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  • . Strakel), transversal gap of the Middle Vistula (by W. Pożaryski and T. Kalicki) and lower reaches of several tributaries of the Lower Vistula (by L. Andrzejewski). There are also detail sedimentological and palynological studies on two lateglacial
  • paleomeanders in the upper Vistula valley (by T. Kalicki and V.P. Zernickaya) and lower Wisłoka (by L. Starkel and W. Ganoszewski). Two other papers by T. Kalicki and M. Krapiec from Wisłoka valley discuss the importance of endrochronological method for dating
  • is a special case of anthropogenic influence that might be an interesting addition to previous studies of human impacts on palaeohydrology, channel change and valley floor development (Gregory, 1995; Brown, 1996; Kalicki,1996).