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Table 1 Thermal conductivity measurements from core

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 1
1854 1.45 1
1902 1.09 ± 0.01 2