Hydrogeology And Geochemistry Of The Unconfined Aquifer, West-Central And Southwestern Delaware

Author(s)Denver, J.M.
Date Accessioned2008-03-28T19:32:16Z
Date Available2008-03-28T19:32:16Z
Publication Date1986-06
AbstractThe unconfined aquifer is the major source of water supply in west-central and southwestern Delaware. The aquifer, which is composed of quartz sand, gravel, clay, and silt, ranges in thickness from 20 to 200 feet. The water table ranges from land surface to about 20 feet below land surface. Analyses of water from wells distributed throughout the area were used to study processes controlling the chemical quality of the water in the unconfined aquifer.en_US
SponsorPrepared under the Joint-Funded Program of the Delaware Geological Survey and the United States Geological Surveyen_US
URLhttp://udspace.udel.edu/handle/19716/3154
Languageen_USen_US
PublisherNewark, DE: Delaware Geological Survey, University of Delawareen_US
Part of SeriesReport of Investigationsen_US
Part of Series41en_US
KeywordsWest-Central Delawareen_US
KeywordsSouthwestern Delawareen_US
Keywordsunconfined aquiferen_US
TitleHydrogeology And Geochemistry Of The Unconfined Aquifer, West-Central And Southwestern Delawareen_US
TypeTechnical Reporten_US
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