The late Little Ice Age landslide calamity in North Bohemia:
Triggers, impacts and post-landslide development reconstructed
from documentary data (case study of the Kozí vrch Hill
landslide)

J 2016

The late Little Ice Age landslide calamity in North Bohemia: Triggers, impacts and post-landslide development reconstructed from documentary data (case study of the Kozí vrch Hill landslide)

RAŠKA, Pavel, Vilém ZÁBRANSKÝ, Rudolf BRÁZDIL a Jana LAMKOVÁ

Základní údaje

Originální název

The late Little Ice Age landslide calamity in North Bohemia: Triggers, impacts and post-landslide development reconstructed from documentary data (case study of the Kozí vrch Hill landslide)

Autoři

RAŠKA, Pavel (203 Česká republika), Vilém ZÁBRANSKÝ (203 Česká republika), Rudolf BRÁZDIL (203 Česká republika, garant, domácí) a Jana LAMKOVÁ (203 Česká republika)

Vydání

Geomorphology, Elsevier Science BV, 2016, 0169-555X

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

Zemský magnetismus, geodesie, geografie

Stát vydavatele

Nizozemské království

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 2.958

Kód RIV

RIV/00216224:14310/16:00087756

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1016/j.geomorph.2015.12.009

UT WoS

000369451100008

Klíčová slova anglicky

Landslide reconstruction; Documentary data; Little Ice Age; North Bohemia

Štítky

AKR, rivok

Změněno: 14. 4. 2017 14:56, Ing. Andrea Mikešková

Anotace

V originále

The beginning of the 1770s in the Czech Lands is well documented for its meteorological extremes and their social impacts. However, the effects of these extremes on geomorphic systems and on landslide occurrence and activity in particular have been minimally studied. In this paper, we use a complex set of written and iconographic documentary data to reconstruct the landslide calamity in North Bohemia, with a detailed case study of the Kozí vrch Hill landslide. The landslide calamity of 1770 is the oldest known landslide calamity in this region, including 14 documented events; and its reconstructionmay therefore provide important data on landslide frequency, triggers, and impacts during the adverse weather patterns in the last part of the Little Ice Age (LIA). We focus on a case study of the Kozí vrch Hill landslide, and we use the documentary evidence and field techniques to reconstruct its location, extent, topography, kinematics, and triggers. Based on precipitation indices and weather descriptions, the extremely wet and rainy preceding year and the 1769/1770 winter were the major triggering factors that resulted inwater saturation of Neogene volcaniclastics underlying the basalt lava flows and their subsequent collapse. Furthermore, we analyse the post-landslide terrain transformation and land use patterns during the 240 years following the landslide to illustrate the persistence of particular landslide features.Weconclude that the major transformations, which obscured most of the landslide features, occurred in only the last 50–60 years. Finally, we discuss the role of documentary data and the current methodological advances in their use for the reconstruction of landslide frequency and impacts during the LIA.

Návaznosti

GAP209/11/0956, projekt VaV

Název: Globální a regionální modelové simulace klimatu ve střední Evropě v 18.-20. století v porovnání s pozorovaným a rekonstruovaným klimatem

Investor: Grantová agentura ČR, Globální a regionální modelové simulace klimatu ve střední Evropě v 18.-20. století v porovnání s pozorovaným a rekonstruovaným klimatem

Citovat

RAŠKA, Pavel, Vilém ZÁBRANSKÝ, Rudolf BRÁZDIL a Jana LAMKOVÁ. The late Little Ice Age landslide calamity in North Bohemia: Triggers, impacts and post-landslide development reconstructed from documentary data (case study of the Kozí vrch Hill landslide). Geomorphology. Elsevier Science BV, 2016, roč. 255, February, s. 95-107. ISSN 0169-555X. Dostupné z: https://dx.doi.org/10.1016/j.geomorph.2015.12.009.

@article{1322780,
   author = {Raška, Pavel and Zábranský, Vilém and Brázdil, Rudolf and Lamková, Jana},
   article_number = {February},
   doi = {http://dx.doi.org/10.1016/j.geomorph.2015.12.009},
   keywords = {Landslide reconstruction; Documentary data; Little Ice Age; North Bohemia},
   language = {eng},
   issn = {0169-555X},
   journal = {Geomorphology},
   title = {The late Little Ice Age landslide calamity in North Bohemia: Triggers, impacts and post-landslide development reconstructed from documentary data (case study of the Kozí vrch Hill landslide)},
   volume = {255},
   year = {2016}
}

TY  - JOUR
ID  - 1322780
AU  - Raška, Pavel - Zábranský, Vilém - Brázdil, Rudolf - Lamková, Jana
PY  - 2016
TI  - The late Little Ice Age landslide calamity in North Bohemia: Triggers, impacts and post-landslide development reconstructed from documentary data (case study of the Kozí vrch Hill landslide)
JF  - Geomorphology
VL  - 255
IS  - February
SP  - 95-107
EP  - 95-107
PB  - Elsevier Science BV
SN  - 0169555X
KW  - Landslide reconstruction
KW  - Documentary data
KW  - Little Ice Age
KW  - North Bohemia
N2  - The beginning of the 1770s in the Czech Lands is well documented for its meteorological extremes and their social impacts. However, the effects of these extremes on geomorphic systems and on landslide occurrence and activity in particular have been minimally studied. In this paper, we use a complex set of written and iconographic documentary data to reconstruct the landslide calamity in North Bohemia, with a detailed case study of the Kozí vrch Hill landslide. The landslide calamity of 1770 is the oldest known landslide calamity in this region, including 14 documented events; and its reconstructionmay therefore provide important data on landslide frequency, triggers, and impacts during the adverse weather patterns in the last part of the Little Ice Age (LIA). We focus on a case study of the Kozí vrch Hill landslide, and we use the documentary evidence and field techniques to reconstruct its location, extent, topography, kinematics, and triggers. Based on precipitation indices and weather descriptions, the extremely wet and rainy preceding year and the 1769/1770 winter were the major triggering factors that resulted inwater saturation of Neogene volcaniclastics underlying the basalt lava flows and their subsequent collapse. Furthermore, we analyse the post-landslide terrain transformation and land use patterns during the 240 years following the landslide to illustrate the persistence of particular landslide features.Weconclude that the major transformations, which obscured most of the landslide features, occurred in only the last 50–60 years. Finally, we discuss the role of documentary data and the current methodological advances in their use for the reconstruction of landslide frequency and impacts during the LIA.
ER  -

RAŠKA, Pavel, Vilém ZÁBRANSKÝ, Rudolf BRÁZDIL a Jana LAMKOVÁ. The late Little Ice Age landslide calamity in North Bohemia: Triggers, impacts and post-landslide development reconstructed from documentary data (case study of the Kozí vrch Hill landslide). \textit{Geomorphology}. Elsevier Science BV, 2016, roč.~255, February, s.~95-107. ISSN~0169-555X. Dostupné z: https://dx.doi.org/10.1016/j.geomorph.2015.12.009.

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