Borjomi water rises to the surface of the Earth from the depths of 8-10 km, with the help of pressure of natural gas and carbon dioxide. In comparison with many other mineral watert, it does not have time to cool under the land and comes to the surface in the form of a warm (38-41 ° С), which «from way to way” is enriched with 60 different mineral composition of the Caucasus Mountains.

The survey results show that in forming Borjomi mineral water the in-depth mineralization, fresh and modern low-mineralized waters participate.
The study held in the 1990s showed that the “Borjomi”, is dramatically different from other mineral waters with hydrogen and isotope ratio.