Potential For Ground-Water Recharge In The Coastal Plain Of Central New Castle County, Delaware

Author(s)Petty, S.
Author(s)Miller, W.D.
Author(s)Lanan, B.A.
Date Accessioned2008-06-04T17:44:27Z
Date Available2008-06-04T17:44:27Z
Publication Date1985-05
DescriptionRevised and edited by Kenneth D. Woodruffen_US
AbstractThis map indicates the possibilities for artificial recharge into both the surficial sediments of Quaternary age (exclusive of soils) and the older, immediately underlying sediments. However, the map can also be used to determine where natural recharge might be entering the ground most readily in those areas relatively free from impermeable cover. The surficial materials include marsh and Delaware River sediments of Holocene age and older Pleistocene sediments of the Columbia Formation. The Columbia Formation is composed of poorly sorted sands with some gravels, silts, and occasional clays. The unit is one of the most important ground-water reservoirs in New Castle County.en_US
URLhttp://udspace.udel.edu/handle/19716/3251
Languageen_USen_US
PublisherNewark, DE: Delaware Geological Survey, University of Delawareen_US
Part of SeriesOpen File Reporten_US
Part of Series28, sheet 2en_US
Keywordsartificial rechargeen_US
Keywordsnatural rechargeen_US
KeywordsCentral New Castle County, Delawareen_US
Keywordsground-water reservoiren_US
TitlePotential For Ground-Water Recharge In The Coastal Plain Of Central New Castle County, Delawareen_US
TypeMapen_US
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