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Problem - The Village of Pulaski in Oswego County, N.Y., obtains its water supply from groundwater that drains under gravity from an unconfined aquifer into three shallow dug wells. The well field is in an area where groundwater discharges to springs along the west edge of the Tug Hill Aquifer, which is comprised of beach and kame deposits of sand and gravel. A numerical groundwater model was constructed previously to simulate groundwater conditions in part of the Tug Hill Aquifer near the Pulaski well field. The modeling work was part of a wellhead protection study to develop a plan to protect the groundwater resources of the Village of Pulaski's public water-supply system. In addition, the USGS, in cooperation...
Categories: Data,
Project;
Types: Downloadable,
Map Service,
OGC WFS Layer,
OGC WMS Layer,
Shapefile;
Tags: Aquifer Mapping,
Aquifer Mapping,
Aquifer Mapping,
Completed,
Cooperative Water Program, All tags...
GW or SW,
GW or SW,
GW or SW,
Groundwater Monitoring,
Groundwater Monitoring,
Groundwater Monitoring,
Groundwater and Streamflow Information,
Groundwater and Streamflow Information,
Groundwater-Flow Modeling,
Groundwater-Flow Modeling,
Groundwater-Flow Modeling,
Hydrogeologic Characterization,
Hydrogeologic Characterization,
Hydrogeologic Characterization,
Oswego County,
Tug Hill,
USGS New York Water Science Center,
WSC,
Water Use and Availability Science,
Water Use and Availability Science, Fewer tags
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