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NANA Geothermal Assessment Project (GAP) Results

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NANA Geothermal Assessment Project (GAP) Results ( nana-geothermal-assessment-project-gap-results )

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fairly high relative to other CAHSB hot springs, meaning that less pumping may be required for production. Division Hot Springs (also called Shungnak HS??) Temp. 68oC / 154oF 56oC / 133oF Flow (LPM) TDS 820 - 2070 - SiO2 geothermometer - - Giggenbach geothermometer - - Several hot springs comprise the Division hot springs, also called Shungnak hot springs and/or Selawik hot springs? They are approximately 40 miles from the Kobuk- Shungnak area and approximately 60 miles from Ambler. They are located on the north side of the Purcell mountains, inside the Selawik National Wildlife Refuge. The lower springs are slightly cooler than the upper springs, so the source of the thermal water is probably topographically high. Like Hawk and South hot springs, the Division hot springs issue from within the Cretaceous-age, anomalously radioactive Wheeler Creek pluton (Miller and Johnson, 1978; see description of Wheeler Creek pluton above). Division hot springs are some of the hottest springs in the NANA region, but they are still significantly below the necessary temperature of ~80 oC for Chena-type power generation. At this time, there are no geothermometer predictions of hotter fluid at depth – but is due to a lack of data. The flow rate of the upper spring is extremely high relative to other CAHSB hot springs, which would reduce the amount of pumping required for production. Hence, based on resource factors alone, these springs should be prospective for development; however their location inside of a National Wildlife Refuge could complicate development plans. Reed River Hot Springs Temp. Flow (LPM) TDS SiO2 geothermometer Giggenbach geothermometer 57oC / 137oF 160 - - - The Reed river hot springs are located in the rugged terrain of the Brooks Range, approximately 50 miles from Kobuk/Shungnak and 70 miles from Ambler, on the east bank of the Reed River. The surrounding bedrock is granite of the Igikpak pluton, but the spring is just a few miles from the contact between the pluton and the country rock (Pessel, 1975). The hot springs are located in the Gates of the Arctic National Park, and are therefore off-limits for exploration and development.in the foreseeable future. Resource-wise, they are some of the coolest hot springs in the NANA region and have the lowest flow rate all of the springs. Hence, these springs should be low priority for development. Identifying Unmapped Geothermal Prospects in NANA Region Geologic data The southernmost half of the NANA region is more prospective than the northern half for geothermal resources. This is because the southern half is closer to known hot springs, and also because it is geologically more favorable for the development of hot springs. Most of this region is covered by geologic maps at relatively coarse scales 6

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