Geotope of boulder accumulations: Possible source of noise in the dendrogeomorphic dating of landslides
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F22%3AN2302DFE" target="_blank" >RIV/61988987:17310/22:N2302DFE - isvavai.cz</a>
Result on the web
<a href="https://www.sciencedirect.com/science/article/pii/S034181622200128X" target="_blank" >https://www.sciencedirect.com/science/article/pii/S034181622200128X</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.catena.2022.106142" target="_blank" >10.1016/j.catena.2022.106142</a>
Alternative languages
Result language
angličtina
Original language name
Geotope of boulder accumulations: Possible source of noise in the dendrogeomorphic dating of landslides
Original language description
Dendrogeomorphic dating is an effective tool for the assessment of past landslide activity. However, some complex landslide areas include zones of accumulated boulders that can represent geotopes with deteriorated conditions for the stable anchoring of tree roots. Under such conditions, wind gusts can easily cause stem tilting and subsequently be a source of growth disturbances and false landslide events. This study evaluated this possible source of uncertainty in tree rings based on the dating of selected flow-like shaped accumulations of boulders in the Outer Western Carpathians. The data from 94 Norway spruce (Picea abies (L.) Karst.) individuals provided evidence of 154 growth disturbances that were fully comparable with the frequency of active landslides. However, geophysical geoelectrical sounding in combination with field mapping suggests that the studied accumulation is stable. Growth disturbances enabled the reconstruction of nine past events, reaching the minimal threshold of the percentage index. Analysis of triggers detected the occurrence of above-average wind gust speeds in event years compared to other years. Moreover, the dated growth disturbances were not present in the reference trees, probably due to the more stable positions of these trees and thus their better resistance to wind forces. Moreover, the duration of growth disturbances in event years was significantly longer than that of disturbances in other years.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10508 - Physical geography
Result continuities
Project
<a href="/en/project/GA19-01866S" target="_blank" >GA19-01866S: Ancient landslides: really inactive?</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2022
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
CATENA
ISSN
0341-8162
e-ISSN
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Volume of the periodical
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Issue of the periodical within the volume
červen
Country of publishing house
NL - THE KINGDOM OF THE NETHERLANDS
Number of pages
10
Pages from-to
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UT code for WoS article
000793184000003
EID of the result in the Scopus database
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