Lake Zavoj
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Lake Zavoj
Zavoj Lake ( Serbian: Завојско језеро, ''Zavojsko jezero'') is an artificial lake in eastern Serbia, on the Visočica River. It was created in 1963 after a major landslide which dammed the river and the natural dam was later replaced with a hydroelectric dam "Zavoj". Location Lake Zavoj is located in eastern Serbia, in the northern part of the Visok region, close to the Serbian-Bulgarian border. Lake is in the valley of the Visočica River which is both its major tributary and outflow, between the mountains of Stara Planina on the north and Vidlič on the south. Lake is located north of the town of Pirot, close to the Visočica mouth into the Temštica river and is not well connected with the rest of Serbia. Settlements in the vicinity of the lake, which is among the least populated in the entire Serbia, include Novi Zavoj, Velika Lukanja and Pakleštica. History On February 25, 1963 a huge landslide from the sunny side of the Stara Planina rushed into the ...
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Pirot District
The Pirot District ( sr, Пиротски Округ, Pirotski Okrug, ) is one of nine administrative districts of Southern and Eastern Serbia. It expands to the south-eastern parts of Serbia. According to the 2011 census results, it has a population of 92,277 inhabitants. The administrative center is the city of Pirot. Municipalities It encompasses the city of Pirot and the following municipalities: * Bela Palanka * Babušnica * Dimitrovgrad Demographics According to the 2011 census results, Pirot District has a population of 92,479 inhabitants. Ethnic groups History and culture The first mention of Pirot are found already in the second century A.D. In its vicinity is the church from the thirteenth century: the Church of St. Petka, and the monastery of St. John the Theologist from the late fourteenth century displays a fine example of the medieval architecture. Features Medicinal water from the Zvonci Spa (Zvonačka Banja), a health resort, was used already in the ancie ...
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Temštica
Temštica ( sr, Темштица) or Temska is a river in Serbia, a right tributary of the river Nišava. The Temštica itself is not very long (23 km), but receives a much longer tributary, the Visočica (Височица), flowing from Bulgaria (16.7 km in length), through Serbia (54 km in length) making ''Visočica and Temštica river system'' 93.7 km long. Temštica (Toplodolska reka) The Temštica, known as the Topli Do river (''Toplodolska reka'', Топлодолска река) in the northern part, originates from five streams from the Stara Planina mountain on the Serbian–Bulgarian border. Three major streams spring out from several peaks of Stara Planina: Midžor/Midzhur (Миџор/Миджур), Vražija Glava/Vrazha glava (Вражија Глава/Вража глава), Bratkova Strana (Браткова Страна) and Gola Glava (Гола Глава). They all join together near the village of Topli Dol, which gives the alternative name ...
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Triassic System Of Europe
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ...
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Lakes Of Serbia
Most lakes of Serbia are artificial, created by damming numerous rivers of Serbia for the purpose of obtaining hydroelectric power or as water reservoirs. Natural lakes in the Pannonian Plain are shallow, occurred as river arms or bogs, or by aeolian erosion. Few natural lakes in the mountains are of glacial origin. List of lakes The list of lakes of Serbia, excluding the territory of Kosovo. *Note: in Serbian, word for lake (''jezero'') is almost always a part of the lake's name. If the name is given as a noun, ''jezero'' precedes it (Jezero Gazivode), if the name is given as an adjective (usually with the ''-ko'' suffix), ''jezero'' comes after (Vlasinsko jezero). See also * List of rivers of Serbia * List of mountains of Serbia References {{Authority control * Serbia Serbia (, ; Serbian: , , ), officially the Republic of Serbia (Serbian: , , ), is a landlocked country in Southeastern and Central Europe, situated at the crossroads of the Pannonian Basin an ...
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List Of Lakes In Serbia
Most lakes of Serbia are artificial, created by damming numerous rivers of Serbia for the purpose of obtaining hydroelectric power or as water reservoirs. Natural lakes in the Pannonian Plain are shallow, occurred as river arms or bogs, or by aeolian erosion. Few natural lakes in the mountains are of glacial origin. List of lakes The list of lakes of Serbia, excluding the territory of Kosovo. *Note: in Serbian, word for lake (''jezero'') is almost always a part of the lake's name. If the name is given as a noun, ''jezero'' precedes it (Jezero Gazivode), if the name is given as an adjective (usually with the ''-ko'' suffix), ''jezero'' comes after (Vlasinsko jezero). See also * List of rivers of Serbia * List of mountains of Serbia References {{Authority control * Serbia Lakes A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are ...
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Mollusk Shell
The mollusc (or molluskOften spelled mollusk shell in the USA; the spelling "mollusc" are preferred by ) shell is typically a calcareous exoskeleton which encloses, supports and protects the soft parts of an animal in the phylum Mollusca, which includes snails, clams, tusk shells, and several other classes. Not all shelled molluscs live in the sea; many live on the land and in freshwater. The ancestral mollusc is thought to have had a shell, but this has subsequently been lost or reduced on some families, such as the squid, octopus, and some smaller groups such as the caudofoveata and solenogastres. Today, over 100,000 living species bear a shell; there is some dispute as to whether these shell-bearing molluscs form a monophyletic group (conchifera) or whether shell-less molluscs are interleaved into their family tree. Malacology, the scientific study of molluscs as living organisms, has a branch devoted to the study of shells, and this is called conchology—although these te ...
