Pieniny Klippen Belt

E676434

Pieniny Klippen Belt is a narrow, geologically complex mountain zone in the Western Carpathians, renowned for its striking limestone cliffs and tectonically deformed rock formations.

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Statements (48)

Predicate Object
instanceOf geological formation
mountain belt
tectonic zone
characterizedBy intense tectonic deformation
klippen
strike-slip faults
thrust faults
contains Cretaceous sediments
Jurassic sediments
Paleogene sediments
highly folded sedimentary sequences
numerous tectonic windows
country Poland
Slovakia
crossedBy Dunajec River NERFINISHED
extendsAlong Poland–Slovakia border NERFINISHED
formedBy Alpine orogeny NERFINISHED
geologicalAge Cenozoic
Mesozoic
hasStructure fault-bounded klippen blocks
imbricated thrust sheets
overthrust nappes
hasTypeLocality Pieniny region NERFINISHED
importantFor paleogeographic reconstructions of the Tethys Ocean margins
reconstruction of Carpathian orogenic evolution
isSubjectOf numerous geological mapping projects
regional tectonic models of the Carpathians
knownFor narrow tectonic zone
steep limestone cliffs
lithology conglomerate
limestone
marl
shale
locatedIn Carpathian Mountains NERFINISHED
Central Europe
maximumWidth several kilometers
namedAfter Pieniny Mountains NERFINISHED
orientation generally east–west
partOf Western Carpathians NERFINISHED
separates Inner Carpathian units NERFINISHED
Outer Carpathian flysch belt NERFINISHED
studiedInDiscipline stratigraphy
structural geology
tectonics
tectonicSetting suture zone between Inner and Outer Carpathians
transpressional shear zone
visibleIn Pieniny National Park (Poland) NERFINISHED
Pieniny National Park (Slovakia) NERFINISHED

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Sokolica peak geologicalFormation Pieniny Klippen Belt