Hydraulic Characteristics Of The Piney Point Aquifer And Overlying Confining Bed Near Dover, Delaware

Author(s)Leahy, P.P.
Date Accessioned2008-03-28T15:51:40Z
Date Available2008-03-28T15:51:40Z
Publication Date1976-06
AbstractThe hydraulic properties of the Piney Point (Eocene) aquifer and overlying basal silt of the Chesapeake Group (Miocene) were determined by a 23-day aquifer test conducted at the Danner Farm Well Field of the City of Dover, Delaware. During the test, head changes were monitored continuously in the Piney Point aquifer, overlying Cheswold (Miocene) aquifer, and the intervening confining bed.en_US
SponsorU.S. Geological Surveyen_US
URLhttp://udspace.udel.edu/handle/19716/3142
Languageen_USen_US
PublisherNewark, DE: Delaware Geological Survey, University of Delawareen_US
Part of SeriesReport of Investigationsen_US
Part of Series26en_US
KeywordsPiney Point aquiferen_US
KeywordsCheswold aquiferen_US
Keywordsbasal silten_US
KeywordsChesapeake Groupen_US
KeywordsDanner Farm Well Fielden_US
KeywordsCity of Dover, Delawareen_US
Keywordsconfining beden_US
TitleHydraulic Characteristics Of The Piney Point Aquifer And Overlying Confining Bed Near Dover, Delawareen_US
TypeTechnical Reporten_US
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