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First dendrogeomorphological dating of DSGSD: specificity of the reconstruction

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F25%3AA2603BCJ" target="_blank" >RIV/61988987:17310/25:A2603BCJ - isvavai.cz</a>

  • Result on the web

    <a href="https://link.springer.com/10.1007/s10346-025-02538-3" target="_blank" >https://link.springer.com/10.1007/s10346-025-02538-3</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s10346-025-02538-3" target="_blank" >10.1007/s10346-025-02538-3</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    First dendrogeomorphological dating of DSGSD: specificity of the reconstruction

  • Original language description

    Globally, one of the most widespread types of slope deformation is DSGSD (deep-seated gravitational slope deformation), which typically takes tens of thousands of years to develop, but can also be catastrophically reactivated and may represent a recent natural hazard. Knowledge of their past evolution is based mostly on absolute dating of old whereas recent evolution can be covered by appropriate monitoring. Bridging these two time periods is currently a major challenge. This study thus presents unique dating of DSGSD evolution using dendrogeomorphic (tree-ring-based) methods over the last 60 years. The uniqueness of the study also lies in the origin of DSGSD, which was anthropogenically induced through deep lignite mining that began in 1962. Tree-ring-based data from 71 disturbed trees (<jats:italic>Fagus sylvatica</jats:italic> L. and <jats:italic>Larix decidua</jats:italic> Mill.) revealed the specific effects of DSGSD movements on the growth of both tree species, which are usable in future research. At the same time, the obtained chronology of movements revealed the occurrence of initial failure of DSGSD and their subsequent cessation, except for one part of the studied slope, in which there is a simultaneous recovery of movements. The dendrogeomorphic analysis confirmed the generally assumed evolution of DSGSD but in a very limited time period, which may be related to the anthropogenic influence on its formation. The research was complemented by an analysis of the dynamics of post-failure evolution of landforms based on anatomical data from exposed tree roots. The results suggest rapid erosional modelling of the newly formed DSGSD.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10508 - Physical geography

Result continuities

  • Project

    <a href="/en/project/GA22-12522S" target="_blank" >GA22-12522S: Tree-ring microscopic anatomy as a chronological data source for optimization of landslide hazard assessment</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2025

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Landslides

  • ISSN

    1612-510X

  • e-ISSN

    1612-5118

  • Volume of the periodical

  • Issue of the periodical within the volume

    8

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    12

  • Pages from-to

    2573-2584

  • UT code for WoS article

    001492095200001

  • EID of the result in the Scopus database

    2-s2.0-105005572569