DSC07869 (2)
Fig. 6. The Mazowian Vistula River channeł between Sandomierz and Northern Poland (simplified and completed)
Mazowickie koryto Wisły pomiędzy Sandomierzem a północną Polską (uproszczone i uzupełnione)
REFERENCES
Harasimiuk M., Henkiel A., 1981, Kopalne formy dolinne w okolicy Łącznej i ich znaczenie dla paleogeografii dorzecza Wieprza, Kwart. Geol., 25.1, pp. 147-161.
Kondratiene O., Evtuchin V., 1974, Novye razrezy butenajskogo (likhvinskogo, gold-steinskogo) mezhlednikovya v kaliningradskoi oblasti. Voprosy izuchenija chetvertichnych otlozhenij Liny, Trudy Litovskogo Nauchno-Issledovatelnogo Geologo-Razvedochnogo Instituta, 27, pp. 123-136.
Kopczyńska-Żandarska K., 1970, Stratygrafia starszego środkowego plejstocenu en północno-zachodniego Pomorza na tle rozwoju paleogeomorfologicznego,
ig. 1 Studia Geologica Polonica, 33, pp. 1-127.
rk Kozarski S., 1966/1967, Origin of the subglacial channels in the North Polish and
n_ | North Cermam Plain, Bulletin de la Societć des Sciences et des Lettres de
Poznań, B, 20, pp. 21-36.
Kurzawa M., 2003, The sedimentary record and rates of Quaternary vertical tectonic movements in NW Poland, Quatemary International. 101-102, pp. 137-148.
Lindner L., Bogutsky A., Gozhik P., Marciniak B., Marks L., Lanczont M.. ,n Wojtanowicz J., 2002, Correlation of main climatic glacial-interglacial and
loess-palaeosol cycles in the Pleistocene of Poland and Ukrainę, Acta Geologica Polonica, 52.4, pp. 459-469.
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