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Hydrologic reconnaissance to identify areas of emergent groundwater, Mineral Creek, near Silverton, Colorado, June 2020

Dates

Publication Date
Start Date
2020-06-25
End Date
2020-06-27

Citation

Hoogenboom, B.E., and Runkel, R.L., 2020, Hydrologic reconnaissance to identify areas of emergent groundwater, Mineral Creek, near Silverton, Colorado, June 2020: U.S. Geological Survey data release, https://doi.org/10.5066/P9MJLI0X.

Summary

Hydrologic reconnaissance of Mineral Creek near Silverton, Colo., was conducted from June 25-27, 2020. Both banks of Mineral Creek and the adjacent hillsides were walked, starting near the ghost town of Chattanooga and proceeding downstream to the confluence of Mineral Creek with the Middle Fork of Mineral Creek. The purpose of this reconnaissance was to identify areas of emergent groundwater on the right (EGR) and left (EGL) banks, a task that was accomplished by following observed surface flows (seeps and springs) upgradient to the point at which they emanated from the subsurface. Coordinates, using a handheld global positioning system (GPS) device, and photographs were obtained at these locations of emergent groundwater. Water [...]

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Mineral_Creek_2020_Recon_Photos.zip 227.66 MB application/zip
Mineral_Creek_2020_Recon.csv 24.72 KB text/csv
Mineral_Creek_2020_Recon.kmz 224.38 MB application/vnd.google-earth.kmz
Mineral_Creek_2020_Recon_DataDictionary.csv 1.78 KB text/csv
IMG_5785.JPG
“Bear Mountain in the background of Mineral Creek near Silverton, Colo.”
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Shapefile: Mineral_Creek_2020_Recon.zip
Mineral_Creek_2020_Recon.cpg 5 Bytes
Mineral_Creek_2020_Recon.dbf 70.18 KB
Mineral_Creek_2020_Recon.prj 167 Bytes
Mineral_Creek_2020_Recon.sbn 1.53 KB
Mineral_Creek_2020_Recon.sbx 188 Bytes
Mineral_Creek_2020_Recon.shp 3.95 KB
Mineral_Creek_2020_Recon.shx 1.2 KB

Purpose

This survey was conducted as part a study of the hydrogeologic framework of the San Juan-Silverton caldera complex. The study was designed to help characterize subsurface rock properties important for understanding surface water and groundwater quality issues, and to improve knowledge of shallow to deep faults and vein-structures that were conduits for hydrothermal fluids that formed mineral deposits. The study also has general applications to mineral resource assessments in other areas of the world, and in identifying possible groundwater flow paths and associated geochemistry important in abandoned mine lands cleanup.

Additional Information

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Type Scheme Key
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