The Morava between Austria and Slovakia
Course of the Morava interactive map
|State (AT)||Lower Austria|
|• location||Králický Sněžník|
|• elevation||1,275 m (4,183 ft)|
|Length||354 km (220 mi)|
|Basin size||27,267 km2 (10,528 sq mi)|
|• average||120 m3/s (4,200 cu ft/s)|
|• left||Krupá, Branná, Desná, Oskava, Bečva, Dřevnice, Olšava, Velička, Myjava|
|• right||Mírovka, Moravská Sázava, Haná, Thaya|
|Progression||Danube→ Black Sea|
The Morava (German : March, Hungarian : Morva, Polish : Morawa) is a river in Central Europe, a left tributary of the Danube. It is the main river of Moravia, which derives its name from it. The river 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.
Though the German name March may refer to Mark, "border, frontier" (cf. English march ), the river's name more probably is derived from Proto-Indo-European *mori, "waters" ( mare ). It was first documented as Maraha in an 892 deed.
The shores of the Morava have been inhabited for a very long time. The village of Stillfried, on the Austrian part of the river, was the location of a human settlement already 30,000 years ago. Agriculture began to be practiced in the Morava valley approximately 7,000 years ago, and fortified settlements began to appear during the New Stone Age.
The lower part of the river, downstream of the confluence with the Thaya at Hohenau an der March, which today marks the Austro-Slovakian border, is one of the oldest national boundaries still extant in continental Europe: it was the eastern boundary of the Carolingian Empire with the Avar Khaganate around 800, and from the 10th century onward marked the border of the Imperial marcha orientalis , later Duchy of Austria, with the Kingdom of Hungary (within the Habsburg Monarchy during 1526–1918 because of imperial expansion). During the Cold War, this section of the river was part of the Iron Curtain, forming the frontier between Austria and Czechoslovakia.
In July 1997, the Morava basin (especially its northern and eastern part) was affected by heavy stratiform rain, which lasted several days and caused catastrophic floods, which also affected the Oder River basin in Poland and Germany. In the Czech Republic, 49 people lost their life, more than 250 villages had to be evacuated and the total damage was 63 billion crowns.
The river originates in the Králický Sněžník mountains in north-western Moravia, not far from the border with Poland. The lowlands formed by the river are the Upper Moravian Vale or Hornomoravský úval and then the Lower Morava Valley or Dolnomoravský úval in Moravia, the Morava Field or Marchfeld in Lower Austria, and the Záhorie Lowland or Záhorská nížina in Slovakia. The latter three are actually continuous parts of one large basin, forming the major part of the Vienna Basin.
In the Czech Republic, there are some larger towns lying upon Morava, particularly Olomouc, Kroměříž, Otrokovice, Uherské Hradiště and Hodonín. Brno, the second largest city of Czech Republic, lies within the river basin. km of its course, Morava feeds the Danube by an average discharge rate of 120 m3/s, gathered from a drainage area of 26 658 km2.The catchment area of the river has a population of c. 3,5 million people. Downstream from Hodonín, the river flows along sparsely inhabited, forested border area, all the way to its outfall into the Danube, just below the Devín Castle at the outskirts of the Slovak capital Bratislava. After 354
The river's longest tributary by far is the Thaya (in German) or Dyje (in Czech),flowing in at the tripoint of Austria, the Czech Republic and Slovakia. The biggest tributary from the left is Bečva .
The Morava is a lowland river with a basin that consists to 51 percent of plains; mountains make up only seven percent of the basin while 35 percent are considered highland. The average slope of the river is 1.8‰ and at the confluence 4‰.The bedrock of the river basin is mostly crystalline bedrock and flysch.
The Morava river is unusual in that it is a European blackwater river.
The Morava river forms an important link between the Danube Valley and the plains of northern Europe, for animals as well as, at least historically, for humans. Its weak slope across flat plains furthermore means that the river is prone to meander and flood, creating vast floodplains. Because of these reasons, the floodplains of the Morava river are among the most biologically diverse ecosystems in Europe.Its richness in plant and animal species (some 12,000 species have been identified) ranks it second in diversity only to the Danube Delta. During the 20th century however, large tracts of the river, especially downstream from Litovel, have been regulated with the ensuing effect of loss of inundation areas (floodplains). Since the river basin is densely populated and, especially the Czech part, industrialised, the river also receives a lot of wastewater. Agriculture also contributes to spreading nitrogen and other nutrients into the river. Nevertheless, the central part of the river has retained much of its natural character and in later years conscious efforts have been made to protect the nature and ecosystem of the river basin.
The Czech Republic is a land-locked country in Central Europe. It is bordered by Germany to the west, Austria to the south, Slovakia to the east and Poland to the north. It consists mostly of low hills and plateaus surrounded along the borders by low mountains. Two areas of lowlands follow the Elbe river and the Morava river. About a third of the area of the Czech Republic is covered by forests.
