WWRC 90-31
Discrimination Between Flow-Through and Pulse-Through Components of an Alpine Carbonate Aquifer, Salt River Range, Wyoming
Abstract
Water chemistry and temperature fluctuations in the discharge of Periodic Spring
indicate the existence of a karstic conduit system in the Madison Limestone that is not
apparent from field observations in the Salt River Range. Contamination in the
recharge area of Periodic Spring would pose both immediate and long term problems for
the Afton, Wyoming water supply.
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