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Phase II, entailed the revision of the USGS ground-water-flow model of the sand-and gravel-aquifer, which is tapped by the Sandy Creek/Lacona municipal wells. A., 2007, Hydrogeology of two areas of the Tug Hill glacial-drift aquifer, Oswego County, New York: U. Geological Survey Scientific Investigations Report 2007–5169, 42 p, online only.
For two municipal well sites (the Villages of Sandy Creek and Lacona, and the Village of Pulaski) that tap a shallow, unconfined aquifer (typically 20-50 ft thick) there were significant discrepancies between ground-w...
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Objectives - Refine the understanding of the ground-water flow system in a shallow, sand-and-gravel aquifer in Oswego County.
Reconcile differences in recharge ages and ground-water-flow rates estimated by numerical ground-water-flow modeling and geochemical techniques for one of the sites (Sandy Creek-Lacona municipal well) that taps the Tug Hill aquifer.