Early geophysical papers of the Early geophysical papers of the Society of Exploration Geophysicists earlygeophysical00soci Year: 1947 28 C. E. VAN ORSTRAND Because of the difficulty experienced in obtaining wells located at a sufficient distance from edge water, the evidence on the variation of temperature over sand lenses is not very complete. However, Mc- Top of Fort Ri/ey limestone- /00°F. isogeother-maf sur-fkce- EL DORADO, KANSAS Fig. 9.—Local variation over granite ridge, El Dorado, Butler County, Kansas. Cutchin's (29) observations in the Haverhill field, Butler County, Kansas (Fi
Early geophysical papers of the Early geophysical papers of the Society of Exploration Geophysicists earlygeophysical00soci Year: 1947 28 C. E. VAN ORSTRAND Because of the difficulty experienced in obtaining wells located at a sufficient distance from edge water, the evidence on the variation of temperature over sand lenses is not very complete. However, Mc- Top of Fort Ri/ey limestone- /00°F. isogeother-maf sur-fkce- EL DORADO, KANSAS Fig. 9.—Local variation over granite ridge, El Dorado, Butler County, Kansas. Cutchin's (29) observations in the Haverhill field, Butler County, Kansas (Fig. 10), located about 7 miles south of El Dorado, Kansas, show a well defined variation. The numbers on the right of the well locations (Fig. 10) represent the depths at which a temperature of 550
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