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shallow groundwater. This is supported by data collected from this study in which higher concentrations of the elements Na, K, Ca, and Si were found (Table 1). Sunbeam Hot Springs issues directly from a fracture network within exposed bedrock above the Salmon River; whereas the Stanley Hot Springs discharge out of unconsolidated alluvial sediments. It also should be noted the predicted temperatures of springs decrease westerly along the Mormon Bend Fault as evidenced by the Elkhorn and Boat Box Hot Springs (Table 2). To further support the idea of non-thermal and thermal water mixing, mixing models using Boron were created. Preliminary work by John Welhan has shown that there is indeed mixing between thermal and non-thermal waters (John Welhan, written communication, 2011). This was obtained through regression analysis of Boron concentrations taken from the literature. Appendix 1 of Task 4 Report contains the values from this analysis. Stanley’s thermal water chemistry is complex, and requires a substantial bit of knowledge regarding the effect of high pH on silica solubility (John Welhan, written communication, 2011). Because the Na-K-Mg-Ca, Na/K and K2/Mg geothermometers are in agreement, it is reasonably safe to take calculated temperatures with significant confidence (John Welhan, written communication, 2011). Local temperature gradients were also produced by temperature logging 6 wells in the Stanley area. The highest gradient observed during this study (Table 3) was that of Well #2 (this study), or Well G-2 of Chapman (1986). It is important to note that most wells with the highest gradient lie north of Stanley and west of the Historical Museum. 5. Geologic and Geophysical Surveys A 2 meter or shallow probe survey consisting of 24 stations was conducted in the Stanley area to try and locate areas of high temperature, possibly caused by upflow of thermal waters along geologic structures (i.e. faults/fractures). An area north of Stanley and west of Highway 75, near the public bathing pool (formerly Stanley Hot Springs) has been identified as an area of high temperatures, ranging from 12.6°C to 15°C. Other areas near Lower Stanley may have geothermal potential but this remains to be confirmed because shallow ground water may have masked any thermal potential in these areas. Three geophysical surveys (gravity, magnetic, and resistivity) were also conducted in the Stanley area to locate local structural features. A gravity profile was established along a transect that crosses both the Stanley Basin and potential geologic structures identified in previous tasks of this project. The gravity data suggests that there are up to 3 faults that are controlling the movement of fluid flow through the Stanley geothermal system. Gravity values range from -213.82 mGals to -211.92 mGals. 6. Proposed Location for Test Well(s) Based on data gathered from this study and data gathered from background literature research, it has been determined that the best location for successful geothermal resource extraction lies near the 4PDF Image | Stanley Geothermal Feasibility Study
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