Results 171 to 180 of about 1,039 (190)

Dinaric Karst

2012
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HETEROGENEITY OF HYDROLOGIC AND HYDROGEOLOGIC PARAMETERS IN KARST: EXAMPLE FROM DINARIC KARST

2000
The paper deals with the heterogeneity of hydrologic and hydrogeologic parameters in karst vadose zone. The karst vadose zone (water unsaturated zone, aerated zone) is generally very deep, ranging from tens to hundreds of meters. It is area of continuous and rapid groundwater level oscillations, with water circulation primarily governed by the dynamics
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Speleologenesis of Dinaric karst area in Croatia

2014
Introduction in speleogenesis of Dinaric Karst in Croatia with numerous examples.
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GEOLOGICAL EVOLUTION OF DINARIC KARST REGION

2010
Dinaric region is a geographical term that comprises NW part of the Balkan peninsula, while Dinaric karst (“Classical karst”) cover its SW part (approx. 800 km long and 200 km wide area). Geologically or tectonically, Dinaric karst comprises mostly External Dinarides along with NE part of the Adriatic foreland, and is partly submerged during Holocene ...
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Interpretation of groundwater level monitoring results in karst aquifers: examples from the Dinaric karst

Hydrological Processes, 2000
Ognjen Bonacci, Tanja Roje-Bonacci
exaly  

Sustainability of the karst environment - Dinaric Karst and Other Karst Regions ABSTRACT BOOK

2009
The objective of the book is to give a theorethical and practical contribution to the sustainable development in kars regions, with a specific emphasis on the experiences achieved in the Dinaric karst region.
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Water losses from the Ričice reservoir built in the Dinaric karst

Engineering Geology, 2008
Ognjen Bonacci, Tanja Roje-Bonacci
exaly  

Sustainability of the karst environment-Dinaric karst and other karst region : abstract book

2009
Karst represents a specific area of surface terrain and surface-subterranean hydrological networks. These networks are created by the circulation of water and its aggresive physical and chemical activity in the small karst fissures, cracks, bedding planes and in the large karst conduits that form in the layers of soluble rocs, such as limestone ...
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Evolution of a karst polje influenced by glaciation: The Gomance piedmont polje (northern Dinaric Alps)

Geomorphology, 2016
Manja Zebre, Uros Stepisnik, Renato R Colucci   +2 more
exaly  

Understanding environmental problems in Dinaric karst:

2003
Na glavnih območjih dinarskega krasa, na Krasu, jadranskih otokih in nizkih ravnikih ob dalmatinski obali prevladujeta tipično sredozemska raba tal, ki povzroča tudi spreminjanje površja, npr. krčenje gozda in urejanje kraškega površja za kmetijstvo, gradnja suhih zidov in terasiranih pobočjih ter pridobivanje kmetijskih zemljišč v dnu vrtač, uval in ...
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