- New Challenges of Safety Monitoring of Rock Slopes: The Third Wave2008 | Faculty of Science
- Old but still active: > 18 ka history of rock slope failures affecting a flysch anticline2021 | Faculty of Science
- Observation of the rock slope thermal regime, coupled with crackmeter stability monitoring: Initial results from three different sites in Czechia (central Europe)2021 | Faculty of Science, Central Library of Charles University
- Cosmogenic age constraints on post-LGM catastrophic rock slope failures in the Tatra Mountains (Western Carpathians)2016 | Faculty of Science
- Rock Slopes of the High Tatra Mountains1994 | First Faculty of Medicine, Faculty of Mathematics and Physics
- Analogy in stability evaluation of high rock slopes1993 | First Faculty of Medicine, Faculty of Mathematics and Physics
- Rock Mass Characterization and Rockfall Monitoring: Traditional Approaches2023 | Faculty of Science
- Nonlinear science issues in the dynamics of unstable rock slopes: new tools for rock fall risk assessment and early warnings2006 | First Faculty of Medicine
- Late Quaternary sackungen in the highest mountains of the Carpathians2017 | Faculty of Science
- Report on radiometric 10Be dating of glacial and periglacial landforms in the Giant Mountains2001 | First Faculty of Medicine, Faculty of Mathematics and Physics
- Time constraints for the evolution of a large slope collapse in karstified mountainous terrain of the southwestern Crimean Mountains, Ukraine2009 | Faculty of Science
- Modern Methods of Rock Mass Characterisation and Rockfall Monitoring: A Review2023 | Faculty of Science
- Rock Surface Strain In Situ Monitoring Affected by Temperature Changes at the Požáry Field Lab (Czechia)2023 | Faculty of Science, Central Library of Charles University
- Microseismic events on the Aknes rockslide in Norway located by a back-projection approach2019 | Faculty of Science
- Sackung and enigmatic mass movement folds on a structurally-controlled mountain ridge2018 | Faculty of Science
- Geomorphological evidence and Be-10 exposure ages for the Last Glacial Maximum and deglaciation of the Velka and Mala Studena dolina valleys in the High Tatra Mountains, central Europe2015 | Faculty of Science