2025
The Mountain Plateau hayl as a Specific Form of Karst Depression in the Al-Hajar Mountains (South-Eastern Arabia)
MATEICIUCOVÁ, Inna; Maximilian WILDING; Miroslav BUBÍK a Jiří OTAVAZákladní údaje
Originální název
The Mountain Plateau hayl as a Specific Form of Karst Depression in the Al-Hajar Mountains (South-Eastern Arabia)
Název česky
Hayl jako specifická forma krasové deprese na náhorních plošinách pohoří Al-Hajar (jihovýchodní Arábie)
Autoři
MATEICIUCOVÁ, Inna; Maximilian WILDING; Miroslav BUBÍK a Jiří OTAVA
Vydání
Open Quaternary, Ubiquity Press Ltd, 2025, 2055-298X
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
60102 Archaeology
Stát vydavatele
Velká Británie a Severní Irsko
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Označené pro přenos do RIV
Ano
Organizační jednotka
Filozofická fakulta
EID Scopus
Klíčová slova anglicky
Al-Hajar Mountains; karst depression; aeolian silt; terra rossa; microfossils; translucent heavy minerals
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 12. 3. 2026 10:59, Mgr. Ester Gaja Pučálková, Ph.D.
Anotace
V originále
This contribution investigates the formation of karst depressions containing metres of fine sediment and prehistoric artefacts at an elevation of around 1000 m a.s.l. in the central part of the Al-Hajar Mountains in south-eastern Arabia. Through field reconnaissance, satellite imagery analysis and laboratory methods, we highlight the origin of their thick sediment deposits and the factors enabling their retention in an otherwise erosional landscape. Comprehensive analyses of heavy minerals and microfossils reveal that the sediment deposits accumulated in the depressions of the Sint Karst Plateau (local term: huyul, sg. hayl) contain alluvially redeposited aeolian materials rather than in situ weathering products. The basal terra rossa incorporates dust from surrounding rock formations, while the overlying silt originates from more distant sources, presumably coastal shelves exposed during marine regression (for instance, from the Arabian Gulf). The sediment aggradation and flooding observable at huyul is attributed to clogging by suspended silt particles during the infiltration of floodwater – a process similar to siltation in modern recharge dams, although occurring at a much different temporal scale and hydraulic pressure. Satellite imagery confirms that similar clusters of karst depressions exist elsewhere in the Al-Hajar Mountains at elevations between 700–1500 m a.s.l. and that they are specifically associated with near-horizontal karst plateaus with a distinctive criss-cross pattern of fractures. These mountain plateau huyul represent valuable palaeoclimatic and palaeoenvironmental archives and have preserved aeolian dust no longer present in steep terrain of equal elevation.
Návaznosti
| MUNI/FF-DEAN/1561/2022, interní kód MU |
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| MUNI/FF-DEAN/1705/2023, interní kód MU |
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