Ústí Nad Labem Region
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Ústí Nad Labem Region
Ústí nad Labem Region or Ústecký Region () is an Regions of the Czech Republic, administrative unit () of the Czech Republic, located in the north-western part of the historical land of Bohemia, and named after the capital, Ústí nad Labem. It covers the majority of the former Administrative divisions of Czechoslovakia, North Bohemia province () and is part of the broader area of North Bohemia. The region borders the regions of Liberec Region, Liberec (east), Central Bohemian Region, Central Bohemia (south), Plzeň Region, Plzeň (southwest), Karlovy Vary Region, Karlovy Vary (west) and the German region of Saxony to the north. The Ústí nad Labem Region comprises a range of very different types of landscape. Between the high escarpment of the Ore Mountains range and the České středohoří, Bohemian Central Uplands with many volcanic hills, there are vast areas devastated by surface coal mining (the Most Basin), partly being recultivated into an artificial landscape with ...
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Regions Of The Czech Republic
Regions of the Czech Republic ( ; singular ) are higher-level territorial self-governing units of the Czech Republic. History The first regions (''kraje'') were created in the Kingdom of Bohemia in the 14th century. At the beginning of the 15th century, Bohemia was already divided into 12 regions, but their borders were not fixed due to the frequent changes in the borders of the estates. During the reign of George of Poděbrady (1458–1471), Bohemia was divided into 14 regions, which remained so until 1714, when their number was reduced to 12 again. From 1751 to 1850, after the four largest regions were divided, the kingdom consisted of 16 regions. Between 1850 and 1862, there were several reforms and the number of regions fluctuated between 7 and 13. Due to the parallel establishment of political districts in 1848, however, their importance declined. In 1862, the regions were abolished, although the regional authorities had some powers until 1868. Moravia was divided into ...
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Karlovy Vary Region
The Karlovy Vary Region () is an administrative unit () of the Czech Republic, located in the westernmost part of the country. It is named after its capital Karlovy Vary. It is known for spas, which include Karlovy Vary and Mariánské Lázně. The Karlovy Vary Region, as a higher territorial self-governing unit, was created in 2000 in the northern part of the West Bohemian Region. The seat of the region is Karlovy Vary. In terms of size, number of municipalities, and population, it ranks among the smaller regions of the Czech Republic. Its area (3,314 km²) covers 4.25% of the territory of the Czech Republic. The Karlovy Vary Region is the third smallest region by area, right after Prague and the Liberec Region. By population, the Karlovy Vary Region is the smallest region in the Czech Republic, with approximately 279,000 inhabitants. Administrative divisions The Karlovy Vary Region is divided into three districts: At a lower level, the region has 134 municipalities, comprisi ...
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Districts Of The Czech Republic
Districts of the Czech Republic are territorial units, formerly used as second-level administrative divisions of the Czech Republic. After their primary administrative function has been abolished in 2003, they still exist for the activities of specific authorities and as statistical units. Their administrative function was moved to selected municipalities. Establishment In 1960, Czechoslovakia was re-divided into districts (''okres'', Grammatical number, plural ''okresy''), often without regard to traditional division and local relationships. In the area of the Czech Republic, there were 75 districts; the 76th Jeseník District was split from Šumperk District in 1996. Three consisted only of the Statutory city (Czech Republic), statutory cities of Brno, Ostrava and Plzeň, which gained the status of districts only in 1971; Ostrava and Plzeň districts were later expanded. The capital city of Prague has a special status, being considered a municipality and region at the same time ...
