@misc{Kraiński_Andrzej_Związek, author={Kraiński, Andrzej}, howpublished={online}, publisher={Zielona Góra: Oficyna Wydawnicza Uniwersytetu Zielonogórskiego}, language={pol}, language={eng}, abstract={The paper presents an analysis concerning a relation between glaciotectonic deformations and glaciotectonic depressions. The research work lead to the conclusion that (it is a rule) the fargest (the longest and the broadest) zones of glaciotectonic deformations occur in the area south of ice marginal valley.}, abstract={Author have proved that the ice marginal valleys have a complex genesis, not only erosive as it has been accepted so far, but they are also in relation with the so called glaciotectonic depressions from which the sediment was pulled out and dislocated southwards forming glaciotectonics ice gloes (in area oj glaciotectonic elevations).}, type={artykuł}, title={Związek zaburzeń glacitektonicznych z pradolinami na terenie Polski zachodniej = Relation between glaciotectonic deformations and ice marginal valleys in west Poland}, keywords={zaburzenia glacitektoniczne, depresja glacitektoniczna, elewacja glacitektoniczna, glaciotectonic deformations, glaciotectonic depression and elevation}, }