Limestone massifs with a high density of dolines form important karst aquifers in most of the Alps, often with groundwater circulating through deep karst conduits and water coming out of closely spaced springs with flow rates of over some cubic meters per second. Although several hydrogeological studies and tracing experiments were carried out in many of these carbonate mountains in the past, the hydrogeology of most of these karst aquifers is still poorly known. Geological, hydrodynamic and hydrochemical investigations have been carried out in one of the most representative of these areas (Cansiglio-Monte Cavallo, NE Italy) since spring 2015, in order to enhance the knowledge on this important type of aquifer system. Additionally, a cave-t...
An important karst aquifer lies below the Cansiglio-Cavallo plateau, a limestone massif located on t...
An important karst aquifer lies below the Cansiglio-Cavallo plateau, a limestone massif located on t...
An important karst aquifer lies below the Cansiglio-Cavallo plateau, a limestone massif located on t...
none12siLimestone massifs with a high density of dolines form important karst aquifers in most of th...
Limestone massifs with a high density of dolines form important karst aquifers in most of the Alps, ...
Limestone massifs with a high density of dolines form important karst aquifers in most of the Alps, ...
Limestone massifs with a high density of dolines form important karst aquifers in most of the Alps, ...
Limestone massifs with a high density of dolines form important karst aquifers in most of the Alps, ...
The Cansiglio-Cavallo plateau is a limestone massif shared between the Italian regions of Veneto and...
The results of a series of continuous characterizations of physical parameters (flow, temperature, w...
Temperature variations in groundwater discharge from the Giordano karst system (northern Apennines) ...
Temperature variations in groundwater discharge from the Giordano karst system (northern Apennines) ...
Temperature variations in groundwater discharge from the Giordano karst system (northern Apennines) ...
Temperature variations in groundwater discharge from the Giordano karst system (northern Apennines) ...
Temperature variations in groundwater discharge from the Giordano karst system (northern Apennines) ...
An important karst aquifer lies below the Cansiglio-Cavallo plateau, a limestone massif located on t...
An important karst aquifer lies below the Cansiglio-Cavallo plateau, a limestone massif located on t...
An important karst aquifer lies below the Cansiglio-Cavallo plateau, a limestone massif located on t...
none12siLimestone massifs with a high density of dolines form important karst aquifers in most of th...
Limestone massifs with a high density of dolines form important karst aquifers in most of the Alps, ...
Limestone massifs with a high density of dolines form important karst aquifers in most of the Alps, ...
Limestone massifs with a high density of dolines form important karst aquifers in most of the Alps, ...
Limestone massifs with a high density of dolines form important karst aquifers in most of the Alps, ...
The Cansiglio-Cavallo plateau is a limestone massif shared between the Italian regions of Veneto and...
The results of a series of continuous characterizations of physical parameters (flow, temperature, w...
Temperature variations in groundwater discharge from the Giordano karst system (northern Apennines) ...
Temperature variations in groundwater discharge from the Giordano karst system (northern Apennines) ...
Temperature variations in groundwater discharge from the Giordano karst system (northern Apennines) ...
Temperature variations in groundwater discharge from the Giordano karst system (northern Apennines) ...
Temperature variations in groundwater discharge from the Giordano karst system (northern Apennines) ...
An important karst aquifer lies below the Cansiglio-Cavallo plateau, a limestone massif located on t...
An important karst aquifer lies below the Cansiglio-Cavallo plateau, a limestone massif located on t...
An important karst aquifer lies below the Cansiglio-Cavallo plateau, a limestone massif located on t...