@ARTICLE{Musiał_Andrzej_Late_1993, author={Musiał, Andrzej and Horodyski, Bogdan and Kossobudzki, Krzysztof}, volume={vol. 14}, number={No 3}, journal={Polish Polar Research}, pages={259-274}, howpublished={online}, year={1993}, publisher={Polish Academy of Sciences}, publisher={Committee on Polar Research}, abstract={Relief of Svalbard is an effect of varied morphogenetic, exogenic and endogenic processes. Tectonic and glacioisostatic movements of the Earth crust have occurred many a time in this region. Glacial, marine and periglacial features are particularly common. During the Late Quaternary the western Nordenskiöld Land underwent several sea transgressions, followed by glacier advances. Basing on erratics of crystalline rocks transported by sea ice, past sea levels have been established up to 250 m a.s.l. Marine terraces above 60 m a.s.l. date back to the Late Pleistocene, the lower ones are of the Holocene age.}, type={Article}, title={Late Quaternary evolutionof the western Nordenskiöld Land}, URL={http://www.journals.pan.pl/Content/111063/PDF-MASTER/1993-3_259-273.pdf}, keywords={Arctic, Spitsbergen, Quaternary evolution}, }