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The information presented here is based on 174 sites; it is a result of a detailed historical collection revision of materials from Silesia and also the first comprehensive paper after the early German and Polish compilations. Though our work includes both quantitative and qualitative updates, it is neither exhaustive nor complete. It is very likely that many finds have not yet been reported to scientific institutions or museums, or else remain in private collections. The localities concerned are dominated by remains found under or within alluvial deposits of the last glaciation or in the context of loess sediments. Most of the documented remains are from the Late Pleistocene. Cold-adapted members of steppe-tundra faunal assemblages, such as Mammuthus primigenius, Equus ferus, Coelodonta antiquitatis, Rangifer tarandus, Ovibos moschatus, and Bison priscus dominate. Most artiodactyls were found in alluvial sediments, in bogs or swamps, while carnivores are represented only by isolated remains. The location of faunal assemblages and isolated finds shows the importance of river valleys as migrations routes. Silesia stretches along the Odra River, which runs in a roughly south-north direction, and connects the Sudety Mts and the Głubczyce Plateau with the wide, open lowlands of Eastern Germany and Western Poland. [ABSTRACT FROM AUTHOR]