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Upper Drina
The Drina ( sr-Cyrl, Дрина, ) is a long river in the Balkans, which forms a large portion of the border between Bosnia and Herzegovina and Serbia. It is the longest tributary of the Sava River and the longest karst river in the Dinaric Alps which belongs to the Danube River drainage basin. Its name is derived from the Ancient Rome, Roman name of the river () which in turn is derived from Greek language, Greek (Ancient Greek: ) which is derived from the native name of Illyrian language, Illyrian origin. But, this etymology is not sure.Illyrian languages are poorly documented (only ~50 glosses, mostly personal/place names). - No surviving texts exist, unlike Thracian (which has ~200 inscriptions and loanwords in Greek). - Scholars often label any pre-Slavic Balkan hydronym as "Illyrian" by default, even without proof.We don’t know if Drinus was Illyrian, Thracian, or another lost Paleo-Balkan language. - The safest claim: Drina derives from a ancient Indo-European roo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drin River
The Drin (; or ; ) is a river in Southeastern Europe with two major tributaries – the White Drin and the Black Drin and two distributary, distributaries – one discharging into the Adriatic Sea, in the Gulf of Drin and the other into the Buna (Adriatic Sea), Buna River. Its drainage basin, catchment area extends across Albania, Kosovo, Serbia, Greece, Montenegro and North Macedonia and is home to more than 1.6 million people. The river and its tributaries form the Gulf of Drin, an ocean basin that encompasses the northern Albanian Adriatic Sea Coast. At long, the Drin is the Rivers of Albania, longest river of Albania and its tributaries cross through both Kosovo and North Macedonia. Its northern tributary, the White Drin starts from the foothills of Žljeb mountain, Žljeb, at White Drin Waterfall in west Kosovo, and flows generally south, whereas its southern tributary, the Black Drin originates from Ohrid lake in the town of Struga, North Macedonia and flows north. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ancient Rome
In modern historiography, ancient Rome is the Roman people, Roman civilisation from the founding of Rome, founding of the Italian city of Rome in the 8th century BC to the Fall of the Western Roman Empire, collapse of the Western Roman Empire in the 5th century AD. It encompasses the Roman Kingdom (753–509 BC), the Roman Republic (50927 BC), and the Roman Empire (27 BC476 AD) until the fall of the western empire. Ancient Rome began as an Italic peoples, Italic settlement, traditionally dated to 753 BC, beside the River Tiber in the Italian peninsula. The settlement grew into the city and polity of Rome, and came to control its neighbours through a combination of treaties and military strength. It eventually controlled the Italian Peninsula, assimilating the Greece, Greek culture of southern Italy (Magna Graecia) and the Etruscans, Etruscan culture, and then became the dominant power in the Mediterranean region and parts of Europe. At its hei ... [...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] |
Albania
Albania ( ; or ), officially the Republic of Albania (), is a country in Southeast Europe. It is located in the Balkans, on the Adriatic Sea, Adriatic and Ionian Seas within the Mediterranean Sea, and shares land borders with Montenegro to the northwest, Kosovo to the northeast, North Macedonia to the east and Greece to the south. With an area of , it has a varied range of climatic, geological, hydrological and morphological conditions. Albania's landscapes range from rugged snow-capped mountains in the Accursed Mountains, Albanian Alps and the Korab, Central Mountain Range, Albania#Skanderbeg Mountains, Skanderbeg, Pindus and Ceraunian Mountains, to fertile lowland plains extending from the Albanian Adriatic Sea Coast, Adriatic and Albanian Ionian Sea Coast, Ionian seacoasts. Tirana is the capital and largest city in the country, followed by Durrës, Vlorë, and Shkodër. Albania was inhabited by several List of Illyrian peoples and tribes, Illyrian tribes, among them the A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ljubovija
