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Morava (river)
The Morava () is a river in Central Europe, a left tributary of the Danube. It is the main river of Moravia historical region in the Czech Republic, which derives its name from the river. The Morava originates on the Králický Sněžník mountain in the north-eastern corner of Pardubice Region, near the border between the Czech Republic and Poland and has a vaguely southward trajectory. The lower part of the river's course forms the border between the Czech Republic and Slovakia and then between Austria and Slovakia. Etymology The root of the river's name, ''mor-'', is derived from the Proto-Indo-European word for 'water', 'marsh', from which the Latin word ''mare'' arose. The suffix ''-ava'' is a Slavic form of the Proto-Germanic word ''ahwa'', meaning 'water', 'river'. The name of the river was first documented as ''Maraha'' in an 892 deed. The river gave its name to the entire historical land of Moravia, yet the oldest surviving record of the land (from 822) is older than the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolní Morava
Dolní Morava () is a municipality and village in Ústí nad Orlicí District in the Pardubice Region of the Czech Republic. It has about 400 inhabitants. Administrative division Dolní Morava consists of three municipal parts (in brackets population according to the 2021 census): *Dolní Morava (94) *Horní Morava (20) *Velká Morava (258) Geography Dolní Morava is located about northeast of Ústí nad Orlicí and east of Pardubice, on the border with Poland. Most of the municipality lies in the Králický Sněžník Mountains. The highest mountain of the range and one of the highest in the country, Králický Sněžník at above sea level, is situated in the northern part of the municipality on the Czech-Polish border. Klepáč, a mountain which is a triple divide, triple point of the European watershed, is also located in the municipality on the Czech-Polish border. The Morava (river), Morava River, which gave the name to the villages in the municipality, originates on Krá ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kroměříž
Kroměříž (; ) is a town in the Zlín Region of the Czech Republic. It has about 28,000 inhabitants. It is known for Kroměříž Castle with its castle gardens, which are a UNESCO World Heritage Site. The historic town centre with the castle complex is well preserved and is protected as an urban monument reservation. Administrative division Kroměříž consists of ten municipal parts (in brackets population according to the 2021 census): *Kroměříž (24,415) *Bílany (323) *Drahlov (155) *Hradisko (226) *Kotojedy (221) *Postoupky (598) *Těšnovice (419) *Trávník (601) *Vážany (1,174) *Zlámanka (148) Etymology The name is derived from the personal name Kroměžir, meaning "Kroměžir's (property)". Geography Kroměříž is located about northwest of Zlín. About two thirds of the municipal territory lies in the Litenčice Hills, the eastern part lies in the Upper Morava Valley. A small southern part extends into the Chřiby range. The highest point of the ter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neolithic
The Neolithic or New Stone Age (from Ancient Greek, Greek 'new' and 'stone') is an archaeological period, the final division of the Stone Age in Mesopotamia, Asia, Europe and Africa (c. 10,000 BCE to c. 2,000 BCE). It saw the Neolithic Revolution, a wide-ranging set of developments that appear to have arisen independently in several parts of the world. This "Neolithic package" included the History of agriculture, introduction of farming, domestication of animals, and change from a hunter-gatherer lifestyle to one of sedentism, settlement. The term 'Neolithic' was coined by John Lubbock, 1st Baron Avebury, Sir John Lubbock in 1865 as a refinement of the three-age system. The Neolithic began about 12,000 years ago, when farming appeared in the Epipalaeolithic Near East and Mesopotamia, and later in other parts of the world. It lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BCE), marked by the development ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Povodeň 1997 Uherské Hradiště - Náměstí 2
''The Flood'' () is a 1958 Czech drama film directed by Martin Frič. Cast * Zdeněk Štěpánek as Ryba * Otomar Krejča as Josef * Slávka Budínová as Josef's wife * Gustav Heverle as Karel * Ivanka Devátá as Zuzka * Karel Fiala as Marko * Jan Pivec as Doctor * Václav Lohniský Václav Lohniský (5 November 1920 – 18 February 1980) was a Czech film actor. He appeared in 120 films and television shows between 1950 and 1980. Selected filmography * '' Případ dr. Kováře'' (1950) * '' September Nights'' (1957) * ... as Ing. Netousek * Zdeněk Řehoř as Ing. zemánek * František Vnouček as Placek * František Holar as Kadlec References External links * 1958 films 1958 drama films 1950s Czech-language films Czechoslovak black-and-white films Films directed by Martin Frič Czechoslovak drama films 1950s Czech films {{1950s-drama-film-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schloss Hof 3
''Schloss'' (; pl. ''Schlösser''), formerly written ''Schloß'', is the German term for a building similar to a château, palace, or manor house. Related terms appear in several Germanic languages. In the Scandinavian languages, the cognate word ''slot''/''slott'' is normally used for what in English could be either a palace or a castle (instead of words in rarer use such as ''palats''/''palæ'', ''kastell'', or ''borg''). In Dutch, the word ''slot'' is considered to be more archaic. Nowadays, one commonly uses ''paleis'' or ''kasteel''. But in English, the term does not appear; for instance, in the United Kingdom, this type of structure would be known as a stately home or country house. Most ''Schlösser'' were built after the Middle Ages as residences for the nobility, not as true fortresses, although originally, they often were fortified. The usual German term for a true castle is ''Burg'', while that for a fortress is ''Festung'' (sometimes also ''Veste'' or ''Feste''), ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Proto-Germanic Language
