| Summary: | Palaeomorphologic evolution of the western part of the Holy Cross region in Pleistocene The collected observations (among others H. Ruszczyńska-Szenajch 1966, Różycki 1972a, Lindner 1971a, 1977a) suggest that the ice sheet of the oldest Scandinavian glaciation — of the Narevian (Günz) Glaciation did not reach the Holy Cross region (Fig. 1 and 2). During that time, the area was in a periglacial zone with developed slope processes which formed various colluvial deposits (Czarnocki 1927, 1931, Łyczewska 1971, 1972, Filonowicz 1972, Hakenberg and Lindner 1971, Lindner 1971a, 1977a). In some of the fossil depressions, these deposits have been dissected by a valley system shown on Fig. 3 presenting a river pattern during the Podlasian Interglacial (Cromerian). The first Scandinavian ice sheet that covered the described area was the ice sheet of the older part of the South-Polish Glaciation. This period, on the ground of data from the interglacial locality at Kozi Grzbiet (Lindner and Głazek 1976, Głazek et al., 1976, 1977 a, b), is considered to be a separate glaciation (Fig. 4) called the Nidanian Glaciation (Mindel I). Till of the Nidanian Glaciation and ice-dammed lacustrine and fluvioglacial deposits of the same age are erosively cut by a valley system presented on Fig. 5. In all previous papers this system was interpreted as created by interstadial river activity (Lindner 1976c, 1976d, 1977a). The faunistic locality at Kozi Grzbiet studied recently, the interglacial features of its fauna (Kowalski 1976, Stworzewicz 1976, Młynarski 1977, Rzebik-Kowalska 1976) and its age determined by means of FC1/P method (Głazek et al., 1977b) enables a change of this interpretation. Thus the valley system of that age may be considered to be created in the Malopolanian (Kozi Grzbiet) Interglacial, separating the South-Polish Glaciation into two individual glaciations (Fig. 2). The younger of the South-Polish glaciations was called the Sanian Glaciation (Mindel II). In the area of Poland this glaciation had its maximum extent and ...
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