Het water van deze hete bron is ongeveer 36°C. Het water komt binnen via de infiltratie door het dak, veroorzaakt door een breuk in het kalkstenen gesteente. Het water bevat ongeveer 30% zeewater, wat aangeeft dat deze breuk verbonden is met de Ionische Zee. Je kunt ook de geur van waterstofsulfide ruiken. De zwavel en het calcium reageren en creëren gipskristallen.
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Source: Elade53
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