Natural mineral waters are characterized, among other features by a constant mineralization. Each water is different from the rest based on composition, the percentage of minerals found in it. The final composition of natural mineral water depends on many factors, some of them resulting from the water’s place of origination (rock composition, porosity…) others inherent to liquid element itself (such as pH, temperature…)

It is the water’s origin what makes it different, what makes it unique.

It is the mineral residue of the water after undergoing a controlled evaporation process.
Between two waters subject to comparison, that having a higher dry residue is said to be more mineralized. It is important to pay attention to the analysis’ individual parameters in order to find out the minerals comprising such resulting dry residue. There may be two waters with the same dry residue, but it does not necessarily mean they are equal regarding mineral composition.