Abstract:Movement of ground water in the area is impeded locally by faults which act as ground-water barriers. There are indications that a fault probably crosses the reservation in an east-west direction; such a fault may interfere with ground-water pumping. The water-table altitude near the northern boundary of the reservation is estimated to be 120 to 130 feet below land-surface datum; the aquifer thickness in the area is unknown.Pumping-test results for wells near the reservation show specific capacities ranging fr… Show more
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