Fig. 6. Plot of water content vs. conductivity for drill hole R-8, using corresponding induction data for each water abundance data point shown in Fig. 5. Blue circles highlight the same data points circled in Fig. 5. Gravimetric water abundance in the Puye dacitic pumice bed is greater than the water abundance in any of the pumice-poor Puye fanglomerates, although the pumice-poor fanglomerates include many outliers of high conductivity. The basal sample from the Guaje Pumice Bed has high conductivity, similar to the other Guaje samples, but lower water content.