The Source

3,300 Feet Down. Flowing Since 1923.

Beneath Bland County, Virginia, there is an aquifer that has been moving under its own pressure for longer than anyone alive can remember. The well was first bored in 1923. No pump has ever been installed. The water rises on its own.

It passes through 443-million-year-old Ordovician limestone — rock that formed before trees existed, before almost everything. The limestone is what gives the water its mineral structure: calcium, magnesium, a TDS of 130 mg/L. Not added. Acquired. Over hundreds of millions of years of geological contact.

We bottle it at the source. Glass. Cork. No plastic touches it from aquifer to table. Nothing is added. Nothing is taken away. Nature needed no help.

3,300 ft — DEPTH

443M yrs — LIMESTONE AGE

130 mg/L — TOTAL DISSOLVED SOLIDS