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Chomutov District
Chomutov District () is a district in the Ústí nad Labem Region of the Czech Republic. Its capital is the city of Chomutov. Administrative division Chomutov District is divided into two administrative districts of municipalities with extended competence: Chomutov and Kadaň. List of municipalities Cities and towns are marked in bold and market towns in ''italics'': Bílence - Blatno - Boleboř - Březno - Černovice - Chbany - Chomutov - Domašín - Droužkovice - Hora Svatého Šebestiána - Hrušovany - Jirkov - Kadaň - Kalek - Klášterec nad Ohří - '' Kovářská'' - Křimov - Kryštofovy Hamry - Libědice - Loučná pod Klínovcem - Málkov - Mašťov - Měděnec - Místo - Nezabylice - Okounov - Otvice - Perštejn - Pesvice - Pětipsy - Račetice - Radonice - Rokle - Spořice - Strupčice - Údlice - Vejprty - Veliká Ves - Vilémov - Vrskmaň - Všehrdy - Všestudy - Výsluní - Vysoká Pec Geography Chomutov District bord ...
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Natural Arch
A natural arch, natural bridge, or (less commonly) rock arch is a natural landform where an arch has formed with an opening underneath. Natural arches commonly form where inland cliffs, Cliffed coast, coastal cliffs, Fin (geology), fins or Stack (geology), stacks are subject to erosion from the sea, rivers or weathering (subaerial processes). Most natural arches are formed from narrow fins and sea stacks composed of sandstone or limestone with steep, often vertical, cliff faces. The formations become narrower due to erosion over geologic time scales. The softer rock stratum erodes away creating rock shelters, or alcoves, on opposite sides of the formation beneath the relatively harder stratum, or caprock, above it. The alcoves erode further into the formation eventually meeting underneath the harder caprock layer, thus creating an arch. The erosional processes exploit weaknesses in the softer rock layers making cracks larger and removing material more quickly than the caprock; ho ...
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Pravčická Brána
The Pravčická brána (in English also ''Pravčice Gate'', ''Pravčická Gate'' or ''Pravcicka Gate''; ) is a narrow rock formation in Bohemian Switzerland in the Czech Republic, approx. 3 km northeast of Hřensko. With a span of 26.5 metres, an inside height of 16 metres, 8 metre maximum width and 3 metre arch, it is the largest natural sandstone arch in Europe, and one of the most striking nature monuments in the Elbe Sandstone Mountains. It is protected as a national nature monument. History In 1826, an inn was built by the Pravčická brána. In 1881, Prince Edmund of Clary-Aldringen had built the Hotel Sokolí hnízdo (that time called ''Falkennest'', both meaning "falcon's nest") with 50 beds. As a result of heavy erosion Erosion is the action of surface processes (such as Surface runoff, water flow or wind) that removes soil, Rock (geology), rock, or dissolved material from one location on the Earth's crust#Crust, Earth's crust and then sediment transpor ...
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Bohemian Switzerland
Bohemian Switzerland (; ), also known as Czech Switzerland, is a nature region in the Elbe Sandstone Mountains in the northwestern Czech Republic, protected as a national park. It has been a protected area (as Elbe Sandstone Mountains Protected Landscape Area) since 1972. The region along the right side of the Elbe became a national park in 2000 and is adjacent to Saxon Switzerland National Park in Germany. Together with Saxon Switzerland, the region is known as Saxon-Bohemian Switzerland. Etymology The concept of Bohemian Switzerland developed in the 18th century as an extension of the Saxon Switzerland, a part of the Elbe Sandstone Mountains in Germany. The name was inspired by the Swiss artists Adrian Zingg and Anton Graff, who were reminded of their homeland by the geography of northern Bohemia. Geography Bohemian Switzerland covers the eastern part of the Czech side of the Elbe Sandstone Mountains. It is located northeast of Děčín, on right bank of the Elbe River, ...
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Sandstone
Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar, because they are the most resistant minerals to the weathering processes at the Earth's surface. Like uncemented sand, sandstone may be imparted any color by impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Because sandstone beds can form highly visible cliffs and other topography, topographic features, certain colors of sandstone have become strongly identified with certain regions, such as the red rock deserts of Arches National Park and other areas of the Southwestern United States, American Southwest. Rock formations composed of sandstone usually allow the p ...
