From the glaciers of the Dolomites and the Alps, it makes a long journey underground and descends to a depth of hundreds of meters. It crosses layers of limestone rocks and gets enriched with precious mineral salts, especially calcium and magnesium.
The water then goes up, traveling through the deep layers of the subsoil. Rocks and sands filter it naturally up to the spring-well. A journey of hundreds of kilometers and hundreds of years.
