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

Author(s)Petty, S.
Author(s)Miller, W.D.
Author(s)Lanan, B.A.
Date Accessioned2008-06-04T17:45:52Z
Date Available2008-06-04T17:45:52Z
Publication Date1983-12
DescriptionRevised and Edited by Kenneth D. Woodruffen_US
AbstractThis map was constructed primarily to indicate the possibilities for artificial recharge into both the surficial sediments of Quaternary age (exclusive of soils) and the older, immediately underlying sediments. However it 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 sediments include micaceous sands and gravels in the vicinity of the Fall Line derived from underlying crystalline rocks, Holocene marsh deposits, Delaware River sediments, and the Columbia Formation of Pleistocene age. 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/19716/3252
Languageen_USen_US
PublisherNewark, DE: Delaware Geological Survey, University of Delawareen_US
Part of SeriesOpen File Reporten_US
Part of Series28, sheet 1en_US
Keywordsground-water reservoirs in New Castle County, Delawareen_US
Keywordssurficial sedimentsen_US
Keywordsartificial rechargeen_US
Keywordsnatural rechargeen_US
TitlePotential For Ground-Water Recharge In The Coastal Plain Of Northern New Castle County, Delawareen_US
TypeMapen_US
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