The geothermal reservoir at Raft River, Idaho, was penetrated with a third deep well in the spring of 1976. The information deduced from this well and the subsequent testing of all three wells is presented in this report. This supplements the paper presented at the 1975 Reservoir Engineering conference ( l ), which discussed in detail the experiences with the first two wells (5000 ft and 6500 ft deep, respectively, 4000 f t apart). Figure 1 shows the location of these wells, and the pipeline between them.

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