The Mroczna Cave is one of the longest caves in the Beskid Niski Mts., located on the south-western slopes of Mt Kornuty, along the main scarp of the landslide. According to the geomechanical criterion, it is dilation cave, where extension has played a major role. Morphotectonic analysis indicates that the main gravitational movement was of a toppling nature but there were also rotation around the vertical axis as well as a backward rotation. The relatively large cave depth (15.5 m) and its shape (cross-section of its passages) indicate that it was formed along a new gravitational cutting surface of the rock massif, associated with joint sets
The occurrence and evolution of crevice-type caves is one of the most spectacular phenomena in the p...
The Czerwone Wierchy Nappe is the main part of the Czerwone Wierchy Massif. Several big cave systems...
International audienceDeep-seated mass movements currently comprise one of the main morphogenetic pr...
The Mroczna Cave is one of the longest caves in the Beskid Niski Mts., located on the south-western ...
Analysis of non-karst caves in the Flysch Carpathians confirms the connection between the tectonic e...
Crevice-type caves, formed along joints, are very common in the Polish Flysch Carpathians (more than...
Crevice-type caves are among the least investigated natural phenomena connected with the development...
The numerous landslides which have developed in the mostly Cretaceous to Eocene turbiditic rocks of ...
Mass movements have been one of the most efficient processes controlling the morphogenesis of the Ou...
The Cyrilka Cave is the second longest pseudokarst cave and the longest crevice-type cave in Czechia...
The study area is located in the Tatra Mts., the part of Western Carpathians. In the Poszukiwaczy Sk...
Detailed structural analysis and geomorphological observations supplemented by the analysis of the d...
The Cyrilka Cave is the second longest pseudokarst cave and the longest crevice-type cave in Czechia...
Detailed structural analysis and geomorphological observations supplemented by the analysis of the d...
Tectonically deformed cave passages in the Tatra Mts (Central Western Carpathians) indicate some fau...
The occurrence and evolution of crevice-type caves is one of the most spectacular phenomena in the p...
The Czerwone Wierchy Nappe is the main part of the Czerwone Wierchy Massif. Several big cave systems...
International audienceDeep-seated mass movements currently comprise one of the main morphogenetic pr...
The Mroczna Cave is one of the longest caves in the Beskid Niski Mts., located on the south-western ...
Analysis of non-karst caves in the Flysch Carpathians confirms the connection between the tectonic e...
Crevice-type caves, formed along joints, are very common in the Polish Flysch Carpathians (more than...
Crevice-type caves are among the least investigated natural phenomena connected with the development...
The numerous landslides which have developed in the mostly Cretaceous to Eocene turbiditic rocks of ...
Mass movements have been one of the most efficient processes controlling the morphogenesis of the Ou...
The Cyrilka Cave is the second longest pseudokarst cave and the longest crevice-type cave in Czechia...
The study area is located in the Tatra Mts., the part of Western Carpathians. In the Poszukiwaczy Sk...
Detailed structural analysis and geomorphological observations supplemented by the analysis of the d...
The Cyrilka Cave is the second longest pseudokarst cave and the longest crevice-type cave in Czechia...
Detailed structural analysis and geomorphological observations supplemented by the analysis of the d...
Tectonically deformed cave passages in the Tatra Mts (Central Western Carpathians) indicate some fau...
The occurrence and evolution of crevice-type caves is one of the most spectacular phenomena in the p...
The Czerwone Wierchy Nappe is the main part of the Czerwone Wierchy Massif. Several big cave systems...
International audienceDeep-seated mass movements currently comprise one of the main morphogenetic pr...