Detailed Information on Publication Record
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.Basic information
Original name
A chronology of landsliding based on archaeological and documentary data: Pavlovské vrchy Hills, Western Carpathian Flysch Belt
Authors
BÍL, Michal (203 Czech Republic, guarantor), Oldřich KREJČÍ (203 Czech Republic), Lukáš DOLÁK (203 Czech Republic), Vladimíra KREJČÍ, Jan MARTÍNEK (203 Czech Republic) and Jiří SVOBODA (203 Czech Republic, belonging to the institution)
Edition
Scientific reports, London, Nature Publishing Group, 2020, 2045-2322
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
50704 Environmental sciences
Country of publisher
United Kingdom of Great Britain and Northern Ireland
Confidentiality degree
není předmětem státního či obchodního tajemství
References:
Impact factor
Impact factor: 4.379
RIV identification code
RIV/00216224:14310/20:00115231
Organization unit
Faculty of Science
UT WoS
000538857500001
Keywords in English
Pavlovské vrchy Hills; landsliding; Natural hazards; Geomorphology
Tags
Tags
Reviewed
Změněno: 2/10/2020 10:56, Mgr. Marie Šípková, DiS.
Abstract
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.