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Keywords = epigene karst system

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16 pages, 6267 KB  
Review
Horst-Controlled Karstification in the Bakony Region (Hungary)
by Márton Veress
Land 2023, 12(3), 682; https://doi.org/10.3390/land12030682 - 14 Mar 2023
Viewed by 2143
Abstract
The karst of the horsts of the Bakony Region belonging to horst types of different development is described. Horsts elevated to the summit position are characterised by the most widespread and diverse karstification (with covered karst, cave-ins and shafts). Cryptopeneplains affect the karstification [...] Read more.
The karst of the horsts of the Bakony Region belonging to horst types of different development is described. Horsts elevated to the summit position are characterised by the most widespread and diverse karstification (with covered karst, cave-ins and shafts). Cryptopeneplains affect the karstification of horsts elevated to the summit position, but karst features also occur in their areas. On threshold surfaces of marginal position, the hypogene branches of regional flow systems influenced the development of spring caves. The karstification of basaltic mountains has been mainly governed by the properties of the basalt caprock (the major features being ponors with blind valleys and caprock dolines). Full article
(This article belongs to the Special Issue Karst Land System and Sustainable Development)
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21 pages, 8871 KB  
Review
Hydrological Characteristics of the Bakony Region (Hungary)
by Márton Veress
Eng 2023, 4(1), 581-601; https://doi.org/10.3390/eng4010035 - 10 Feb 2023
Cited by 2 | Viewed by 2232
Abstract
In this study, the karst systems (karst types) of the Bakony Region are classified and described. The karst features and the groundwater (karstwater) flow, their horst (block) types and the hydrological cycle of horst types were taken into consideration. In the mountains, regional [...] Read more.
In this study, the karst systems (karst types) of the Bakony Region are classified and described. The karst features and the groundwater (karstwater) flow, their horst (block) types and the hydrological cycle of horst types were taken into consideration. In the mountains, regional flow with a hypogene branch (hypogene karst system) and epigene karsts systems of local flow were distinguished. Among local epigene systems, epigene karst system, mixed epigene karst system, complex mixed epigene karst system, incomplete epigene karst system and semi-closed epigene karst system were distinguished. Local epigene systems are only temporarily (but not all of them) separated from the regional system that developed below and around them. During their development, separated local systems are more and more becoming the descending branches of regional systems. Full article
(This article belongs to the Section Chemical, Civil and Environmental Engineering)
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