Problem - The entire Tug Hill glacial aquifer is a 47-mile-long, crescent-shaped mixture of glacial deposits of predominantly sand and gravel on the western side of the Tug Hill Plateau in Jefferson, Oswego, and Oneida Counties in north central New York. The Tug Hill aquifer can be divided into three parts (northern, central, and southern) based on geohydrological setting, depositional history, and type of glacial deposits (fig. 1). In this study, the name “Tug Hill glacial aquifer” refers only to the 29-mi-long northern and central parts of the Tug Hill aquifer. (The southern part was not included in this investigation.) For this study, the division between the northern and central parts of the aquifer was placed...
Categories: Data,
Project;
Types: Downloadable,
Map Service,
OGC WFS Layer,
OGC WMS Layer,
Shapefile;
Tags: Completed,
GW Model,
GW Model,
GW model,
GW or SW, All tags...
GW or SW,
GW or SW,
Groundwater-Quality Monitoring,
Groundwater-Quality Monitoring,
Groundwater-Quality Monitoring,
Hydrogeologic Characterization,
Hydrogeologic Characterization,
Hydrogeologic Characterization,
Hydrologic Networks and Analysis,
Jefferson, Oswego,Oneida Counties,
New York,
USGS New York Water Science Center,
WSC,
Water Quality,
Water Quality,
Water Quality,
Water Quality,
Water Use and Availability Science,
Water Use and Availability Science,
Water quality,
hydrogeology, Fewer tags
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