Lower Morava Valley
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 Carpathians (Ždánice Forest, Kyjov Hills and Mikulov Hills) in the west and Bílé Karpaty and 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. Soil horizon – mainly sand, fluvisol and loess, partly chernozem .
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Lower Morava Valley
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 Carpathians (Ždánice Forest, Kyjov Hills and Mikulov Hills) in the west and Bílé Karpaty and 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. Soil horizon – mainly sand, fluvisol and loess, partly chernozem .
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The Lower Morava Valley (Czech ...... and loess, partly chernozem .
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44,279,579
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1,024,769,836
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Gravel and Sand
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Žerotín
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48.5615 17.814
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The Lower Morava Valley (Czech ...... and loess, partly chernozem .
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Lower Morava Valley
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4.85615e+1