tds grid.zip

URL: https://gdr.openei.org/files/718/FORGE_TDSgrid.zip

Groundwater geochemistry data was collected from ~20 wells across the region northeast of Milford. The major ions are Na and Cl, the principal sources of TDS. This model shows a plume of high TDS thermal water emanating from the north end of the Opal Mound Fault and Roosevelt Hot Springs. TDS concentrations decrease to the west of the FORGE site, The high TDS concentrations also indicate that the groundwater beneath the Milford site is not potable.

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Last updated July 20, 2016
Created July 20, 2016
Format application/zip
License Creative Commons Attribution 4.0
createdover 3 years ago
formatZIP
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mimetypeapplication/zip
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resource typesite
revision id49022caa-8af9-457a-b9cd-6c6fb125df83
size43.6 KiB
stateactive