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@article{2401321,
author = {Holuša, Jakub and Hanáček, Martin and Nývlt, Daniel and Woronko, Barbara and Stuchlík, Radim},
article_number = {September 2024},
doi = {http://dx.doi.org/10.1016/j.aeolia.2024.100927},
keywords = {Aeolian sediments; Central Europe; Colluvial redeposition; European Ice Sheet Complex; Periglacial environment; Pleistocene; Quartz grain morphology},
language = {eng},
issn = {1875-9637},
journal = {Aeolian Research},
title = {Evolution of Weichselian aeolian strata on a coarse-grained substrate in a rugged piedmont topography: A case study from the foothills of the eastern Sudetes Mts., Czechia},
url = {https://www.sciencedirect.com/science/article/pii/S1875963724000387},
volume = {67-69},
year = {2024}
}
TY - JOUR
ID - 2401321
AU - Holuša, Jakub - Hanáček, Martin - Nývlt, Daniel - Woronko, Barbara - Stuchlík, Radim
PY - 2024
TI - Evolution of Weichselian aeolian strata on a coarse-grained substrate in a rugged piedmont topography: A case study from the foothills of the eastern Sudetes Mts., Czechia
JF - Aeolian Research
VL - 67-69
IS - September 2024
SP - 1-19
EP - 1-19
PB - Elsevier B.V.
SN - 18759637
KW - Aeolian sediments
KW - Central Europe
KW - Colluvial redeposition
KW - European Ice Sheet Complex
KW - Periglacial environment
KW - Pleistocene
KW - Quartz grain morphology
UR - https://www.sciencedirect.com/science/article/pii/S1875963724000387
N2 - The southern margins of the northern European loess belt on the foothills of Eastern Sudetes Mountains are less explored sedimentation zones. This study provides new data about the development of aeolian silty-sandy sediments overlying the glaciofluvial succession on the rugged topography near the village of Kolnovice. The Kolnovice sand quarry (360 × 200 m), which lies at the margin of the upland plateau, is the only active-mined outcrop on the foothills of the Eastern Sudetes and is large enough to study Pleistocene (peri-)glacial sediments. To examine the origin of these sediments, we applied lithofacies analysis (both macro-description of outcrop walls and micromorphological study of thin sections) and surface analysis of quartz grains. Periglacial structures have been identified within the sediments, allowing us to further interpret the post-sedimentary evolution of the sedimentary succession. The studied sediments resulted from colluvial redeposition of aeolian sediments, which was controlled particularly by the topography, glaciofluvial substrate, and climatic conditions. The underlying glaciofluvial sediments are the most crucial source of the studied sediments, although the fine-grained material could have been transported from more distant areas.
ER -
HOLUŠA, Jakub, Martin HANÁČEK, Daniel NÝVLT, Barbara WORONKO and Radim STUCHLÍK. Evolution of Weichselian aeolian strata on a coarse-grained substrate in a rugged piedmont topography: A case study from the foothills of the eastern Sudetes Mts., Czechia. \textit{Aeolian Research}. Elsevier B.V., 2024, 67-69, September 2024, p.~1-19. ISSN~1875-9637. Available from: https://dx.doi.org/10.1016/j.aeolia.2024.100927.
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