Direct-Current Resistivity At Lahaina-Kaanapali Area (Thomas, 1986)

From Open Energy Information

Exploration Activity: Direct-Current Resistivity At Lahaina-Kaanapali Area (Thomas, 1986)

Exploration Activity Details
Location Lahaina-Kaanapali Area
Exploration Technique Direct-Current Resistivity Survey
Activity Date
Usefulness not indicated
DOE-funding Unknown

 
Notes
Four Schlumberger soundings were performed along the coastal strip adjacent to Lahaina town (Fig. 22). Three of the four soundings were able to detect a moderate to low-resistivity basement that was interpreted to be basalt saturated with seawater at 20degrees C (Mattice, 1981). None of the resistivity sounding data in this area indicated subsurface resistivities lower than could be accounted for by local ambient temperatures (Mattice and Lienert, 1980).

 
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Additional References


<metadesc> Direct-Current Resistivity At Lahaina-Kaanapali Area (Thomas, 1986): geothermal exploration activity. </metadesc>