Zur Struktur und Entstehung von Eiskeil–Grossformen in Lieth/Elmshorn (Schleswig-Holstein)
The deposits near the surface of the Permian and Quarternary in the western part of the “Lieth lime quarry” have been intensively periglacially modified. Three ice-wedge pseudomorphs, which run approximately parallel, are 0.5 m wide and reach a depth of more than 3 meters. These features are of part...
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| Format: | Article |
| Language: | deu |
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Copernicus Publications
2007-12-01
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| Series: | Eiszeitalter und Gegenwart |
| Online Access: | https://www.eg-quaternary-sci-j.net/56/283/2007/egqsj-56-283-2007.pdf |