The development and genesis of a small thaw lake filling the Skaliska Basin during the Late Glacial and Holocene
The northern part of the Mazury Lake District is marked by the presence of a depression described as the Skaliska Basin. At the end of the Pleistocene, the Skaliska Basin was the site of functioning of a thaw lake, within series of laminated clayey sediments were formed. The surface of the clayey se...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
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W. Szafer Institute of Botany, Polish Academy of Sciences
2013-06-01
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| Series: | Acta Palaeobotanica |
| Subjects: | |
| Online Access: | http://www.degruyter.com/view/j/acpa.2013.53.issue-1/acpa-2013-0005/acpa-2013-0005.xml?format=INT |