A geology-shaped tradition
American mineral springs cluster in four distinct geological zones: the Ouachita uplift in Arkansas, the Cretaceous limestone belt of Texas, the Adirondack fault system of upstate New York, and the Piedmont-Appalachian fall line across Georgia and the Carolinas. Each zone produces water with a distinctive mineral fingerprint — bicarbonate-rich in Saratoga, chloride-sodium in Mineral Wells, silica-rich in Hot Springs.
Most of these springs were the heart of 19th-century spa towns. Saratoga Springs, Hot Springs Arkansas, Mineral Wells Texas and Warm Springs Georgia all built grand resorts around their waters — many still operate today, and several still bottle their original spring source.
