Geomorphic differences in the salt crust are caused by differences in their hydrologic environments. Five major types of salt crust were recognized on the Salt Flats, but only one type was observed in Pilot Valley. The Pilot Valley salt crust and surrounding playa have been largely unused.Įvaporite minerals on the Salt Flats and the Pilot Valley playa are concentrated in three zones: (1) a carbonate zone composed mainly of authigenic clay-size carbonate minerals, (2) a sulfate zone composed mainly of authigenic gypsum, and (3) a chloride zone composed of crystalline halite (the salt crust). Much of the Bonneville Racetrack has become rougher, and there has also been an increase in the amount of sediment on the south end of the racetrack. In recent years, there has been an apparent conflict between these two major uses of the area as the salt crust has diminished in both thickness and extent. The salt crust on the Salt Flats has been used for many years for automobile racing, and brines from shallow lacustrine deposits have been used for the production of potash. Both areas lack any noticeable surface relief (in 1976, 1.3 feet on the Bonneville salt crust and 0.3 foot on the Pilot Valley salt crust). The Bonneville salt crust covered about 40 square miles in the fall of 1976, and the salt crust in Pilot Valley covered 7 square miles. The areas are separate, though similar, hydrologic basins, and both contain a salt crust. The Bonneville Salt Flats and Pilot Valley are in the western part of the Great Salt Lake Desert in northwest Utah.
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