<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>G. D. Casey</dc:contributor>
  <dc:contributor>R.A. Mondazzi</dc:contributor>
  <dc:contributor>T.W. Frick</dc:contributor>
  <dc:creator>J. R. Stone</dc:creator>
  <dc:date>1997</dc:date>
  <dc:description>Contamination of ground water by volatile organic compounds and inorganic constituents has been identified at a number of industrial  sites in the Town of Wolcott, Connecticut. Contamination is also present  at a municipal landfill in the City of Waterbury that is upgradient from  the industrial sites in the local ground-water-flow system. The study area, which lies in the Western Highlands of Connecticut,  is in the Mad River Valley, a tributary to the Naugatuck River. Geohydrologic units (aquifer materials) include unconsolidated glacial  sediments (surficial materials) and fractured crystalline (metamorphic)  bedrock. Surficial materials include glacial till, coarse-grained andfine-grained glacial stratified deposits, and postglacial floodplain  alluvium and swamp deposits. The ground-water-flow system in the surficial aquifer is complex because the hydraulic properties of the  surficial materials are highly variable. In the bedrock aquifer, ground  water moves exclusively through fractures. Hydrologic characteristics of  the crystalline bedrock-degree of confinement, hydraulic conductivity,  storativity, and porosity-are poorly defined in the study area. Further  study is needed to adequately assess ground-water flow and contaminant migration under current or past hydrologic conditions.  All known water-supply wells in the study area obtain water from the  bedrock aquifer. Twenty households in a hillside residential area on  Tosun Road currently obtain drinking water from private wells tapping  the bedrock aquifer. The extent of contamination in the bedrock aquifer  and the potential for future contamination from known sources of  contamination in the surficial aquifer is of concern to regulatory  agencies.  Previous investigations have identified ground-water contamination by  volatile organic compounds at the Nutmeg Valley Road site area. Contamination has been associated with on-site disposal of heavy metals,  chlorinated and non-chlorinated volatile organic compounds, and cyanide.  Concentrations of volatile organic compounds detected in water samples  collected from bedrock wells during 1981-95 at the Nutmeg Valley Road  site area show a general downward trend through time. Water samples  collected from wells completed in surficial materials were not collected  systematically, and a trend in concentration cannot be identified.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr97219</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey ;&#13;
Information Services [distributor],</dc:publisher>
  <dc:title>Preliminary hydrogeologic assessment of a ground-water contamination area in Wolcott, Connecticut</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>