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the whole region was ice-covered, now verified by glacial erratic rocks from Scandinavia placed for decoration in the town. The Bastau depression, a late-Saalian Weser bed, became a marshy peat-covered area; the peat is completely exhausted for its use in firing. In the time of Weichselian glaciation the glacier did not reach this region. In the periglacial climate of that time fine material

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