Science – Society – Technology
From: Effect of an 860-m thick, cold, freshwater aquifer on geothermal potential along the axis of the eastern Snake River Plain, Idaho
Depth (m)
Thermal conductivity (W m−1 K−1)
Number of sample runs
983
1.93 ± 0.00
2
1550
1.59
1
1807
1.60
1854
1.45
1902
1.09 ± 0.01