Počet záznamů: 1
A chronology of landsliding based on archaeological and documentary data: Pavlovské vrchy Hills, Western Carpathian Flysch Belt
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SYSNO ASEP 0531862 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název A chronology of landsliding based on archaeological and documentary data: Pavlovské vrchy Hills, Western Carpathian Flysch Belt Tvůrce(i) Bíl, M. (CZ)
Krejčí, O. (CZ)
Dolák, L. (CZ)
Krejčí, V. (CZ)
Martínek, J. (CZ)
Svoboda, Jiří (ARUB-Q) RID, ORCID, SAICelkový počet autorů 6 Číslo článku 976 Zdroj.dok. Scientific Reports. - : Nature Publishing Group - ISSN 2045-2322
Roč. 10, č. 1 (2020)Poč.str. 12 s. Forma vydání Tištěná - P Jazyk dok. eng - angličtina Země vyd. GB - Velká Británie Klíč. slova shallow landslides ; flysch ; Pavlovské vrchy Hills ; geomorphological mapping ; gravitational slope deformations ; mass movements ; rockfall ; loess ; sequence Vědní obor RIV AC - Archeologie, antropologie, etnologie Obor OECD Archaeology Způsob publikování Open access Institucionální podpora ARUB-Q - RVO:68081758 UT WOS 000538857500001 EID SCOPUS 85078164257 DOI 10.1038/s41598-020-57551-4 Anotace Pavlovské vrchy Hills represent a distinctive elevation near the Czech-Austrian border where the active, dormant and relict landslides cover 12% of the area. Here we focused on the chronology of landsliding in this area using geological, archaeological and historical evidence. The earliest records of landsliding were determined in locations underlying the dated archaeological settlements. The Upper Paleolithic settlement complex dated between 37–24 ka cal BP, was originally deposited over these landslides. It was consequently destroyed in certain places by additional landslides preceding the last (Upper Pleniglacial) loess deposition (22 ka cal BP). These landslides took place before and after the Upper Paleolithic occupation of this area. This Pleistocene landslide event ranks among the oldest (albeit indirectly) dated landslide within the Czech part of the Western Carpathian Flysch Belt. The chronology of later, historical, landsliding was determined using written records (chronicles, official reports, archival evidence, etc.). Continuous records of landsliding were available as of the middle of the seventeenth century. The major concentration of landslides occurred at the beginning of the twentieth century (1910–1915). The 1663 landslide is currently the oldest landslide, in the Czech part of the Western Carpathian Flysch Belt, which was dated on the basis of documentary data. Pracoviště Archeologický ústav Brno Kontakt Hedvika Břínková, brinkova@arub.cz, Tel.: +420 515 911 112 Rok sběru 2021 Elektronická adresa https://www.nature.com/articles/s41598-020-57551-4
Počet záznamů: 1