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Morava (river)

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.

Morava
The Morava between Austria and Slovakia
Course of the Morava interactive map
Location
Countries
Regions (CZ)
Regions (SK)
State (AT)Lower Austria
Cities
Physical characteristics
Source 
 • locationKrálický Sněžník
 • coordinates50°12′18″N 16°50′57″E / 50.20500°N 16.84917°E / 50.20500; 16.84917
 • elevation1,275 m (4,183 ft)[1]
MouthDanube
 • location
Devín
 • coordinates
48°10′27″N 16°58′32″E / 48.17417°N 16.97556°E / 48.17417; 16.97556Coordinates: 48°10′27″N 16°58′32″E / 48.17417°N 16.97556°E / 48.17417; 16.97556
Length352 km (219 mi)[2]
Basin size26,658 km2 (10,293 sq mi)[2]
Discharge 
 • locationmouth
 • average110 m3/s (3,900 cu ft/s)[2]
Basin features
ProgressionDanubeBlack Sea
Tributaries 
 • leftKrupá, Branná, Desná, Oskava, Bečva, Dřevnice, Olšava, Velička, Myjava
 • rightMírovka, Moravská Sázava, Haná, Thaya

Etymology

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.

History

The shores of the Morava have been inhabited for a very long time. The village of Stillfried [de], on the Austrian part of the river, was the location of a human settlement already 30,000 years ago.[1] 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.[1]

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.[citation needed]

History of the river

Course

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.[1] The catchment area of the river has a population of c. 3,5 million people.[1] 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 352 km (219 mi) of its course, the Morava feeds the Danube by an average discharge rate of 110 m3/s (3,900 cu ft/s), gathered from a drainage area of 26,658 km2 (10,293 sq mi).[2]

The river's longest tributary by far is the Thaya (in German) or Dyje (in Czech),[1] flowing in at the tripoint of Austria, the Czech Republic and Slovakia. The confluence of Thaya and Morava is the southernmost and the lowest point of Moravia. 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‰.[1] The bedrock of the river basin is mostly crystalline bedrock and flysch.[1]

The Morava river is unusual in that it is a European blackwater river.

Course of the river

Ecology

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.[1] 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.[1]

Ecology of the river

See also

References

  1. ^ a b c d e f g h i j Tockner, Klement; Uehlinger, Urs; Robinson, Christopher T. (2009). Rivers of Europe. Academic Press. pp. 86–88. ISBN 9780080919089.
  2. ^ a b c d "Danube River Basin District, Part A - Roof Report" (PDF). ICPDR. April 2004. p. 12.

External links

morava, river, rivers, serbia, great, morava, south, morava, west, morava, other, uses, morava, disambiguation, morava, german, march, hungarian, morva, polish, morawa, river, central, europe, left, tributary, danube, main, river, moravia, which, derives, name. For the rivers in Serbia see Great Morava South Morava and West Morava For other uses see Morava disambiguation 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 Kralicky Sneznik 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 MoravaThe Morava between Austria and SlovakiaCourse of the Morava interactive mapLocationCountriesCzech RepublicSlovakiaAustriaRegions CZ PardubiceOlomoucZlinSouth MoravianRegions SK TrnavaBratislavaState AT Lower AustriaCitiesOlomoucKromerizUherske HradisteHodoninHolicBratislavaMarcheggPhysical characteristicsSource locationKralicky Sneznik coordinates50 12 18 N 16 50 57 E 50 20500 N 16 84917 E 50 20500 16 84917 elevation1 275 m 4 183 ft 1 MouthDanube locationDevin coordinates48 10 27 N 16 58 32 E 48 17417 N 16 97556 E 48 17417 16 97556 Coordinates 48 10 27 N 16 58 32 E 48 17417 N 16 97556 E 48 17417 16 97556Length352 km 219 mi 2 Basin size26 658 km2 10 293 sq mi 2 Discharge locationmouth average110 m3 s 3 900 cu ft s 2 Basin featuresProgressionDanube Black SeaTributaries leftKrupa Branna Desna Oskava Becva Drevnice Olsava Velicka Myjava rightMirovka Moravska Sazava Hana Thaya Contents 1 Etymology 2 History 2 1 History of the river 3 Course 3 1 Course of the river 4 Ecology 4 1 Ecology of the river 5 See also 6 References 7 External linksEtymology EditThough 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 History EditThe shores of the Morava have been inhabited for a very long time The village of Stillfried de on the Austrian part of the river was the location of a human settlement already 30 000 years ago 1 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 1 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 citation needed History of the river Edit Skeletons of a family 9th century BC of the Urnfield culture site at Stillfried An allegorical representation of Morava at Schloss Hof in Austria The flood of 1997 in Uherske HradisteCourse EditThe river originates in the Kralicky Sneznik mountains in north western Moravia not far from the border with Poland The lowlands formed by the river are the Upper Moravian Vale or Hornomoravsky uval and then the Lower Morava Valley or Dolnomoravsky uval in Moravia the Morava Field or Marchfeld in Lower Austria and the Zahorie Lowland or Zahorska nizina 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 Kromeriz Otrokovice Uherske Hradiste and Hodonin Brno the second largest city of Czech Republic lies within the river basin 1 The catchment area of the river has a population of c 3 5 million people 1 Downstream from Hodonin the river flows along sparsely inhabited forested border area all the way to its outfall into the Danube just below the Devin Castle at the outskirts of the Slovak capital Bratislava After 352 km 219 mi of its course the Morava feeds the Danube by an average discharge rate of 110 m3 s 3 900 cu ft s gathered from a drainage area of 26 658 km2 10 293 sq mi 2 The river s longest tributary by far is the Thaya in German or Dyje in Czech 1 flowing in at the tripoint of Austria the Czech Republic and Slovakia The confluence of Thaya and Morava is the southernmost and the lowest point of Moravia The biggest tributary from the left is Becva 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 1 The bedrock of the river basin is mostly crystalline bedrock and flysch 1 The Morava river is unusual in that it is a European blackwater river Course of the river Edit The source of the Morava on Kralicky Sneznik The confluence of the Morava and the Danube Morava in Olomouc Thaya Morava confluence intersection of three borders Austrian Czech and SlovakEcology EditThe 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 1 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 1 Ecology of the river Edit Flooded forest Flooded meadow One of many oxbow lakes of the Morava Nature park Straznicke Pomoravi in Czech Republic one of several protected natural areas along the MoravaSee also EditMarch of Austria March of MoraviaReferences Edit a b c d e f g h i j Tockner Klement Uehlinger Urs Robinson Christopher T 2009 Rivers of Europe Academic Press pp 86 88 ISBN 9780080919089 a b c d Danube River Basin District Part A Roof Report PDF ICPDR April 2004 p 12 External links Edit Wikimedia Commons has media related to Morava River Geographic data related to Morava river at OpenStreetMap Retrieved from https en wikipedia org w index php title Morava river amp oldid 1124258655, wikipedia, wiki, book, books, library,

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