Our trace minerals come from a rare deposit of bentonitic clay, deep in the southeastern United States — a site that remains untouched, quiet, and naturally rich in the Earth’s original mineral composition.
This deposit is formed from two distinct geological layers.
The upper layer carries terrestrial organic matter — shaped by forests, plant life, and time.
The lower layer dates back over 33.9 million years, when this land was submerged beneath ancient ocean waters — leaving behind a foundation of marine minerals and deep-earth elements.
Together, these layers create a uniquely balanced mineral matrix — combining freshwater and oceanic origins into a source that is both complex and naturally harmonious.
We extract from this deposit using purified water only — never solvents, acids, or synthetic chemicals — preserving the integrity of the material exactly as it exists in nature.
This isn’t just a mine.
It’s a convergence of time, environment, and natural process.
Every drop carries that origin — shaped slowly, sourced carefully, and handled with respect.