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Thermae of Ischia: Thermae: Hydrogeological map
13 Novembre 2019
Thermal Establishments: Casamicciola Forio Ischia Lacco Ameno Serrara Fontana Barano
Group C (transition facies)
The waters ascribable to transition facies represent about 1/3 of the examined samples. Part of these waters are located along a probable blending line between the above-mentioned bicarbonate-alkaline and sulphate-chloride-alkaline waters. Due to the relation between chloride and alkaline ions as well as for other reasons, the same waters may be considered to be an intermediate chemism limit between those in groups B and D. As far as the temperature trend and the conductibility of this group is concerned, a decrease in temperature is observed as one moves closer to the coastline, in the area of the Ischia Graben, in the north-western sector of the island; conductibility (varying from 10000 to 20000 mS/cm) assumes generally higher values to those of bicarbonate-alkaline waters and lower values with respect to those typical of sulphate-chloride-alkaline waters. The waters that can be traced back to these facies were generally sampled from wells in the basic table of the marginal area of the island; in the depressed area of Ischia they were sampled up to a considerable distance from the coastline.




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