The development and genesis of a small thaw lake filling the Skaliska Basin during the Late Glacial and Holocene

@inproceedings{StachowiczRybka2013TheDA,
  title={The development and genesis of a small thaw lake filling the Skaliska Basin during the Late Glacial and Holocene},
  author={Renata Stachowicz-Rybka and Andrzej J. Obidowicz},
  year={2013}
}
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 sediments was overlain by a sandy fan. Blocks of dead ice underlying the fan and the overlying surface of the clayey sediments were the origin of small isolated water basins. Since the Allerød they… CONTINUE READING

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