CHALLENGES OF MANAGING THE HOT CREEK THERMAL AREA, INYO NATIONAL FOREST, CALIFORNIA
The thermal springs range from small seeps to fountaining springs and azure blue pools 10m across, some at ambient boiling temperature (93oC). The locations and discharge rates change when spring vents become sealed by mineral deposition and new springs emerge, sometimes suddenly, when the mineral seals are fractured from ground shaking during local earthquakes.
In May 2006, three subaqueous springs in and near the most popular swimming areas suddenly began fountaining, sending hot sediment laden water spouts to 2 m above the stream surface. The fountaining is randomly cyclical with a period of several minutes between eruptions. These characteristics led the Forest Service to temporarily close the area to swimming. The cause of the sudden change in spring behavior is unclear but may relate to increases in temperature in the shallow thermal aquifer supplying the springs.
The Forest Service is currently deciding what is the appropriate level of geologic monitoring for this site and how it can be completed using limited staff and funding. The goal of the Forest Service is to educate the public on the on the natural geologic phenomena, balance the needs and expectations of the different recreational user groups, while protecting there health and safety while visiting the Hot Creek Geologic Site.