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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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
