Piotr Moska, Grzegorz Adamiec, Zdzisław Jary, Andrzej Bluszcz, Grzegorz Poręba, Natalia Piotrowska, Marcin Krawczyk and Jacek Skurzyński
where the loess cover is preserved and its thickness rarely exceeds a few meters. In south-western Poland, several independent loess cover forms can be seen. Each form can be characterized by different sediment thickness, stratigraphy or physical properties. Such a large variety of loess deposits depending on their east-west geographical location is explained by the influence of continental climate in the eastern part of Poland and more oceanic in the western part ( Cegła, 1972 ; Jersak, 1973 ; Jary, 2007 ). Investigations showing the distribution of loess cover in
can be avoided);
– stratum — spatially defined entity of homogenous content, distinguished by stratigraphic context, physical features and cultural content of illegible, primary character.
Thus in this article, when describing the anthropogenic origin of the substrata of the Main Market Square in Kra-kow, the terms ‘deposit’, ‘strata’ and ‘stratum’ will be used — when we have in mind their successive formation as a consequence of their self-accumulation, or intention-al accumulation of matter (including waste) as a consequnce of the functioning of the town
Małgorzata Gutry-Korycka, Dariusz Woronko and Jarosław Suchożebrski
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Katarzyna Górniak, Tadeusz Szydłak, Adam Gaweł, Agnieszka Klimek, Anna Tomczyk, Jerzy Motyka and Krzysztof Bahranowski
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