Advances in Karst Research: Theory, Fieldwork and Applications
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Karst landscapes and karst aquifers are composed of a variety of soluble rocks, such as salt, gypsum, anhydrite, limestone, dolomite and quartzite. They are fascinating areas of exploration, study and research. As karst rocks are abundant on the Earth’s surface, the fast evolution of karst landscapes and the rapid flow of water through karst aquifers present many challenges from a number of different perspectives. This collection of 25 papers deals with different aspects of these challenges, including karst geology, geomorphology and speleogenesis, karst hydrogeology, karst modelling, and karst hazards and management. Together these papers provide a state-of-the-art review of the current challenges and solutions we face in describing karst from a scientific perspective, while at the same time providing useful data and information for managing karst territories to land planners, developers, and managers of show caves, natural parks and reserves in karst terrains.
Relations between surface and underground karst forms inferred from terrestrial laser scanning
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Published:January 01, 2018
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CiteCitation
Aleksandar S. Petrović, Jelena Ćalić, Aleksandra Spalević, Marko Pantić, 2018. "Relations between surface and underground karst forms inferred from terrestrial laser scanning", Advances in Karst Research: Theory, Fieldwork and Applications, M. Parise, F. Gabrovsek, G. Kaufmann, N. Ravbar
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Abstract
This paper details methods that contribute towards solving the problem of the spatial relations between surface and underground karst morphology – relationships that are often unclear. The karst landforms studied in this context are karst valleys, through-caves and natural bridges. Two study sites are situated in the Carpatho-Balkan Mountains of eastern Serbia: the dry valley of the Radovanska Reka River on Mt Kučaj (together with the Pećura through-cave) and the Zamna Cave in the wider area of the Danube Gorge. The caves and the closest adjoining parts of the valleys were measured in detail using the terrestrial laser scanning method. The data obtained showed that some previous measurements at these locations, performed with classical traditional instruments, are insufficiently accurate and may lead to wrong conclusions.
- Balkan Mountains
- Carpathians
- caves
- Danube Valley
- data acquisition
- data processing
- Europe
- geomorphology
- gorges
- instruments
- karst
- landforms
- laser methods
- mapping
- measurement
- natural bridges
- relief
- Serbia
- solution features
- Southern Europe
- valleys
- terrestrial laser scanning methods
- Danube Gorge
- Radovanska Reka River
- Pecura Cave
- Mount Kucaj
- Zamna Cave
- Zamna River