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water courses, which changed their location and size depending on the materials and quantities of water being carried. Today there is a large number of dry oxbow lakes, river beds and branches in the water meadows. Climatic conditions and erosion also changed the landscape around the streams of the glacial valley. For example the wind formed inland sand dunes parallel to the river, especially on the northern side of the valley, around which the river sometimes snaked in meanders.

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