J 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.