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Deep-seated gravitational slope deformations in neovolcanic mountain ranges of Slovakia
Summary Deep-seated gravitational slope deformations in neovolcanic mountain ranges in Slovakia arise in places where brittle volcanic rocks (andesites, basalts and their pyroclastic material) rest on plastic Paleogene or Neogene rocks. Where such a structure is associated with tectonic elevations, block rifts, bulging phenomena, block fields, landslides, rockfalls and earthflows occur. The deformations are most frequent on the peripheries of the Vtáčnik and the Kremnické hory Mts. (on an area of 186 sq.km), on the periphery of the Slánske vrchy Mts. (120 sq.km). The deformations cover smaller areas in other mountain ranges. Active block movements are a serious geotechnical problem, since they are most dangerous in Slovakia.
Deep-seated gravitational slope deformations in neovolcanic mountain ranges of Slovakia
Summary Deep-seated gravitational slope deformations in neovolcanic mountain ranges in Slovakia arise in places where brittle volcanic rocks (andesites, basalts and their pyroclastic material) rest on plastic Paleogene or Neogene rocks. Where such a structure is associated with tectonic elevations, block rifts, bulging phenomena, block fields, landslides, rockfalls and earthflows occur. The deformations are most frequent on the peripheries of the Vtáčnik and the Kremnické hory Mts. (on an area of 186 sq.km), on the periphery of the Slánske vrchy Mts. (120 sq.km). The deformations cover smaller areas in other mountain ranges. Active block movements are a serious geotechnical problem, since they are most dangerous in Slovakia.
Deep-seated gravitational slope deformations in neovolcanic mountain ranges of Slovakia
Malgot, J. (author)
1977
Article (Journal)
Electronic Resource
English
BKL:
56.00$jBauwesen: Allgemeines
/
38.58
Geomechanik
/
38.58$jGeomechanik
/
56.20
Ingenieurgeologie, Bodenmechanik
/
56.00
Bauwesen: Allgemeines
/
56.20$jIngenieurgeologie$jBodenmechanik
RVK:
ELIB18
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