- Are the highest parts of the Sudetes above the upper timber line a periglacial domain?2010 | Faculty of Science
- Gravity Disturbances, Marussi Tensor, Invariants and Other Functions of the Geopotential Represented by EGM 20082014 | Faculty of Science
- Periglacial landforms above alpine timberline in the High Sudetes2007 | Faculty of Science
- Natural relations of spatial distribution of periglacial landforms above the alpine timberline in the Giant Mts. (Czech Republic)2007 | Faculty of Science
- Periglacial Landforms of the Hrubý Jeseník Mountains2016 | Faculty of Science
- PERICLIMv1.0: a model deriving palaeo-air temperatures from thaw depth in past permafrost regions2021 | Faculty of Science
- Periglacial features and their protection2019 | Faculty of Science
- Morphostructural evolution of the relief in the locality of the Geodynamic Observatory at Pecný, the Ondřejovská vrchovina Highland, Czech Republic2007 | Faculty of Science
- Dynamics of landform evolution in the Makalu ? Barun region, Nepal2007 | Faculty of Science
- Landform evolution in the Nagar region2007 | Faculty of Science
- Landform evolution of the Makalu - Barun region in the East Nepal Himalaya2013 | Faculty of Science, Central Library of Charles University
- Mass distribution of Earth landforms determined by aspects of the geopotential as computed from the global gravity field model EGM 20082013 | Faculty of Science
- The geomorphological evolution and environmental hazards of the Prague area2016 | Faculty of Science
- The Dynamics of Geomorphic Evolution in the Makalu Barun Area of the Nepal Himalaya2020 | Faculty of Science
- Landforms and morphogenetic processes in the locality of Geodetic Observatory Pecný, Ondřejovská vrchovina Highland2017 | Faculty of Science