McLing et al 2016 Paper on Wellbore and...
URL: https://www.sciencedirect.com/science/article/pii/S0377027316300385
McLing et al, 2016. "Wellbore and Groundwater Temperature Distribution Eastern Snake River Plain, Idaho: Implications for Groundwater Flow and Geothermal Potential." A map of groundwater temperatures from the Eastern Snake River Plain (ESRP) regional aquifer can be used to identify and interpret important features of the aquifer, including aquifer flow direction, aquifer thickness, and potential geothermal anomalies. The ESRP is an area of high heat flow, yet most of this thermal energy fails to reach the surface, due to the heat being swept downgradient by the aquifer to the major spring complexes near Thousand Springs, ID, a distance of 300 km.
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