Carpathian Flysch Belt
The Carpathian Flysch Belt is an arcuate tectonic zone included in the megastructural elevation of the Carpathians on the external periphery of the mountain chain. Geomorphologically it is a portion of Outer Carpathians. Geologically it is a thin-skinned thrust belt, formed by rootles nappes consisting of so-called flysch - alternating marine deposits of claystones, shales and sandstones which were detached from their substratum and moved tens of kilometers to the north (generally). The Flysch Belt is together with Neogene volcanic complexes only tectonic zone occurring along the whole Carpathian arc.
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Carpathian Flysch Belt
The Carpathian Flysch Belt is an arcuate tectonic zone included in the megastructural elevation of the Carpathians on the external periphery of the mountain chain. Geomorphologically it is a portion of Outer Carpathians. Geologically it is a thin-skinned thrust belt, formed by rootles nappes consisting of so-called flysch - alternating marine deposits of claystones, shales and sandstones which were detached from their substratum and moved tens of kilometers to the north (generally). The Flysch Belt is together with Neogene volcanic complexes only tectonic zone occurring along the whole Carpathian arc.
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Flisz karpacki – określenie re ...... lański – oraz Liptów i Spisz).
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The Carpathian Flysch Belt is ...... long the whole Carpathian arc.
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34,518,339
Wikipage revision ID
736,482,729
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Flisz karpacki – określenie re ...... , frakcjonalnego uwarstwienia.
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The Carpathian Flysch Belt is ...... long the whole Carpathian arc.
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Carpathian Flysch Belt
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Flisz karpacki
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