Ljubovija ( sr-cyr, Љубовија, ) is a small town and municipality located in the Mačva District The Mačva District (, ) is one of administrative districts of Serbia. It lies in the western part of Serbia, in the geographical regions of Mačva, Podrinje, Posavina, and Pocerina. According to the 2022 census, it has a population of 265,3 ... of western Serbia. As of 2022, the population of the municipality is 12,168 inhabitants. Settlements Aside from the town of Ljubovija, the municipality includes the following settlements: * Berlovine * Vrhpolje * Gornja Ljuboviđa * Gornja Orovica * Gornja Trešnjica * Gornje Košlje * Gračanica * Grčić * Donja Ljuboviđa * Donja Orovica * Drlače * Duboko * Leović * Lonjin * Orovička Planina * Podnemić * Postenje * Rujevac * Savković * Selenac * Sokolac * Tornik * Uzovnica * Caparić * Crnča * Čitluk Demographics According to the 2022 census results, the municipality of Ljubovija has 12,168 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bajina Bašta
Bajina Bašta ( sr-Cyrl, Бајина Башта, ) is a town and municipality located in the Zlatibor District of western Serbia. The town lies in the valley of the Drina river at the eastern edge of Tara National Park. According to the 2022 census, the town's population is 8,971 inhabitants, while the municipality has 23,533 inhabitants. Etymology The name comes from the vast orchards and vegetable gardens, that used to be located on the left bank of the Pilica River, which belonged to a Turkish feudal owner, Baja Osman, who established the town's modern image in the mid-19th century. In English, the name ' literally means "Baja’s Garden". History In 1834 was established on the remains of the old Turkish community of Pljeskovo which was situated on the right bank of the Drina, Drina River between the Rača River, Rača and Pilica River, Pilica Rivers, under the eastern foothills of Tara Mountain. By the end of the 19th century, in accordance with the Serbian-Turkish agr ... [...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] |
Flysch
Flysch () is a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones. It is deposited when a deep basin forms rapidly on the continental side of a mountain building episode. Examples are found near the North American Cordillera, the Alps, the Pyrenees and the Carpathians. Sedimentological properties Flysch consists of repeated sedimentary cycles with upwards fining of the sediments. There are sometimes coarse conglomerates or breccias at the bottom of each cycle, which gradually evolve upwards into sandstone and shale/mudstone. Flysch typically consists of a sequence of shales rhythmically interbedded with thin, hard, graywacke-like sandstones. Typically the shales do not contain many fossils, while the coarser sandstones often have fractions of micas and glauconite. Tectonics In a continental collision, a subducting tectonic plate pushes on the plate above it, making the rock fold, often t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meandering Ratio
Sinuosity, sinuosity index, or sinuosity coefficient of a continuously differentiable curve having at least one inflection point is the ratio of the curvilinear length (along the curve) and the Euclidean distance (straight line) between the end points of the curve. This dimensionless quantity can also be rephrased as the "actual path length" divided by the "shortest path length" of a curve. The value ranges from 1 (case of straight line) to infinity (case of a closed loop, where the shortest path length is zero for an infinitely-long actual path). Interpretation The curve must be continuous (no jump) between the two ends. The sinuosity value is really significant when the line is continuously differentiable (no angular point). The distance between both ends can also be evaluated by a plurality of segments according to a broken line passing through the successive inflection points (sinuosity of order 2). The calculation of the sinuosity is valid in a 3-dimensional space (e.g. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tara (Drina)
The Tara ( sr-cyrl, Тара) is a river in Montenegro and Bosnia and Herzegovina. It emerges from the confluence of the Opasnica and Veruša rivers in the Komovi Mountains, part of the Dinaric Alps of Montenegro. The total length is , of which are in or on the border of Montenegro,Statistical Yearbook of Montenegro 2017, Geography Statistical Office of Montenegro it also forms the border between the two countries in several places. The Tara flows from south to north - north-west and converges with the Piva at the Bosnia and Herzegovina and Montenegro border between the villages of Šćepan Polje (Montenegro) and Hum (Bosnia and Herzegovina) to form the |
