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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.

The revision included converting the existing two-dimensional model to a three-dimensional model.

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.

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Determine whether there are significant vertical flow components within the sand and gravel aquifer and (or) whether there are sources of older water, such as bedrock, that discharge into the sand-and-gravel aquifer.

The new data collected in this study will be used to revise the ground-water-flow model of the area previously built by the USGS. Phase I included test drilling and water sampling for age determination.

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