@ARTICLE{Górska_Maria_Fennoscandian_2006,
 author={Górska, Maria},
 volume={Vol. 23},
 journal={Studia Quaternaria},
 pages={11-15},
 howpublished={online},
 year={2006},
 publisher={Committee for Quaternary Research PAS},
 publisher={Institute of Geological Sciences PAS},
 abstract={In the glacial deposits of the Polish Lowland, there are erratic boulders drifted with the last continental ice sheet. Their outcrops are situated in the Baltic Shield area as well as south of it, in the bottom of the central and southern Baltic Sea. Indicator erratics, statistical erratics and the others can be distinguished in coarse-gravels associations. The studies on identification of the indicator erratics are designed for specification of the Scandinavian and Baltic alimentation centres of glacial tills of different age and their fluvioglacial counterparts; they are also aimed at determining the direction of the distant transport as well as the ice-sheet and its streams' transgression routes to the deposition places. Effectiveness of the analysis depends to a large extent on the correct classification of erratics, and this ability happens in turn to be burdened with a subjective evaluation of the clearly visible features of an erratic. In the present paper, an attention is paid to advantages and disadvantages of the analysis on the indicator boulders of the glacial deposits.},
 type={Article},
 title={Fennoscandian erratics in glacial deposits of the polish lowland - Methodical aspects},
 URL={http://www.journals.pan.pl/Content/119391/PDF-MASTER/str_11_15.pdf},
 keywords={indicator and statistical erratics, glacial deposits, Polish Lowland, Vistulian},
}