The spring itself and the geology of the Ozark karst
Bennett Spring emerges from a horizontal cave opening at the base of a 30-foot dolomite bluff and produces a daily average flow of roughly 100 million gallons — making it the seventh-largest spring in Missouri and one of the larger karst springs in the central United States. The water that emerges at Bennett Spring is geologically old — typically estimated at several years to several decades of subsurface residence time between rainfall infiltration in the surrounding Ozark watershed and emergence at the spring. The spring's flow varies modestly across the year depending on regional rainfall and seasonal recharge, but the cold-water temperature is essentially constant at 57°F year-round.
The Ozark Plateau on which Lebanon and Bennett Spring sit is one of the largest karst landscapes in North America — a region underlain by water-soluble carbonate bedrock (primarily dolomite and limestone in the Bennett Spring area) that has been dissolved over millions of years by acidic groundwater. The result is a landscape of caves, sinkholes, losing streams (creeks that disappear underground), springs (where the underground water re-emerges), and complex aquifer systems. Bennett Spring is one of the more accessible and visually dramatic surface expressions of this underground hydrology and serves as a natural classroom for understanding the broader Ozark karst.
The nature center near the park entrance includes substantial interpretive exhibits on Ozark karst geology, the specific Bennett Spring watershed, the local cave system, and the biological communities the cold-water spring supports. The exhibits are reasonably well-designed for both casual visitors and more serious natural-science interest, and the center serves as a useful orientation point for a park visit.