Lower Morava Valley
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.
Including low watershed Dyje-Morava in Lanžhot.
The Lower Morava Valley is a nordest part of Vienna basin and the corridor to Napajedla Gate, Upper Morava Valley, Moravian Gate and later in final goal North European Plain since ancient times. Here ran one arm of the most important trade routes from southern Europe to the Baltic Sea and also routes from Moravia to Upper Silesia and Lesser Poland. The Emperor Ferdinand Northern Railway built in 1840-41 from Břeclav to Přerov also traversed the Lower Morava Valley.
The Morava and Dyje rivers, Myjava, Chvojnice, Trkmanka, Kyjovka as well among others, finishing here in theirs floodplains, and the towns include Břeclav, Hodonín, Uherské Hradiště, Valtice, Poštorná and Mikulčice.
Soil horizon - mainly sand, fluvisol and loess, partly chernozem.
