Age of Blown Sand in the East Slovak Lowland—Case Study from Svätuše Sand Pit, Slovakia

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.

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Publication Details

Journal
Geosciences
Published
2025-11-12
DOI
https://doi.org/10.3390/geosciences15110429
Primary Topic
Geology and Paleoclimatology Research
Type
article
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article

Age of Blown Sand in the East Slovak Lowland—Case Study from Svätuše Sand Pit, Slovakia

Roman Farkašovský, Róbert Hinca, Diana Dirnerová
Geosciences
Geology and Paleoclimatology Research
article

Age of Blown Sand in the East Slovak Lowland—Case Study from Svätuše Sand Pit, Slovakia

Roman Farkašovský, Róbert Hinca, Diana Dirnerová
article en

Abstract

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.

GeosciencesVol. 15(11)
Slovak University of Technology in Bratislava (SK), Technical University of Košice (SK)
Openalex Percentile: Top 61%
Geology and Paleoclimatology Research
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Age of Blown Sand in the East Slovak Lowland—Case Study from Svätuše Sand Pit, Slovakia — Roman Farkašovský, Róbert Hinca, et al. · Geosciences (2025) | TGRS Research Map | TGRS