The Kamienne Mountains—Late Palaeozoic Volcanic Terrain Shaped by Late Quaternary Landslides

P Migoń - Landscapes and landforms of Poland, 2024 - Springer
Abstract The Kamienne Mountains are an elongated medium-altitude mountain range in the
central part of the Sudetes, built mainly of volcanic and subvolcanic rocks of Permian age. In …

[PDF][PDF] Osuwiska w Sudetach

R Sikora, T Wojciechowski - Przegląd Geologiczny, 2019 - bibliotekanauki.pl
This paper presents the results of analysis of landslides distribution in the Sudetes (SW
Poland). Our study was based on the analysis of the LiDAR-data digital elevation model and …

MONITORING OF ANTHROPOGENIC LANDSLIDE ACTIVITY WITH COMBINED UAV AND LIDAR-DERIVED DEMS-A CASE STUDY OF THE CZERWONY WAWOZ …

A Kowalski, J Wajs, D Kasza - Acta Geodynamica et Geromaterialia, 2018 - go.gale.com
The paper presents the results of fieldwork and geodetic surveys carried out on a landslide
in Wlen (Western Sudetes, Izerskie Foothills). This reactivated landslide occured firstly in …

Geomorphological heritage of cretaceous sandstone terrains in SW Poland: diversity, conservation and interpretation issues

F Duszyński, P Migoń - Geoheritage, 2022 - Springer
The Sudetes mountain range in SW Poland include several areas, where distinctive
topography has developed upon layered sedimentary successions of Cretaceous age, with …

Multistage structural evolution of the end-Cretaceous–Cenozoic Wleń Graben (the Sudetes, NE Bohemian Massif): a contribution to the post-Variscan tectonic history …

A Kowalski - Annales Societatis Geologorum Poloniae, 2021 - yadda.icm.edu.pl
Results of a new mapping and structural field study of the Wleń Graben (North Sudetic
Synclinorium, SW Poland), made up of a post-Variscan volcano-sedimentary succession …

Nowo rozpoznane formy osuwiskowe w dolinie Kaczawy na Pogórzu Kaczawskim (Sudety Zachodnie)

A Kowalski, J Wojewoda - Landform Analysis, 2017 - yadda.icm.edu.pl
Autorzy przedstawiają wyniki badań terenowych i analiz geomorfometrycznych nieznanych
form osuwiskowych położonych w dolinie Kaczawy pomiędzy Sędziszową a Nowym …

Not simply volcanoes–the geoheritage of the Cretaceous system in the Land of the Extinct Volcanoes Geopark, West Sudetes (SW Poland)

P Migoń, E Pijet-Migoń - Geotourism/Geoturystyka, 2021 - infona.pl
Volcanic geoheritage is emphasized as the main asset and distinctive characteristic of the
Land of Extinct Volcanoes Geopark in the West Sudetes (SW Poland). However, the …

[PDF][PDF] Structural control of mass movements on slopes formed of magmatic and metamorphic rocks: the case study of Wielisławka Mt.(SW Poland, Sudetes Mts.)

A Kowalski, D Kasza, J Wajs - Geological Quarterly, 2019 - bibliotekanauki.pl
We indicate the structural controls on, and provide an evolutionary model of, mass
movements which developed on the slopes of a rhyolitic lava dome built of massive, sub …

[PDF][PDF] Geneza i geologiczne uwarunkowania rozwoju form osuwiskowych w środkowej części Obniżenia Noworudzkiego w Sudetach

A Kowalski - Przegląd Geologiczny, 2021 - bibliotekanauki.pl
The paper presents the results of field mapping and structural analyses conducted within the
landslides situated near Ludwikowice K³odzkie, in the central part of the Nowa Ruda Basin …

[PDF][PDF] Przydatność pomiarów georadarowych i analiz geomorfometrycznych do rozpoznania wewnętrznej struktury płytkich osuwisk: na przykładzie góry Średniak w …

M Makoś, A Sobczyk - Przegląd Geologiczny, 2018 - bibliotekanauki.pl
The paper reviews an application of non-destructive electromagnetic imaging of shallow
bedrock and landslide colluvium horizons performed with ground-penetrating radar (GPR) …