A sedimentary profile consisting of blown sand capped by a sand-loam bedded interval was analysed in the Svätuše sand pit in the East Slovak Lowland. Stratigraphically, blown sands from this lowland have so far only been indirectly classified into the Weichselian glacial, mainly into its middle and upper stages. The age classification presented in this study results from the optically stimulated luminescence dating method. It identifies the blown sand from the Svätuše as originating during the Early Glacial and Early Pleniglacial phases of the Weichselian glacial (MIS 4–5d). At the end of the Early Glacial phase of the Weichselian glacial, palaeoenvironmental conditions changed. The deposition of blown sand became episodic rather than continuous. As a result, the analysed sedimentary record is composed of a sand-loam interbedded interval in the uppermost part.

Jacko Stanislav, Dirnerová Diana, Milovský Rastislav, Aimbetov Izzet Kallievich, Bekimbetov Ruslan Tursinbaevich, Iskenderov Bakhtiyar Kauenderovich, Dospanov Rakhim Rauaj uli. Episodes -0001;0:. https://doi.org/10.18814/epiiugs/2025/025049