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FOSSIL FUEL AND GEOTHERMAL ENERGY SOURCES FOR LOCAL USE

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FOSSIL FUEL AND GEOTHERMAL ENERGY SOURCES FOR LOCAL USE ( fossil-fuel-and-geothermal-energy-sources-for-local-use )

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Fossil Fuel and Geothermal Energy Sources for Local Use in Alaska Chapter L, Yukon–Koyukuk/Upper Tanana important and relatively cost-effective insights into the structure, fill, and gas resource potential of the Yukon Flats and Middle Tanana basins. The collection of high-quality seismic data, although expensive, would significant improve our knowledge of these basins. To be able to stimulate future exploration by industry, the State could consider exercising its right to publicly release currently confidential seismic data to the public if and when the exploration license for the Nenana area terminates. Unconventional oil and gas recommendations Coalbed methane. Thick, coal-bearing sections are known in the Middle Tanana basin and are suspected in the subsurface of the Yukon Flats basin. A recent shallow test well near Fort Yukon documented the presence of coal and methane, but gas saturation levels were too low due to the low rank of the coal. It is possible that higher rank coals could be present deeper in the basin, and may include higher gas saturation levels. A deeper coalbed methane test well might be justified in this basin, but the cost of drilling and testing such a well versus the risk of failure/benefits from success must be weighed. The coalbed methane potential of the Middle Tanana basin is poorly known, but the presence of thick coals along the Alaska Range mountain front combined with the basin’s proximity to transportation infrastructure make the basin an attractive target for future coalbed methane exploration and development. One or more coalbed methane test wells could be drilled, targeting the most attractive parts of the Middle Tanana basin. Despite the attractive characteristics of both basins, it is important to bear in mind that regardless of how much effort and investment are expended, all exploration programs carry inherent risk of failure. Tight gas sands. The tight gas sand potential in the region is probably low. The presence of tightly cemented Cretaceous-age sandstones is well documented, but the apparent absence of suitable source rocks throughout most of the region suggest tight gas sands are not present. The Kandik basin is an exception, as organic-rich source rocks and tightly cemented sandstones are known in this basin. Shale gas. With the exception of the Kandik basin, the shale gas potential in the region is considered low. Organic- rich mature source rocks are known in the Kandik basin and, given available information, shale gas potential cannot be ruled out. Additional work to characterize the petrophysical and organic geochemical properties of these rocks might be warranted. Methane hydrates. Due to the lack of extensive, continuous permafrost in most of central Alaska, the likelihood of finding gas hydrates in the region are very low, therefore no further action is recommended. Geothermal resource recommendation Surface indications of geothermal activity are known at several locations throughout the region. Most hot springs include only low-grade thermal springs that are too far from communities to warrant further action. Manley Hot Springs is a notable exception, being co-located with the community of Manley and including characteristics that suggest it could provide energy for local use. Additional characterization is warranted. The presence of shallow heat flow at hot springs across the region is a positive indication of a locally elevated geothermal gradient, allowing for the possibility of additional hidden geothermal resources elsewhere in the region. Exploring directly for these potential resources would be difficult and expensive. One option to assist in the identification of areas of higher potential would be to include evaluation of local and regional geothermal gradients during mineral resource exploration activities, such as airborne geophysical surveys and core drilling. REFERENCES CITED AND SELECTED BIBLIOGRAPHY Alaska Energy Authority (AEA), 2009, Alaska energy—A first step toward energy independence: Alaska Energy Authority, 245 pages. Available online at http://www. akenergyauthority.org/pdf files/AK Energy Final.pdf (ac- cessed November 12, 2009). Barker, J.C., 1981, Coal and uranium investigation of the Yukon Flats Cenozoic basin: U.S. Bureau of Mines Open File Report 140-81, 63 p. ———2006, Evidence for geothermal tungsten and ger- manium mineralization in Eocene coal and associated sediments, Fort Hamlin Hills, area, Interior Alaska: Alaska Division of Geological & Geophysical Surveys Preliminary Interpretive Report 2006-1, 24 p. Barnes, F.F., 1967, Coal resources of Alaska: U.S. Geologi- cal Survey Bulletin 1242-B, p. B1–B36, 1 sheet, scale 1:2,500,000. Belowich, M.A., 1986, Basinal trends in coal, petrographic, and elemental composition with applications toward seam correlation, Jarvis Creek coal field, Alaska, in Rao, P.D., ed., Focus on Alaska’s Coal ’86: University of Alaska Fairbanks Mineral Industry Research Laboratory Report No. 72, p. 300–335. ———1988, Stratigraphy, petrology, and depositional en- vironments of the Jarvis Creek coal field, east-central Alaska: Fairbanks, Alaska, University of Alaska Fair- banks, Master of Science thesis, 135 p., 2 sheets. Bickel, R.S., and Patton, W.W., Jr., 1957, Preliminary geo- logic map of the Nulato and Kateel Rivers area, Alaska: U.S. Geological Survey Miscellaneous Investigations 249, 1 sheet, scale 1:125,000. Bundtzen, T.K., and Kline, J.T., 1986, Coal, peat, and geo- thermal potential of the Kuskokwim Area Plan: Alaska Page 133 Yukon–Koyukuk/Upper Tanana

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