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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 the 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beljanica
Beljanica () is a mountains of Serbia, mountain in the Homolje region in eastern Serbia, near the town of Žagubica. 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 2022 census, the town has a total population of 3,595, while the municipality has a population of 18,278. 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 had 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) * Vojnik * Dv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ottoman Empire
The Ottoman Empire (), also called the Turkish Empire, was an empire, imperial realm that controlled much of Southeast Europe, West Asia, and North Africa from the 14th to early 20th centuries; it also controlled parts of southeastern Central Europe, between the early 16th and early 18th centuries. The empire emerged from a Anatolian beyliks, ''beylik'', or principality, founded in northwestern Anatolia in by the Turkoman (ethnonym), Turkoman tribal leader Osman I. His successors Ottoman wars in Europe, conquered much of Anatolia and expanded into the Balkans by the mid-14th century, transforming their petty kingdom into a transcontinental empire. The Ottomans ended the Byzantine Empire with the Fall of Constantinople, conquest of Constantinople in 1453 by Mehmed II. With its capital at History of Istanbul#Ottoman Empire, Constantinople (modern-day Istanbul) and control over a significant portion of the Mediterranean Basin, the Ottoman Empire was at the centre of interacti ... [...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, Strmosten and Jelovac since the mid-19th century. After World War II World War II or the Second World War (1 September 1939 – 2 September 1945) was a World war, global conflict between two coalitions: the Allies of World War II, Allies and the Axis powers. World War II by country, Nearly all of the wo ..., 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 Pomoravlj ... [...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 the 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pannonian Basin
The Pannonian Basin, with the term Carpathian Basin being sometimes preferred in Hungarian literature, is a large sedimentary basin situated in southeastern Central Europe. After the Treaty of Trianon following World War I, the geomorphological term Pannonian Plain was also used for roughly the same region, referring to the lowlands in the area occupied by the Pannonian Sea during the Pliocene Epoch, however some consider the term "Pannonian Plain" not only unhistorical but also topologically erroneous. Terminology The term Pannonian Plain refers to the lowland parts of the Pannonian Basin as well as those of some adjoining regions like Lower Austria, Moravia, and Silesia (Czech Republic and Poland). The lands adjoining the plain proper are sometimes also called ''peri-Pannonian''. In English language, the terms "Pannonian Basin" and "Carpathian Basin" may sometimes be used synonymously, although the latter holds an irredentist Hungarian connotation. The name "Pannon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), 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 (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Resava River
Resava ( sr-Cyrl, Ресава) refers to several toponyms and related topics, all of them located around the river Resava in central Serbia: * Resava (river), a river * Resava (region) 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 the popular ..., a region, surrounding the river ** Upper Resava ** Lower Resava * Resava Monastery, a monastery * Resava school, a cultural movement in 14th-15th century started and funded by Stefan Lazarević * 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] |
Drainage Basin
A drainage basin is an area of land in which 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 the drainage divide line. A drainage basin's boundaries are determined by watershed delineation, a common task in environmental engineering and science. In a closed drainage basin, or endorheic basin, rather than flowing to the ocean, water converges toward the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Black Sea
The Black Sea is a marginal sea, marginal Mediterranean sea (oceanography), mediterranean sea 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 (country), Georgia, Romania, Russia, Turkey, and Ukraine. The Black Sea is Inflow (hydrology), supplied by major rivers, principally the Danube, Dnieper and Dniester. Consequently, while six countries have a coastline on the sea, its drainage basin includes parts of 24 countries in Europe. The Black Sea, not including the Sea of Azov, covers , 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
