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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