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Tethys Ocean
The Tethys Ocean ( el, Τηθύς ''Tēthús''), also called the Tethys Sea or the Neo-Tethys, was a prehistoric ocean that covered most of the Earth during much of the Mesozoic Era and early Cenozoic Era, located between the ancient continents of Gondwana and Laurasia, before the opening of the Indian and Atlantic oceans during the Cretaceous Period. It was preceded by the Paleo-Tethys Ocean, which lasted between the Cambrian and the Early Triassic, while the Neotethys formed during the Late Triassic and lasted until the early Eocene (about 50 million years ago) when it completely closed. A portion known as the Paratethys formed during the Late Jurassic, was isolated during the Oligocene (34 million years ago) and lasted up to the Pliocene (about 5 million years ago), when it largely dried out. Many major seas and lakes of Europe and Western Asia, including the Mediterranean Sea, the Black Sea, the Caspian Sea, and the Aral Sea are thought to be remnants of the Paratethys. Ety ...
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Upper Triassic
The Late Triassic is the third and final epoch of the Triassic Period in the geologic time scale, spanning the time between Ma and Ma (million years ago). It is preceded by the Middle Triassic Epoch and followed by the Early Jurassic Epoch. The corresponding series of rock beds is known as the Upper Triassic. The Late Triassic is divided into the Carnian, Norian and Rhaetian Ages. Many of the first dinosaurs evolved during the Late Triassic, including ''Plateosaurus'', ''Coelophysis'', and ''Eoraptor''. The Triassic–Jurassic extinction event began during this epoch and is one of the five major mass extinction events of the Earth. Etymology The Triassic was named in 1834 by Friedrich von Alberti, after a succession of three distinct rock layers (Greek meaning 'triad') that are widespread in southern Germany: the lower Buntsandstein (colourful sandstone'')'', the middle Muschelkalk (shell-bearing limestone) and the upper Keuper (coloured clay). The Late Triassic Series co ...
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Freiburg
Freiburg im Breisgau (; abbreviated as Freiburg i. Br. or Freiburg i. B.; Low Alemannic: ''Friburg im Brisgau''), commonly referred to as Freiburg, is an independent city in Baden-Württemberg, Germany. With a population of about 230,000 (as of 31 December 2018), Freiburg is the fourth-largest city in Baden-Württemberg after Stuttgart, Mannheim, and Karlsruhe. The population of the Freiburg metropolitan area was 656,753 in 2018. In the south-west of the country, it straddles the Dreisam river, at the foot of the Schlossberg. Historically, the city has acted as the hub of the Breisgau region on the western edge of the Black Forest in the Upper Rhine Plain. A famous old German university town, and archiepiscopal seat, Freiburg was incorporated in the early twelfth century and developed into a major commercial, intellectual, and ecclesiastical center of the upper Rhine region. The city is known for its medieval minster and Renaissance university, as well as for its high stand ...
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Paleobiology
Paleobiology (or palaeobiology) is an interdisciplinary field that combines the methods and findings found in both the earth sciences and the life sciences. Paleobiology is not to be confused with geobiology, which focuses more on the interactions between the biosphere and the physical Earth. Paleobiological research uses biological field research of current biota and of fossils millions of years old to answer questions about the molecular evolution and the evolutionary history of life. In this scientific quest, macrofossils, microfossils and trace fossils are typically analyzed. However, the 21st-century biochemical analysis of DNA and RNA samples offers much promise, as does the biometric construction of phylogenetic trees. An investigator in this field is known as a paleobiologist. Important research areas *Paleobotany applies the principles and methods of paleobiology to flora, especially green land plants, but also including the fungi and seaweeds (algae). See also myc ...
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Zavojsko Jezero
Zavoj Lake (Serbian: Завојско језеро, ''Zavojsko jezero'') is an artificial lake in eastern Serbia, on the Visočica River. It was created in 1963 after a major landslide which dammed the river and the natural dam was later replaced with a hydroelectric dam "Zavoj". Location Lake Zavoj is located in eastern Serbia, in the northern part of the Visok region, close to the Serbian- Bulgarian border. Lake is in the valley of the Visočica River which is both its major tributary and outflow, between the mountains of Stara Planina on the north and Vidlič on the south. Lake is located north of the town of Pirot, close to the Visočica mouth into the Temštica river and is not well connected with the rest of Serbia. Settlements in the vicinity of the lake, which is among the least populated in the entire Serbia, include Novi Zavoj, Velika Lukanja and Pakleštica. History On February 25, 1963 a huge landslide from the sunny side of the Stara Planina rushed into th ...
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Politika
''Politika'' ( sr-Cyrl, Политика; ''Politics'') is a Serbian daily newspaper, published in Belgrade. Founded in 1904 by Vladislav F. Ribnikar, it is the oldest daily newspaper still in circulation in the Balkans. Publishing and ownership ''Politika'' is published by Politika novine i magazini (PNM), a joint venture between Politika AD and ''East Media Group''. The current director of PNM is Mira Glišić Simić. PNM also publishes: *''Sportski žurnal'' *'' Politikin zabavnik'' *'' Svet kompjutera'' *''Ilustrovana politika'' *''Bazar'' Editorial history *Vladislav F. Ribnikar (1904–1915) *Miomir Milenović i Jovan Tanović (1915–1941) *Živorad Minović (1985–1991) *Aleksandar Prlja (1991–1994) *Boško Jakšić (1994) *Dragan Hadži Antić (1994–2000) *Vojin Partonić (2000–2001) *Milan Mišić (2001–2005) *Ljiljana Smajlović (2005–2008) *Radmilo Kljajić (2008) *Dragan Bujošević (2008–2013) *Ljiljana Smajlović (2013–2016) *Žarko Rakić (2016- ...
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