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Granite Mountain Hot Springs Temp. Flow (LPM) TDS SiO2 geothermometer 49oC / 120oF 1630 260 121.7 oC 117.5 oC Giggenbach geothermometer 100.7 oC 95.7 oC Granite Mountain hot springs is located approximately 40 miles south of Buckland and 60 miles south of Deering. The springs issue from the contact between the anomalously radioactive Granite Mountain pluton and the Cretaceous age volcanic rocks. The Granite Mountain pluton is uranium-enriched, however not enough to be commercial (Gault and others, 1951). The springs are located on Spring Creek, a tributary of Sweepstakes Creek. The temperature of these hot springs is significantly below the temperature of the fluids utilized for power generation at Chena Hot Springs (~80 oC) However, if the geothermometer predictions are correct and there is hotter fluid at depth, these springs could be suitable for development. The flow rate is fairly high relative to other CAHSB hot springs, meaning that less pumping may be required for production. Hawk Hot Springs Temp. Flow (LPM) TDS SiO2 geothermometer Giggenbach geothermometer 43oC / 109oF 400 - - - Hawk hot springs is located approximately 50 miles south of the Kobuk- Shungnak area, 60 miles south of Ambler, and 80 miles east of Buckland in the Purcell Mountains. The springs are located on the Hawk River, near the faulted contact of a Cretaceous pluton and older volcanic rocks (Gassaway and Abramson, 1978). The pluton, called the “Wheeler creek pluton” contains anomalous uranium concentrations (Miller and Johnson, 1978) and is highly fractured and faulted. The temperature of these hot springs is significantly below the temperature of the fluids utilized for power generation at Chena Hot Springs (~80 oC), and there are no geothermometer predictions of hotter fluid at depth. Moreover, the flow rate is fairly low relative to other CAHSB hot springs, meaning that significant pumping may be required for production. Hence, based on resource factors alone, these springs should not be top priority for development. South Hot Springs Temp. Flow (LPM) TDS SiO2 geothermometer Giggenbach geothermometer 67oC / 153oF 1350 114.5 92.2 South hot springs is located approximately 50 miles south of the Kobuk- Shungnak area. Like Hawk and Division hot springs, the South hot springs issue from the Wheeler Creek pluton (see description of Wheeler Creek pluton above). They are located very near to the contact between the pluton and older volcanic rocks. No fault has been identified in the area, but the springs are situated on a prominent lineament in the landscape (Gassaway and Abramson, 1978). The temperature of these hot springs is significantly below the temperature of the fluids utilized for power generation at Chena Hot Springs (~80 oC). However, if the geothermometer predictions are correct and there is hotter fluid at depth, these springs would be suitable for development. The flow rate is 5PDF Image | NANA Geothermal Assessment Project (GAP) Results
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