manasija was built between 1406-1418 and is one of the most significant monuments of Serbian culture, belonging to the "Resava school" (Serbian architecture) From 1929 to 1941, Despotovac was part of the Morava Banovina of the Kingdom of Yugoslavia. Demographics As of 2011 census results, the municipality has 22,995 inhabitants. Ethnic groups The ethnic composition of the municipality: Settlements Aside from the town of Despotovac, the municipality includes the following settlements: * Balajnac * Beljajka * Bogava * Brestovo * Bukovac * Despotovac (town) * Despotovac * Dvori ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ottoman Empire
The Ottoman Empire, * ; is an archaic version. The definite article forms and were synonymous * and el, Оθωμανική Αυτοκρατορία, Othōmanikē Avtokratoria, label=none * info page on book at Martin Luther University) // CITED: p. 36 (PDF p. 38/338) also known as the Turkish Empire, was an empire that controlled much of Southeast Europe, Western Asia, and Northern Africa between the 14th and early 20th centuries. It was founded at the end of the 13th century in northwestern Anatolia in the town of Söğüt (modern-day Bilecik Province) by the Turkoman tribal leader Osman I. After 1354, the Ottomans crossed into Europe and, with the conquest of the Balkans, the Ottoman beylik was transformed into a transcontinental empire. The Ottomans ended the Byzantine Empire with the conquest of Constantinople in 1453 by Mehmed the Conqueror. Under the reign of Suleiman the Magnificent, the Ottoman Empire marked the peak of its power and prosperity, as well a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Resavica (Despotovac)
Resavica ( sr-cyr, Ресавица) is a mining town located in the municipality of Despotovac, central Serbia. As of 2011 census, it has a population of 2,035 inhabitants. Mining history Resavica lies at the core of a brown coal basin of central-eastern Serbia. The coal was exploited in the area, with shafts in Senjski Rudnik Senjski Rudnik ( sr-cyr, Сењски Рудник) is a village located in the municipality of Despotovac, eastern Serbia. According to the 2011 census, it had a population of 438 inhabitants. It is the site of the oldest preserved coal mine in S ..., Strmosten and Jelovac since the mid-19th century. After World War II, the mines were nationalized, and a state-owned company "Senje-Resava Brown Coal Mines" was formed, with the seat in Resavica. It went through several renames and reorganizations, and today Resavica is the seat of mine company "Rembas", with shafts in Jelovac, Strmosten and Senjski Rudnik. References Populated places in Pomoravlje D ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Resava Coal Mines
Resava (Serbian Cyrillic: Ресава) refers to several toponyms and related topics, all of them located around the river Resava in central Serbia: * Resava (river), a river * Resava, a region, surrounding the river * Resava, a monastery * Resava school, a cultural movement in 14th-15th century started and funded by Stefan Lazarević Stefan Lazarević ( sr-Cyrl, Стефан Лазаревић, 1377 – 19 July 1427), also known as Stefan the Tall ( sr, Стефан Високи / ''Stefan Visoki''), was the ruler of Serbia as prince (1389–1402) and despot (1402–1427), ... * Resava Coal Mines, (or REMBAS) coal mines in the Resava river valley * Resava Cave, a cave and popular tourist attraction {{disambig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pannonian Plain
The Pannonian Basin, or Carpathian Basin, is a large basin situated in south-east Central Europe. The geomorphological term Pannonian Plain is more widely used for roughly the same region though with a somewhat different sense, with only the lowlands, the plain that remained when the Pliocene Epoch ''Pannonian Sea'' dried out. It is a geomorphological subsystem of the Alps-Himalaya system, specifically a sediment-filled back-arc basin which spread apart during the Miocene. The plain or basin is diagonally bisected by the Transdanubian Mountains, separating the larger Great Hungarian Plain (including the Eastern Slovak Lowland) from the Little Hungarian Plain. It forms a topographically discrete unit set in the European landscape, surrounded by imposing geographic boundaries—the Carpathian Mountains and the Alps. The Rivers Danube and Tisza divide the basin roughly in half. It extends roughly between Vienna in the northwest, Košice in the northeast, Zagreb in the southwe ... [...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] |
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] |
Resava River
The Resava ( sr-Cyrl, Ресава) is a river in central Serbia, a 65 km-long right tributary to the Velika Morava. It also gives the name to the surrounding Resava region, the Resava Monastery, the coal mines in its valley and a popular tourist destination of Resava Cave. River The Resava originates from the Homolje region in eastern Serbia. It springs out at an altitude of 1,100 m and flows westward between the mountains of Beljanica (on the north) and Kučaj (on the south). In its upper course, the Resava runs parallel to its left tributary, the ''Kločanica'', and area around the villages of Strmosten, Vodna and Stenjevac is known for many caves ('' Resava Cave'', ''Sokolica'', ''Crystal'', etc.). The Resava carved a 25 km-long and 400 m-deep gorge, with a central part of it representing a typical canyon valley, the ''Sklop''. In the gorge, the river becomes a sinking river for a while and creates a 25 m-high waterfall, until recently, the highest one in cen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Black Sea
The Black Sea is a marginal mediterranean sea of the Atlantic Ocean lying between Europe and Asia, east of the Balkans, south of the East European Plain, west of the Caucasus, and north of Anatolia. It is bounded by Bulgaria, Georgia, Romania, Russia, Turkey, and Ukraine. The Black Sea is supplied by major rivers, principally the Danube, Dnieper, and Don. Consequently, while six countries have a coastline on the sea, its drainage basin includes parts of 24 countries in Europe. The Black Sea covers (not including the Sea of Azov), has a maximum depth of , and a volume of . Most of its coasts ascend rapidly. These rises are the Pontic Mountains to the south, bar the southwest-facing peninsulas, the Caucasus Mountains to the east, and the Crimean Mountains to the mid-north. In the west, the coast is generally small floodplains below foothills such as the Strandzha; Cape Emine, a dwindling of the east end of the Balkan Mountains; and the Dobruja Plateau considerably farth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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