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Information about the morphology and alluvial sediments of the Dnieper Valley is reviewed. The Dnieper Valley originated in the Late Miocene. The Middle Dnieper Valley is an intercontinental alluvial basin and the Lower Dnieper Valley is a shallow canyon that ends with a delta. Identification of the alluvial dynamic fades (channel, overbank, abandoned channel) is crucial for stratigraphical analysis. The dynamic fades form regular sequences -alluvial suites that combine into series. Individual suites and series are characterized by their mode of occurrence, fades composition, lithological features and expression in the modern landscape. Their stratigraphic position is established with reference to index beds and palaeontological, geochronological and archaeological research, allowing them to be correlated along the valley. Correlation between different parts of the Dnieper system uses a combination of fades and geomorphological analyses, whereas correlation with other river systems makes use of mammalian and molluscan biostratigraphy. Global events (marine regressions and glaciations) that brought about similar reactions in different fluvial systems can be also used for correlation.