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From July 2011 to November 2016, the U.S. Geological Survey, in cooperation with the Town of Newfield and the Tompkins County Planning Department, collected horizontal-to-vertical seismic surveys at 58 locations in the West Branch Cayuga Inlet and Fish Kill valleys to help determine thickness of unconsolidated deposits and depth to bedrock. The HVSR technique, commonly referred to as the passive-seismic method, is used to estimate the thickness of unconsolidated sediments and the depth to bedrock (Lane and others, 2008). The passive-seismic method uses a single, broad-band three-component (two horizontal and one vertical) seismometer to record ambient seismic noise. In areas that have a strong acoustic contrast...


    map background search result map search result map Horizontal-to-Vertical Spectral Ratio Soundings and Depth-to-Bedrock Data for Geohydrology and Water Quality of the Stratified-Drift Aquifer in West Branch Cayuga Inlet and Fish Kill Valleys, Town of Newfield, Tompkins County, New York, 2011 - 2016 Aquifer Boundaries in the Enfield Creek Valley Geologic Cross Section Lines in the Enfield Creek Valley Moraines and Ice Margins in the Enfield Creek Valley Discharge and Surface Water Quality Sites in the Enfield Creek Valley Surficial Geology in the Enfield Creek Valley Overburden Thickness in the Enfield Creek Valley Records of Selected Wells in the Enfield Creek Valley Discharge and Surface Water Quality Sites in the Enfield Creek Valley Geologic Cross Section Lines in the Enfield Creek Valley Horizontal-to-Vertical Spectral Ratio Soundings and Depth-to-Bedrock Data for Geohydrology and Water Quality of the Stratified-Drift Aquifer in West Branch Cayuga Inlet and Fish Kill Valleys, Town of Newfield, Tompkins County, New York, 2011 - 2016 Aquifer Boundaries in the Enfield Creek Valley Moraines and Ice Margins in the Enfield Creek Valley Overburden Thickness in the Enfield Creek Valley Records of Selected Wells in the Enfield Creek Valley Surficial Geology in the Enfield Creek Valley