1. The Formation of the Aquifer
In the wider Souroti area, nature has created a unique hydrogeological system over thousands of years. Within this system lies the aquifer from which SOUROTI natural mineral and curative water originate.
2. From Rain and Snow to the Underground
The journey begins with rainwater and melting snow, which gradually infiltrate the ground through pores, fractures and rock formations, slowly making their way to greater depths.
3. An Underground Journey Lasting Decades
This is not a rapid process. The water may reach depths exceeding 500 metres, while its underground residence and circulation within this unique geological environment are estimated to exceed 50 years.
4. Natural Enrichment with Minerals
During its long underground journey, the water comes into contact with different geological formations. Through this entirely natural process, it becomes enriched with bicarbonates and essential minerals, including calcium, magnesium and potassium.
5. Deeper Physicochemical Conditions
At greater depths, the interaction between the water, the geological formations and the area’s geothermal field creates unique physicochemical conditions. There, the water undergoes further natural enrichment with lithium and silica.
6. Natural Filtration and Upward Movement
As it passes through the rock formations, the water undergoes a natural filtration and purification process, without mixing with surface waters such as rivers or lakes. Its final route is guided by the geological structure of the area, particularly the Anthemountas Fault, which extends for more than 30 kilometres.
7. Emerging at the Spring
The natural presence of carbon dioxide in the water contributes to its upward movement, naturally driving it towards the spring. In this way, the water completes a remarkable journey that began as rain and snow, continued underground for decades and finally emerges at the point of abstraction.