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Problem The Tully Valley, located in southern Onondaga County has been the source of sediment and brackish water discharge to Onondaga Creek, a tributary to the Seneca and Oswego Rivers and eventually Lake Ontario. Information on the origin of the Tully Valley mudboils, their persistence, and the possible extent of their migration within the Tully Valley is needed to mitigate or remediate (1)the discharge of turbid water and fine-grained sediment from the mudboils, (2) land-surface subsidence caused by the removal of sediment from below the land surface, and (3) degradation of Onondaga Creek by turbidity, fine-sediment deposition, and chloride loading. Objectives To define the glacial stratigraphy and hydraulic-head...
Categories: Data,
Project;
Types: Downloadable,
Map Service,
OGC WFS Layer,
OGC WMS Layer,
Shapefile;
Tags: Cooperative Research Units,
Cooperative Water Program,
GW or SW,
GW or SW,
GW or SW, All tags...
Geophysics,
Geophysics,
Groundwater Monitoring,
Groundwater Monitoring,
Groundwater Monitoring,
Groundwater and Streamflow Information,
Groundwater and Streamflow Information,
Hydrogeologic Characterization,
Hydrogeologic Characterization,
Hydrogeologic Characterization,
Landslide Hazards,
New York,
Sediment,
Sediment,
Sediment,
Tully Valley, Southern Onondaga County,
USGS New York Water Science Center,
WSC, Fewer tags
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