The geology: how an artesian spring ended up in the desert
The Blue Hole is part of an interconnected system of seven artesian springs and sinkholes in the Santa Rosa area, generally referred to as the Santa Rosa Sinks. The system is fed by an underground aquifer that flows through Permian-era limestone and gypsum bedrock beneath the surrounding desert. Water enters the aquifer from precipitation and runoff hundreds of miles away in the higher elevations of the Sangre de Cristo Mountains to the north, percolates through the porous rock over what geologists estimate is years to decades of underground travel time, and eventually emerges at the springs around Santa Rosa.
The Blue Hole specifically is the deepest and most visible of the Santa Rosa sinks — a roughly 81-foot vertical shaft created by the collapse of a limestone cavern roof, with the resulting void filling with artesian spring water. The continuous water flow of roughly 3,000 gallons per minute means the entire volume of the pool is replaced approximately every six hours, which keeps the water exceptionally clean, the temperature remarkably stable, and the visibility consistently high. There is no algae growth on the rocks, no warming of the surface water in summer or freezing in winter, and minimal sediment because the constant flow flushes out any settling particles.
The bell-shaped underwater profile — narrow at the rim, wider below — is the natural result of the cave-collapse geology. The original underground cavern was substantially wider than the modern opening, and as the cavern roof collapsed over thousands of years, the surface opening was constrained by the surrounding rock while the deeper void retained its original volume. Modern scuba divers descending into the Blue Hole describe the experience as initially feeling like a narrow vertical tube, then opening into a substantially larger underwater chamber at depth.