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The eastern part of Saratoga County, N.Y., has undergone considerable population growth and development since 1963, when the completion of Interstate 87 increased accessibility to the Capital District, 30 miles to the south. Since then, nearly all housing developments along the Interstate 87 corridor have obtained their water supply from discontinuGus Pleistocene-age sand and gravel aquifers. This report describes the generalized stratigraphy of Pleistocene and Holocene (recent) sediments, as well as two general types of aquifer (bedrock and unconsolidated), and presents data on 1988-89 ground-water pumpage in eastern Saratoga County. Surficial geology, locations of preglacial buried bedrock channels, and ground-water pumpage by facilities that withdraw at least 10,000 gallons per day are indicated on eight 1:24,000-scale topographic 71t 2-minute quadrangle sheets (Gansevoort, Quaker Springs, Saratoga Springs, Middle Grove, Round Lake, Mechanicville, Niskayuna, and Troy North). In general, water suppliers obtain more water from unconsolidated aquifers than from bedrock aquifers because the unconsolidated aquifers are more productive. The most productive confined aquifers in the area are kame and lacustrine deltaic deposits, and the most productive unconfined aquifers are outwash or alluvial deposits that are hydraulically connected to surface-water bodies. Lacustrine sand forms a thin, but extensive, aquifer best suited for pumping by shallow wells. The water-resource potential of exposed kame and buried-channel deposits north of Saratoga Lake is largely unknown.

Generalized stratigraphy, surficial geology, types of aquifers, and 1988-89 ground-water pumpage in eastern Saratoga County, New York