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Thermae of Ischia: Thermae: Hydrogeological map
20 Settembre 2020
Thermal Establishments: Casamicciola Forio Ischia Lacco Ameno Serrara Fontana Barano
Group D (Sulphate-chloride-alkaline facies)
The water samples examined belong to the sulphate-chloride-alkaline group and their composition is similar to that of seawater. However, they do not derive from the blending of marine and phreatic waters. These waters can be distinguished for their high level of conductibility, which often exceeds 40000 mS/cm. Temperatures vary according to the acquiferous portion considered: in the north-eastern sector of the island, which coincides with the Ischia Graben, the temperatures are relatively low and limited to a relatively restricted interval (from 20 to 40°C); whereas, in the marginal sector of Mount Epomeo, the temperatures are generally higher and do not always decrease as one moves towards the coastline. On the contrary, in some cases they actually exceed 80°C. These waters generally characterise the wells near the coastline, including both superficial wells and the deeper ones that go beyond the water interface of the marine ingression water table. Obviously, the latter reveal higher levels of salinity and chloride.




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