Geothermometry At Clear Lake Area (Thompson, Et Al., 1992)

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Exploration Activity: Geothermometry At Clear Lake Area (Thompson, Et Al., 1992)

Exploration Activity Details
Location Clear Lake Area
Exploration Technique Geothermometry
Activity Date

Usefulness useful
DOE-funding Unknown

 
Notes
Based on the above discussion, we favor a model in which thermal water rises somewhere between Howard and Seigler Springs. At Howard Springs we see evidence for the most representative deep thermal water because the C1 is elevated (highest measured C1 concentrations occur at Howard Springs). Moreover, the Na-Li, Na-K and Na-K-Ca geothermometers suggest temperatures greater than 240 degrees C.

 
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Additional References