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Passive seismic depth to bedrock data collected along headwater stream corridors in the Neversink River watershed, NY, USA

Dates

Publication Date
Start Date
2019-06-24
End Date
2020-11-19

Citation

Briggs, M.A, Woda, J., Williams, J., and Trottier, B., 2020, Passive seismic depth to bedrock data collected along headwater stream corridors in the Neversink River watershed, NY, USA: U.S. Geological Survey data release, https://doi.org/10.5066/P9CFSPH3.

Summary

The Neversink River watershed (above the Neversink Reservoir) has been a focus of U.S. Geological Survey (USGS) research regarding stream geochemistry, acidification, and ecology dynamics for decades. In 2019, the Water Mission Area Next Generation Water Observing Systems Program augmented the existing stream gage network there, including instrumentation to specifically characterize various aspects of groundwater discharge to streams. An important control on the spatiotemporal dynamics of groundwater discharge can be stream valley corridor depth to bedrock, otherwise conceptualized as the thickness of unconsolidated sediments sediments over the contiguous bedrock interface. In June 2019, and November 2020, passive seismic recordings [...]

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Attached Files

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README.txt 2.05 KB
streamside_HVSR.jpg thumbnail 4.84 MB
Raw_Data.zip 34.27 MB
Processed_Data.zip 12.66 MB
Shapefile: XYNeversink_HVSR_Arcmap.zip
XYNeversink_HVSR_Arcmap.dbf 13.89 KB
XYNeversink_HVSR_Arcmap.prj 167 Bytes
XYNeversink_HVSR_Arcmap.shp 1.19 KB
XYNeversink_HVSR_Arcmap.shx 420 Bytes

Purpose

Depth to bedrock along stream corridors can directly influence patterns of streamflow, valley groundwater flow, and groundwater/surface water exchange but is often ill-defined in mountain headwater catchments. These HVSR data were collected to support process-based interpretation of stream temperature and chemical dynamics, and to aid in groundwater flow model development.

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9CFSPH3

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