The Remedy selected for a deep aquifer at the Madisonville Creosote Works, which have a potential threat of contamination from a nearby contaminated shallow aquifer is presented. The remedy includes monitoring, in consideration of the low permeability of the clay unit separating the two aquifers and the limited transport potential of the dissolved polycyclic aromatic hydrocarbons. A computer model was used for predication of the potential fate and transport of contaminants to the deep drinking water supply aquifer. The model results show conservative breakthrough of naphthalene from the source creosote in the shallow water bearing zone at about 150 years.