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Czech Republic
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The Czech Republic, also known as Czechia, is a nation state in Central Europe bordered by Germany to the west, Austria to the south, Slovakia to the east and Poland to the northeast. The Czech Republic covers an area of 78,866 square kilometres with mostly temperate continental climate and it is a unitary parliamentary republic, has 10.5 million inhabitants and the capital and largest city is Prague, with over 1.2 million residents. The Czech Republic includes the territories of Bohemia, Moravia. The Czech state was formed in the late 9th century as the Duchy of Bohemia under the Great Moravian Empire, after the fall of the Empire in 907, the centre of power transferred from Moravia to Bohemia under the Přemyslid dynasty. In 1002, the duchy was formally recognized as part of the Holy Roman Empire, becoming the Kingdom of Bohemia in 1198 and reaching its greatest territorial extent in the 14th century. Following the Battle of Mohács in 1526, the whole Crown of Bohemia was gradually integrated into the Habsburg Monarchy alongside the Archduchy of Austria, the Protestant Bohemian Revolt against the Catholic Habsburgs led to the Thirty Years War. After the Battle of the White Mountain, the Habsburgs consolidated their rule, reimposed Roman Catholicism, the Czech part of Czechoslovakia was occupied by Germany in World War II, and was liberated in 1945 by the armies of the Soviet Union and the United States. The Czech country lost the majority of its German-speaking inhabitants after they were expelled following the war, the Communist Party of Czechoslovakia won the 1946 elections. Following the 1948 coup détat, Czechoslovakia became a one-party communist state under Soviet influence, in 1968, increasing dissatisfaction with the regime culminated in a reform movement known as the Prague Spring, which ended in a Soviet-led invasion. Czechoslovakia remained occupied until the 1989 Velvet Revolution, when the communist regime collapsed, on 6 March 1990, the Czech Socialistic Republic was renamed to the Czech Republic. On 1 January 1993, Czechoslovakia peacefully dissolved, with its constituent states becoming the independent states of the Czech Republic and the Slovak Republic. The Czech Republic joined NATO in 1999 and the European Union in 2004, it is a member of the United Nations, the OECD, the OSCE, and it is a developed country with an advanced, high income economy and high living standards. The UNDP ranks the country 14th in inequality-adjusted human development, the Czech Republic also ranks as the 6th most peaceful country, while achieving strong performance in democratic governance. It has the lowest unemployment rate in the European Union, the traditional English name Bohemia derives from Latin Boiohaemum, which means home of the Boii. The current name comes from the endonym Čech, spelled Cžech until the reform in 1842. The name comes from the Slavic tribe and, according to legend, their leader Čech, the etymology of the word Čech can be traced back to the Proto-Slavic root *čel-, meaning member of the people, kinsman, thus making it cognate to the Czech word člověk. The country has traditionally divided into three lands, namely Bohemia in the west, Moravia in the southeast, and Czech Silesia in the northeast. Following the dissolution of Czechoslovakia at the end of 1992, the Czech part of the former nation found itself without a common single-word geographical name in English, the name Czechia /ˈtʃɛkiə/ was recommended by the Czech Ministry of Foreign Affairs
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Districts of the Czech Republic
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In 1960, Czechoslovakia was re-divided into districts often without regard to traditional division and local relationships. In the area of the Czech Republic, there were 75 districts, a reform in effect since January 2003 replaced the districts with 204 Municipalities with Extended Competence (obce s rozšířenou působností, also obce III. Stupně - third-level municipalities, unofficially also called little districts which took over most of the administration of the district authorities. Some of these are divided between Municipalities with Commissioned Local Authority. The old districts still exist as units and remain as seats of some of the offices, especially courts, police. In 2007 the borders of the districts were slightly adjusted and 119 municipalities are now within different districts, regions of the Czech Republic ISO 3166-2, CZ http, //www. czso. cz/lexikon/mos2003. nsf/index
3.
Elbe
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The Elbe is one of the major rivers of Central Europe. It rises in the Krkonoše Mountains of the northern Czech Republic before traversing much of Bohemia, then Germany and its total length is 1,094 kilometres. The Elbes major tributaries include the rivers Vltava, Saale, Havel, Mulde, Schwarze Elster, the Elbe river basin, comprising the Elbe and its tributaries, has a catchment area of 148,268 square kilometres, the fourth largest in Europe. The basin spans four countries, with its largest parts in Germany, much smaller parts lie in Austria and Poland. The basin is inhabited by 24.5 million people, the Elbe rises at an elevation of about 1,400 metres in the Krkonoše on the northwest borders of the Czech Republic near Labská bouda. Of the numerous small streams whose waters compose the infant river, here the Elbe enters the vast vale named Polabí, and continues on southwards through Hradec Králové and then to Pardubice, where it turns sharply to the west. At Kolín some 43 kilometres further on, it bends gradually towards the north-west, at the village of Káraný, a little above Brandýs nad Labem, it picks up the Jizera. At Mělník its stream is more than doubled in volume by the Vltava, or Moldau, upstream from the confluence the Vltava is in fact much longer, and has a greater discharge and a larger drainage basin. Some distance lower down, at Litoměřice, the waters of the Elbe are tinted by the reddish Ohře, in its northern section both banks of the Elbe are characterised by flat, very fertile marshlands, former flood plains of the Elbe now diked. At Magdeburg there is a viaduct, the Magdeburg Water Bridge, from the sluice of Geesthacht on downstream the Elbe is subject to the tides, the tidal Elbe section is called the Low Elbe. Within the city-state the Unterelbe has a number of streams, such as Dove Elbe, Gose Elbe, Köhlbrand, Northern Elbe, Reiherstieg. Some of which have been disconnected for vessels from the stream by dikes. In 1390 the Gose Elbe was separated from the stream by a dike connecting the two then-islands of Kirchwerder and Neuengamme. The Dove Elbe was diked off in 1437/38 at Gammer Ort and these hydraulic engineering works were carried out to protect marshlands from inundation, and to improve the water supply of the Port of Hamburg. The Northern Elbe passes the Elbe Philharmonic Hall and is then crossed under by the old Elbe Tunnel, a bit more downstream the Low Elbes two main anabranches Northern Elbe and the Köhlbrand reunite south of Altona-Altstadt, a locality of Hamburg. Right after both anabranches reunited the Low Elbe is passed under by the New Elbe Tunnel, the last structural road link crossing the river before the North Sea. At the bay Mühlenberger Loch in Hamburg at kilometre 634, the Northern Elbe and the Southern Elbe used to reunite, leaving the city-state the Lower Elbe then passes between Holstein and the Elbe-Weser Triangle with Stade until it flows into the North Sea at Cuxhaven. Near its mouth it passes the entrance to the Kiel Canal at Brunsbüttel before it debouches into the North Sea, the Elbe has been navigable by commercial vessels since 1842, and provides important trade links as far inland as Prague
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Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
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Central European Summer Time
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It corresponds to UTC + two hours. Other names which have been applied to Central European Summer Time are Middle European Summer Time, Central European Daylight Saving Time, and Bravo Time. Since 1996 European Summer Time has been observed between 1,00 UTC on the last Sunday of March and 1,00 on the last Sunday of October, the following countries and territories use Central European Summer Time. In addition, Libya used CEST during the years 1951–1959, 1982–1989, 1996–1997, European Summer Time Other countries and territories in UTC+2 time zone Other names of UTC+2 time zone
