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Direct-Current Resistivity At Kawaihae Area (Thomas, 1986)
ExplorationOutcome not indicated  +
ExplorationTechnique Direct-Current Resistivity Survey +
Notes In addition to the aeromagnetic data, the
In addition to the aeromagnetic data, the field survey program in Kawaihae included six Schlumberger resistivity soundings between Kawaihae and Waimea (Kauahikaua and Mattice, 1981). The results of these sounding (Fig. 35) detected apparent resistivity differences in the surface rock depending on whether the soundings were done on Kohala or Mauna Kea lavas (Figs 36, 37), whereas uniform resistivities of 650- 850 ohm.m were found at depths of approximately 30 m. Basement resistivities for these soundings ranged from 7.9 to 10,000 ohm-m. The former resistivity was interpreted to correspond to basalt saturated with seawater, whereas the latter, located to the west of Puu Loa, was tentatively interpreted to indicate the presence of a dense intrusive body associated with the Puu Loa cinder cone (Kauahikaua and Mattice, 1981).
inder cone (Kauahikaua and Mattice, 1981).  +
OpenEI/PageDescription Direct-Current Resistivity At Kawaihae Area (Thomas, 1986): geothermal exploration activity.  +
OpenEI/PageKeyword Geothermal  + , Kawaihae Area  + , Direct-Current Resistivity Survey  +
Place Kawaihae Area +
Reference material Geothermal Resources Assessment In Hawaii +
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Direct-Current Resistivity At Kawaihae Area (Thomas, 1986) + , Direct-Current Resistivity At Kawaihae Area (Thomas, 1986) +
Categories Exploration Activities , Geothermal
Modification date
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22:56:44, 27 March 2013  +
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