2020
A chronology of landsliding based on archaeological and documentary data: Pavlovské vrchy Hills, Western Carpathian Flysch Belt
BÍL, Michal, Oldřich KREJČÍ, Lukáš DOLÁK, Vladimíra KREJČÍ, Jan MARTÍNEK et. al.Základní údaje
Originální název
A chronology of landsliding based on archaeological and documentary data: Pavlovské vrchy Hills, Western Carpathian Flysch Belt
Autoři
BÍL, Michal (203 Česká republika, garant), Oldřich KREJČÍ (203 Česká republika), Lukáš DOLÁK (203 Česká republika), Vladimíra KREJČÍ, Jan MARTÍNEK (203 Česká republika) a Jiří SVOBODA (203 Česká republika, domácí)
Vydání
Scientific reports, London, Nature Publishing Group, 2020, 2045-2322
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
50704 Environmental sciences
Stát vydavatele
Velká Británie a Severní Irsko
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 4.379
Kód RIV
RIV/00216224:14310/20:00115231
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000538857500001
Klíčová slova anglicky
Pavlovské vrchy Hills; landsliding; Natural hazards; Geomorphology
Štítky
Příznaky
Recenzováno
Změněno: 2. 10. 2020 10:56, Mgr. Marie Šípková, DiS.
Anotace
V originále
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.