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Table 1 Thermal conductivity measurements from core

From: Evaluation of the geothermal potential of the western Snake River Plain based on a deep corehole on the Mountain Home AFB near Mountain Home, Idaho

Depth (m) Thermal gradient (°C/km) Depth (m) Conductivity [W/(m K)] Calculated heat flow (mW/m2)
200–600 56 ± 5 169 1.86 ± 0.1 104 ± 16
640–800 81 ± 4 758 1.29 ± 0.1 104 ± 13
1200–1500 73 ± 7 1200 1.35 ± 0.1 99 ± 16
   1794 1.53 ± 0.1