Lower Morava Valley
Lower Morava Valley | |
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File:Soutok Moravy a Dyje - český břeh obr2.jpg | |
Highest point | |
Peak | Žerotín (Zierotin) |
Elevation | Lua error in Module:Convert at line 1851: attempt to index local 'en_value' (a nil value). |
Dimensions | |
Length | Lua error in Module:Convert at line 1851: attempt to index local 'en_value' (a nil value). |
Area | Lua error in Module:Convert at line 1851: attempt to index local 'en_value' (a nil value). |
Geography | |
Location | Dolnomoravský úval CZ IV1 A-2.png |
Country | Moravia |
State | Czech Republic |
Range coordinates | Lua error in package.lua at line 80: module 'strict' not found. |
Parent range | Carpathians |
Geology | |
Orogeny | Alpide belt |
Age of rock | Neogene |
Type of rock | Gravel and Sand |
The Lower Morava Valley Czech: Dolnomoravský úval /Jihomoravská pánev also, German: Nieder March Talsenke, Slovak: Dolnomoravský úval) is a geomorphological formation (special type of Valley) in the Moravia (Czech Republic). It is formed by the depression in the western Carpathian Mountains (Ždánice Forest, Kyjov Hills and Mikulov Hills) 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.
Including low watershed Dyje-Morava in Lanžhot.[2]
The Lower Morava Valley is a nordest part of Vienna basin (Carpathians) and the corridor to Napajedla Gate, Upper Morava Valley, Moravian Gate and later in final goal North European Plain (Poland- Lower Silesia - Galicia) since ancient times. Here ran one arm of the most important trade routes from southern Europe to the Baltic Sea (e.g. the Amber Road - eastern branch) and also routes from Moravia to Upper Silesia and Lesser Poland. The Emperor Ferdinand Northern Railway (one part) built in 1840-41 from Břeclav (Vienna) to Přerov also traversed the Lower Morava Valley.
The Morava and Dyje rivers, Myjava (river), Chvojnice, Trkmanka, Kyjovka as well among others, finishing here in theirs floodplains,[3] and the towns include Břeclav, Hodonín, Uherské Hradiště, Valtice, Poštorná and Mikulčice.
Soil horizon - mainly sand, fluvisol and loess, partly chernozem .
See also
- Vyškov Gate
- Subcarpathia
- Outer Carpathian depressions
- South-Moravian Carpathians
- Upper Morava Valley
- Dyje–Svratka Valley
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Geomorfologické clenení Ceska.jpg
Lower Morava Valley (olive green) down right
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Morava Dyje confluence - riparian forest
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Morava hodonin holic.jpg
Lower Morava Valley landscape Hodonín surrounding
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Náklo (vrch), altán.jpg
View from Náklo Hill (265 m) to the Lower Morava Valley landscape
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Uherské Hradiště, archeologická lokalita Sady "Špitálky".jpg
View of the Lower Morava Valley from the Sady archaeological site
References
- ↑ Riparian forest Morava-Dyje confluence
- ↑ Functioning of South Moravian Floodplain Forests
- ↑ FIELD TRIP to the floodplain forests of the Lower Morava Biosphere Reserve
Further reading
- (1993) Geografický místopisný slovník, Academia, Praha. ISBN 80-200-0445-9
- (1997) Plašienka, D., Grecula, P., Putiš, M., Kováč, M. a Hovorka, D.,: Evolution and structure of the Western Carpathians: an overview. Mineralia Slovaca - Monograph, Košice, s. 1 – 24.
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