Hydrological aspects of superficial and underground karst, and water circulation problems in increasing-permeability ground. After showing the importance of rock permeability and solubility and defining ground with an increasing permeability rate, the Author states a limiting principle for the generalisation of conclusions drawn from regional survey data. He then examines the most interesting problems related to the circulation of water in increasing-permeability ground and shows the advisability of carrying out systematic surveys of certain zones. Referring to the karst formations in Venezia Giulia, he comments on the results of his own surveys and research on the distribution, number, and mean depths of numerous cavities and the total ha...
An important karst aquifer lies below the Cansiglio-Cavallo plateau, a limestone massif located on t...
The Cansiglio-Cavallo plateau is a limestone massif shared between the Italian regions of Veneto and...
L'avant-pays de Chartreuse est une zone de transition entre les chaînes subalpines (massif de la Gra...
Identifiant notice SUDOC : http://www.sudoc.fr/103147098IdRef : 055790224Worldcat.org : 3A493701973T...
The creation of large reservoirs in the poljes of the Dinaric Karst has given occasion for an import...
The Cansiglio-Cavallo plateau is a limestone massif shared between the Italian regions of Veneto and...
Quantitative distribution of the superficial and underground karstic phenomena after lithology on th...
National audienceHydrogeology and water balance in karst terrain Jacques Mudry Chrono-Environnement,...
In the hydrogeological sense the karst aquifer of Classical Karst / Kras is a uniform unit, but poli...
Karst is characterized particularly by special landforms and sub surface drainage. The various acti...
Karstification is a dissolving process which enlarges some channels, clefts and fractures and eventu...
Underground water movements in the artesian basin of the Apulian Plateau (Tavoliere). Some new aspe...
Sinkholes are one of the most hazardous phenomena due to their occurrence and unpredictability. In ...
Geological structure of artesian karsts. In an artesian karst, the water flow, on its way to the out...
Conditions of underground water circulation in the gypsum karsts of the french inner Alps. The Trias...
An important karst aquifer lies below the Cansiglio-Cavallo plateau, a limestone massif located on t...
The Cansiglio-Cavallo plateau is a limestone massif shared between the Italian regions of Veneto and...
L'avant-pays de Chartreuse est une zone de transition entre les chaînes subalpines (massif de la Gra...
Identifiant notice SUDOC : http://www.sudoc.fr/103147098IdRef : 055790224Worldcat.org : 3A493701973T...
The creation of large reservoirs in the poljes of the Dinaric Karst has given occasion for an import...
The Cansiglio-Cavallo plateau is a limestone massif shared between the Italian regions of Veneto and...
Quantitative distribution of the superficial and underground karstic phenomena after lithology on th...
National audienceHydrogeology and water balance in karst terrain Jacques Mudry Chrono-Environnement,...
In the hydrogeological sense the karst aquifer of Classical Karst / Kras is a uniform unit, but poli...
Karst is characterized particularly by special landforms and sub surface drainage. The various acti...
Karstification is a dissolving process which enlarges some channels, clefts and fractures and eventu...
Underground water movements in the artesian basin of the Apulian Plateau (Tavoliere). Some new aspe...
Sinkholes are one of the most hazardous phenomena due to their occurrence and unpredictability. In ...
Geological structure of artesian karsts. In an artesian karst, the water flow, on its way to the out...
Conditions of underground water circulation in the gypsum karsts of the french inner Alps. The Trias...
An important karst aquifer lies below the Cansiglio-Cavallo plateau, a limestone massif located on t...
The Cansiglio-Cavallo plateau is a limestone massif shared between the Italian regions of Veneto and...
L'avant-pays de Chartreuse est une zone de transition entre les chaînes subalpines (massif de la Gra...