Relation Of Ground Water To Surface Water In Four Small Basins Of The Delaware Coastal Plain

Author(s)Johnston, R.H.
Date Accessioned2008-03-28T15:49:21Z
Date Available2008-03-28T15:49:21Z
Publication Date1976-02
AbstractBeaverdam Branch, the Nanticoke River, Sowbridge Branch, and Stockley Branch drain small basins in the Delaware Coastal Plain that are characterized by similar climate, topography, geology, and land use. Withdrawals of ground water and surface water are very small, there is little urbanization, and other man-made effects, which include minor regulation on Sowbridge Branch and construction of drainage ditches in the Nanticoke basin, probably have had minimal effect on the natural hydrologic regimen. These are virtually natural-flow streams, which, because of similar basin characteristics, have nearly identical rates of evapotranspiration and runoff. During the 10-year period, 1959-68, precipitation averaged 40-42 inches annually, runoff averaged 16-17 inches annually, and evapotranspiration averaged 23-25 inches annually.en_US
SponsorU.S. Geological Surveyen_US
URLhttp://udspace.udel.edu/handle/19716/3141
Languageen_USen_US
PublisherNewark, DE: Delaware Geological Survey, University of Delawareen_US
Part of SeriesReport of Investigationsen_US
Part of Series24en_US
KeywordsBeaverdam Branchen_US
KeywordsNanticoke Riveren_US
KeywordsSowbridge Branchen_US
KeywordsStockley Branchen_US
KeywordsDelaware Coastal Plainen_US
Keywordshydrologic regimenen_US
Keywordstopographyen_US
Keywordsgeologyen_US
Keywordsland useen_US
TitleRelation Of Ground Water To Surface Water In Four Small Basins Of The Delaware Coastal Plainen_US
TypeTechnical Reporten_US
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