Titlebook: Cave and Karst Systems of Hungary; Márton Veress,Szabolcs Leél-?ssy Book 2022 Springer Nature Switzerland AG 2022 Hungarian karst areas.Ka

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,The Caves of Aggtelek Karst, Szalonna Karst and Rudabánya Mountains,cave system is an excellent example of a fluvially modelled ‘ideal watertable cave’. Several multi-level caves were formed by allogenic sinking streams at the edge of karst plateaus or along traverse valleys. The Baradla–Domica cave system hosts more than 500 animal species and played an important r

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The Caves of the Northeastern Part of the Transdanubian Mountains, water passages in Molnár János Cave. József-hegy Cave, Citadella Crystal Cave and Királylaki Cave are accessible for research projects only. There are fewer, but very interesting, caves in the Triassic limestone of the Pilis Hills. The intensively investigated Ariadne Cave System is now nearly 20?k

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Monitoring and Geochemical Investigations of Caves in Hungary: Implications for Climatological, Hydnstruct past climate and environmental fluctuations. In addition, the equations that best describe the carbonate-water oxygen isotope fractionation and best reflect the temperature dependence of the isotopic composition of precipitations were identified for paleotemperature reconstruction. The inves

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Age, Depositional Environment, and Geochemistry of Freshwater Carbonates (Travertine, Tufa) from Hu oil reservoir rocks. Furthermore, the recent deposits can be used for the calibration of the oxygen- and clumped isotope paleothermometers. The aim of this chapter is to provide a short review of the most important Hungarian travertine and tufa deposits including the achievements of most recent res

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The Vegetation of Karsts in Hungary, and this trend will probably continue in coming decades. The capacity of karstic refugia to buffer against the negative effects of climate oscillations on vegetation is likely to be exceeded if the current management practices will remain unchanged. In this chapter, the phytogeography, community st

Mosaic

https://doi.org/10.1007/978-3-8348-9357-4Hill. The work of Hungarian cave researchers contributed to solving the problems of several special karstic phenomena (e.g. the formation of helictites, the effect of tidal phenomena on the discharge of karst springs). Furthermore, the contribution of Hungarian cave researchers was also important in

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arthroscopy

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https://doi.org/10.1007/978-3-8348-9437-3es, mixing of meteoric and basinal and waters of local, intermediate and regional groundwater flow systems and potential locations of epigene and hypogene speleogenesis can be revealed and explained. The Hungarian karst areas reflect different properties but there are similarities regarding their hy

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,Erweiterter Koh?renzmatrizen-Kalkül,also provided here. During the last centuries, Hungarian karst terrains have undergone significant landscape changes. Based on earlier series of military maps, satellite images and other databases (e.g. CORINE), these landscape changes have been studied by several authors using GIS methodology. More