Moravia is a historical region in the east of the Czech Republic and one of three historical Czech lands, with Bohemia and Czech Silesia.
Pardubice Region is an administrative unit of the Czech Republic, located mainly in the eastern part of its historical region of Bohemia, with a small part in northwestern Moravia. It is named after its capital Pardubice. As an administrative unit, Pardubice Region has existed three times in the course of history. It was established for the first time in 1850, and extended from Český Brod to the Bohemian-Moravian border. In its second existence, it was one of 19 regions as they were set between 1949 and 1960. After 1960, Pardubice became the capital of Pardubice district, which was part of the Eastern Bohemian Region. The Pardubice Region, as it is now, was reestablished in 2000.
Zlín Region is an administrative unit of the Czech Republic, located in the south-eastern part of the historical region of Moravia. It is named after its capital Zlín. Together with the Olomouc Region it forms a cohesion area of Central Moravia. It is located in the eastern part of the Czech Republic, where the borders with Slovakia are formed by its eastern edge. It borders the South Moravian Region in the southwest, the Olomouc Region in the northwest and the Moravian-Silesian Region in the north. Culturally, the region is composed of parts of three traditional Moravian regions: Hanakia, the Moravian Slovakia and the Moravian Wallachia, as the city of Zlín lies roughly at their tripoint.
Uherské Hradiště is a town in the Zlín Region of the Czech Republic. It is located 23 km (14 mi) southwest of Zlín on the Morava River. It is the capital of the Uherské Hradiště District. The town itself has a population of around 25,000. The agglomeration with the two neighbouring towns of Staré Město and Kunovice has over 38,000 people.
The Leitha is a river in Austria and Hungary, a right tributary of the Danube. It is 120.8 km (75.1 mi) long.
The Thaya is a river in Central Europe, the longest tributary to the river Morava. It is 224 km (139 mi) long and meanders from west to east in the border area between Lower Austria (Austria) and South Moravia, though the frontier does not exactly follow the river's course in most parts. Its source is in two smaller rivers, namely the German Thaya and the Moravian Thaya, flowing together at Raabs.
The Pannonian Basin, or Carpathian Basin, is a large basin in Central Europe. The geomorphological term Pannonian Plain is more widely used for roughly the same region though with a somewhat different sense, with only the lowlands, the plain that remained when the Pliocene Epoch Pannonian Sea dried out.
Moravian Slovakia or Slovácko is a cultural region in the southeastern part of the Czech Republic, Moravia on the border with Slovakia and Austria, known for its characteristic folklore, music, wine, costumes and traditions. The area forms part of both the Zlín and South Moravian administrative regions.
Králický Sněžník or Śnieżnik Kłodzki is a mountain in Eastern Bohemia, located on the border between the Czech Republic and Poland. The name Sněžník or Śnieżnik derives from the word for "snow"; the mountain has snow cover for up to eight months a year. In Czech the adjective Králický is added to distinguish it from the mountain called Děčínský Sněžník. An alternative Polish name is Śnieżnik Kłodzki, from the town of Kłodzko. In German the mountain is known as Glatzer Schneeberg, Grulicher Schneeberg, or Spieglitzer Schneeberg.
Šumperk District is a district (okres) within the Olomouc Region of the Czech Republic Its administrative centre is the town of Šumperk.
The Mikulov Highlands is a mountain range in South Moravia, Czech Republic. The Highlands, together with the Waschberg Zone and Lower Austria Inselberg threshold, form the South-Moravian Carpathians.
The Vienna Basin is a geologically young tectonic burial basin and sedimentary basin in the seam area between the Alps, the Carpathians and the Pannonian Plain. Although it topographically separates the Alps from the Western Carpathians, it connects them geologically via corresponding rocks underground.
The South-Moravian Carpathians, also called Austrian - South-Moravian Carpathians are a mountain range of the Outer Western Carpathians along the border of the Czech Republic and Austria.
The Margraviate of Moravia was one of the lands of the Bohemian Crown existing from 1182 to 1918. It was officially administrated by a margrave in cooperation with a provincial diet. It was variously a de facto independent state, and also subject to the Duchy, later the Kingdom of Bohemia. It comprised the region called Moravia within the modern Czech Republic.
The Dyje–Svratka Valley is a geomorphological feature in Moravia. The highest prominence over the Dyje–Svratka Valley is Děvín Peak at 549 metres (1,801 ft).
The Lower Morava Valley is a geomorphological formation in the Moravia. It is formed by the depression in the Western Carpathians in the west and Bílé Karpaty and Chvojnice hills in the east. The drainage to the River Morava of the Danube basin runs finally to the Black Sea.
|Wikimedia Commons has media related to Morava River .|