- Geological Formations and Processes Exploration
- Landslides and related hazards
- Geology and Paleoclimatology Research
- Groundwater flow and contamination studies
- Soil erosion and sediment transport
- Marine and environmental studies
- Soil and Unsaturated Flow
- Soil Geostatistics and Mapping
- Remote Sensing and LiDAR Applications
- Peripheral Nerve Disorders
- Cryospheric studies and observations
- Geological and Geochemical Analysis
- Geological Modeling and Analysis
- Geochemistry and Geologic Mapping
- Land Use and Ecosystem Services
- Remote Sensing in Agriculture
- Liver Disease Diagnosis and Treatment
- Karst Systems and Hydrogeology
- Geological formations and processes
- 3D Surveying and Cultural Heritage
- Pleistocene-Era Hominins and Archaeology
- Hydrology and Watershed Management Studies
- Groundwater and Watershed Analysis
- Tree Root and Stability Studies
- Geology and Environmental Impact Studies
Comenius University Bratislava
2015-2024
University Library in Bratislava
2018-2022
University of Ostrava
2007-2015
Airborne and terrestrial laser scanning close-range photogrammetry are frequently used for very high-resolution mapping of land surface. These techniques require a good strategy to provide full visibility all areas otherwise the resulting data will contain with no (data shadows). Especially, deglaciated rugged alpine terrain abundant large boulders, vertical rock faces polished roche-moutones surfaces complicated by poor accessibility still challenge. In this paper, we present novel...
Abstract The Tatra Mts area, located in the northernmost part of Central Western Carpathians on border between Slovakia and Poland, underwent a complex Alpine tectonic evolution. This study integrates structural, sedimentary, geomorphological data combined with fission track from Variscan granite rocks to discuss Cretaceous Quaternary landscape evolution Mts. presented can be correlated five principal stages (TS), including neotectonics. TS-1 (~95-80 Ma) is related mid-Cretaceous nappe...
By interpretations related to energy, elementary land surface segmentation can be treated as a physical problem. Many pieces of such view found in the literature combined into synthetic comprehensive approach. The has preceded by defining character and size searched units result from segmentation. A high-resolution digital elevation model (DEM) is key input for this task; it should generalized resolution best expressing information about units. Elementary characterized various parts...
Third-order geomorphometric variables (based on third derivatives of the altitudinal field) have been neglected in geomorphometry, but their application to delimitation surface objects will lead increasing significance future. New techniques computation, presented and evaluated here, facilitate use. This paper summarizes recent knowledge concerning definition, computation geomorphologic interpretation these variables. Formulae defining various third-order are unified based physical...
Abstract The history of Quaternary sea-level changes in the Caspian Sea, world’s largest lake, is partly enigmatic, and so geomorphic response its coasts. Late Pleistocene transgressions during Early Khvalynian (ca. 40–25 ka) inundated extensive portions flat, low-lying semi-desert western Kazakhstan. Cliffs cut these highstands form a prominent escarpment tens kilometers to several hundred from present coast Sea. Satellite images, digital terrain analysis, field mapping reveal that...
Late Miocene and Pliocene history of the Danube Basin: inferred from development depositional systems timing sedimentary facies changes The northern Basin (nDB) was closely related to geodynamic evolution Pannonian System. It started with a wide rifting which led subsidence several basin depocenters were gradually filled during Early Pliocene. In continued only in basin's central part, while marginal zone suffered inversion uplifted fill began be eroded. Individual stages are well recorded...
Neogene and Quaternary development of the Turiec Basin landscape in its catchment: a tentative mass balance model The evolution catchment has been reconstructed by methods geological research (structural geology, sedimentology, paleoecology, geochronological data) as well geophysics geomorphology. basin surrounding mountains were subject study during periods tectonic activity, accompanied considerable altitudinal differentiation relief also quiet periods, characterized planation surfaces...