Meer bei Meerdorf (Toteis-Loch oder Söller)
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As a load, the glacier carried rock material in the ice and at the base and deposited it as ground or terminal moraines. Parallel to the edge of the ice, a mighty glacial valley was formed through which the meltwater could flow towards the North Sea. When the glacier retreated, it left behind large chunks of ice because the ice mass thawed from the crevasses to the base and broke into pieces.
After the ice melted away, distinctive, often circular depressions, the so-called "Sölle" (singular: "Soll") or dead ice holes were left behind.
A fine, water-tight mud was deposited at the bottom of these holes, giving rise to the typical small bodies of water formed during the Ice Age.
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More information
- This location is part of the geopark.
Discover more geosites in the Peiner Land region at: www.tourismus-peine.de/unterwegs/geopark/. Author
der jeweilige Veranstaltende
Organization
wito gmbh/Tourist-Info-Service Peiner Land
Ilseder Hütte 1031241 IlsedeLicense (master data)
wito gmbh/Tourist-Info-Service Peiner Land








