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Geohydrology of the valley-fill aquifer in the Bath area, Lower Cohocton River, Steuben County, New York

Water-Resources Investigations Report 85-4095

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Abstract

The Bath valley-fill aquifer, southern New York, composed of outwash, ice-contact, and ice-disintegration sand and gravel, is highly productive and is in many areas in hydraulic contact with the Cohocton River. Potential well yields range 50 to more than 1,000 gallons per minute. Most of the aquifer is under shallow water-table conditions and vulnerable to surface contamination. Thickness ranges from 20 to 40 feet. Buried aquifers are present locally. The aquifer system underlies an area containing only a few small communities and therefore is not heavily pumped. Geohydrologic data are compiled on six maps at 1:24,000 scale and on a sheet of geologic sections. The maps depict surficial geology, soil-infiltration capacity, potentiometric surface, aquifer thickness, well yields, and land use. This map report set is one in a series of four that depict selected aquifers in Wester New York. It supplements a series that is being done by the U.S. Geological Survey in cooperation with State agencies. The maps are based largely on published reports, data filled in several State agencies, and some additional field data collection. (USGS)

Additional Publication Details

Publication type:
Report
Publication Subtype:
USGS Numbered Series
Title:
Geohydrology of the valley-fill aquifer in the Bath area, Lower Cohocton River, Steuben County, New York
Series title:
Water-Resources Investigations Report
Series number:
85-4095
Edition:
-
Year Published:
1984
Language:
ENGLISH
Description:
6 maps and 1 section on 7 sheets ; 92 x 117 cm. and 104 x 115 cm., folded in envelope 39 x 30 cm.