The Spring

The famous spring rises to the surface at the break between two vertical geological synclines of Oriskany sandstone that form the symmetrical backbone between White Cliff and Bear Ridge.  The estimated depth of the underground aquifer where the spring water is stored is about 1,600 feet.  Rainfall has been recharging this deep reservoir for centuries, taking up to 70 years to complete the water cycle and seep back to the surface.  The last 300 feet the water passes through the sandstone formation, which, because of its porous nature, serves as a natural filter. Our spring water flows at a constant rate of about 60 gallons per minute, 65% of which is needed when inventory and stocking.  Because the water when it reaches the surface maintains 65-degree temperature, it is geologically classified as a warm spring. 

Benefit to the Body

The hydrogeology (the science of the movement of water below the Earth’s surface) of the area produces an alkaline water with a pH of 7.2.  This proper balance allows for Spring water to neutralize the buildup of acid in the body, providing a multitude of health benefits.  Since the human body is over 60% water, having good, clean water is essential to our well-being.  And because of the 300′ filter, it has a sweet clean taste, improving drinkability, which leads to better overall hydration.