Geochemistry played no part in discovering the Desert Peak thermal anomaly or in siting the stratigraphie tests and deep production tests, as there is no surface water to sample within the Hot Springs Mountains and only a few seeps are present near the margins of the range. Water-level measurements in the stratigraphie tests have shown that the water table is often deeper than the bottom of most of the shallow temperature in ° F

temperature in ° F

--12-27-76 after well was static for 10 days

--5-15-77 after well was static for 58 days

FIGURE 30. Nonequilibrium reservoir temperature profiles of Desert Peak well B21-2.

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