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
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F24%3A10169292" target="_blank" >RIV/00025798:_____/24:10169292 - isvavai.cz</a>
Alternative codes found
RIV/00216224:14310/24:00135991
Result on the web
<a href="https://doi.org/10.1016/j.aeolia.2024.100927" target="_blank" >https://doi.org/10.1016/j.aeolia.2024.100927</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.aeolia.2024.100927" target="_blank" >10.1016/j.aeolia.2024.100927</a>
Alternative languages
Result language
angličtina
Original language name
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
Original language description
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 x 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.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10505 - Geology
Result continuities
Project
<a href="/en/project/EF16_013%2F0001708" target="_blank" >EF16_013/0001708: ECOPOLARIS - Changes in structure and function of components of terrestrial polar ecosystems (CzechPolar2)</a><br>
Continuities
V - Vyzkumna aktivita podporovana z jinych verejnych zdroju
Others
Publication year
2024
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Aeolian Research
ISSN
1875-9637
e-ISSN
2212-1684
Volume of the periodical
67-69
Issue of the periodical within the volume
100927
Country of publishing house
NL - THE KINGDOM OF THE NETHERLANDS
Number of pages
19
Pages from-to
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UT code for WoS article
001238770300001
EID of the result in the Scopus database
2-s2.0-85192099968