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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>D. Nielson</dc:contributor>
  <dc:contributor>T. Lachmar</dc:contributor>
  <dc:contributor>E. H. Christiansen</dc:contributor>
  <dc:contributor>L. Morgan</dc:contributor>
  <dc:contributor>Wayne C. Shanks</dc:contributor>
  <dc:contributor>C. Delahunty</dc:contributor>
  <dc:contributor>D.R. Schmitt</dc:contributor>
  <dc:contributor>L.M. Liberty</dc:contributor>
  <dc:contributor>D.D. Blackwell</dc:contributor>
  <dc:contributor>J. M. Glen</dc:contributor>
  <dc:contributor>J.A. Kessler</dc:contributor>
  <dc:contributor>K.E. Potter</dc:contributor>
  <dc:contributor>M.M. Jean</dc:contributor>
  <dc:contributor>C.J. Sant</dc:contributor>
  <dc:contributor>T. Freeman</dc:contributor>
  <dc:creator>J.W. Shervais</dc:creator>
  <dc:date>2012</dc:date>
  <dc:description>The Snake River volcanic province (SRP) overlies a thermal anomaly that extends deep into the mantle; it represents one of the highest heat flow provinces in North America. The primary goal of this project is to evaluate geothermal potential in three distinct settings: (1) Kimama site: inferred high sub-aquifer geothermal gradient associated with the intrusion of mafic magmas, (2) Kimberly site: a valley-margin setting where surface heat flow may be driven by the up-flow of hot fluids along buried caldera ringfault complexes, and (3) Mountain Home site: a more traditional fault-bounded basin with thick sedimentary cover. The Kimama hole, on the axial volcanic zone, penetrated 1912 m of basalt with minor intercalated sediment; no rhyolite basement was encountered. Temperatures are isothermal through the aquifer (to 960 m), then rise steeply on a super-conductive gradient to an estimated bottom hole temperature of ~98°C. The Kimberly hole is on the inferred margin of a buried rhyolite eruptive center, penetrated rhyolite with intercalated basalt and sediment to a TD of 1958 m. Temperatures are isothermal at 55-60°C below 400 m, suggesting an immense passive geothermal resource. The Mountain Home hole is located above the margin of a buried gravity high in the western SRP. It penetrates a thick section of basalt and lacustrine sediment overlying altered basalt flows, hyaloclastites, and volcanic sediments, with a TD of 1821 m. Artesian flow of geothermal water from 1745 m depth documents a power-grade resource that is now being explored in more detail. In-depth studies continue at all three sites, complemented by high-resolution gravity, magnetic, and seismic surveys, and by downhole geophysical logging.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>Geothermal Resources Council</dc:publisher>
  <dc:title>Hotspot: the Snake River Geothermal Drilling Project--initial report</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>