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Polabí
Polabí () is the traditional and informal name for a lowland region located mainly in the Central Bohemian Region of the Czech Republic. Etymology The name comes from Czech ''po Labi'', meaning "along the Elbe". The same linguistic construction gave its name to the extinct Polabian Slavs in today's Germany. Geography The region, without clear boundaries, extends along the river Elbe, approximately between the towns of Pardubice and Mělník, where the Elbe flows together with Vltava. In wider sense, it stretches further westward to the lowland along the Ohře river. Its elevation ranges roughly between 150 and 300 metres above sea level. Agriculture Polabí is the most fertile part of Bohemia and the core area, from where the medieval state of the Czechs The Czechs (, ; singular Czech, masculine: ''Čech'' , singular feminine: ''Češka'' ), or the Czech people (), are a West Slavs, West Slavic ethnic group and a nation native to the Czech Republic in Central Europe, who s ...
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Porta Bohemica
Porta can refer to: People * Porta (rapper) (born 1988), stagename of Christian Jiménez Bundo, a Spanish rap singer * Porta (surname), surname Places * La Porta, a commune in the Haute-Corse department of France on the island of Corsica * Porta (Barcelona) a neighbourhood of Barcelona, Spain * Porta, Pyrénées-Orientales, a commune in the Pyrénées-Orientales department in southern France * Porta, Thessaly, a pass and settlement in Thessaly, central Greece * Porta, Xanthi, a district of Xanthi in Thrace, northeastern Greece * ''Porta'', the Hungarian name for Poarta village, Bran Commune, Braşov County, Romania * Porta del Sol, a tourism region in western Puerto Rico * Porta Littoria, the name applied from 1939 to 1946 for the town of La Thuile in the Valle d’Aosta, Italy * Porta Westfalica in Germany * Porta Nigra in Trier, Germany Convents * Porta Coeli (Moravia), in the Czech Republic, a convent from 1239 after which an asteroid is named * Porta Coeli (Puerto R ...
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Elbe
The Elbe ( ; ; or ''Elv''; Upper Sorbian, Upper and , ) is one of the major rivers of Central Europe. It rises in the Giant Mountains of the northern Czech Republic before traversing much of Bohemia (western half of the Czech Republic), then Germany and flowing into the North Sea at Cuxhaven, northwest of Hamburg. Its total length is . The Elbe's major Tributary, tributaries include the rivers Vltava, Ohře, Saale, Havel, Mulde, and Schwarze Elster. The Elbe river basin, comprising the Elbe and its tributaries, has a catchment area of , the twelfth largest in Europe. The basin spans four countries; however, it lies almost entirely just in two of them, Germany (65.5%) and the Czech Republic (33.7%, covering about two thirds of the nation's territory). On its southeastern edges, the Elbe river basin also comprises small parts of Austria (0.6%) and Poland (0.2%). The Elbe catchment area is inhabited by 24.4 million people; its biggest cities are Berlin, Hamburg, Prague, Dresden a ...
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Most Basin
The Most Basin (also known as North Bohemian Basin; , ) is a structural basin and geomorphological mesoregion of the Czech Republic. It is named after the city of Most. It forms the southwestern and central parts of the Ústí nad Labem Region. It is among the richest European deposits of lignite, which has been extracted here since the second half of 19th century, mostly by extensive surface mining. Geomorphology The Most Basin is a mesoregion of the Podkrušnohorská Macroregion within the Bohemian Massif. It is further subdivided into the microregions of Žatec Basin and Chomutov-Teplice Basin. A flat landscape without peaks is typical for the Most Basin. The highest point of the territory is a contour line near Libouchec, at above sea level. There are several low hills with an elevation of 350–380 in the southwestern part of the basin. Adjacent landscapes The basin lies between the Central and Eastern Ore Mountains to the north and the Rakovník Uplands to the south. ...
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