Wells For The Observation Of Chloride And Water Levels In Aquifers That Cross The Chesapeake And Delaware Canal

Author(s)Rasmussen, W.C.
Author(s)Groot, J.J.
Author(s)Beamer, N.H.
Date Accessioned2008-03-11T12:46:40Z
Date Available2008-03-11T12:46:40Z
Publication Date1958-08
AbstractThree test wells were drilled near the banks of the Chesapeake and Delaware Canal, in aquifers formed by sand beds in two geologic units, the nonmarine Cretaceous sediments and the Magothy formation, which crop out along the sides and across the bottom of the canal. The canal carries tidal flow from the Delaware River to and from Chesapeake Bay. The purpose of the wells was to determine whether salt water from the canal has entered the water-bearing beds of these formations, and to determine the head of water in them. It was found that the sands contain fresh water, uncontaminated, and that apparently there was discharge of fresh water from the aquifers to the canal under low head, at least from the winter of late 1955 through early autumn 1957.en_US
SponsorU.S. Geological Survey and U.S. Army Corps of Engineersen_US
URLhttp://udspace.udel.edu/handle/19716/3094
Languageen_USen_US
PublisherNewark, DE: Delaware Geological Survey, University of Delawareen_US
Part of SeriesReport of Investigationsen_US
Part of Series3en_US
Keywordschlorideen_US
Keywordswater levelsen_US
Keywordsfresh wateren_US
Keywordsaquiferen_US
KeywordsChesapeake and Delaware Canalen_US
TitleWells For The Observation Of Chloride And Water Levels In Aquifers That Cross The Chesapeake And Delaware Canalen_US
TypeTechnical Reporten_US
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