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This report presents public water-supply data and geohydrologic data along a 50-mile segment of the Connecticut River valley from Windsor to Vernon, Vermont. An inventory of wells indicates that domestic ground-water supplies come primarily from bedrock, whereas public water supplies are derived from discontinuous, glacial sand and gravel deposits. Self-supplied industries generally use surface-water supplies. Data from eight seismic-refraction surveys, and from a seismic-reflection survey along this 50-mile reach of the Connecticut River, were compared with stratigraphic information from 217 drillers' logs. These data indicate that stratified-drift deposits range from 0 to 270 feet and average about 65 feet. Stratigraphic information from drillers' logs and seismic-reflection records show that predominantly fine-grained stratified drift fills the valley and that coarser sand and gravel deposits exist discontinuously within this area.

Summary of public water-supply withdrawals and geohydrologic data for the lower Connecticut River valley from Windsor to Vernon, Vermont