Condensation-corrosion speleogenesis above a carbonate-saturated aquifer: Devils Hole Ridge, Nevada

- Thermal aquifer underlying the Devils Hole Ridge is saturated with respect to calcite.
- The saturated state persisted for at least 800,000 years.
- Solutional cavities and a cave were found in the carbonate rock above the water table.
- The cavities are due to condensation corrosion.

The Devils Hole Ridge, a small block of Paleozoic carbonate rocks surrounded by the Amargosa Desert in southern Nevada, is located at the discharge end of the Ash Meadows regional carbonate groundwater flow system. The massif hosts the famous Devils Hole, a near-vertical extensional fracture which intersects slightly thermal groundwater (33.6 °C) and whose walls are coated below the water table by thick mammillary calcite. The latter was deposited continuously over the last ca. 600 kyr, indicating that the water underneath Devils Hole Ridge was supersaturated with respect to calcite during this time span. Rocks, located more than 9 m above the present-day water table, remained in the unsaturated (vadose) zone. Continuous, long-term presence of thermal water and the extensional tectonic setting, creating underground thermal lakes in open fractures, is associated with intense dissolution above the water table. Condensation corrosion is responsible for modifications of the morphology of the subaerial parts of the tectonic caves. We also describe, for the first time, the Devils Hole Prospect Cave, which was created almost entirely by condensation corrosion. Caves and cavities in the Devils Hole Ridge are an interesting example of hypogene speleogenesis, by condensation corrosion, operating above an aquifer which was demonstrably supersaturated with respect to calcite for hundreds of thousands of years.