A preserved spring
Ventadour is born from the coolness of a spring, shaped by the authenticity of a volcanic terroir, and carried by an elegant, timeless purity.

The character
of young volcanoes

The volcanoes of Souilhol, Thueyts, and Montpezat, among the youngest in Ardèche, shaped thousands of years ago a unique volcanic landscape of lava flows and deep, fissured basaltic rocks. These rocks allow water to circulate slowly at depth, reaching balance and mineralizing over time.
It is through a long underground journey that Ventadour takes form. At great depth, it balances, mineralizes, and refines over time in contact with rock. Through a major fracture, Ventadour rises to the surface, naturally charged with carbon dioxide. This singular, nearly untouched geology gives Ventadour its freshness and purity.
A naturally
sparkling water
Buried deep within the Ardèche massif, the Ventadour spring emerges spontaneously sparkling. Its effervescence comes from a rare phenomenon that is clearly documented. Deep‑origin carbon dioxide infuses the water during its slow underground journey. This journey yields a natural sparkle, balanced minerality, and a distinctive taste.



The Sources
du Pestrin
The Pestrin site today hosts several springs. Though born from the same terroir, each has a distinctive signature.
Chantemerle
Julie
Saint-Henri, Saint-Michel & Saint-Charles
Source du Bois
Our spring today.
Naturally sparkling, it leads the Pestrin revival in both still and sparkling expressions.
Previously exploited, this spring produced a delicate still water after degassing. Its name remains tied to the memory of the place and may one day return to enchant tables.
Referenced for a long time, accessible through a vaulted cavity. It has inspired many stories and legends.
Three emerging waters on the right bank of the Fontaulière, witnesses to the valley’s underground richness.
A discreet spring nestled not far from the production site.
Understanding
the different waters
In France, three families of bottled waters are sold. They do not all offer the same qualities.
Basalt flow
CO₂ pathway: 40–50 years
Crystalline massif fractured by earthquakes preceding volcanic eruptions.