A chronology of landsliding based on archaeological and documentary data: Pavlovské vrchy Hills, Western Carpathian Flysch Belt. [PDF]
Sci Rep, 2020 AbstractPavlovské vrchy Hills represent a distinctive elevation near the Czech-Austrian border where the active, dormant and relict landslides cover 12% of the area. Here we focused on the chronology of landsliding in this area using geological, archaeological and historical evidence.
Bíl M +5 more
europepmc +4 more sources
Sandstone dikes in the Rača unit Slovak Outer flysch belt [PDF]
Acta Montanistica Slovaca, 2008 In the study area by geological mapping we localized Zlín Formation, situated in north - east area of Outer Western Carpathians,near the Nová Polianka village.
Stanislav Jacko, Martin Udič
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Structure and dynamics of deep-seated slope failures in the Magura Flysch Nappe, outer Western Carpathians (Czech Republic) [PDF]
Natural Hazards and Earth System Sciences, 2004 Deep-seated mass movements currently comprise one of the main morphogenetic processes in the Flysch Belt of the Western Carpathians of Central Europe. These mass movements result in a large spectrum of slope failures, depending on the type of movement ...
I. Baron +5 more
doaj +3 more sources
Contributions to Geophysics and Geodesy, 2012 A positive gravity anomaly was observed in the Flysch belt realm. Based on this fact and available geological knowledge we suppose that the source of gravity anomaly might be carbonate rocks lying perhaps in the footwall of Flysch sediments.
Ľudovít KUCHARIČ +3 more
doaj +2 more sources
Numerical analysis of deep-seated mass movements in the Magura Nappe; Flysch Belt of the Western Carpathians (Czech Republic) [PDF]
Natural Hazards and Earth System Sciences, 2005 Deep-seated slope failures are common features in the mountains of the Raca Unit, Magura Nappe of the Flysch Belt of Western Carpathians. Since they represent very complicated system, understanding of their evolution and triggers still remains unclear ...
I. Baron +4 more
doaj +6 more sources
SOME CHARACTERISTICS OF EOCENE FLYSCH GENESIS, COMPOSITION AND WEATHERING IN CROATIAN COAST BELT
Rudarsko-geološko-naftni Zbornik, 2012 The most common lithotypes of the Eocene flysch in the Croatian coast belt are breccias, conglomerates, (bio)calcirudites, (bio)calcarenites, sandstones, siltstones, shales and marls. Olistolithes also can be constitutive part of Eocene flysch.
Aleksandar Toševski +2 more
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Gravitational dismantling of the Miocene mountain front of the Gibraltar Arc system deduced from the analysis of an olistostromic complex (western Betics) [PDF]
Geologica Acta, 2013 A mélange complex seals the internal-external zone boundary of the western part of the Gibraltar Arc orogenic belt and constitutes a key element to establish milestones of the Betic-Rif tectonic evolution.
E. SUADES, A. CRESPO-BLANC
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Contributions to Geophysics and Geodesy, 2014 The locality of the northeastern most part of Slovakian Flysch belt belongs to interesting areas in terms of the interpretation of geothermal conditions in mutual relation with the lithosphere structure and their tectonic development.
Dušan MAJCIN +5 more
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Investigation of recent catastrophic landslides in the flysch belt of Outer Western Carpathians (Czech Republic): progress towards better hazard assessment [PDF]
Natural Hazards and Earth System Sciences, 2009 Rapid snow melting and intense precipitation triggered and reactivated tens of mostly shallow landslides in the eastern part of the Czech Republic at the turn of March and April 2006.
J. Klimeš +6 more
doaj +4 more sources
Mélange, Flysch and Cliffs in the Pieniny Klippen Belt (Poland): An Overview
Minerals, 2022 The Pieniny Klippen Belt (PKB) is located in the suture zone between the Central and Outer (Flysch) Carpathians. Its structure is an effect of prolonged processes of the Cretaceous–Miocene folding, thrusting and uplifting. In this zone, tectonic components of different ages and features, including strike-slip-bounded tectonic blocks, thrust units, as ...
Jan Golonka +8 more
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