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The Dyje–Svratka Valley
Valley
(Czech: Dyjsko-svratecký úval, German: Thaya-Schwarza Talsenke, Slovak: Dyjsko-svratecký úval) is a geomorphological feature (specifically a special type of vale) in Moravia
Moravia
(The Czech Republic). The highest prominence over the Dyje–Svratka Valley
Valley
is Děvín Peak at 549 metres (1,801 ft).

Contents

1 History 2 Access 3 Geography 4 See also 5 References

History[edit] The Dyje–Svratka Valley
Valley
has been a natural pass between the Vienna Basin (Carpathians) and the Vyškov Gate, the Upper Morava Valley, Moravian Gate
Moravian Gate
and later, the North European Plain
North European Plain
( Poland
Poland
- Lower Silesia - Galicia) since ancient times. It served as an arm of several important trade routes from southern Europe
Europe
to the Baltic Sea
Baltic Sea
such as the Amber Road, as well as routes from Moravia
Moravia
to Upper Silesia
Upper Silesia
and Lesser Poland. The Emperor Ferdinand Northern Railway
Emperor Ferdinand Northern Railway
from Břeclav
Břeclav
to Brno
Brno
traverses the Dyje–Svratka Valley. Access[edit] Highways that traverse the Dyje-Svratka Valley
Valley
include D1 from Prague to Brno, D2 from Brno
Brno
to Břeclav
Břeclav
and Bratislava, and D52 from Brno
Brno
to Vienna). Geography[edit] The floodplains of several rivers end in the Dyje-Svratka Valley, including Svratka, Jihlava, Svitava, Dyje, Jevišovka and Litava. Many towns are located within it, including the southern districts of Brno, Slavkov/Austerlitz, Židlochovice, Pohořelice, Hrušovany nad Jevišovkou and Mikulov. The Lowlands are poorly forested, mostly by riparian forest (oaks, populus and willows), with higher areas forested by false akacia (Robinia pseudoacacia[1]). The Lowlands are intensively farmed, with significant numbers of orchards (peaches, walnuts, apricots and almonds), vineyards and small woods. Only a few small sections are still covered by natural vegetation.[2] The west valley contains numerous vineyards that are part of the wine making sub-regions of Mikulovská and Znojemská. It is formed by the depression between the Carpathian Mountains
Carpathian Mountains
in the east (Ždánice Forest, Kyjov Hills
Kyjov Hills
and Mikulov
Mikulov
Hills) and the Bohemian massif in the west. Drainage runs into the River Morava, from there into the Danube basin
Danube basin
and finally into the Black Sea. It includes the low drainage divide Svratka- Dyje
Dyje
close to Mušov. Its soils mainly consist of chernozem and loess, local fluvisol and sand.

Pavlov and Pavlov lake

Svratka river south of Brno

Look from Výhon, Akátová tower to the south

Moravian Dyje–Svratka Valley: view from Dolní Kounice to the southeast, Palava Hills on the horizon

Look from Roman fortress vallum ruins to Dyje–Svratka confluence riparian forest

Vineyards below the Pálava Hills

Svratka river in Rajhrad

See also[edit]

Vyškov Gate Subcarpathia Outer Carpathian depressions South-Moravian Carpathians Upper Morava Valley Lower Morava Valley

References[edit]

^ Horník, Some results of biogeographic research on meadows in the Dyje–Svratka basin in the Czech Republic ^ Penka, After Water management

(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. [author missing] [title missing] Mineralia Slovaca - Monograph, Košice, s. 1 – 24. ISBN 978-80-967018-7-2 (2010) Filip, A., Krejčí, J. (Photo), : Brno
Brno
- City Guide: Brno, K-Public. ISBN 978-80-87028-08-7

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