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Tarsoly, Peter
2025-08-05T10:28:09Z
2025-08-05T10:28:09Z
2025
1785-8860hu_HU
http://hdl.handle.net/20.500.14044/31911
This paper provides a quantitative study of the Hungarian non-karstic cave geometries and topologies, to define the relationship between speleogenetic processes and cave patterns. To study the planar and morphological characteristic of non-karstic caves, define similarities and differences between them, order groups we used cave-map based topological and geometrical parameters. The recognized characteristics are in a tight context with the development of cave morphology, and the morphometrical characteristics can be generalized. The topological and geometrical parameters show for a cave or a cave- section the most important cave developing force (among other forces), which can be the base point to place a cave in a speleogenetic-system. This study demonstrates that modelling topological parameters such as connectivity, density of connections and passage density can effectively classify non-karst caves into different morphological categories, revealing that most Hungarian non-karst caves exhibit simple geometry and only 11% of them show complex, networked structurehu_HU
dc.description.abstracthu_HU
dc.formatPDFhu_HU
enhu_HU
Topological Analyses of the Hungarian Non-Karstic Caveshu_HU
Open accesshu_HU
Óbudai Egyetemhu_HU
Budapesthu_HU
Óbudai Egyetemhu_HU
Természettudományok - kémiai tudományokhu_HU
non-karstic caveshu_HU
topologyhu_HU
morphologyhu_HU
cave developing forceshu_HU
Tudományos cikkhu_HU
Acta Polytechnica Hungaricahu_HU
local.tempfieldCollectionsFolyóiratcikkekhu_HU
10.12700/APH.22.8.2025.8.6
Kiadói változathu_HU
16 p.hu_HU
8. sz.hu_HU
22. évf.hu_HU
2025hu_HU
Óbudai Egyetemhu_HU


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