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.
|Last updated||July 20, 2016|
|Created||July 20, 2016|
|License||Creative Commons Attribution 4.0|
|created||over 4 years ago|
|resource group id||a53f736f-88f9-4c25-a4cb-45770f784cd5|