About: Geomorphological, pedological and dendrochronological signatures of a relict landslide terrain, Mt Garbatka (Kamienne Mts), SW Poland     Goto   Sponge   NotDistinct   Permalink

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  • In the Kamienne Mountains the largest concentration of apparently relict landslides in the Sudetes range occurs. Geomorphic signatures of mass movement are subdued, suggesting that considerable time has elapsed since the origin of the landslide and that large-scale mass movements are likely pre-Holocene in age. This is consistent with the results of an extensive soil survey within the landslide body and on the surrounding slopes. Dendrogeomorphological research, in turn, yielded evidence of numerous growth disturbances recorded in tree rings of Norway spruce growing on the landslide body. These signals are interpreted that the slope surface is not entirely stable under current environmental conditions. Flow or creep of landslide material is not very likely, given the characteristics of cover materials, and it is hypothesized that dendrochronological signals develop in response to ground deformation through piping and throughflow.
  • In the Kamienne Mountains the largest concentration of apparently relict landslides in the Sudetes range occurs. Geomorphic signatures of mass movement are subdued, suggesting that considerable time has elapsed since the origin of the landslide and that large-scale mass movements are likely pre-Holocene in age. This is consistent with the results of an extensive soil survey within the landslide body and on the surrounding slopes. Dendrogeomorphological research, in turn, yielded evidence of numerous growth disturbances recorded in tree rings of Norway spruce growing on the landslide body. These signals are interpreted that the slope surface is not entirely stable under current environmental conditions. Flow or creep of landslide material is not very likely, given the characteristics of cover materials, and it is hypothesized that dendrochronological signals develop in response to ground deformation through piping and throughflow. (en)
Title
  • Geomorphological, pedological and dendrochronological signatures of a relict landslide terrain, Mt Garbatka (Kamienne Mts), SW Poland
  • Geomorphological, pedological and dendrochronological signatures of a relict landslide terrain, Mt Garbatka (Kamienne Mts), SW Poland (en)
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  • Geomorphological, pedological and dendrochronological signatures of a relict landslide terrain, Mt Garbatka (Kamienne Mts), SW Poland
  • Geomorphological, pedological and dendrochronological signatures of a relict landslide terrain, Mt Garbatka (Kamienne Mts), SW Poland (en)
skos:notation
  • RIV/61988987:17310/14:A1501CJO!RIV15-MSM-17310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • S
http://linked.open...iv/cisloPeriodika
  • Aug 15
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 18287
http://linked.open...ai/riv/idVysledku
  • RIV/61988987:17310/14:A1501CJO
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Landslides; Dendrochronology; Geomorphological mapping; Soils; Electrical resistivity tomography; Sudetes (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • NL - Nizozemsko
http://linked.open...ontrolniKodProRIV
  • [6EE0CC92B299]
http://linked.open...i/riv/nazevZdroje
  • GEOMORPHOLOGY
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 219
http://linked.open...iv/tvurceVysledku
  • Pánek, Tomáš
  • Owczarek, Piotr
  • Migoń, Piotr
  • Malik, Ireneusz
  • Kacprzak, Andrzej
  • Kasprzak, Marek
  • Wistuba, Małgorzata
http://linked.open...ain/vavai/riv/wos
  • 000339775100018
issn
  • 0169-555X
number of pages
http://localhost/t...ganizacniJednotka
  • 17310
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