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Spring Valley, Newark Basin, Rockland County
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Groundwater in the Newark basin aquifer flows primarily through discrete water-bearing zones parallel to the strike and dip of bedding, whereas flow perpendicular to the strike is restricted, thereby imparting anisotropy to the groundwater flow field. The finite-element model SUTRA was used to represent bedrock structure in the aquifer by spatially varying the orientation of the hydraulic conductivity tensor to reflect variations in the strike and dip of the bedding. Directions of maximum and medium hydraulic conductivity were oriented parallel to the bedding, and the direction of minimum hydraulic conductivity was oriented perpendicular to the bedding. Groundwater flow models were prepared to simulate local flow...
Categories: Data,
Project;
Types: Downloadable,
Map Service,
OGC WFS Layer,
OGC WMS Layer,
Shapefile;
Tags: Completed,
Cooperative Water Program,
GW Model,
GW Model,
GW model, All tags...
Groundwater-Flow Modeling,
Groundwater-Flow Modeling,
Groundwater-Flow Modeling,
New York,
Spring Valley, Newark Basin, Rockland County,
USGS New York Water Science Center,
WSC,
Water Use and Availability Science,
Water Use and Availability Science, Fewer tags
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