Browsing The Geothermal Collection by Title

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  • (State of Hawaii, Department of Land and Natural Resources, 1991)
    Prepared by the Department of Land and Natural Resources State of Hawaii in response to Section 1960-11, Hawaii Revised Statutes. Includes related memos and correspondence. This report reviews the Department's past-year ...
  • (R.A. Patterson & Associates, 1992-11-09)
    As a result of recommendations made in the "Independent Technical Investigation of the Puna Geothermal Venture Unplanned Steam Release", of June 12-13, 1991, the Department of Land and Natural Resources, State of Hawaii, ...
  • Thomas, Donald M. (Hawaii Institute of Geophysics and Planetology, 1994-03-18)
    The geochemical monitoring program has undertaken two related responsibilities: 1) Conduct a detailed analysis of the chemistry and dynamics of the shallow groundwater system on the Lower East Rift (LERZ); and 2) Evaluate ...
  • GeothermEx, Inc. (Department of Business and Economic Development, 1991)
    Summary of geophysical data available for prospective geothermal resource areas in the state of Hawaii.
  • GeothermEx, Inc. (GeothermEx, Inc., 1991-11)
    "GeothermEx, Inc., has been contracted by DBED to provide various consulting services relating to the development of the geothermal resource of Hawaii. These services include preparation of a draft preliminary report ...
  • Hawaiian Dredging & Construction Company; Pirelli Cable Corporation; Makai Ocean Engineering, Inc. (Hawaiian Dredging and Construction Company / Pirelli Cable Corporation / Makai Ocean Engineering, 1986-12)
    The Hawaii Deep Water Cable (HDWC) program has a major objective of determining the technical feasibility of deploying and operating, over a service life of thirty years, a submarine power transmission cable between Kohala ...
  • (Environmental Capital Managers, Inc., 1984)
    This section on the social impact analysis of geothermal resource areas gives emphasis to people's perceptions, attitudes, and concerns regarding geothermal resource development and-operation. Considerations are based on ...
  • Bowden, RJ.; D'Olier, W.L.; Goyal, K.P.; Patterson, R.A. (R.A. Patterson & Associates, 1990-12)
    This review is focused on analyses of operational and management objectives, priorities, costs, and procedures, as used in the initial SOH and as can be applied to improve future SOH operations. Scientific evaluations of ...
  • D'Olier, W.L.; Iovenitti, J.L. (Thermal Power Company, 1984)
    Thermal Power Company, Operator for the Puna Geothermal Venture which includes AMFAC and Dillingham, has drilled and tested two geothermal wells in the Puna Geothermal Field, Hawaii, USA. The field is located in the East ...
  • Keller, George V. (Golden, CO: Colorado School of Mines, 1974)
    A borehole has been drilled to a depth of 1262 m beneath the summit of Kilauea Volcano on the island of Hawaii. The purposes were twofold: to obtain engineering information related to the possible occurrence of geothermal ...
  • Gardner, Murray C.; Klein, Christopher W.; GeothermEx, Inc. (Richmond, CA: GeothermEx, Inc., 1984)
    Discussion of the drilling program and interpretation of downhole geology based on cuttings samples from the Lanipuna 6 well.
  • Colp, J.L.; Okamura, RT (Sandia Laboratories, 1978-01-01)
    The scientific feasibility of extracting energy directly from buried circulating magma resources is being assessed. One of the tasks of the project is the study of geophysical measuring systems to locate and define buried ...
  • (Northwest Economic Associates, 1990-03-01)
    In early 1989 the Pele Defense Fund requested that Northwest Economic Associates (NEA) update their 1987 economic analysis of the proposed Hawaii Geothermal Development And Inter-island Cable Transmission System Project. ...
  • Peterson, Richard E. (Hawaii Geothermal Project, University of Hawaii / National Technical Information Service, 1975-04)
    If it is economically feasible to exploit a resource, the period of exploitation will be affected by a number of economic factors. In the discussion below, the role of the following variables in the lifetime of oil, gas, ...
  • Peterson, Richard E. (Hawaii Geothermal Project, University of Hawaii, 1975-03)
    Both replenishable and nonreplenishable resources are exhaustible and even finite nonreplaceable resources can have infinite economic lives. The concept of ecological equilibrium) in which total recruitment of new mass is ...
  • State of Hawaii, Department of Land and Natural Resources, Division of Water and Land Development (State of Hawaii, Department of Land and Natural Resources, Division of Water and Land Development, 1984)
    Summary of economic impacts associated with development of geothermal resources on lands for which Geothermal Resource Subzones were proposed.
  • (State of Hawaii, Department of Land and Natural Resources, Division of Water and Land Development, 1984-09)
    To facilitate this economic assessment, two assumptions are made: (1) a 20 to 30 megawatt (MW) plant would be constructed, and (2) the application of the geothermal wells would be for the production of electricity for local ...
  • (University of Nevada, Reno, 1989)
    This study was performed under a grant (Grant #9-1-337-5152-002) from the UNR Foundation with funds provided by the Nevada Mining Association. Published for the Nevada Department of Minerals. In the Western United States ...
  • Group Seven (Missing pages / "An electrical resistivity survey was carried out over the Kilauea shield area in Puna and the Kau district of the Island of Hawaii during the period from May through July, 1973. for the purpose of locating areas favorable for the presence of geothermal reservoirs. The technique employed was the dipole mapping technique, which is widely used as a reconnaisance method in prospecting for geothermal reservoirs. It was found that the flanks of Mauna Loa are underlain by rocks of high resistivity, and that such rocks probably extend into the Puna area along the projection of an ancient rift zone of the volcano. Mauna Loa. The high resistivities probably represent the presence of dense, cool dike complexes, so that this portion of the area is unlikely to have such prospect for geothermal development. On the other hand, resistivities as low as two ohm-meters were mapped along the lower part of the East Rift of Kilauea. Assuming reasonable values of porosity and water salinity, such resistivity values are compatible with the presence of thermal waters with temperatures above 1800 C., probably extending to a depth of two kilometers below sea level. Measurements made around the summit area of Kilauea confirm the existence of a brackish-water geothermal system along the south side of Kilauea Caldera, in the vicinity of the Kilauea Geothermal Test Well. It is recommended that further detailed work be carried out in the vicinity of the areas with anomalously low resistivity in Puna, so that the best location for a test hole may be found.", 1973-07-31)
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