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Lines G1 and G2


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Near Hwy-68 is a small anomaly that corresponds with the approximate eastern edge of the buried Servilleta basalt flows. Both lines also show small anomalies that may be small buried faults. The Town Yard water well is situated just north of the gravity line. Pennsylvanian bedrock was encountered at approximately 700 ft in the well. This point indicates that the basin is shallow at least 3 km from the mountain front.

 

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(the PDF download page has Adobe Acrobat versions of the gravity profiles).

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