The Surface Morphology of Karsts in Hungary

Veress, Márton

doi:10.1007/978-3-030-92960-2_8

Cited by 3 publications

(3 citation statements)

References 26 publications

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“…The plateaus are separated from each other by valleys that are mostly of tectonic origin but also fluvially formed. Almost all of the sinkholes are of solution origin, and only a small number of collapse features and depressions of suffosion origin occur [11,20,71,80,81]. Along the contact zones of karst and non-karst units, stream sinks and springs are found at the input and output sides, respectively [68,81,82].…”

Section: Study Areamentioning

confidence: 99%

“…Almost all of the sinkholes are of solution origin, and only a small number of collapse features and depressions of suffosion origin occur [11,20,71,80,81]. Along the contact zones of karst and non-karst units, stream sinks and springs are found at the input and output sides, respectively [68,81,82]. In the depths, there are caves with diverse speleo-features and genetics; thus, their geodiversity is outstanding, which is the main reason why these caves have been declared a UNESCO World Heritage Site [83].…”

Section: Study Areamentioning

confidence: 99%

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LiDAR-Based Morphometry of Dolines in Aggtelek Karst (Hungary) and Slovak Karst (Slovakia)

Telbisz,

Mari,

Székely

2024

Remote Sensing

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LiDAR-based digital terrain models (DTMs) represent an advance in the investigation of small-scale geomorphological features, including dolines of karst terrains. Important issues in doline morphometry are (i) which statistical distributions best model the size distribution of doline morphometric parameters and (ii) how to characterize the volume of dolines based on high-resolution DTMs. For backward compatibility, how previous datasets obtained predominantly from topographic maps relate to doline data derived from LiDAR is also examined. Our study area includes the karst plateaus of Aggtelek Karst and Slovak Karst national parks, whose caves are part of the UNESCO World Heritage. To characterize the study area, the relationships between doline parameters and topography were studied, as well as their geological characteristics. Our analysis revealed that the LiDAR-based doline density is 25% higher than the value calculated from topographic maps. Furthermore, LiDAR-based doline delineations are slightly larger and less rounded than in the case of topographic maps. The plateaus of the study area are characterized by low (5–10 km−2), moderate (10–30 km−2), and medium (30–35 km−2) doline densities. In terms of topography, the slope trend is decisive since the doline density is negligible in areas where the general slope is steeper than 12°. As for the lithology, 75% of the dolines can be linked to Wetterstein Limestone. The statistical distribution of the doline area can be well modeled by the lognormal distribution. To describe the DTM-based volume of dolines, a new parameter (k) is introduced to characterize their 3D shape: it is equal to the product of the area and the depth divided by the volume. This parameter indicates whether the idealized shape of the doline is closer to a cylinder, a bowl (calotte), a cone, or a funnel shape. The results show that most sinkholes in the study area have a transitional shape between a bowl (calotte) and a cone.

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Section: Study Areamentioning

confidence: 99%

Section: Study Areamentioning

confidence: 99%

LiDAR-Based Morphometry of Dolines in Aggtelek Karst (Hungary) and Slovak Karst (Slovakia)

Telbisz,

Mari,

Székely

2024

Remote Sensing

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“…elevated blocks (for example the Dudar Basin) their roof level is uniformly covered with superficial deposit, those with a larger elevation are covered in bigger patches (for example Mester-Hajag, Tés Plateau), while the most elevated ones are uncovered or only small patches of the cover survived (for example Kőris Block). On the peneplains of the blocks, abrasion peneplains, pediments (Pécsi, 1963(Pécsi, , 1970(Pécsi, , 1980 and epigenetic valleys (these are often gorges or of gorge character) are widespread, while on terrains covered mostly with thin, permeable cover, suffosion dolines occur frequently (Veress, 2022). Under superficial unconsolidated (?)…”

Section: The Bakony Region and Research Areasmentioning

confidence: 99%

The vertical electrical sounding (VES) of the epikarst: A case study of the covered karst of the Bakony region (Hungary)

Márton,

Deák,

Mitre

2023

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The epikarsts of five covered karst areas in the Bakony region are compared. The comparison is based on the specific resistances of the bedrock resistance averages measured by vertical electrical sounding (VES). The average largest specific resistance differences (per area) and the mean values (per profile) were calculated to investigate the characteristics of the epikarst. The mean values of specific resistance were compared using analysis of variance (ANOVA) to determine whether the specific resistances of the areas showed significant differences. The studied karst areas can be categorised as high or low specific resistance areas, and the ANOVA method could be applied to three areas based on the available data. It can be concluded that the mean values of their specific resistances are significantly different. The mean values and standard deviation of the specific resistances of the different areas were analysed. It is described that the karst receives less water in the case of areas with lower specific resistance, while it receives more water in the case of areas with higher specific resistance. Areas with a high specific resistance are less karstified, while areas with a low specific resistance are more karstified. Low specific resistances and small mean values indicate a higher degree of cavity formation in the epikarst, while the decrease in mean values and standard deviation indicates increasing uniformity of the degree of cavity formation in the epikarst. The different degree of cavity formation is explained by the different karstification rates and the exposure of different time of certain areas.

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Development of Epikarst and Dolines in the Bakony Region (Hungary)

Veress

2024

Advances in Karst Science

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The Surface Morphology of Karsts in Hungary

Cited by 3 publications

References 26 publications

LiDAR-Based Morphometry of Dolines in Aggtelek Karst (Hungary) and Slovak Karst (Slovakia)

LiDAR-Based Morphometry of Dolines in Aggtelek Karst (Hungary) and Slovak Karst (Slovakia)

The vertical electrical sounding (VES) of the epikarst: A case study of the covered karst of the Bakony region (Hungary)

Development of Epikarst and Dolines in the Bakony Region (Hungary)

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