Each water has a different composition and depends on the specific hydrogeological conditions and the hydrogeological model of the aquifer in each region.
The uniqueness of the hydrogeological profile of Souroti, the particular stratigraphy and composition of the rocks through which the groundwater resource passes, and the long time it takes to move through the rocks, creates a water of unique composition. The journey starts with the rainwater descends to great depths, passes through the rocks that enrich it with ions and trace elements and, protected from external surface influences and environmental pollutants, gushes out into the Souroti area.
Throughout this journey, it is filtered and cleaned naturally. Through the carbonate rocks (limestones, dolomites) it passes through, it is enriched with valuable minerals such as calcium, magnesium, carbon dioxide CO2 and bicarbonates (HCO3-).
By contact with geothermal fluids at a great depth it is enriched with silica (SiO2) and lithium (Li). It springs from the heart of the earth through geological faults at the SOUROTI water source and is bottled directly.
Both the origin, the circulation pattern up to the water intake point and the specificity of the chemical composition of the water have been analysed and studied by a series of hydrogeological – geophysical studies and the protection zones of the natural resource have been defined, within which all anthropogenic activity is strictly controlled.
The source of water abstraction and the underground reserves are controlled and monitored continuously and systematically, in cooperation with specialist scientists and University Institutions, in order to ensure the rational management of the natural resource, stability and sustainability.