Proto-Germanic (abbreviated PGmc; also called Common Germanic) is the reconstructed proto-language of the Germanic branch of the Indo-European languages. Proto-Germanic eventually developed from pre-Proto-Germanic into three Germanic branches during the fifth century BC to fifth century AD: West Germanic, East Germanic and North Germanic. North Germanic remained in contact with the other branches over a considerable time, especially with the Ingvaeonic languages (including English), which arose from West Germanic dialects, and had remained in contact with the Norse. A defining feature of Proto-Germanic is the completion of the process described by Grimm's law, a set of sound changes that occurred between its status as a dialect of Proto-Indo-European and its gradual divergence into a separate language. The end of the Common Germanic period is reached with the beginning of the Migration Period in the fourth century AD. The alternative term " Germanic parent langua ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Proto-Indo-European Language
Proto-Indo-European (PIE) is the reconstructed common ancestor of the Indo-European language family. No direct record of Proto-Indo-European exists; its proposed features have been derived by linguistic reconstruction from documented Indo-European languages. Far more work has gone into reconstructing PIE than any other proto-language, and it is the best understood of all proto-languages of its age. The majority of linguistic work during the 19th century was devoted to the reconstruction of PIE and its daughter languages, and many of the modern techniques of linguistic reconstruction (such as the comparative method) were developed as a result. PIE is hypothesized to have been spoken as a single language from approximately 4500 BCE to 2500 BCE during the Late Neolithic to Early Bronze Age, though estimates vary by more than a thousand years. According to the prevailing Kurgan hypothesis, the original homeland of the Proto-Indo-Europeans may have been in the Pon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Poland
Poland, officially the Republic of Poland, is a country in Central Europe. It extends from the Baltic Sea in the north to the Sudetes and Carpathian Mountains in the south, bordered by Lithuania and Russia to the northeast, Belarus and Ukraine to the east, Slovakia and the Czech Republic to the south, and Germany to the west. The territory has a varied landscape, diverse ecosystems, and a temperate climate. Poland is composed of Voivodeships of Poland, sixteen voivodeships and is the fifth most populous member state of the European Union (EU), with over 38 million people, and the List of European countries by area, fifth largest EU country by area, covering . The capital and List of cities and towns in Poland, largest city is Warsaw; other major cities include Kraków, Wrocław, Łódź, Poznań, and Gdańsk. Prehistory and protohistory of Poland, Prehistoric human activity on Polish soil dates to the Lower Paleolithic, with continuous settlement since the end of the Last Gla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moravia
Moravia ( ; ) is a historical region in the eastern Czech Republic, roughly encompassing its territory within the Danube River's drainage basin. It is one of three historical Czech lands, with Bohemia and Czech Silesia. The medieval and early modern Margraviate of Moravia was a crown land of the Lands of the Bohemian Crown from 1348 to 1918, an imperial state of the Holy Roman Empire from 1004 to 1806, a crown land of the Austrian Empire from 1804 to 1867, and a part of Austria-Hungary from 1867 to 1918. Moravia was one of the five lands of First Czechoslovak Republic, Czechoslovakia founded in 1918. In 1928 it was merged with Czech Silesia, and then dissolved in 1948 during the abolition of the land system following the 1948 Czechoslovak coup d'état, communist coup d'état. Its area of 22,623.41 km2 is home to about 3.0 million of the Czech Republic's 10.9 million inhabitants. The people are historically named Moravians, a subgroup of Czechs, the other group being calle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Europe
Central Europe is a geographical region of Europe between Eastern Europe, Eastern, Southern Europe, Southern, Western Europe, Western and Northern Europe, Northern Europe. Central Europe is known for its cultural diversity; however, countries in this region also share some historical and cultural similarities. The region is variously defined, but it’s minimum definition could be considered of consisting of Austria, Bosnia and Herzegovina, Croatia, the Czech Republic, eastern France, Germany, Liechtenstein, Luxembourg, Poland, Slovakia, Slovenia and Switzerland. But also the Baltic States, the Alsace in north-east France, and South Tyrol, northern Belluno , and Friuli-Venezia Giulia in north-east Italy are culturally usually considered to be part of Central Europe. From the early 16th century until the early 18th century, parts of Croatia and Hungary were ruled by the Ottoman Empire. During the 17th century, the empire also occupied southern parts of present-day Slovakia. During ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River
A river is a natural stream of fresh water that flows on land or inside Subterranean river, caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth. Water first enters rivers through precipitation, whether from rainfall, the Runoff (hydrology), runoff of water down a slope, the melting of glaciers or snow, or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins, or catchments, areas where surface water eventually flows to a common outlet. Rivers have a great effect on the landscape around them. They may regularly overflow their Bank (geography), banks and flood the surrounding area, spreading nutrients to the surrounding area. Sedime ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
